The State of the Oligocene Icehouse World: Sedimentology, Provenance, and Stable Isotopes of Marine Sediments from the Antarctic Continental Margin
The Oligocene Epoch (34-23 Ma) was a dynamic time in Antarctica, with previous ice volume estimates suggesting fluctuations from below 50 % up to 140 % of modern all while atmospheric CO2 decreased from above 1,000 ppm in the Early Oligocene to near modern levels by the Late Oligocene. Most of what...
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Format: | Doctoral or Postdoctoral Thesis |
Language: | English |
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CUNY Academic Works
2015
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Online Access: | https://academicworks.cuny.edu/gc_etds/966 https://academicworks.cuny.edu/cgi/viewcontent.cgi?article=1980&context=gc_etds |