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 faunas of...
Published in: | Geology |
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Main Authors: | , , , , , , |
Format: | Text |
Language: | unknown |
Published: |
ScholarWorks
2015
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Subjects: | |
Online Access: | https://scholarworks.boisestate.edu/geo_facpubs/261 https://doi.org/10.1130/G36664.1 |