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...

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Bibliographic Details
Published in:Geology
Main Authors: Selkin, Peter A., Strömberg, Caroline A. E., Dunn, Regan, Kohn, Matthew J., Carlini, Alfredo A., Davies-Vollum, K. Siân, Madden, Richard H.
Format: Text
Language:unknown
Published: ScholarWorks 2015
Subjects:
Online Access:https://scholarworks.boisestate.edu/geo_facpubs/261
https://doi.org/10.1130/G36664.1