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...

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Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Galeotti, Simone, Lanci, Luca, Florindo, Fabio, Naish, Tim R., Sagnotti, Leonardo, Sandroni, Sonia, Talarico, Franco Maria
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/11365/8110
https://doi.org/10.1016/j.palaeo.2011.08.011