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The Antarctic ice sheets and the Southern Ocean have played a central role in controlling global sea level and deep and intermediate water formation, upwelling intensity, and ultimately the storage and exchange of carbon dioxide with the atmosphere. Major goals in this Antarctic Pliocene and upper Miocene research include determining the presence and behavior of Antarctic ice sheets using the sediment record from ODP sediment cores and well-logs. This knowledge of the patterns and rates of past ice behavior can provide important analogues for predicting ice sheet retreat over the next few decades and centuries as atmospheric carbon dioxide levels exceed the present 410 ppm CO2 and temperatures increase by more than 1 degree Celsius.

MULTIPLE PROXIES FOR INVESTIGATING GLACIAL HISTORY OF ANTARCTICA FROM ODP SITES 696 & 697