Arctic closure as a trigger for Atlantic overturning at the Eocene-Oligocene Transition
Abstract
The Eocene-Oligocene Transition (EOT), approximately 34 Ma ago, marks a period of major global cooling and inception of the Antarctic ice sheet. Proxies of deep circulation suggest a contemporaneous onset or strengthening of the Atlantic meridional overturning circulation (AMOC). Proxy evidence of gradual salinification of the North Atlantic and tectonically driven isolation of the Arctic suggest that closing the Arctic-Atlantic gateway could...
Paper Details
Title
Arctic closure as a trigger for Atlantic overturning at the Eocene-Oligocene Transition
Published Date
Aug 22, 2019
Journal
Volume
10
Issue
1
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