Evidence for a Highly Dynamic West Antarctic Ice Sheet During the Pliocene-Reference-Cited by-同舟云学术

Evidence for a Highly Dynamic West Antarctic Ice Sheet During the Pliocene

Published:2021-07-20 Issue:14 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Gohl Karsten¹^ORCID,Uenzelmann‐Neben Gabriele¹^ORCID,Gille‐Petzoldt Johanna¹^ORCID,Hillenbrand Claus‐Dieter²^ORCID,Klages Johann P.¹^ORCID,Bohaty Steven M.³^ORCID,Passchier Sandra⁴^ORCID,Frederichs Thomas⁵^ORCID,Wellner Julia S.⁶^ORCID,Lamb Rachel¹^ORCID,Leitchenkov German⁷^ORCID,

Affiliation:

1. Alfred Wegener Institute Helmholtz‐Center for Polar and Marine Research Division of Geosciences Bremerhaven Germany

2. British Antarctic Survey Cambridge UK

3. National Oceanography Centre Southampton University of Southampton Southampton UK

4. Department of Earth and Environmental Studies Montclair State University Montclair NJ USA

5. Department of Geosciences University of Bremen Bremen Germany

6. Department of Earth and Atmospheric Sciences University of Houston Houston TX USA

7. VNIIOkeangeologia and St. Petersburg State University St. Petersburg Russia

Funder

Deutsche Forschungsgemeinschaft

Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research

Natural Environment Research Council

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL093103

Reference62 articles.

1. Cenozoic Glacial History of the Ross Sea Revealed by Intermediate Resolution Seismic Reflection Data Combined with Drill Site Information

2. The International Bathymetric Chart of the Southern Ocean (IBCSO) Version 1.0-A new bathymetric compilation covering circum-Antarctic waters

3. Proceedings of the ocean drilling program, scientific results;Barker P. F.,2002

4. Early stall of West Antarctic Ice Sheet advance on the eastern Ross Sea middle shelf followed by retreat at 27,50014C yr BP

5. Did the Antarctic ice sheets expand during the early Pliocene?

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