{"id":20859,"date":"2017-02-28T18:35:46","date_gmt":"2017-02-28T18:35:46","guid":{"rendered":"https:\/\/usoceandiscovery.org\/?page_id=20859"},"modified":"2024-08-21T13:00:22","modified_gmt":"2024-08-21T13:00:22","slug":"past-schlanger-fellows","status":"publish","type":"page","link":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/","title":{"rendered":"Past Schlanger Fellows"},"content":{"rendered":"<p><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-1 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-0 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-1{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-1{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-1 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2023-2024 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-0{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-0 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-0{width:100% !important;}.fusion-builder-column-0 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-0{width:100% !important;}.fusion-builder-column-0 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-1 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-1 hover-type-none\"><img decoding=\"async\" width=\"230\" height=\"300\" title=\"Li\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Li.jpg\" alt class=\"img-responsive wp-image-28331\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Li-200x261.jpg 200w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Li.jpg 230w\" sizes=\"(max-width: 640px) 100vw, 230px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-1\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/shihan-li\/\">Shihan Li<\/a><\/h5>\n<p><strong><span class=\"institution\">Texas A&M University<br \/>\n<\/span><\/strong><\/p>\n<p><em>Data-driven solution of the carbon emission conundrum over the Paleocene-Eocene Thermal Maximum (PETM) event<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-1{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-1 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-1{width:25% !important;order : 0;}.fusion-builder-column-1 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-1{width:100% !important;order : 0;}.fusion-builder-column-1 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-2 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-2 hover-type-none\"><img decoding=\"async\" width=\"230\" height=\"300\" title=\"Mason\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Mason.jpg\" alt class=\"img-responsive wp-image-28330\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Mason-200x261.jpg 200w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Mason.jpg 230w\" sizes=\"(max-width: 640px) 100vw, 230px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-2\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/andrea-mason\/\">Andrea Mason<\/a><\/h5>\n<p><strong><span class=\"institution\">Brown University<br \/>\n<\/span><\/strong><\/p>\n<p><em>Congo Basin climate and ecosystem sensitivity during the Pleistocene<\/em><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-2{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-2 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-2{width:25% !important;order : 0;}.fusion-builder-column-2 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-2{width:100% !important;order : 0;}.fusion-builder-column-2 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-3 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-3 hover-type-none\"><img decoding=\"async\" width=\"230\" height=\"300\" title=\"Nirenberg-1\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Nirenberg-1.jpg\" alt class=\"img-responsive wp-image-28325\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Nirenberg-1-200x261.jpg 200w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Nirenberg-1.jpg 230w\" sizes=\"(max-width: 640px) 100vw, 230px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-3\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/jared-nirenberg\/\">Jaren Nirenberg<\/a><\/h5>\n<p><strong><span class=\"institution\">Brown University<br \/>\n<\/span><\/strong><\/p>\n<p><em>Southern Ocean and East Antarctic Temperature Evolution during the Middle Miocene<\/em><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-3{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-3 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-3{width:25% !important;order : 0;}.fusion-builder-column-3 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-3{width:100% !important;order : 0;}.fusion-builder-column-3 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-4 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-4 hover-type-none\"><img decoding=\"async\" width=\"230\" height=\"300\" title=\"Pallone\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Pallone.jpg\" alt class=\"img-responsive wp-image-28329\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Pallone-200x261.jpg 200w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Pallone.jpg 230w\" sizes=\"(max-width: 640px) 100vw, 230px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-4\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/celeste-pallone\/\">Celeste Pallone<\/a><\/h5>\n<p><strong><span class=\"institution\">Lamont-Doherty Earth Observatory<br \/>\n<\/span><\/strong><\/p>\n<p><i>Paleo-productivity in the Late Pleistocene Eastern Equatorial Pacific<\/i><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-4{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-4 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-4{width:25% !important;order : 0;}.fusion-builder-column-4 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-4{width:100% !important;order : 0;}.fusion-builder-column-4 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-5 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-5 hover-type-none\"><img decoding=\"async\" width=\"230\" height=\"300\" title=\"Wood\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Wood.jpg\" alt class=\"img-responsive wp-image-28328\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Wood-200x261.jpg 200w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Wood.jpg 230w\" sizes=\"(max-width: 640px) 100vw, 230px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-5\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/madison-wood\/\">Madison Wood<\/a><\/h5>\n<p><strong><span class=\"institution\">University of California, Santa Cruz<br \/>\n<\/span><\/strong><\/p>\n<p><i>Reconstructing seawater \u03b488\/86Sr response to climate-induced sea level fluctuations and neritic carbonate burial using novel pore fluid archive<\/i><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-5{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-5 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-5{width:25% !important;order : 0;}.fusion-builder-column-5 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-5{width:100% !important;order : 0;}.fusion-builder-column-5 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-6 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-6 hover-type-none\"><img decoding=\"async\" width=\"230\" height=\"300\" title=\"Zhang\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Zhang.jpg\" alt class=\"img-responsive wp-image-28327\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Zhang-200x261.jpg 200w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Zhang.jpg 230w\" sizes=\"(max-width: 640px) 100vw, 230px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-6\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/yan-zhang\/\">Yan Zhang<\/a><\/h5>\n<p><strong><span class=\"institution\">University of California, Santa Cruz<br \/>\n<\/span><\/strong><\/p>\n<p><i>The evolution of inter-basin \u03b415N gradients since the Miocene: Insights from a new simple realistic global N cycle model<\/i><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-6{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-6 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-6{width:25% !important;order : 0;}.fusion-builder-column-6 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-6{width:100% !important;order : 0;}.fusion-builder-column-6 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-1{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-2 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-7 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-2{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-2{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-2 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2022-2023 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-7{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-7 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-7{width:100% !important;}.fusion-builder-column-7 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-7{width:100% !important;}.fusion-builder-column-7 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-8 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-7 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Cunningham\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Cunningham-150x150.jpg\" alt class=\"img-responsive wp-image-28601\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Cunningham-66x66.jpg 66w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Cunningham-150x150.jpg 150w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-7\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/emily-cunningham\/\" target=\"_blank\" rel=\"noopener\">Emily Cunningham<\/a><\/h5>\n<p><strong><span class=\"institution\">University of Utah<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>The Northeast Atlantic break up: Why so much magma?<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-8{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-8 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-8{width:25% !important;order : 0;}.fusion-builder-column-8 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-8{width:100% !important;order : 0;}.fusion-builder-column-8 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-9 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-8 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Dove\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Dove-150x150.jpg\" alt class=\"img-responsive wp-image-28602\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Dove-66x66.jpg 66w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Dove-150x150.jpg 150w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-8\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/isabel-dove\/\" target=\"_blank\" rel=\"noopener\">Isabel Dove<\/a><\/h5>\n<p><strong><span class=\"institution\">University of Rhode Island<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>Tracking oceanographic changes and climate implications in Holocene Antarctic coastal zones<\/em><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-9{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-9 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-9{width:25% !important;order : 0;}.fusion-builder-column-9 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-9{width:100% !important;order : 0;}.fusion-builder-column-9 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-10 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-9 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Hess\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Hess-150x150.jpg\" alt class=\"img-responsive wp-image-28603\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Hess-66x66.jpg 66w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Hess-150x150.jpg 150w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-9\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/anya-hess\/\" target=\"_blank\" rel=\"noopener\">Anya Hess<\/a><\/h5>\n<p><strong><span class=\"institution\">Rutgers University<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>Evolution of the Arabian Sea Oxygen Deficient Zone following the Middle Miocene Climate Optimum: Global and Regional Drivers<\/em><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-10{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-10 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-10{width:25% !important;order : 0;}.fusion-builder-column-10 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-10{width:100% !important;order : 0;}.fusion-builder-column-10 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-11 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-10 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Hollister\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Hollister-150x150.jpg\" alt class=\"img-responsive wp-image-28604\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Hollister-66x66.jpg 66w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Hollister-150x150.jpg 150w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-10\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/kayla-hollister\/\" target=\"_blank\" rel=\"noopener\">Kayla Hollister<\/a><\/h5>\n<p><strong><span class=\"institution\">University of Notre Dame<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><i>Investigating the influence of sea surface temperatures on Southeastern African hydroclimate during the mid-Pleistocene Transition<\/i><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-11{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-11 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-11{width:25% !important;order : 0;}.fusion-builder-column-11 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-11{width:100% !important;order : 0;}.fusion-builder-column-11 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-12 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-11 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Wee\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Wee-150x150.jpg\" alt class=\"img-responsive wp-image-28605\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Wee-66x66.jpg 66w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2024\/04\/Wee-150x150.jpg 150w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-11\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/shu-ying-wee\/\" target=\"_blank\" rel=\"noopener\">Shu Ying Wee<\/a><\/h5>\n<p><strong><span class=\"institution\">Texas A&M University<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><i>Metagenomic comparison of subsurface basement sites<\/i><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-12{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-12 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-12{width:25% !important;order : 0;}.fusion-builder-column-12 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-12{width:100% !important;order : 0;}.fusion-builder-column-12 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-2{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-3 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-13 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-3{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-3{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-3 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2021-2022 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-13{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-13 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-13{width:100% !important;}.fusion-builder-column-13 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-13{width:100% !important;}.fusion-builder-column-13 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-14 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-12 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Davidson\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Davidson-150x150.jpg\" alt class=\"img-responsive wp-image-24476\"\/><\/span><\/div><div class=\"fusion-text fusion-text-12\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/peter-davidson\/\" target=\"_blank\" rel=\"noopener\">Peter Davidson<\/a><\/h5>\n<p><strong><span class=\"institution\">Oregon State University<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>Re-examining the temporal history of the Ontong Java Nui Large Igneous Province and its causal relations to OAE1A<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-14{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-14 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-14{width:25% !important;order : 0;}.fusion-builder-column-14 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-14{width:100% !important;order : 0;}.fusion-builder-column-14 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-15 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-13 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Hasim\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Hasim-150x150.jpg\" alt class=\"img-responsive wp-image-24477\"\/><\/span><\/div><div class=\"fusion-text fusion-text-13\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/mohammed-hashim\/\" target=\"_blank\" rel=\"noopener\">Mohammed Hashim<\/a><\/h5>\n<p><strong><span class=\"institution\">Western Michigan University<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>Parsing the diagenetic pathways of carbonate metastable sediments on the slope of the Great Bahama Bank<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-15{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-15 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-15{width:25% !important;order : 0;}.fusion-builder-column-15 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-15{width:100% !important;order : 0;}.fusion-builder-column-15 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-16 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-14 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Marcks\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Marcks-150x150.jpg\" alt class=\"img-responsive wp-image-24478\"\/><\/span><\/div><div class=\"fusion-text fusion-text-14\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/basia-marcks\/\" target=\"_blank\" rel=\"noopener\">Basia Marcks<\/a><\/h5>\n<p><strong><span class=\"institution\">University of Rhode Island<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>Did iron fertilization increase biogenic sediment accumulation in the subantarctic across the Mid-Pleistocene Transition?<\/em><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-16{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-16 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-16{width:25% !important;order : 0;}.fusion-builder-column-16 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-16{width:100% !important;order : 0;}.fusion-builder-column-16 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-17 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-15 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Rattanasriampaipong\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Rattanasriampaipong-150x150.jpg\" alt class=\"img-responsive wp-image-24479\"\/><\/span><\/div><div class=\"fusion-text fusion-text-15\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/ronnakrit-rattanasriampaipong\/\" target=\"_blank\" rel=\"noopener\">Ronnakrit Rattanasriampaipong<\/a><\/h5>\n<p><strong><span class=\"institution\">Texas A&M University<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><i>Long-term continuous sea surface temperature record of tropical Atlantic across the Cenozoic era<\/i><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-17{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-17 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-17{width:25% !important;order : 0;}.fusion-builder-column-17 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-17{width:100% !important;order : 0;}.fusion-builder-column-17 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-18 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-16 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Schartman\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Schartman-150x150.jpg\" alt class=\"img-responsive wp-image-24480\"\/><\/span><\/div><div class=\"fusion-text fusion-text-16\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/anna-schartman\/\" target=\"_blank\" rel=\"noopener\">Anna Schartman<\/a><\/h5>\n<p><strong><span class=\"institution\">University of California, Santa Cruz<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><i>The origins of an ecosystem: Rooting the African Savanna in the middle Miocene<\/i><\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-18{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-18 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-18{width:25% !important;order : 0;}.fusion-builder-column-18 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-18{width:100% !important;order : 0;}.fusion-builder-column-18 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-19 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-17 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Stout\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Stout-150x150.jpg\" alt class=\"img-responsive wp-image-24481\"\/><\/span><\/div><div class=\"fusion-text fusion-text-17\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/rebecca-cleveland-stout\/\" target=\"_blank\" rel=\"noopener\">Rebecca Stout<\/a><\/h5>\n<p><strong><span class=\"institution\">University of Washington<br \/>\n<\/span><\/strong><\/p>\n<p> <\/p>\n<p><i>Fingerprinting low-frequency Holocene climate variability across spatial scales<\/i><\/p>\n<p> <\/p>\n<p><em>\u00a0<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-19{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-19 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-19{width:25% !important;order : 0;}.fusion-builder-column-19 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-19{width:100% !important;order : 0;}.fusion-builder-column-19 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-20 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-18 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Tandy\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2021\/09\/Tandy-150x150.jpg\" alt class=\"img-responsive wp-image-24482\"\/><\/span><\/div><div class=\"fusion-text fusion-text-18\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/hannah-tandy\/\" target=\"_blank\" rel=\"noopener\">Hannah Tandy<\/a><\/h5>\n<p><strong><span class=\"institution\">University of California, Los Angeles<\/span><\/strong><\/p>\n<p> <\/p>\n<p><em>Novel constraints on pole-to-equator temperature gradients over the Paleocene-Eocene Thermal Maximum<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-20{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-20 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-20{width:25% !important;order : 0;}.fusion-builder-column-20 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-20{width:100% !important;order : 0;}.fusion-builder-column-20 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-3{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-4 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-21 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-4{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-4{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-4 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2020-2021 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-21{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-21 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-21{width:100% !important;}.fusion-builder-column-21 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-21{width:100% !important;}.fusion-builder-column-21 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-22 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-19 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"McGrath\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2020\/06\/McGrath-150x150.jpg\" alt class=\"img-responsive wp-image-23434\"\/><\/span><\/div><div class=\"fusion-text fusion-text-19\" style=\"text-align:center;\"><h5><a href=\"\/sarah-mcgrath\/\" target=\"_blank\" rel=\"noopener\">SARAH MCGRATH<\/a><\/h5>\n<p><strong>Brown University<\/strong><br \/>\n<em>What drives the Indian Summer Monsoon? New perspectives from the Bay of Bengal<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-22{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-22 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-22{width:25% !important;order : 0;}.fusion-builder-column-22 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-22{width:100% !important;order : 0;}.fusion-builder-column-22 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-23 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-20 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Meyer\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2020\/06\/Meyer-150x150.jpg\" alt class=\"img-responsive wp-image-23435\"\/><\/span><\/div><div class=\"fusion-text fusion-text-20\" style=\"text-align:center;\"><h5><a href=\"\/nicolette-meyer\/\" target=\"_blank\" rel=\"noopener\">NICOLETTE MEYER<\/a><\/h5>\n<p><strong>Stanford University<\/strong><br \/>\n<em>Fire and famine: Controls on microbial activity in the deep hydrothermal subsurface of the Guaymas Basin<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-23{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-23 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-23{width:25% !important;order : 0;}.fusion-builder-column-23 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-23{width:100% !important;order : 0;}.fusion-builder-column-23 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-24 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-21 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Sullivan\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2020\/06\/Sullivan-150x150.jpg\" alt class=\"img-responsive wp-image-23436\"\/><\/span><\/div><div class=\"fusion-text fusion-text-21\" style=\"text-align:center;\"><h5><a href=\"\/nicholas-sullivan\/\" target=\"_blank\" rel=\"noopener\">NICHOLAS SULLIVAN<\/a><\/h5>\n<p><strong>University of Wisconsin-Madison <\/strong><em>The integration of astrochronology and constrained optimization (CONOP) to resolve the history of the Southern Ocean during the neogene<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-24{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-24 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-24{width:25% !important;order : 0;}.fusion-builder-column-24 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-24{width:100% !important;order : 0;}.fusion-builder-column-24 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-25 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-22 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Wagner\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2020\/06\/Wagner-150x150.jpg\" alt class=\"img-responsive wp-image-23437\"\/><\/span><\/div><div class=\"fusion-text fusion-text-22\" style=\"text-align:center;\"><h5><a href=\"\/courtney-wagner\/\" target=\"_blank\" rel=\"noopener\">COURTNEY WAGNER<\/a><\/h5>\n<p><strong>University of Utah<\/strong><br \/>\n<em>Quantifying magnetofossil assemblages: Implications for paleoecology, diagenesis, and past, present, and future global change<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-25{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-25 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-25{width:25% !important;order : 0;}.fusion-builder-column-25 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-25{width:100% !important;order : 0;}.fusion-builder-column-25 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-26 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-23 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Zhou\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2020\/06\/Zhou-150x150.jpg\" alt class=\"img-responsive wp-image-23438\"\/><\/span><\/div><div class=\"fusion-text fusion-text-23\" style=\"text-align:center;\"><h5><a href=\"\/yuxin-zhou\/\" target=\"_blank\" rel=\"noopener\">YUXIN ZHOU<\/a><\/h5>\n<p><strong>Lamont-Doherty Earth Observatory<\/strong><br \/>\n<em>Heinrich Event ocean circulation and iceberg melting in the North Atlantic during the last glacial period<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-26{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-26 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-26{width:25% !important;order : 0;}.fusion-builder-column-26 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-26{width:100% !important;order : 0;}.fusion-builder-column-26 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-4{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-5 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-27 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-5{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-5{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-5 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2019-2020 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-27{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-27 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-27{width:100% !important;}.fusion-builder-column-27 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-27{width:100% !important;}.fusion-builder-column-27 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-28 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-24 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Kimberly_Beryl_deLong\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kimberly_Beryl_deLong-150x150.jpg\" alt class=\"img-responsive wp-image-22830\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kimberly_Beryl_deLong-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kimberly_Beryl_deLong-500x500.jpg 500w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kimberly_Beryl_deLong-570x570.jpg 570w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kimberly_Beryl_deLong-1000x1000.jpg 1000w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-24\" style=\"text-align:center;\"><h5><a href=\"\/kimberly-beryl-delong\/\">KIMBERLY BERYL DELONG<\/a><\/h5>\n<p><strong>University of California, Santa Cruz<\/strong> <em>Reconstructing Nitrogen Cycling and Ecosystem Structure in the Bering Sea Through the Anomalously Warm, High- Productivity, Hypoxic Bolling-Allerod Event<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-28{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-28 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-28{width:25% !important;order : 0;}.fusion-builder-column-28 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-28{width:100% !important;order : 0;}.fusion-builder-column-28 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-29 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-25 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"metcalfe_headshot copy\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-150x150.png\" alt class=\"img-responsive wp-image-22828\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-150x150.png 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-300x300.png 300w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-500x500.png 500w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-570x570.png 570w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-700x701.png 700w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy-768x770.png 768w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/metcalfe_headshot-copy.png 976w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-25\" style=\"text-align:center;\"><h5><a href=\"\/kyle-metcalfe\/\">KYLE METCALFE<\/a><\/h5>\n<p><strong>California Institute of Technology<\/strong><br \/>\n<em>Mineral-Associated Microbial Ecology of the Deep Subsurface, Nankai Trough, Japan<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-29{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-29 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-29{width:25% !important;order : 0;}.fusion-builder-column-29 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-29{width:100% !important;order : 0;}.fusion-builder-column-29 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-30 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-26 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Kelli Mullane – Headshot\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kelli-Mullane-Headshot-150x150.jpeg\" alt class=\"img-responsive wp-image-22829\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kelli-Mullane-Headshot-150x150.jpeg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kelli-Mullane-Headshot-500x500.jpeg 500w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kelli-Mullane-Headshot-570x570.jpeg 570w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Kelli-Mullane-Headshot-1000x1000.jpeg 1000w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-26\" style=\"text-align:center;\"><h5><a href=\"\/kelli-mullane\/\">KELLI MULANE<\/a><\/h5>\n<p><strong>Scripps Institution of Oceanography<\/strong><br \/>\n<em>Investigating the Piezophilic Microbial Communities of Mariana Forearc Serpentinite Mud Volcanoes<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-30{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-30 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-30{width:25% !important;order : 0;}.fusion-builder-column-30 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-30{width:100% !important;order : 0;}.fusion-builder-column-30 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-31 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-27 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Phelps_Headshot-2018\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Phelps_Headshot-2018-150x150.jpg\" alt class=\"img-responsive wp-image-22831\"\/><\/span><\/div><div class=\"fusion-text fusion-text-27\" style=\"text-align:center;\"><h5><a href=\"\/samuel-phelps\/\">SAMUEL PHELPS<\/a><\/h5>\n<p><strong>Lamont-Doherty Earth Observatory<\/strong><br \/>\n<em>The Role of Atmospheric CO2 in Late Miocene Environmental Change: A Multi-Proxy Study<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-31{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-31 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-31{width:25% !important;order : 0;}.fusion-builder-column-31 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-31{width:100% !important;order : 0;}.fusion-builder-column-31 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-32 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-28 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Srisharan_Pic\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Srisharan_Pic-150x150.jpg\" alt class=\"img-responsive wp-image-22832\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Srisharan_Pic-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Srisharan_Pic-500x500.jpg 500w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2019\/03\/Srisharan_Pic-570x570.jpg 570w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-28\" style=\"text-align:center;\"><h5><a href=\"\/shrisharan-shreedharan\/\">SHRISHARAN SHREEDHARAN<\/a><\/h5>\n<p><strong>Pennsylvania State University<\/strong><br \/>\n<em>Fault Healing and Shallow Slow Slip at the Hikurangi Subduction Margin: The Impact of Normal Stress and Loading-Rate on Friction<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-32{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-32 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-32{width:25% !important;order : 0;}.fusion-builder-column-32 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-32{width:100% !important;order : 0;}.fusion-builder-column-32 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-5{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-6 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-33 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-6{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-6{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-6 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2018-2019 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-33{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-33 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-33{width:100% !important;}.fusion-builder-column-33 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-33{width:100% !important;}.fusion-builder-column-33 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-34 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-29 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"cluett\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/cluett-150x150.jpg\" alt class=\"img-responsive wp-image-21984\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/cluett-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/cluett-500x500.jpg 500w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/cluett-570x570.jpg 570w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/cluett-1000x1000.jpg 1000w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-29\" style=\"text-align:center;\"><h5><a href=\"\/allison-cluett\/\">ALLISON CLUETT<\/a><\/h5>\n<p><strong>University at Buffalo, The State University of New York<\/strong><br \/>\n<em>Hydroclimate of Southern Greenland during interglacials of the past 600,000 years based on terrestrial leaf wax biomarker isotopes preserved in ocean sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-34{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-34 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-34{width:25% !important;order : 0;}.fusion-builder-column-34 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-34{width:100% !important;order : 0;}.fusion-builder-column-34 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-35 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-30 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"colin\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/colin-150x150.png\" alt class=\"img-responsive wp-image-21985\"\/><\/span><\/div><div class=\"fusion-text fusion-text-30\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/colin-jones\/\">COLIN JONES<\/a><\/h5>\n<p><strong>University of Rhode Island<\/strong><br \/>\n<em>Oceanographic controls on mid-Holocene nutrient consumption at Palmer Deep, West Antarctic Peninsula<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-35{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-35 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-35{width:25% !important;order : 0;}.fusion-builder-column-35 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-35{width:100% !important;order : 0;}.fusion-builder-column-35 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-36 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-31 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Megan_Mullis_Headshot\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/Megan_Mullis_Headshot-150x150.png\" alt class=\"img-responsive wp-image-21986\"\/><\/span><\/div><div class=\"fusion-text fusion-text-31\" style=\"text-align:center;\"><h5><a href=\"\/megan-mullis\/\">MEGAN MULLIS<\/a><\/h5>\n<p><strong>Texas A&M University,Corpus Christi <\/strong><em>Active microbial community survival in Mariana Forarc sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-36{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-36 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-36{width:25% !important;order : 0;}.fusion-builder-column-36 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-36{width:100% !important;order : 0;}.fusion-builder-column-36 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-37 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-32 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Schlanger photo\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/Schlanger-photo-150x150.jpg\" alt class=\"img-responsive wp-image-21987\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/Schlanger-photo-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/Schlanger-photo-500x500.jpg 500w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/Schlanger-photo-570x570.jpg 570w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2018\/05\/Schlanger-photo-1000x1000.jpg 1000w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-32\" style=\"text-align:center;\"><h5><a href=\"\/sarah-trubovitz\/\">SARAH TRUBOVITZ<\/a><\/h5>\n<p><strong>University of Nevada<\/strong><br \/>\n<em>What drives plankton evolution? : An investigation of the paleoenvironmental impacts on radiolarian macroevolution using the contrasting histories of tropical and polar Neogene oceans<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-37{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-37 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-37{width:25% !important;order : 0;}.fusion-builder-column-37 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-37{width:100% !important;order : 0;}.fusion-builder-column-37 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-6{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-7 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-38 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-7{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-7{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-7 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2017-2018 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-38{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-38 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-38{width:100% !important;}.fusion-builder-column-38 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-38{width:100% !important;}.fusion-builder-column-38 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-39 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-33 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"Haynes\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Haynes-113x150.jpg\" alt class=\"img-responsive wp-image-20929\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Haynes-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Haynes-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Haynes-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Haynes-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Haynes.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-33\" style=\"text-align:center;\"><h5><a href=\"\/2017-schlanger-fellow-laura-haynes\">LAURA HAYNES<\/a><\/h5>\n<p><strong>Lamont-Doherty Earth Observatory<\/strong> <em>Assessing Deep Pacific Carbon Storage Across the Mid-Pleistocene Transition<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-39{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-39 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-39{width:25% !important;order : 0;}.fusion-builder-column-39 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-39{width:100% !important;order : 0;}.fusion-builder-column-39 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-40 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-34 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"jones\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/jones-113x150.jpg\" alt class=\"img-responsive wp-image-20930\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/jones-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/jones-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/jones-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/jones-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/jones.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-34\" style=\"text-align:center;\"><h5><a href=\"\/2017-schlanger-fellow-heather-jones\/\">HEATHER JONES<\/a><\/h5>\n<p><strong>Pennsylvania State University<\/strong><br \/>\n<em>Survivorship and recovery of calcareous nannoplankton following the K\/Pg mass extinction at \u201cground zero\u201d<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-40{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-40 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-40{width:25% !important;order : 0;}.fusion-builder-column-40 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-40{width:100% !important;order : 0;}.fusion-builder-column-40 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-41 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-35 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"Kuzminov\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Kuzminov-113x150.jpg\" alt class=\"img-responsive wp-image-20931\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Kuzminov-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Kuzminov-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Kuzminov-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Kuzminov-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/Kuzminov.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-35\" style=\"text-align:center;\"><h5><a href=\"\/2017-schlanger-fellow-amy-kuzminov\/\">AMY KUZMINOV<\/a><\/h5>\n<p><strong>Rutgers University<\/strong><br \/>\n<em>Uranium isotope ratios: a proxy to understand carbon burial in varying redox environments in Ocean Anoxic Event 2<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-41{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-41 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-41{width:25% !important;order : 0;}.fusion-builder-column-41 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-41{width:100% !important;order : 0;}.fusion-builder-column-41 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-42 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-36 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"white\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/white-113x150.jpg\" alt class=\"img-responsive wp-image-20932\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/white-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/white-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/white-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/white-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/03\/white.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-36\" style=\"text-align:center;\"><h5><a href=\"\/2017-schlanger-fellow-sarah-white\/\">SARAH WHITE<\/a><\/h5>\n<p><strong>University of California, Santa Cruz<\/strong> <em>Constraining the effect of dissolution on Pliocene West Pacific Warm Pool SSTs and the \u201cpermanent El Nino-like state\u201d<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-42{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-42 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-42{width:25% !important;order : 0;}.fusion-builder-column-42 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-42{width:100% !important;order : 0;}.fusion-builder-column-42 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-7{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-8 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-43 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-8{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-8{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-8 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2016-2017 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-43{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-43 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-43{width:100% !important;}.fusion-builder-column-43 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-43{width:100% !important;}.fusion-builder-column-43 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-44 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-37 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"Berg\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Berg-113x150.jpg\" alt class=\"img-responsive wp-image-17961\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Berg-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Berg-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Berg-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Berg-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Berg.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-37\" style=\"text-align:center;\"><h5><a href=\"\/schlanger-fellows-2016-2017\/2016-schlanger-fellow-rick-berg\/\">RICHARD BERG<\/a><\/h5>\n<p><strong>University of Washington<\/strong><br \/>\n<em>Quantifying Global Rates of Magnesium Uptake into Marine Sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-44{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-44 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-44{width:25% !important;order : 0;}.fusion-builder-column-44 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-44{width:100% !important;order : 0;}.fusion-builder-column-44 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-45 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-38 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"Poirer\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Poirer-113x150.jpg\" alt class=\"img-responsive wp-image-17962\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Poirer-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Poirer-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Poirer-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Poirer-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Poirer.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-38\" style=\"text-align:center;\"><h5><a href=\"\/schlanger-fellows-2016-2017\/2016-schlanger-fellow-robert-poirier\/\">ROBERT POIRIER<\/a><\/h5>\n<p><strong>Rensselaer Polytechnic Institute<\/strong> <em>Assessing Millennial-Scale Variability in the Densest Limb of Meridional Overturning Circulation During the Prism Timeslice<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-45{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-45 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-45{width:25% !important;order : 0;}.fusion-builder-column-45 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-45{width:100% !important;order : 0;}.fusion-builder-column-45 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-46 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-39 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"Staudigel2\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Staudigel2-e1459364773199-150x150.jpg\" alt class=\"img-responsive wp-image-17963\"\/><\/span><\/div><div class=\"fusion-text fusion-text-39\" style=\"text-align:center;\"><h5><a href=\"\/schlanger-fellows-2016-2017\/2016-schlanger-fellow-philip-staudigel\/\">PHILIP STAUDIGEL<\/a><\/h5>\n<p><strong>University of Miami<\/strong><br \/>\n<em>The Application of Clumped Isotopes in Studying the Post-Depositional Alternation of Marine Carbonates<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-46{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-46 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-46{width:25% !important;order : 0;}.fusion-builder-column-46 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-46{width:100% !important;order : 0;}.fusion-builder-column-46 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-47 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-40 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"Wycech\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Wycech-113x150.jpg\" alt class=\"img-responsive wp-image-17964\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Wycech-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Wycech-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Wycech-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Wycech-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/Wycech.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-40\" style=\"text-align:center;\"><h5><a href=\"\/schlanger-fellows-2016-2017\/2016-schlanger-fellow-jody-wycech\/\">JODY WYCECH<\/a><\/h5>\n<p><strong>University of Wisconsin-Madison<\/strong> <em>Evaluating the Impact of Central American Seaway Closure on Pliocene Walker Circulation<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-47{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-47 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-47{width:25% !important;order : 0;}.fusion-builder-column-47 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-47{width:100% !important;order : 0;}.fusion-builder-column-47 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-48 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-41 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"zinke\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/zinke-113x150.jpg\" alt class=\"img-responsive wp-image-17965\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/zinke-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/zinke-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/zinke-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/zinke-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/03\/zinke.jpg 225w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-41\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/schlanger-fellows-2016-2017\/2016-schlanger-fellow-laura-zinke\/\">LAURA ZINKE<\/a><\/h5>\n<p><strong>University of Southern California<\/strong> <em>Active Microbial Carbon Cycling in Baltic Sea Basin Sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-48{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-48 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-48{width:25% !important;order : 0;}.fusion-builder-column-48 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-48{width:100% !important;order : 0;}.fusion-builder-column-48 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-8{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-9 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-49 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-9{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-9{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-9 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2014-2015 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-49{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-49 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-49{width:100% !important;}.fusion-builder-column-49 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-49{width:100% !important;}.fusion-builder-column-49 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-50 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-42 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Wang_Tony_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Tony_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19120\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Tony_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Tony_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Tony_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Tony_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Tony_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-42\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2014-2015-schlanger-fellow-xingchen-wang\/\">XINGCHEN WANG<\/a><\/h5>\n<p><strong>Princeton University<\/strong><br \/>\n<em>Exploring the Late Pleistocene Marine Nitrogen Cycle in the South Pacific using Nitrogen Isotopes from Fossil Corals from Tahiti<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-50{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-50 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-50{width:25% !important;order : 0;}.fusion-builder-column-50 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-50{width:100% !important;order : 0;}.fusion-builder-column-50 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-51 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-43 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Sauvage_Schlanger2\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Sauvage_Schlanger2-125x150.jpg\" alt class=\"img-responsive wp-image-19119\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Sauvage_Schlanger2-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Sauvage_Schlanger2-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Sauvage_Schlanger2-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Sauvage_Schlanger2-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Sauvage_Schlanger2.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-43\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2014-2015-schlanger-fellow-justine-sauvage\/\">JUSTINE SAUVAGE<\/a><\/h5>\n<p><strong>University of Rhode Island<\/strong><br \/>\n<em>Global Estimate of Radiolytic Hydrogren Production in Subseafloor Sediment: Importance of Nuclear-Fueled Life in the Deep Seafloor?<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-51{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-51 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-51{width:25% !important;order : 0;}.fusion-builder-column-51 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-51{width:100% !important;order : 0;}.fusion-builder-column-51 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-52 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-44 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Hardisty_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hardisty_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19118\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hardisty_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hardisty_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hardisty_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hardisty_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hardisty_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-44\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2014-2015-schlanger-fellow-dalton-hardisty\/\">DALTON HARDISTY<\/a><\/h5>\n<p><strong>University of California \u2013 Riverside<\/strong> <em>A Holocene Record of Temporal and Spatial Variability in Oxygen Deficiency in the Baltic Sea<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-52{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-52 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-52{width:25% !important;order : 0;}.fusion-builder-column-52 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-52{width:100% !important;order : 0;}.fusion-builder-column-52 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-53 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-45 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Foreman_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Foreman_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19117\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Foreman_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Foreman_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Foreman_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Foreman_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Foreman_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-45\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2014-2015-schlanger-fellow-alan-foreman\/\">ALAN FOREMAN<\/a><\/h5>\n<p><strong>University of California \u2013 San Diego<\/strong> <em>Evolution of Deep Ocean Temperature Across the Mid-Pleistocene in a South Atlantic Depth Transect<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-53{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-53 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-53{width:25% !important;order : 0;}.fusion-builder-column-53 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-53{width:100% !important;order : 0;}.fusion-builder-column-53 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-54 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-46 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Drake_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Drake_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19116\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Drake_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Drake_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Drake_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Drake_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Drake_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-46\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2014-2015-schlanger-fellow-michelle-drake\/\">MICHELLE DRAKE<\/a><\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>A Record of Ice-Rafting in the Bering Sea 1.3-1.6 Ma: Exploring the Influence of Obliquity and Precession on Ice-Sheet Behavior<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-54{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-54 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-54{width:25% !important;order : 0;}.fusion-builder-column-54 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-54{width:100% !important;order : 0;}.fusion-builder-column-54 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-9{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-10 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-55 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-10{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-10{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-10 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2013-2014 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-55{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-55 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-55{width:100% !important;}.fusion-builder-column-55 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-55{width:100% !important;}.fusion-builder-column-55 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-56 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-47 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Liddy-Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Liddy-Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19122\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Liddy-Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Liddy-Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Liddy-Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Liddy-Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Liddy-Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-47\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/2013-2014-schlanger-fellow-hannah-liddy\/\">HANNAH LIDDY<\/a><\/h5>\n<p><strong>University of Southern California<\/strong> <em>Pliocene Northeast African Vegetation Change: Implications for Hominin Evolution and Climate During a Mild Greenhouse<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-56{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-56 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-56{width:25% !important;order : 0;}.fusion-builder-column-56 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-56{width:100% !important;order : 0;}.fusion-builder-column-56 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-57 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-48 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Trembath-Reichert-Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Trembath-Reichert-Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19125\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Trembath-Reichert-Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Trembath-Reichert-Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Trembath-Reichert-Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Trembath-Reichert-Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Trembath-Reichert-Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-48\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2013-2014-schlanger-fellow-elizabeth-trembath-reichert\/\">ELIZABETH TREMBATH-REICHERT<\/a><\/h5>\n<p><strong>California Institute of Technology<\/strong> <em>Characterizing Microbial Transformations of Carbon and Nitrogen in Reducing Subseafloor Coal and Shale Environments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-57{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-57 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-57{width:25% !important;order : 0;}.fusion-builder-column-57 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-57{width:100% !important;order : 0;}.fusion-builder-column-57 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-58 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-49 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Schnur-Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schnur-Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19124\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schnur-Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schnur-Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schnur-Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schnur-Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schnur-Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-49\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2013-2014-schlanger-fellow-susan-schnur\/\">SUSAN SCHNUR<\/a><\/h5>\n<p><strong>Oregon State University<\/strong><br \/>\n<em>A Synthesis of the Volcanostratigraphy and Porosity of Pacific Intra-plate Seamounts<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-58{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-58 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-58{width:25% !important;order : 0;}.fusion-builder-column-58 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-58{width:100% !important;order : 0;}.fusion-builder-column-58 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-59 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-50 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Rabinowitz-Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Rabinowitz-Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19123\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Rabinowitz-Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Rabinowitz-Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Rabinowitz-Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Rabinowitz-Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Rabinowitz-Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-50\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2013-2014-schlanger-fellow-hannah-rabinowitz\/\">HANNAH RABINOWITZ<\/a><\/h5>\n<p><strong>Columbia University<\/strong><br \/>\n<em>Determining the Frictional Temperature Rise During the 2011 Tohoku Earthquake<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-59{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-59 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-59{width:25% !important;order : 0;}.fusion-builder-column-59 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-59{width:100% !important;order : 0;}.fusion-builder-column-59 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-60 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-51 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Hong-Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hong-Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19121\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hong-Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hong-Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hong-Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hong-Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Hong-Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-51\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/2013-2014-schlanger-fellow-weili-hong\/\">WEILI HONG<\/a><\/h5>\n<p><strong>Oregon State University<\/strong><br \/>\n<em>Constraining the Environmental Forcing of Methane Flux Along the Cascadia Margin<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-60{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-60 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-60{width:25% !important;order : 0;}.fusion-builder-column-60 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-60{width:100% !important;order : 0;}.fusion-builder-column-60 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-10{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-11 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-61 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-11{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-11{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-11 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2012-2013 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-61{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-61 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-61{width:100% !important;}.fusion-builder-column-61 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-61{width:100% !important;}.fusion-builder-column-61 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-62 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-52 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Zhang_Schlanger1\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Zhang_Schlanger1-125x150.jpg\" alt class=\"img-responsive wp-image-19130\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Zhang_Schlanger1-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Zhang_Schlanger1-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Zhang_Schlanger1-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Zhang_Schlanger1-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Zhang_Schlanger1.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-52\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2012-2013-schlanger-fellow-yi-ge-zhang\/\">YI GE ZHANG<\/a><\/h5>\n<p><strong>Yale University<\/strong> <em>Late Miocene\u2013Pliocene Evolution of the Pacific Warm Pool and Cold Tongue: Implications for El Ni\u00f1o<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-62{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-62 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-62{width:25% !important;order : 0;}.fusion-builder-column-62 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-62{width:100% !important;order : 0;}.fusion-builder-column-62 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-63 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-53 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Snow_Schlanger1\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Snow_Schlanger1-125x150.jpg\" alt class=\"img-responsive wp-image-19129\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Snow_Schlanger1-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Snow_Schlanger1-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Snow_Schlanger1-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Snow_Schlanger1-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Snow_Schlanger1.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-53\" style=\"text-align:center;\"><h5><a href=\"\/2012-2013-schlanger-fellow-tasha-snow\/\">TASHA SNOW<\/a><\/h5>\n<p><strong>University of South Florida<\/strong><br \/>\n<em>Early Circum-Arctic Glacial Decay During Major Deglaciations of the Past 500 kyr<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-63{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-63 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-63{width:25% !important;order : 0;}.fusion-builder-column-63 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-63{width:100% !important;order : 0;}.fusion-builder-column-63 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-64 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-54 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Knudson_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knudson_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19127\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knudson_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knudson_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knudson_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knudson_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knudson_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-54\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2012-2013-schlanger-fellow-karla-knudson\/\">KARLA KNUDSON<\/a><\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>Abrupt Changes in Oxygen Recorded in New Laminated Sediments from the Bering Sea (1.2-0 Ma)<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-64{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-64 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-64{width:25% !important;order : 0;}.fusion-builder-column-64 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-64{width:100% !important;order : 0;}.fusion-builder-column-64 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-65 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-55 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Russell_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Russell_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19128\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Russell_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Russell_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Russell_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Russell_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Russell_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-55\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2012-2013-schlanger-fellow-joseph-russell\/\">JOSEPH RUSSELL<\/a><\/h5>\n<p><strong>University of Delaware<\/strong> <em>Genomic Analyses of Microbial Cultivations in Unexplored Sub-seafloor Ridge Flank and Continental Margin Environments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-65{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-65 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-65{width:25% !important;order : 0;}.fusion-builder-column-65 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-65{width:100% !important;order : 0;}.fusion-builder-column-65 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-66 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-56 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Childress_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Childress_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19126\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Childress_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Childress_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Childress_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Childress_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Childress_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-56\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2012-2013-schlanger-fellow-laurel-childress\/\">LAUREL CHILDRESS<\/a><\/h5>\n<p><strong>Northwestern University<\/strong><br \/>\n<em>Tracking Multicycle Carbon in Active Margin Environments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-66{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-66 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-66{width:25% !important;order : 0;}.fusion-builder-column-66 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-66{width:100% !important;order : 0;}.fusion-builder-column-66 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-11{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-12 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-67 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-12{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-12{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-12 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2011-2012 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-67{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-67 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-67{width:100% !important;}.fusion-builder-column-67 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-67{width:100% !important;}.fusion-builder-column-67 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-68 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-57 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Wang_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19134\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Wang_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-57\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2011-2012-schlanger-fellow-huapei-wang\/\">HUAPEI WANG<\/a><\/h5>\n<p><strong>Rutgers \u2013 The State University of New Jersey<\/strong> <em>Paleomagnetic Inclination Flattening Corrections of IODP\/ODP\/DSDP Cores by Comparing Inclination Distributions to the TK03.GAD Model: Implications for Paleo-latitudes and Plate Tectonics<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-68{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-68 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-68{width:25% !important;order : 0;}.fusion-builder-column-68 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-68{width:100% !important;order : 0;}.fusion-builder-column-68 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-69 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-58 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Oehlert_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Oehlert_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19133\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Oehlert_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Oehlert_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Oehlert_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Oehlert_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Oehlert_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-58\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2011-2012-schlanger-fellow-amanda-oehlert\/\">AMANDA OEHLERT<\/a><\/h5>\n<p><strong>University of Miami<\/strong> <em>Decoupling of Organic and Inorganic \u03b413C Records in Periplatform Sediments: A global phenomenon<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-69{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-69 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-69{width:25% !important;order : 0;}.fusion-builder-column-69 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-69{width:100% !important;order : 0;}.fusion-builder-column-69 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-70 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-59 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Batista_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Batista_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19132\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Batista_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Batista_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Batista_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Batista_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Batista_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-59\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/2011-2012-schlanger-fellow-fabian-batista\/\">FABIAN BATISTA<\/a><\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>Nitrogen Dynamics of the Western Pacific from the Warm Pliocene and into the Ice Ages<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-70{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-70 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-70{width:25% !important;order : 0;}.fusion-builder-column-70 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-70{width:100% !important;order : 0;}.fusion-builder-column-70 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-71 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-60 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Babila_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Babila_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19131\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Babila_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Babila_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Babila_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Babila_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Babila_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-60\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2011-2012-schlanger-fellow-tali-babila\/\">TALI BABILA<\/a><\/h5>\n<p><strong>Rutgers \u2013 The State University of New Jersey<\/strong> <em>Assessing the Phase Relationship of Temperature and pCO2 during the Paleocene-Eocene Thermal Maximum<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-71{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-71 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-71{width:25% !important;order : 0;}.fusion-builder-column-71 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-71{width:100% !important;order : 0;}.fusion-builder-column-71 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-12{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-13 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-72 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-13{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-13{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-13 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2010-2011 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-72{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-72 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-72{width:100% !important;}.fusion-builder-column-72 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-72{width:100% !important;}.fusion-builder-column-72 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-73 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-61 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Schneider_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19139\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-61\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2010-2011-schlanger-fellow-julia-schneider\/\">JULIA SCHNEIDER<\/a><\/h5>\n<p><strong>University of Texas at Austin<\/strong><br \/>\n<em>Resedimentation of Nankai Mudstones to Illuminate Lithologic Control on Permeability and Compressibility<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-73{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-73 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-73{width:25% !important;order : 0;}.fusion-builder-column-73 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-73{width:100% !important;order : 0;}.fusion-builder-column-73 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-74 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-62 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Jungbluth_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Jungbluth_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19138\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Jungbluth_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Jungbluth_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Jungbluth_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Jungbluth_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Jungbluth_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-62\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2010-2011-schlanger-fellow-sean-jungbluth\/\">SEAN JUNGBLUTH<\/a><\/h5>\n<p><strong>University of Hawaii at Manoa<\/strong><br \/>\n<em>Application of Environmental Genomics to Understanding the Potential Impact of Microorganisms on the Biogeochemistry of the Sediment-Covered Oceanic Basement<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-74{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-74 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-74{width:25% !important;order : 0;}.fusion-builder-column-74 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-74{width:100% !important;order : 0;}.fusion-builder-column-74 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-75 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-63 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Joo_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Joo_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19137\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Joo_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Joo_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Joo_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Joo_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Joo_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-63\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2010-2011-schlanger-fellow-young-ji-joo\/\">YOUNG JI JOO<\/a><\/h5>\n<p><strong>Northwestern University<\/strong><br \/>\n<em>Relative Roles of Carbon, Nitrogen, Phosphorus, and Sulfur During Cretaceous Oceanic Anoxic Events\u2019s<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-75{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-75 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-75{width:25% !important;order : 0;}.fusion-builder-column-75 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-75{width:100% !important;order : 0;}.fusion-builder-column-75 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-76 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-64 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Gehrke_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Gehrke_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19136\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Gehrke_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Gehrke_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Gehrke_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Gehrke_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Gehrke_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-64\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/2010-2011-schlanger-fellow-gretchen-gehrke\/\">GRETCHEN GEHRKE<\/a><\/h5>\n<p><strong>University of Michigan<\/strong><br \/>\n<em>Mercury Deposition and Cycling During the Paleocene-Eocene Thermal Maximum: An Investigation Using Mercury Stable Isotopes<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-76{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-76 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-76{width:25% !important;order : 0;}.fusion-builder-column-76 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-76{width:100% !important;order : 0;}.fusion-builder-column-76 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-77 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-65 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Dyck_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Dyck_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19135\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Dyck_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Dyck_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Dyck_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Dyck_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Dyck_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-65\" style=\"text-align:center;\"><h5><a href=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/2010-2011-schlanger-fellow-kelsey-dyck\/\">KELSEY DYCK<\/a><\/h5>\n<p><strong>University of California \u2013 Santa Cruz <\/strong> <em>Western Pacific Warm Pool Sensitivity to Climate Change<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-77{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-77 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-77{width:25% !important;order : 0;}.fusion-builder-column-77 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-77{width:100% !important;order : 0;}.fusion-builder-column-77 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-13{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-14 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-78 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-14{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-14{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-14 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2009-2010 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-78{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-78 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-78{width:100% !important;}.fusion-builder-column-78 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-78{width:100% !important;}.fusion-builder-column-78 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-79 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-66 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Woodard_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Woodard_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19144\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Woodard_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Woodard_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Woodard_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Woodard_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Woodard_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-66\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2009-2010-schlanger-fellow-stella-woodard\/\">STELLA WOODARD<\/a><\/h5>\n<p><strong>Texas A&M University<\/strong><br \/>\n<em>Early Paleogene Eolian Dust in the Pacific Ocean: Is There a Connection Between Dust Flux and Orbitally Paced Lithologic Cycles?<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-79{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-79 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-79{width:25% !important;order : 0;}.fusion-builder-column-79 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-79{width:100% !important;order : 0;}.fusion-builder-column-79 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-80 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-67 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Schneider_Leah_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Leah_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19143\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Leah_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Leah_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Leah_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Leah_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Schneider_Leah_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-67\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2009-2010-schlanger-fellow-leah-schneider\/\">LEAH SCHNEIDER<\/a><\/h5>\n<p><strong>Pennsylvania State University<\/strong><br \/>\n<em>The Influence of Nannoplankton and the Oceanic Biological Pump on Eocene Climate Change<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-80{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-80 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-80{width:25% !important;order : 0;}.fusion-builder-column-80 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-80{width:100% !important;order : 0;}.fusion-builder-column-80 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-81 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-68 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Paquay_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Paquay_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19142\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Paquay_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Paquay_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Paquay_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Paquay_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Paquay_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-68\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2009-2010-schlanger-fellow-francois-paquay\/\">FRANCOIS PAQUAY<\/a><\/h5>\n<p><strong>University of Hawaii at Manoa<\/strong><br \/>\n<em>Marine Osmium and Molybdenum Isotopes as Proxies for the Late Paleocence-Early Eocene Arctic Ventilation and Paleo-Redox Changes<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-81{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-81 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-81{width:25% !important;order : 0;}.fusion-builder-column-81 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-81{width:100% !important;order : 0;}.fusion-builder-column-81 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-82 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-69 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Knuth_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knuth_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19141\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knuth_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knuth_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knuth_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knuth_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Knuth_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-69\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2009-2010-schlanger-fellow-matthew-knuth\/\">MATTHEW KNUTH<\/a><\/h5>\n<p><strong>University of Wisconsin \u2013 Madison<\/strong> <em>Dynamic Velocity Under Stress During Shear: A New Technique Using P and S-Waves to Study the Frictional Mechanics of the Upper Nankai Trough Accretionary Prism<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-82{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-82 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-82{width:25% !important;order : 0;}.fusion-builder-column-82 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-82{width:100% !important;order : 0;}.fusion-builder-column-82 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-83 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-70 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Ford_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ford_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19140\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ford_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ford_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ford_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ford_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ford_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-70\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2009-2010-schlanger-fellow-heather-ford\/\">HEATHER FORD<\/a><\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>Investigating ENSO Variability Over the Past 5 Million Years<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-83{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-83 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-83{width:25% !important;order : 0;}.fusion-builder-column-83 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-83{width:100% !important;order : 0;}.fusion-builder-column-83 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-14{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-15 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-84 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-15{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-15{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-15 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2008-2009 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-84{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-84 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-84{width:100% !important;}.fusion-builder-column-84 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-84{width:100% !important;}.fusion-builder-column-84 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-85 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-71 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Viesca_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Viesca_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19149\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Viesca_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Viesca_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Viesca_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Viesca_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Viesca_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-71\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2008-2009-schlanger-fellow-robert-viesca\/\">ROBERT VIESCA<\/a><\/h5>\n<p><strong>Harvard University<\/strong> <em>Fundamental Modeling of the Initiation and Propagation of Submarine Sediment Failure<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-85{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-85 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-85{width:25% !important;order : 0;}.fusion-builder-column-85 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-85{width:100% !important;order : 0;}.fusion-builder-column-85 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-86 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-72 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Ren_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ren_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19148\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ren_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ren_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ren_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ren_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Ren_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-72\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2008-2009-schlanger-fellow-haojia-abby-ren\/\">HAOJIA (ABBY) REN<\/a><\/h5>\n<p><strong>Princeton University<\/strong> <em>Study of Ocean Nitrate \u03b415N Changes over Glacial Cycles at ODP Site 999 Using Foraminifera Bound Nitrogen<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-86{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-86 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-86{width:25% !important;order : 0;}.fusion-builder-column-86 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-86{width:100% !important;order : 0;}.fusion-builder-column-86 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-87 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-73 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Krishnan_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Krishnan_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19147\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Krishnan_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Krishnan_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Krishnan_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Krishnan_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Krishnan_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-73\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2008-2009-schlanger-fellow-srinath-krishnan\/\">SRINATH KRISHNAN<\/a><\/h5>\n<p><strong>Yale University<\/strong> <em>Investigation of the Global Hydrological Cycle During Greenhouse-Gas Induced Warming<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-87{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-87 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-87{width:25% !important;order : 0;}.fusion-builder-column-87 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-87{width:100% !important;order : 0;}.fusion-builder-column-87 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-88 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-74 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Horn_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Horn_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19146\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Horn_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Horn_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Horn_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Horn_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Horn_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-74\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2008-2009-schlanger-fellow-greg-horn\/\">GREG HORN<\/a><\/h5>\n<p><strong>University of Southern California<\/strong> <em>Encouraging Life in the Slow Lane: Development of Solid-Substrate Coninuous Culture Techniques for the Enrichment of Deep-Biosphere Organisms<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-88{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-88 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-88{width:25% !important;order : 0;}.fusion-builder-column-88 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-88{width:100% !important;order : 0;}.fusion-builder-column-88 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-89 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-75 hover-type-none\"><img decoding=\"async\" width=\"125\" height=\"150\" title=\"Erhardt_Schlanger\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Erhardt_Schlanger-125x150.jpg\" alt class=\"img-responsive wp-image-19145\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Erhardt_Schlanger-125x150.jpg 125w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Erhardt_Schlanger-141x169.jpg 141w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Erhardt_Schlanger-165x198.jpg 165w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Erhardt_Schlanger-217x260.jpg 217w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/Erhardt_Schlanger.jpg 250w\" sizes=\"(max-width: 125px) 100vw, 125px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-75\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2008-2009-schlanger-fellow-andrea-erhardt\/\">ANDREA ERHARDT<\/a><\/h5>\n<p><strong>Stanford University<\/strong> <em>Using Molybdenum Isotopes and Concentrations in Marine Barite to Document Changes in Ocean Anoxia<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-89{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-89 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-89{width:25% !important;order : 0;}.fusion-builder-column-89 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-89{width:100% !important;order : 0;}.fusion-builder-column-89 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-15{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-16 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-90 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-16{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-16{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-16 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2007-2008 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-90{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-90 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-90{width:100% !important;}.fusion-builder-column-90 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-90{width:100% !important;}.fusion-builder-column-90 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-91 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-76 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"fellow-tominaga\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-tominaga-113x150.jpg\" alt class=\"img-responsive wp-image-19154\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-tominaga-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-tominaga-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-tominaga-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-tominaga-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-tominaga.jpg 216w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-76\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2007-2008-schlanger-fellow-masako-tominaga\/\">MASAKO TOMINAGA<\/a><\/h5>\n<p><strong>Texas A&M University<\/strong> <em>Determination of Volcanostratigraphy of ODP\/IODP Hole 1256D: Core-log Integration of Oceanic Crust Formed at a Superfast Spreading Rate<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-91{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-91 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-91{width:25% !important;order : 0;}.fusion-builder-column-91 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-91{width:100% !important;order : 0;}.fusion-builder-column-91 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-92 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-77 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"fellow-sosdian\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-sosdian-113x150.jpg\" alt class=\"img-responsive wp-image-19153\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-sosdian-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-sosdian-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-sosdian-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-sosdian-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-sosdian.jpg 216w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-77\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2007-2008-schlanger-fellow-sindia-sosdian\/\">SINDIA SOSDIAN<\/a><\/h5>\n<p><strong>Rutgers University<\/strong> <em>The Mid-Pleistocene Transition: Deep Sea Temperature and Global Ice Volume from Mg\/Ca and \u03b418O in Benthic Foraminifera<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-92{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-92 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-92{width:25% !important;order : 0;}.fusion-builder-column-92 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-92{width:100% !important;order : 0;}.fusion-builder-column-92 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-93 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-78 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"fellow-schrum\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-schrum-113x150.jpg\" alt class=\"img-responsive wp-image-19152\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-schrum-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-schrum-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-schrum-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-schrum-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-schrum.jpg 216w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-78\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2007-2008-schlanger-fellow-heather-schrum\/\">HEATHER SCHRUM<\/a><\/h5>\n<p><strong>University of Rhode Island<\/strong> <em>Quantification of Low Rates of Metabolic Activity in the Deep Subseafloor Using Sulfate Oxygen Isotopic Compositions<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-93{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-93 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-93{width:25% !important;order : 0;}.fusion-builder-column-93 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-93{width:100% !important;order : 0;}.fusion-builder-column-93 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-94 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-79 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"fellow-murphy\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-murphy-113x150.jpg\" alt class=\"img-responsive wp-image-19151\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-murphy-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-murphy-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-murphy-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-murphy-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-murphy.jpg 216w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-79\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2007-2008-schlanger-fellow-daniel-murphy\/\">DANIEL MURPHY<\/a><\/h5>\n<p><strong>Texas A&M University<\/strong> <em>North Pacific Intermediate Water Circulation Over the Last 60 kyr: Southern California Margin<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-94{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-94 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-94{width:25% !important;order : 0;}.fusion-builder-column-94 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-94{width:100% !important;order : 0;}.fusion-builder-column-94 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-95 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-80 hover-type-none\"><img decoding=\"async\" width=\"113\" height=\"150\" title=\"fellow-harrison\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-harrison-113x150.jpg\" alt class=\"img-responsive wp-image-19150\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-harrison-113x150.jpg 113w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-harrison-127x169.jpg 127w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-harrison-149x198.jpg 149w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-harrison-195x260.jpg 195w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2016\/06\/fellow-harrison.jpg 216w\" sizes=\"(max-width: 113px) 100vw, 113px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-80\" style=\"text-align:center;\"><h5><a href=\"\/past-schlanger-fellows\/2007-2008-schlanger-fellow-benjamin-harrison\/\">BENJAMIN HARRISON<\/a><\/h5>\n<p><strong>California Institute of Technology<\/strong> <em>Novel Methods for Characterizing Microbe Mineral Colonization Patterns in Deep Subsurface Marine Sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-95{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-95 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-95{width:25% !important;order : 0;}.fusion-builder-column-95 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-95{width:100% !important;order : 0;}.fusion-builder-column-95 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-16{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-17 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-96 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-17{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-17{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-17 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2006-2007 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-96{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-96 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-96{width:100% !important;}.fusion-builder-column-96 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-96{width:100% !important;}.fusion-builder-column-96 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-97 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-81 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-81\" style=\"text-align:center;\"><h5>HEATHER MCCARREN<\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>Depth Dependent Variations in Deep Water Chemistry & Temperature Across the P\/E Boundary<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-97{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-97 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-97{width:25% !important;order : 0;}.fusion-builder-column-97 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-97{width:100% !important;order : 0;}.fusion-builder-column-97 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-98 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-82 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-82\" style=\"text-align:center;\"><h5>SAM VANLANINGHAM<\/h5>\n<p><strong>Oregon State University<\/strong><br \/>\n<em>Documenting the Source of the Meiji Toungue Over the Last 200,000 Years: Implications for Deep Water Dynamics in the North Pacific<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-98{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-98 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-98{width:25% !important;order : 0;}.fusion-builder-column-98 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-98{width:100% !important;order : 0;}.fusion-builder-column-98 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-99 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-83 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-83\" style=\"text-align:center;\"><h5>PATRICK RAFTER<\/h5>\n<p><strong>Scripps Institution of Oceanography<\/strong> <em>Tropical Pacific Nutrient Dynamics Over the Past 1 Million Years: Mechanistic Insight to the Origin of the 100 Kyr Climate Cycle<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-99{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-99 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-99{width:25% !important;order : 0;}.fusion-builder-column-99 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-99{width:100% !important;order : 0;}.fusion-builder-column-99 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-100 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-84 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-84\" style=\"text-align:center;\"><h5>MICAH NICOLO<\/h5>\n<p><strong>Rice University<\/strong> <em>Eolian Grain-Size Records Across the Paleocene-Eocene Transition: Constraints on Atmospheric Circulation During Global Climate Change<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-100{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-100 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-100{width:25% !important;order : 0;}.fusion-builder-column-100 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-100{width:100% !important;order : 0;}.fusion-builder-column-100 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-101 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-85 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-85\" style=\"text-align:center;\"><h5>MARK LEVER<\/h5>\n<p><strong>University of North Carolina at Chapel Hill<\/strong> <em>Community Composition, Metabolism and Activity of Methanogens at Two Ocean Drilling Program Sites<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-101{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-101 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-101{width:25% !important;order : 0;}.fusion-builder-column-101 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-101{width:100% !important;order : 0;}.fusion-builder-column-101 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-102 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-86 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-86\" style=\"text-align:center;\"><h5>HIROKO KITAJIMA<\/h5>\n<p><strong>Texas A&M University<\/strong> <em>Sediment Consolidation State and Fluid Flow Properties of Nankai Trough and Cascadia Margin Accretionary Zones<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-102{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-102 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-102{width:25% !important;order : 0;}.fusion-builder-column-102 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-102{width:100% !important;order : 0;}.fusion-builder-column-102 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-103 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-87 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-87\" style=\"text-align:center;\"><h5>PAUL CRADDOCK<\/h5>\n<p><strong>Woods Hole Oceanographic Institution<\/strong> <em>Using New In Situ Laser-Ablation ICP-MS Techniques to Examine Geochemical Heterogeneity Within Hydrothermal Vent Deposits<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-103{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-103 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-103{width:25% !important;order : 0;}.fusion-builder-column-103 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-103{width:100% !important;order : 0;}.fusion-builder-column-103 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-104 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-88 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-88\" style=\"text-align:center;\"><h5>ALEXANDRA ABRAJEVITCH<\/h5>\n<p><strong>University of Michigan<\/strong><br \/>\n<em>Rock Magnetic Record of the Asian Monsoon Preserved in Bengal Fan Sediment: A New Look at an Old Problem<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-104{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-104 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-104{width:25% !important;order : 0;}.fusion-builder-column-104 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-104{width:100% !important;order : 0;}.fusion-builder-column-104 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-17{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-18 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-105 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-18{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-18{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-18 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2005-2006 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-105{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-105 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-105{width:100% !important;}.fusion-builder-column-105 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-105{width:100% !important;}.fusion-builder-column-105 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-106 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-89 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-89\" style=\"text-align:center;\"><h5>HEATHER MCCARREN<\/h5>\n<p><strong>University of California \u2013 Santa Cruz <\/strong><em>Depth Dependent Variations in Deep Water Chemistry & Temperature Across the P\/E Boundary <\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-106{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-106 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-106{width:25% !important;order : 0;}.fusion-builder-column-106 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-106{width:100% !important;order : 0;}.fusion-builder-column-106 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-107 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-90 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-90\" style=\"text-align:center;\"><h5>SAMUEL HULME<\/h5>\n<p><strong>University of Hawaii at Manoa<\/strong><br \/>\n<em>Lateral and Vertical Biogeochemical Fluxes in a Juan de Fuca Ridge Flank Hydrothermal Reservoir: Minor and Trace Element Systematics<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-107{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-107 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-107{width:25% !important;order : 0;}.fusion-builder-column-107 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-107{width:100% !important;order : 0;}.fusion-builder-column-107 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-108 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-91 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-91\" style=\"text-align:center;\"><h5>GRAHAM BAINES<\/h5>\n<p><strong>University of Wyoming<\/strong><br \/>\n<em>Thermal and Tectonic Evolution of Lower Oceanic Crust at an Ultra-Slow Spreading Ridge<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-108{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-108 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-108{width:25% !important;order : 0;}.fusion-builder-column-108 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-108{width:100% !important;order : 0;}.fusion-builder-column-108 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-18{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-19 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-109 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-19{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-19{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-19 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2004-2005 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-109{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-109 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-109{width:100% !important;}.fusion-builder-column-109 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-109{width:100% !important;}.fusion-builder-column-109 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-110 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-92 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-92\" style=\"text-align:center;\"><h5>XIAOLI LIU<\/h5>\n<p><strong>Pennsylvania State University<\/strong><br \/>\n<em>Multiphase Flow Modeling of Gas Hydrate systems at Hydrate Ridge and Blake Ridge<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-110{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-110 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-110{width:25% !important;order : 0;}.fusion-builder-column-110 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-110{width:100% !important;order : 0;}.fusion-builder-column-110 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-111 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-93 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-93\" style=\"text-align:center;\"><h5>JENNIFER BIDDLE<\/h5>\n<p><strong>Pennsylvania State University<\/strong><br \/>\n<em>Exploration of Subsurface Microorganisms: FISH-SIMS and Cultivation Studies of Sediment Gathered on ODP Leg 201<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-111{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-111 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-111{width:25% !important;order : 0;}.fusion-builder-column-111 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-111{width:100% !important;order : 0;}.fusion-builder-column-111 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-112 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-94 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-94\" style=\"text-align:center;\"><h5>SHARON HOFFMAN<\/h5>\n<p><strong>Woods Hole Oceanographic Institution<\/strong> <em>Pa\/Th and Stable Isotopic Records of Deep Water Circulation During the Last Interglacial<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-112{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-112 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-112{width:25% !important;order : 0;}.fusion-builder-column-112 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-112{width:100% !important;order : 0;}.fusion-builder-column-112 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-113 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-95 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-95\" style=\"text-align:center;\"><h5>ALEXANDRA TURCHYN<\/h5>\n<p><strong>Harvard University<\/strong><br \/>\n<em>Oxygen Isotopes in Marine Sulfate Over the Cenozoic<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-113{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-113 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-113{width:25% !important;order : 0;}.fusion-builder-column-113 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-113{width:100% !important;order : 0;}.fusion-builder-column-113 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-19{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-20 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-114 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-20{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-20{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-20 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2003-2004 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-114{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-114 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-114{width:100% !important;}.fusion-builder-column-114 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-114{width:100% !important;}.fusion-builder-column-114 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-115 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-96 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-96\" style=\"text-align:center;\"><h5><strong>IVAN SAVOV<\/strong><\/h5>\n<p><strong>University of South Florida<\/strong><br \/>\n<em>The Role of Forearc in Subduction Zone Chemical Cycles: Elemental and Light Isotope Signatures for Serpentinites from South Chamorro and Conical Seamount<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-115{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-115 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-115{width:25% !important;order : 0;}.fusion-builder-column-115 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-115{width:100% !important;order : 0;}.fusion-builder-column-115 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-116 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-97 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-97\" style=\"text-align:center;\"><h5>STEPHANIE HEALEY<\/h5>\n<p><strong>University of South Carolina<\/strong><br \/>\n<em>A 500,000 Year Record of Deep Sea Temperature and Ice Volume Based on Benthic Foraminiferal Mg\/Ca and d18O<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-116{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-116 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-116{width:25% !important;order : 0;}.fusion-builder-column-116 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-116{width:100% !important;order : 0;}.fusion-builder-column-116 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-117 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-98 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-98\" style=\"text-align:center;\"><h5>MATTHEW O\u2019REGAN<\/h5>\n<p><strong>University of Rhode Island<\/strong><br \/>\n<em>Lateral Fluid Flow in the Nankai Trough Study Area<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-117{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-117 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-117{width:25% !important;order : 0;}.fusion-builder-column-117 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-117{width:100% !important;order : 0;}.fusion-builder-column-117 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-118 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-99 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-99\" style=\"text-align:center;\"><h5>JOSHUA FEINBERG<\/h5>\n<p><strong>University of California \u2013 Berkeley<\/strong> <em>Magnetization of Seafloor Gabbros: Characterization of Crystallographically Oriented Magnetite Inclusions<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-118{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-118 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-118{width:25% !important;order : 0;}.fusion-builder-column-118 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-118{width:100% !important;order : 0;}.fusion-builder-column-118 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-119 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-100 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-100\" style=\"text-align:center;\"><h5>KRISTINA DAHL<\/h5>\n<p><strong>Woods Hole Oceanographic Institution<\/strong> <em>Holocene Reconstruction of the Summer and Winter South Asian Monsoon<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-119{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-119 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-119{width:25% !important;order : 0;}.fusion-builder-column-119 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-119{width:100% !important;order : 0;}.fusion-builder-column-119 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-120 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-101 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-101\" style=\"text-align:center;\"><h5>ANNA CIPRIANI<\/h5>\n<p><strong>Lamont-Doherty Earth Observatory<\/strong> <em>Space\/Time Mantle Heterogeneity Below the Mid Atlantic Ridge: an Isotopic Study of Peridotites and Gabbros Drilled during Leg 209<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-120{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-120 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-120{width:25% !important;order : 0;}.fusion-builder-column-120 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-120{width:100% !important;order : 0;}.fusion-builder-column-120 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-20{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-21 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-121 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-21{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-21{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-21 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2002-2003 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-121{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-121 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-121{width:100% !important;}.fusion-builder-column-121 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-121{width:100% !important;}.fusion-builder-column-121 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-122 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-102 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-102\" style=\"text-align:center;\"><h5>KRISTEN AVERYT<\/h5>\n<p><strong>Stanford University<\/strong><br \/>\n<em>Marine Barite as a Monitor of Seawater Sr\/Ca Ratios<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-122{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-122 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-122{width:25% !important;order : 0;}.fusion-builder-column-122 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-122{width:100% !important;order : 0;}.fusion-builder-column-122 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-123 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-103 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-103\" style=\"text-align:center;\"><h5>MATTHEW SCHMIDT<\/h5>\n<p><strong>University of California \u2013 Davis<\/strong><br \/>\n<em>Temperature and Hydrological Changes in the Western Caribbean and the Tropical Pacific During the Last 750 kyr<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-123{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-123 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-123{width:25% !important;order : 0;}.fusion-builder-column-123 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-123{width:100% !important;order : 0;}.fusion-builder-column-123 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-124 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-104 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-104\" style=\"text-align:center;\"><h5>MATTHEW MAKOWSKI<\/h5>\n<p><strong>MIT\/WHOI Joint Program<\/strong><br \/>\n<em>Characteristics of Aeolian Organic Matter in a Terrestrial-to-Marine Depositional Transect and Impliations for Millennial-Scale Tropical Climate Change<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-124{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-124 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-124{width:25% !important;order : 0;}.fusion-builder-column-124 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-124{width:100% !important;order : 0;}.fusion-builder-column-124 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-125 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-105 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-105\" style=\"text-align:center;\"><h5>MICHAEL HUTNAK<\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>The Thermal and Hydrothermal State of Subducting Lithosphere: Costa Rica Margin\u201d ODP Leg 205<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-125{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-125 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-125{width:25% !important;order : 0;}.fusion-builder-column-125 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-125{width:100% !important;order : 0;}.fusion-builder-column-125 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-126 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-106 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-106\" style=\"text-align:center;\"><h5>HEATHER BENWAY<\/h5>\n<p><strong>Oregon State University<\/strong><br \/>\n<em>Reconstructing Pycnocline Intensity in the Gulf of Panama to Monitor Low-Latitude Response to Neogene Closure of the Panama Isthmus<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-126{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-126 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-126{width:25% !important;order : 0;}.fusion-builder-column-126 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-126{width:100% !important;order : 0;}.fusion-builder-column-126 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-127 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-107 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-107\" style=\"text-align:center;\"><h5>LORRAINE LISIECKI<\/h5>\n<p><strong>Brown University<\/strong><br \/>\n<em>Faster and More Accurate Construction of Composite Depth Sections Using Dynamic Programming<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-127{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-127 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-127{width:25% !important;order : 0;}.fusion-builder-column-127 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-127{width:100% !important;order : 0;}.fusion-builder-column-127 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-128 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-108 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-108\" style=\"text-align:center;\"><h5>NICHOLAS DRENZEK<\/h5>\n<p><strong>Woods Hole Oceanographic Institution<\/strong> <em>Spatial and Temporal Variations in the Mixed Layer Radiocarbon Reservoir Age Through the Last Glacial Maximum<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-128{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-128 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-128{width:25% !important;order : 0;}.fusion-builder-column-128 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-128{width:100% !important;order : 0;}.fusion-builder-column-128 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-21{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-22 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-129 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-22{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-22{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-22 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2001-2002 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-129{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-129 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-129{width:100% !important;}.fusion-builder-column-129 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-129{width:100% !important;}.fusion-builder-column-129 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-130 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-109 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-109\" style=\"text-align:center;\"><h5>MATTHEW SCHMIDT<\/h5>\n<p><strong>University of California \u2013 Davis<\/strong> <em>Temperature and Hydrological Changes in the Western Caribbean and the Tropical Pacific During the Last 750 kyr<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-130{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-130 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-130{width:25% !important;order : 0;}.fusion-builder-column-130 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-130{width:100% !important;order : 0;}.fusion-builder-column-130 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-131 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-110 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-110\" style=\"text-align:center;\"><h5>CARA SANTELLI<\/h5>\n<p><strong>MIT\/WHOI Joint Program<\/strong> <em>The Role of Microorganisms in Alteration of Basaltic Glass in Deep Oceanic Subsurface Environments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-131{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-131 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-131{width:25% !important;order : 0;}.fusion-builder-column-131 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-131{width:100% !important;order : 0;}.fusion-builder-column-131 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-132 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-111 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-111\" style=\"text-align:center;\"><h5>MARIA PROKOPENKO<\/h5>\n<p><strong>University of Southern California<\/strong> <em>Fractionation of Nitrogen Isotopes During Early Diagenesis in the Sediments of Peru Margin<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-132{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-132 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-132{width:25% !important;order : 0;}.fusion-builder-column-132 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-132{width:100% !important;order : 0;}.fusion-builder-column-132 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-133 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-112 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-112\" style=\"text-align:center;\"><h5>BENJAMIN CRAMER<\/h5>\n<p><strong>Rutgers University<\/strong> <em>Evolution of a Warm Climate: Long-Term Paleoceanographic Trends and Short-Term Orbital Forcing of Climate in the Late Paleocene-Early Eocene<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-133{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-133 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-133{width:25% !important;order : 0;}.fusion-builder-column-133 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-133{width:100% !important;order : 0;}.fusion-builder-column-133 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-22{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-23 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-134 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-23{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-23{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-23 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">2000-2001 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-134{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-134 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-134{width:100% !important;}.fusion-builder-column-134 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-134{width:100% !important;}.fusion-builder-column-134 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-135 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-113 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-113\" style=\"text-align:center;\"><h5>JENNIFER LATIMER<\/h5>\n<p><strong>Indiana University-Purdue University Indianapolis<\/strong> <em>The Influence of Dust Inputs on Biogeochemical Cycles in the Southern Ocean<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-135{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-135 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-135{width:25% !important;order : 0;}.fusion-builder-column-135 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-135{width:100% !important;order : 0;}.fusion-builder-column-135 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-136 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-114 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-114\" style=\"text-align:center;\"><h5>ARADHNA TRIPATI<\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>Tropical Sea Surface Temperature Reconstruction for the Early Paleogene Using Mg\/Ca Ratios of Planktonic Foraminifera<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-136{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-136 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-136{width:25% !important;order : 0;}.fusion-builder-column-136 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-136{width:100% !important;order : 0;}.fusion-builder-column-136 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-137 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-115 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-115\" style=\"text-align:center;\"><h5>JOAN STEURER<\/h5>\n<p><strong>University of Missouri-Columbia<\/strong> <em>Composition, Intrinsic Shear Strength, Physical Properties, and Texture of Sediment at the Nankai Trough, Leg 190: An Integrated Approach<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-137{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-137 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-137{width:25% !important;order : 0;}.fusion-builder-column-137 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-137{width:100% !important;order : 0;}.fusion-builder-column-137 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-138 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-116 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-116\" style=\"text-align:center;\"><h5>THOMAS WERTH<\/h5>\n<p><strong>Scripps Institution of Oceanography<\/strong> <em>Hunting the Geomagnetic Field<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-138{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-138 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-138{width:25% !important;order : 0;}.fusion-builder-column-138 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-138{width:100% !important;order : 0;}.fusion-builder-column-138 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-139 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-117 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-117\" style=\"text-align:center;\"><h5>KEVIN THEISSEN<\/h5>\n<p><strong>Stanford University<\/strong> <em>A Quaternary-Pliocene Foraminifera Stable Istope Record for Prydz Bay, Antarctica<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-139{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-139 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-139{width:25% !important;order : 0;}.fusion-builder-column-139 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-139{width:100% !important;order : 0;}.fusion-builder-column-139 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-140 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-118 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-118\" style=\"text-align:center;\"><h5>KAREN MCCLAUGHLIN<\/h5>\n<p><strong>Stanford University<\/strong> <em>d18O of Phosphate in Organic Matter from Marine Sediments: A Tracer for Paleoenvironmental Conditions<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-140{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-140 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-140{width:25% !important;order : 0;}.fusion-builder-column-140 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-140{width:100% !important;order : 0;}.fusion-builder-column-140 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-23{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-24 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-141 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-24{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-24{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-24 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">1999-2000 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-141{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-141 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-141{width:100% !important;}.fusion-builder-column-141 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-141{width:100% !important;}.fusion-builder-column-141 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-142 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-119 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-119\" style=\"text-align:center;\"><h5>ROBERT VALENTINE<\/h5>\n<p><strong>Washington University \u2013 St. Louis<\/strong> <em>Crustal Recycling at the Izu-Bonin-Mariana Convergent Margin: Constraints from B-, Li-, Be-, and Pb- Isotopes and Trace Element Systematics<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-142{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-142 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-142{width:25% !important;order : 0;}.fusion-builder-column-142 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-142{width:100% !important;order : 0;}.fusion-builder-column-142 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-143 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-120 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-120\" style=\"text-align:center;\"><h5>BRANDON DUGAN<\/h5>\n<p><strong>Pennsylvania State University<\/strong><br \/>\n<em>Sediment Loading, Lateral Fluid Flow, and Erosion of the Continental Slope in Offshore New Jersey<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-143{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-143 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-143{width:25% !important;order : 0;}.fusion-builder-column-143 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-143{width:100% !important;order : 0;}.fusion-builder-column-143 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-144 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-121 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-121\" style=\"text-align:center;\"><h5>MICHELLE SHEARER<\/h5>\n<p><strong>Rice University<\/strong><br \/>\n<em>Quaternary Carbonate Preservation and Dissolution in the Caribbean Sea<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-144{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-144 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-144{width:25% !important;order : 0;}.fusion-builder-column-144 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-144{width:100% !important;order : 0;}.fusion-builder-column-144 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-24{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-25 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-145 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-25{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-25{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-25 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">1998-1999 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-145{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-145 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-145{width:100% !important;}.fusion-builder-column-145 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-145{width:100% !important;}.fusion-builder-column-145 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-146 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-122 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-122\" style=\"text-align:center;\"><h5>MICHAEL WARA<\/h5>\n<p><strong>University of California \u2013 Santa Cruz <\/strong><em>Boron Isotopes in Foraminifera as Tracers of Ocean pH: ODP Site 803D<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-146{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-146 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-146{width:25% !important;order : 0;}.fusion-builder-column-146 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-146{width:100% !important;order : 0;}.fusion-builder-column-146 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-147 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-123 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-123\" style=\"text-align:center;\"><h5>DEBORAH THOMAS<\/h5>\n<p><strong>University of North Carolina at Chapel Hill<\/strong> <em>Reconstruction of Latest Paleocene Thermal Maximum Deep-water Circulation from Neodymian Isotope Records<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-147{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-147 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-147{width:25% !important;order : 0;}.fusion-builder-column-147 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-147{width:100% !important;order : 0;}.fusion-builder-column-147 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-148 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-124 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-124\" style=\"text-align:center;\"><h5>PETER SELKIN<\/h5>\n<p><strong>Scripps Institution of Oceanography<\/strong> <em>Magnetization and Remagnetization of Seafloor Extrusives: Paleointensity, CRM and VRM Experiments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-148{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-148 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-148{width:25% !important;order : 0;}.fusion-builder-column-148 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-148{width:100% !important;order : 0;}.fusion-builder-column-148 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-25{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-26 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-149 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-26{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-26{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-26 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">1997-1998 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-149{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-149 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-149{width:100% !important;}.fusion-builder-column-149 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-149{width:100% !important;}.fusion-builder-column-149 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-150 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-125 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-125\" style=\"text-align:center;\"><h5>KATHERINE MCINTYRE<\/h5>\n<p><strong>University of California \u2013 Santa Cruz <\/strong><em>Early Pleistocene Climate Change: The 1.6 Ma Transition<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-150{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-150 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-150{width:25% !important;order : 0;}.fusion-builder-column-150 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-150{width:100% !important;order : 0;}.fusion-builder-column-150 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-151 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-126 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-126\" style=\"text-align:center;\"><h5>MARK PAGANI<\/h5>\n<p><strong>Pennsylvania State University<\/strong> <em>The Carbon Cycle and its Relationship to Climatic Variability in the North Atlantic<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-151{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-151 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-151{width:25% !important;order : 0;}.fusion-builder-column-151 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-151{width:100% !important;order : 0;}.fusion-builder-column-151 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-152 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-127 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-127\" style=\"text-align:center;\"><h5>HELEN PERKS<\/h5>\n<p><strong>Scripps Institution of Oceanography<\/strong> <em>Oxygen Demand Analysis as a Tool for Measuring the Organic Matter Content in Carbonate-rich Sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-152{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-152 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-152{width:25% !important;order : 0;}.fusion-builder-column-152 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-152{width:100% !important;order : 0;}.fusion-builder-column-152 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-153 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-128 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-128\" style=\"text-align:center;\"><h5>THOMAS MARCHITTO<\/h5>\n<p><strong>MIT\/WHOI Joint Program <\/strong><em>Development and Application of Zinc as a Paleoceanographic Tracer<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-153{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-153 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-153{width:25% !important;order : 0;}.fusion-builder-column-153 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-153{width:100% !important;order : 0;}.fusion-builder-column-153 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-154 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-129 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-129\" style=\"text-align:center;\"><h5>STEPHEN SCHELLENBERG<\/h5>\n<p><strong>University of Southern California <\/strong><em>Geochemical and Faunal Analyses of Ddeep-ocean Ostracodes During Two Transient Climate Extrema of the Paleogene: A Test of Benthic Foram O-based Climate Reconstructions Using Ostracode Mg:Ca Ratios<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-154{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-154 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-154{width:25% !important;order : 0;}.fusion-builder-column-154 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-154{width:100% !important;order : 0;}.fusion-builder-column-154 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-155 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-130 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-130\" style=\"text-align:center;\"><h5>MICHAEL HELGERUD<\/h5>\n<p><strong>Stanford University <\/strong><em>Experimental Measurement and Theoretical Modeling of the Physical Properties of Sediments Containing Gas Hydrate<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-155{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-155 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-155{width:25% !important;order : 0;}.fusion-builder-column-155 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-155{width:100% !important;order : 0;}.fusion-builder-column-155 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-156 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-131 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-131\" style=\"text-align:center;\"><h5>STEFANIE BRACHFELD<\/h5>\n<p><strong>University of Minnesota <\/strong><em>Rock-magnetic and Paleomagnetic Techniques for the Examination, Correlation, and Dating of Holocene Paleoclimate Signals in Antarctic Glacial-marine Sediments<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-156{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-156 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-156{width:25% !important;order : 0;}.fusion-builder-column-156 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-156{width:100% !important;order : 0;}.fusion-builder-column-156 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-26{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-27 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-157 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-27{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-27{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-27 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">1996-1997 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-157{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-157 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-157{width:100% !important;}.fusion-builder-column-157 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-157{width:100% !important;}.fusion-builder-column-157 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-158 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-132 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-132\" style=\"text-align:center;\"><h5>DANIEL SIGMAN<\/h5>\n<p><strong>MIT\/WHOI Joint Program <\/strong><em>Tracking the History of Nutrient Conditions in Southern Ocean Surface Waters Using the Nitrogen Isotopic Composition of Sediments and Sediment Fractions<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-158{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-158 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-158{width:25% !important;order : 0;}.fusion-builder-column-158 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-158{width:100% !important;order : 0;}.fusion-builder-column-158 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-159 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-133 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-133\" style=\"text-align:center;\"><h5>KATHARINA BILLUPS<\/h5>\n<p><strong>University of California \u2013 Santa Cruz <\/strong> <em>Reconstructing Pliocene Equatorial Atlantic Surface Water Hydrography<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-159{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-159 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-159{width:25% !important;order : 0;}.fusion-builder-column-159 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-159{width:100% !important;order : 0;}.fusion-builder-column-159 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-160 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-134 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-134\" style=\"text-align:center;\"><h5>MARK PAGANI<\/h5>\n<p><strong>Pennsylvania State University <\/strong><em>The Carbon Cycle and its Relationship to Climatic Variability in the North Atlantic<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-160{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-160 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-160{width:25% !important;order : 0;}.fusion-builder-column-160 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-160{width:100% !important;order : 0;}.fusion-builder-column-160 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-161 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-135 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-135\" style=\"text-align:center;\"><h5>PHILIP STAUFFER<\/h5>\n<p><strong>University of California \u2013 Santa Cruz<\/strong> <em>Modeling Deformation and Dewatering in the Barbados Accretionary Complex: Implications for Proto-decollement Evolution<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-161{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-161 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-161{width:25% !important;order : 0;}.fusion-builder-column-161 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-161{width:100% !important;order : 0;}.fusion-builder-column-161 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-27{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><div class=\"fusion-fullwidth fullwidth-box fusion-builder-row-28 fusion-flex-container nonhundred-percent-fullwidth non-hundred-percent-height-scrolling\" style=\"background-color: rgba(255,255,255,0);background-position: center center;background-repeat: no-repeat;border-width: 0px 0px 0px 0px;border-color:var(--awb-color3);border-style:solid;\" ><div class=\"fusion-builder-row fusion-row fusion-flex-align-items-stretch\" style=\"max-width:1456px;margin-left: calc(-4% \/ 2 );margin-right: calc(-4% \/ 2 );\"><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-162 fusion_builder_column_1_1 1_1 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-blend-mode: overlay;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;padding: 0px 0px 20px 0px;\"><style type=\"text\/css\">@media only screen and (max-width:1024px) {.fusion-title.fusion-title-28{margin-top:10px!important; margin-right:0px!important;margin-bottom:15px!important;margin-left:0px!important;}}@media only screen and (max-width:640px) {.fusion-title.fusion-title-28{margin-top:10px!important; margin-right:0px!important;margin-bottom:10px!important; margin-left:0px!important;}}<\/style><div class=\"fusion-title title fusion-title-28 sep-underline sep-solid fusion-title-text fusion-title-size-three\" style=\"border-bottom-color:var(--awb-color5);margin-top:10px;margin-right:0px;margin-bottom:15px;margin-left:0px;\"><h3 class=\"title-heading-left fusion-responsive-typography-calculated\" style=\"margin:0;--fontSize:24;--minFontSize:24px;line-height:var(--awb-typography1-line-height);\">1995-1996 SCHLANGER FELLOWS<\/h3><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-162{width:100% !important;margin-top : 0px;margin-bottom : 0px;}.fusion-builder-column-162 > .fusion-column-wrapper {padding-top : 0px !important;padding-right : 0px !important;margin-right : 1.92%;padding-bottom : 20px !important;padding-left : 0px !important;margin-left : 1.92%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-162{width:100% !important;}.fusion-builder-column-162 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-162{width:100% !important;}.fusion-builder-column-162 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-163 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-136 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-136\" style=\"text-align:center;\"><h5>ROISIN LAKINGS<\/h5>\n<p><strong>Duke University <\/strong><em>Paleomagnetic and Rock Magnetic Constraints on Large-Scale Normal Faults on the MAR: Gabbros and Serpentinites from ODP Leg 153<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-163{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-163 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-163{width:25% !important;order : 0;}.fusion-builder-column-163 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-163{width:100% !important;order : 0;}.fusion-builder-column-163 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-164 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-137 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-137\" style=\"text-align:center;\"><h5>DANIEL SIGMAN<\/h5>\n<p><strong>MIT\/WHOI Joint Program <\/strong><em>Tracking the History of Nutrient Conditions in Southern Ocean Surface Waters Using the Nitrogen Isotopic Composition of Sediments and Sediment Fractions<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-164{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-164 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-164{width:25% !important;order : 0;}.fusion-builder-column-164 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-164{width:100% !important;order : 0;}.fusion-builder-column-164 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><div class=\"fusion-layout-column fusion_builder_column fusion-builder-column-165 fusion_builder_column_1_4 1_4 fusion-flex-column\"><div class=\"fusion-column-wrapper fusion-column-has-shadow fusion-flex-justify-content-flex-start fusion-content-layout-column\" style=\"background-position:left top;background-repeat:no-repeat;-webkit-background-size:cover;-moz-background-size:cover;-o-background-size:cover;background-size:cover;box-shadow:2px 2px 20px 10px var(--awb-color3);;padding: 15px 5px 0px 5px;\"><div style=\"text-align:center;\"><span class=\" fusion-imageframe imageframe-none imageframe-138 hover-type-none\"><img decoding=\"async\" width=\"150\" height=\"150\" title=\"default-person\" src=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg\" alt class=\"img-responsive wp-image-20916\" srcset=\"https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person-150x150.jpg 150w, https:\/\/usoceandiscovery.org\/wp-content\/uploads\/2017\/02\/default-person.jpg 219w\" sizes=\"(max-width: 150px) 100vw, 150px\" \/><\/span><\/div><div class=\"fusion-text fusion-text-138\" style=\"text-align:center;\"><h5>KARIN BERNET<\/h5>\n<p><strong>University of Miami<\/strong> <em>The Record of Hierarchies of Sea Level Fluctuations in Cores, Logs, and Seismic Data Along the Great Bahama Bank Transect<\/em><\/p>\n<\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-builder-column-165{width:25% !important;margin-top : 0px;margin-bottom : 20px;}.fusion-builder-column-165 > .fusion-column-wrapper {padding-top : 15px !important;padding-right : 5px !important;margin-right : 7.68%;padding-bottom : 0px !important;padding-left : 5px !important;margin-left : 7.68%;}@media only screen and (max-width:1024px) {.fusion-body .fusion-builder-column-165{width:25% !important;order : 0;}.fusion-builder-column-165 > .fusion-column-wrapper {margin-right : 7.68%;margin-left : 7.68%;}}@media only screen and (max-width:640px) {.fusion-body .fusion-builder-column-165{width:100% !important;order : 0;}.fusion-builder-column-165 > .fusion-column-wrapper {margin-right : 1.92%;margin-left : 1.92%;}}<\/style><\/div><\/div><style type=\"text\/css\">.fusion-body .fusion-flex-container.fusion-builder-row-28{ padding-top : 0px;margin-top : 0px;padding-right : 0px;padding-bottom : 0px;margin-bottom : 0px;padding-left : 0px;}<\/style><\/div><\/p>\n","protected":false},"excerpt":{"rendered":"","protected":false},"author":5,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"100-width.php","meta":{"_exactmetrics_skip_tracking":false,"_exactmetrics_sitenote_active":false,"_exactmetrics_sitenote_note":"","_exactmetrics_sitenote_category":0,"jetpack_post_was_ever_published":false,"footnotes":""},"class_list":["post-20859","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.6 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Past Schlanger Fellows - U.S. Science Support Program<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Past Schlanger Fellows - U.S. Science Support Program\" \/>\n<meta property=\"og:url\" content=\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/\" \/>\n<meta property=\"og:site_name\" content=\"U.S. Science Support Program\" \/>\n<meta property=\"article:modified_time\" content=\"2024-08-21T13:00:22+00:00\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"144 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/\",\"url\":\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/\",\"name\":\"Past Schlanger Fellows - U.S. Science Support Program\",\"isPartOf\":{\"@id\":\"\/#website\"},\"datePublished\":\"2017-02-28T18:35:46+00:00\",\"dateModified\":\"2024-08-21T13:00:22+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/\"]}]},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\/\/usoceandiscovery.org\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Past Schlanger Fellows\"}]},{\"@type\":\"WebSite\",\"@id\":\"\/#website\",\"url\":\"\/\",\"name\":\"U.S. Science Support Program\",\"description\":\"Supporting Research in the International Ocean Discovery Program\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Past Schlanger Fellows - U.S. Science Support Program","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/","og_locale":"en_US","og_type":"article","og_title":"Past Schlanger Fellows - U.S. Science Support Program","og_url":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/","og_site_name":"U.S. Science Support Program","article_modified_time":"2024-08-21T13:00:22+00:00","twitter_misc":{"Est. reading time":"144 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/","url":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/","name":"Past Schlanger Fellows - U.S. Science Support Program","isPartOf":{"@id":"\/#website"},"datePublished":"2017-02-28T18:35:46+00:00","dateModified":"2024-08-21T13:00:22+00:00","breadcrumb":{"@id":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/usoceandiscovery.org\/past-schlanger-fellows\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/usoceandiscovery.org\/"},{"@type":"ListItem","position":2,"name":"Past Schlanger Fellows"}]},{"@type":"WebSite","@id":"\/#website","url":"\/","name":"U.S. Science Support Program","description":"Supporting Research in the International Ocean Discovery Program","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"}]}},"jetpack_sharing_enabled":true,"jetpack_shortlink":"https:\/\/wp.me\/P5Mw1w-5qr","_links":{"self":[{"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/pages\/20859","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/users\/5"}],"replies":[{"embeddable":true,"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/comments?post=20859"}],"version-history":[{"count":0,"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/pages\/20859\/revisions"}],"wp:attachment":[{"href":"https:\/\/usoceandiscovery.org\/wp-json\/wp\/v2\/media?parent=20859"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}