Climate, dust, and fire across the Eocene-Oligocene transition, Patagonia

The Eocene-Oligocene transition (EOT) is typically interpreted as a time of drastic global cooling and drying associated with massive growth of a glacial icecap in Antarctica and the shift to an "icehouse" climate. The effects of this transition on the terrestrial environments, floras, and...

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Bibliographic Details
Published in:Geology
Main Authors: Selking, Peter A., Stromberg, Caroline, Dunn, Regan, Khon, Matthew J., Carlini, Alfredo Armando, Davies-Vollum, K. Siân, Madden, Richard H.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society of America
Subjects:
Eot
Online Access:http://hdl.handle.net/11336/78364