I/Ca evidence for upper ocean deoxygenation during the PETM-Reference-Cited by-同舟云学术

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I/Ca evidence for upper ocean deoxygenation during the PETM

Published:2014-10 Issue:10 Volume:29 Page:964-975
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Zhou Xiaoli¹,Thomas Ellen²³,Rickaby Rosalind E. M.⁴,Winguth Arne M. E.⁵,Lu Zunli¹

Affiliation:

1. Department of Earth Sciences; Syracuse University; Syracuse New York USA

2. Department of Geology and Geophysics; Yale University; New Haven Connecticut USA

3. Department of Earth and Environmental Sciences; Wesleyan University; Middletown Connecticut USA

4. Department of Earth Sciences; University of Oxford; Oxford UK

5. Department of Earth and Environmental Sciences; University of Texas; Arlington Texas USA

Funder

NSF OCE

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014PA002702/fullpdf

Reference92 articles.

1. Comparative analysis of marine paleogene sections and biota from West Siberia and the Arctic Region;Akhmet'ev;Stratigr. Geol. Correl.,2010

2. Extinction and recovery of benthic foraminifera across the Paleocene-Eocene Thermal Maximum at the Alamedilla section (Southern Spain);Alegret;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2009

3. What happens when the ocean is overheated? The foraminiferal response across the Paleocene-Eocene Thermal Maximum at the Alamedilla section (Spain);Alegret;Geol. Soc. Am. Bull.,2010

4. Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions;Algeo;Paleoceanography,2006

5. Redox renaissance;Anbar;Geology,2008

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