Antarctic glaciation caused ocean circulation changes at the Eocene–Oligocene transition

A. Goldner (), N. Herold and M. Huber ()
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A. Goldner: Atmospheric, and Planetary Sciences, Purdue University
N. Herold: University of New Hampshire
M. Huber: University of New Hampshire

Nature, 2014, vol. 511, issue 7511, 574-577

Abstract: A climate model is used to show that the growth of the Antarctic ice sheet at about 34 Myr ago drove changes in ocean circulation, but the opening of ocean gateways had relatively little impact.

Date: 2014
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DOI: 10.1038/nature13597

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