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...
Published in: | Geology |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Society of America
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Subjects: | |
Online Access: | http://hdl.handle.net/11336/78364 |