Patterns and magnitude of deep sea carbonate dissolution during Eocene Thermal Maximum 2 and H2, Walvis Ridge, southeastern Atlantic Ocean-Reference-Cited by-同舟云学术

Patterns and magnitude of deep sea carbonate dissolution during Eocene Thermal Maximum 2 and H2, Walvis Ridge, southeastern Atlantic Ocean

Published:2009-03 Issue:1 Volume:24 Page:n/a-n/a
ISSN:0883-8305
Container-title:Paleoceanography
language:en
Short-container-title:Paleoceanography

Author:

Stap Lucy¹,Sluijs Appy²,Thomas Ellen³,Lourens Lucas¹

Affiliation:

1. Faculty of Geosciences; Utrecht University; Utrecht Netherlands

2. Palaeoecology, Laboratory of Palaeobotany and Palynology, Institute of Environmental Biology; Utrecht University; Utrecht Netherlands

3. Centre for the Study of Global Change, Department of Geology and Geophysics; Yale University; New Haven Connecticut USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Oceanography

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4. Geol. Soc. Spec. Publ.;Dickens,2001

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