Results of recent studies have led scientists to assume that a strong link exists between atmospheric carbon dioxide and the Earth’s climatic character. The establishment of ancient pCO2 (partial pressure of carbon dioxide) records not only provides evidence for or against this assumption, but also allows the exploration of linkages between the carbon cycle, biology, and tectonics. Recent pCO2 reconstructions, as well as isotope and sedimentological evidence for the early Paleogene, suggest the assumed CO2-climate relationship is largely valid. For example, the decline in pCO2 from the mid-Eocene to Oligocene tracks increasingly colder bottom-water and global temperatures. In addition, data reconstructions show that hyperthermals of the Eocene, such as the Paleocene-Eocene thermal maximum (PETM) and associated ocean acidification, undeniably resulted from massive inputs of carbon. However, there are times – during the Miocene (~24-5 Ma) – when the relationship between climate change and CO2 appears less robust, suggesting that climate sensitivity to CO2 was higher, or that ocean circulation and/or tectonics played increasingly important climatic roles. Further, the evolution of CO2 and terrestrial photosynthesis are likely linked given our recent understanding of the origin of photosynthetic pathways during the Cenozoic, as well as the probable influence that photosynthetic respiration exerted on the rate of silicate chemical weathering and CO2 draw-down over long time scales.
Dr. Pagani’s research relies on biomarkers, as well as foraminifera from cores recovered by the Deep Sea Drilling Program, Ocean Drilling Program, and Integrated Ocean Drilling Program.
LECTURE SCHEDULE
September 9, 2008 – Dickinson College
February 3, 2009 – Lawrence University
March 5, 2009 – Syracuse University
March 16, 2009 – Western Michigan University
March 20, 2009 – University of Montana-Western
April 2, 2009 – Muskingum College
May 1, 2009 – Maryland Science Center
September 18, 2009 – Florida A&M University