The Evolving Paleobathymetry of the Circum‐Antarctic Southern Ocean Since 34 Ma: A Key to Understanding Past Cryosphere‐Ocean Developments-Reference-Cited by-同舟云学术

The Evolving Paleobathymetry of the Circum‐Antarctic Southern Ocean Since 34 Ma: A Key to Understanding Past Cryosphere‐Ocean Developments

Published:2020-08 Issue:8 Volume:21 Page:
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Hochmuth K.¹²^ORCID,Gohl K.¹^ORCID,Leitchenkov G.³⁴^ORCID,Sauermilch I.⁵^ORCID,Whittaker J. M.⁵^ORCID,Uenzelmann‐Neben G.¹^ORCID,Davy B.⁶^ORCID,De Santis L.⁷^ORCID

Affiliation:

1. Alfred Wegener Institute Helmholtz‐Centre for Polar and Marine Research Bremerhaven Germany

2. School of Geology, Geography and the Environment University of Leicester Leicester UK

3. Department of Antarctic Geoscience All Russia Scientific Research Institute for Geology and Mineral Resources of the Ocean St. Petersburg Russia

4. St. Petersburg State University St. Petersburg Russia

5. Institute for Marine and Antarctic Studies University of Tasmania Hobart Australia

6. GNS Science Lower Hutt New Zealand

7. National Institute of Oceanography and Applied Geophysics, OGS Trieste Italy

Funder

Australian Research Council

Deutsche Forschungsgemeinschaft

Ministry of Education- New Zealand

Russian Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GC009122

Reference131 articles.

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