Response to comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"

Sosdian, Sindia ORCID: https://orcid.org/0000-0002-4599-5529 and Rosenthal, Yair 2010. Response to comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions". Science 328 (5985) , p. 1480. 10.1126/science.1186768

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Abstract

Yu and Broecker argue that the paleoceanographic interpretation of our 3.2-million-year record of North Atlantic deep-sea temperature hinges on the determination of whether temperature or carbonate saturation is the primary driver of benthic foraminiferal magnesium/calcium ratios from the North Atlantic. Here, we present evidence supporting our argument that bottom-water temperature variability is the primary control on benthic foraminiferal Mg/Ca at our site.

Item Type:	Article
Date Type:	Publication
Status:	Published
Schools:	Schools > Earth and Environmental Sciences
Subjects:	Q Science > QE Geology
Additional Information:	Technical comments
Publisher:	AAAS
ISSN:	0036-8075
Related URLs:	http://dx.doi.org/10.1126/science.118654... http://dx.doi.org/10.1126/science.116993...
Last Modified:	18 Oct 2022 12:21
URI:	https://orca.cardiff.ac.uk/id/eprint/9555

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