James T. Hall
Wesleyan University, Middletown, CT
Activity
2016
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ECCENTRICITY IS THE DOMINANT ORBITAL FORCING FACTOR AT ODP SITE 693 ON THE ANTARCTIC CONTINENTAL MARGIN IN THE MIDDLE AND LATE PLIOCENE
T145 Sedimentary, Paleobiologic, and Geochemical Studies of Deep Time Ocean-Climate Perturbations II: Honoring the Scientific Contributions of Michael A. ArthurMonday, 26 September 20161:30 PM - 5:30 PMRoom 402
2015
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THE WEDDELL SEA IN THE PLIOCENE: INTERPRETING THE SEDIMENT RECORD FROM ODP SITES 693 AND 697
40 Paleoclimatology/Paleoceanography (Posters)Sunday, 1 November 20159:00 AM - 5:30 PMExhibit Hall
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EAST ANTARCTIC ICE SHEET BEHAVIOR DURING THE PLIOCENE
3 Climate Change in Space & Time: An UpdateMonday, 23 March 20158:00 AM - 12:00 PMReagan Room
2014
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COMPARISON OF XRF AND SPECTRAL REFLECTANCE DERIVED CYCLICITY IN PLIOCENE AND PLEISTOCENE SEDIMENTS FROM ODP SITE 693, DRONNING MAUD LAND ANTARCTICA
T143 Sedimentary Geology: The Now and the Next Generations of Scientists (Posters)Monday, 20 October 20149:00 AM - 6:30 PMExhibition Hall C