Rapid and sustained surface ocean acidification during the Paleocene-Eocene Thermal Maximum-Reference-Cited by-同舟云学术

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Rapid and sustained surface ocean acidification during the Paleocene-Eocene Thermal Maximum

Published:2014-05 Issue:5 Volume:29 Page:357-369
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Penman Donald E.¹,Hönisch Bärbel²,Zeebe Richard E.³,Thomas Ellen⁴⁵,Zachos James C.¹

Affiliation:

1. University of California; Santa Cruz California USA

2. Department of Earth and Environmental Sciences; Lamont-Doherty Earth Observatory of Columbia University; Palisades New York USA

3. University of Hawai‘i at Mānoa; Honolulu Hawaii USA

4. Yale University; New Haven Connecticut USA

5. Wesleyan University; Middletown Connecticut USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

Reference68 articles.

1. The planktic foraminiferal B/Ca proxy for seawater carbonate chemistry: A critical evaluation;Allen;Earth Planet. Sci. Lett.,2012

2. Controls on boron incorporation in cultured tests of the planktic foraminifer Orbulina universa;Allen;Earth Planet. Sci. Lett.,2011

3. Environmental controls on B/Ca in calcite tests of the tropical planktic foraminifer species Globigerinoides ruber and Globigerinoides sacculifer;Allen;Earth Planet. Sci. Lett.,2012

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

5. Biostratigraphy, phylogeny and systematics of Paleocene trochospiral planktic foraminifera;Berggren;Micropaleontol,1997

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