SDSU Geological Sciences - Thesis Defense - Emily Allen

submitted by: tcarrasc
Ocean acidification during the Paleocene-Eocene Thermal Maximum at Contessa Road, Italy: Insights from weight percent carbonate content Emily Allen B.S. Candidate Department of Geological Sciences San Diego State University Advisors Dr. Stephen Schellenberg -------------------------------------------------------------------------------- ABSTRACT The Paleocene-Eocene Thermal Maximum (PETM; ~55 Ma) is defined as a period of time during which thousands of petagrams of carbon were...

SDSU Geological Sciences Webinar - Sandra Kirtland

submitted by: tcarrasc
Beyond the PETM: Are hyperthermals common features of a high CO2 world? Sandra Kirtland Ph.D. Candidate Scripps Institution of Oceanography University of California, San Diego Wednesday, April 6th, 2011 -------------------------------------------------------------------------------- Abstract: The early Eocene was a time of extreme global warmth, high atmospheric greenhouse gas concentrations, and no permanent polar ice caps. During this epoch, Earth reached the highest...

SDSU Geological Sciences Webinar - Kathleen R. Johnson

submitted by: tcarrasc
Reconstructing Asian Monsoon History from Chinese Speleothems; Kathleen R. Johnson, Department of Earth System Science, University of California, Irvine: While we know that modern anthropogenic climate change is superimposed upon significant natural climate variability, the instrumental record of climate is too short to capture the full range of this variability. In order to fully understand and predict future changes, therefore, high-resolution, welldated paleoclimate records are needed to...