The respective role of atmospheric carbon dioxide and orbital parameters on ice sheet evolution at the Eocene-Oligocene transition-Reference-Cited by-同舟云学术

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The respective role of atmospheric carbon dioxide and orbital parameters on ice sheet evolution at the Eocene-Oligocene transition

Published:2014-08 Issue:8 Volume:29 Page:810-823
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Ladant Jean-Baptiste¹,Donnadieu Yannick¹,Lefebvre Vincent¹,Dumas Christophe¹

Affiliation:

1. Laboratoire des Sciences du Climat et de l'Environnement; CEA-CNRS-UVSQ; Gif-sur-Yvette France

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference56 articles.

1. Convergent Cenozoic CO2 history;Beerling;Nat. Geosci.,2011

2. Foraminiferal Mg/Ca evidence for Southern Ocean cooling across the Eocene-Oligocene transition;Bohaty;Earth Planet. Sci. Lett.,2012

3. Global implications of lower to middle Eocene sequence boundaries on the New Jersey coastal plain: The icehouse cometh;Browning;Geology,1996

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