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

Author

Listed:
  • A. Goldner

    (Atmospheric, and Planetary Sciences, Purdue University
    American Geophysical Union)

  • N. Herold

    (University of New Hampshire)

  • M. Huber

    (University of New Hampshire
    Earth Systems Research Center, Institute for Earth, Ocean and Space Sciences, University of New Hampshire)

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.

Suggested Citation

  • A. Goldner & N. Herold & M. Huber, 2014. "Antarctic glaciation caused ocean circulation changes at the Eocene–Oligocene transition," Nature, Nature, vol. 511(7511), pages 574-577, July.
    • Handle: RePEc:nat:nature:v:511:y:2014:i:7511:d:10.1038_nature13597
    DOI: 10.1038/nature13597
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    Cited by:

    1. Isabel Sauermilch & Joanne M. Whittaker & Andreas Klocker & David R. Munday & Katharina Hochmuth & Peter K. Bijl & Joseph H. LaCasce, 2021. "Gateway-driven weakening of ocean gyres leads to Southern Ocean cooling," Nature Communications, Nature, vol. 12(1), pages 1-8, December.
    2. Jinzhou Peng & Dengfeng Li & Simon W. Poulton & Gary J. O’Sullivan & David Chew & Yu Fu & Xiaoming Sun, 2024. "Episodic intensification of marine phosphorus burial over the last 80 million years," Nature Communications, Nature, vol. 15(1), pages 1-9, December.

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