Chairs: Chris Lowery, University of Massachusetts, Amherst, MA, United States, Jeremy D Owens, Florida State University, Tellahassee, United States, Zunli Lu, Syracuse University, Department of Earth and Environmental Sciences, Syracuse, NY, United States and Noah Planavsky, Yale University, Department of Earth and Planetary Sciences, New Haven, CT, United States
Primary Convener: Chris Lowery, University of Massachusetts, Amherst, MA, United States
Co-conveners: Jeremy D Owens, Florida State University, Tellahassee, United States, Zunli Lu, Syracuse University, Department of Earth and Environmental Sciences, Syracuse, NY, United States and Noah Planavsky, Yale University, Department of Earth and Planetary Sciences, New Haven, CT, United States
OSPA Liaison: Chris Lowery, University of Massachusetts, Amherst, MA, United States
Oceanic oxygen in a warming climate: mechanisms, patterns, and timescales (Invited) (26996)
Curtis A Deutsch, University of Washington, School of Oceanography, Seattle, WA, United States, Alexander van Geen, Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, United States, William Berelson, University of Southern California, Earth Sciences, Los Angeles, United States, Takamitsu Ito, Georgia Institute of Technology, School of Earth & Atmospheric Sciences, Atlanta, United States and Thomas Weber, University of Washington Seattle Campus, School of Oceanography, Seattle, WA, United States
A New Approach to Reconstruct Ancient Bottom Water Oxygen Levels (25361)
Anthony Earl Rathburn1, Jake Willingham1, Bruce H Corliss2, Ashley M Burkett3 and Wiebke Ziebis4, (1)Indiana State University, Terre Haute, IN, United States, (2)University of Rhode Island Narragansett Bay, Narragansett, RI, United States, (3)Indiana State University, Earth and Environmental Systems, Terre Haute, IN, United States, (4)University of Southern California, Biological Sciences, Los Angeles, CA, United States
The Paleocene – Eocene Thermal Maximum: Temperature and Ecology in the Tropics (16387)
Joost Frieling1, Holger Gebhardt2, Olabisi A. Adekeye3, Samuel OLUMIDE Akande3, Gert-Jan Reichart4, Jack J Middelburg5, Stefan Schouten6,7, Matthew Huber8 and Appy Sluijs1, (1)Marine Palynology and Paleoceanography, Department of Earth Sciences, Faculty of Geosciences, Utrecht University. Laboratory of Palaeobotany and Palynology, Budapestlaan 4, 3584CD, Utrecht, Netherlands, (2)Geologische Bundesanstalt, Vienna, Austria, (3)University of Ilorin, Department of Geology and Mineral Sciences, Ilorin, Nigeria, (4)NIOZ Royal Netherlands Institute for Sea Research, Geology and Chemical Oceanography, 1790AB, Den Burg, Texel, Netherlands, (5)Utrecht University, Utrecht, Netherlands, (6)NIOZ Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, Texel, Netherlands, (7)Utrecht University, Department of Earth Sciences, Utrecht, Netherlands, (8)University of New Hampshire Main Campus, Durham, NH, United States
Detrital sources and water mass circulation in the tropical North Atlantic during the Late Cretaceous to Paleogene (17408)
Ellen E. Martin, University of Florida, Gainesville, United States, Emily Pugh, Chevron Midland, Midland, TX, United States; University of Florida, Gainesville, FL, United States, George D Kamenov, University of Florida, Department of Geological Sciences, Gainesville, FL, United States and Kenneth G MacLeod, University of Missouri Columbia, Columbia, MO, United States
