Cyclochronology of the Eocene-Oligocene transition from the Cape Roberts Project-3 core, Victoria Land basin, Antarctica
About 34 million years ago, at the Eocene-Oligocene (E-O) transition, Earth's climate underwent a substantial change from relatively ice-free "green house" conditions to a glacial state marked by the establishment of a permanent ice sheet on Antarctica. Our understanding of the Antarc...
Published in: | Palaeogeography, Palaeoclimatology, Palaeoecology |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2012
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Subjects: | |
Online Access: | http://hdl.handle.net/11365/8110 https://doi.org/10.1016/j.palaeo.2011.08.011 |