Extreme warming of tropical waters during the Paleocene–Eocene Thermal Maximum-Reference-Cited by-同舟云学术

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Extreme warming of tropical waters during the Paleocene–Eocene Thermal Maximum

Published:2014-09 Issue:9 Volume:42 Page:739-742
ISSN:1943-2682
Container-title:Geology
language:en
Short-container-title:

Author:

Aze T.,Pearson P.N.,Dickson A.J.,Badger M.P.S.,Bown P.R.,Pancost R.D.,Gibbs S.J.,Huber B.T.,Leng M.J.,Coe A.L.,Cohen A.S.,Foster G.L.

Publisher

Geological Society of America

Subject

Geology

Link

http://pubs.geoscienceworld.org/geology/article-pdf/42/9/739/3546468/739.pdf

Reference28 articles.

1. Re-evaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised palaeotemperature equations;Bemis;Paleoceanography,1998

2. A revised tropical to subtropical Paleogene planktonic foraminiferal zonation;Berggren;Journal of Foraminiferal Research,2005

3. Calcareous plankton evolution and the Paleocene/Eocene thermal maximum event: New evidence from Tanzania;Bown;Marine Micropaleontology,2009

4. Techniques;Bown,1998

5. Late Cretaceous–Neogene trends in deep ocean temperature and continental ice volume: Reconciling records of benthic foraminiferal geochemistry (δ18O and Mg/Ca) with sea level history;Cramer;Journal of Geophysical Research,2011

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