Midlatitude Southern Hemisphere Temperature Change at the End of the Eocene Greenhouse Shortly Before Dawn of the Oligocene Icehouse-Reference-Cited by-同舟云学术

Midlatitude Southern Hemisphere Temperature Change at the End of the Eocene Greenhouse Shortly Before Dawn of the Oligocene Icehouse

Published:2019-12 Issue:12 Volume:34 Page:1995-2004
ISSN:2572-4517
Container-title:Paleoceanography and Paleoclimatology
language:en
Short-container-title:Paleoceanography and Paleoclimatology

Author:

Haiblen A. M.¹²^ORCID,Opdyke B. N.¹,Roberts A. P.¹^ORCID,Heslop D.¹^ORCID,Wilson P. A.³^ORCID

Affiliation:

1. Research School of Earth Sciences The Australian National University Canberra Australia

2. Now at Geoscience Australia Symonston Australia

3. National Oceanography Centre Southampton University of Southampton Southampton UK

Funder

Australian Research Council

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Atmospheric Science,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019PA003679

Reference67 articles.

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3. Foraminiferal Mg/Ca evidence for Southern Ocean cooling across the Eocene–Oligocene transition

4. Middle Eocene climate cyclicity in the southern Pacific: Implications for global ice volume

5. Export of nutrient rich Northern Component Water preceded early Oligocene Antarctic glaciation

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