Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”

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 Atla...

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Published in:Science
Main Authors: Sosdian, S., Rosenthal, Y.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2010
Subjects:
North Atlantic
Online Access:http://dx.doi.org/10.1126/science.1186768
https://www.science.org/doi/pdf/10.1126/science.1186768
id craaas:10.1126/science.1186768
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spelling craaas:10.1126/science.1186768 2024-06-09T07:48:00+00:00 Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” Sosdian, S. Rosenthal, Y. 2010 http://dx.doi.org/10.1126/science.1186768 https://www.science.org/doi/pdf/10.1126/science.1186768 en eng American Association for the Advancement of Science (AAAS) Science volume 328, issue 5985, page 1480-1480 ISSN 0036-8075 1095-9203 journal-article 2010 craaas https://doi.org/10.1126/science.1186768 2024-05-16T12:54:57Z 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. Article in Journal/Newspaper North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 328 5985 1480 1480
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description 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.
format Article in Journal/Newspaper
author Sosdian, S.
Rosenthal, Y.
spellingShingle Sosdian, S.
Rosenthal, Y.
Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
author_facet Sosdian, S.
Rosenthal, Y.
author_sort Sosdian, S.
title Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
title_short Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
title_full Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
title_fullStr Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
title_full_unstemmed Response to Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
title_sort response to comment on “deep-sea temperature and ice volume changes across the pliocene-pleistocene climate transitions”
publisher American Association for the Advancement of Science (AAAS)
publishDate 2010
url http://dx.doi.org/10.1126/science.1186768
https://www.science.org/doi/pdf/10.1126/science.1186768
genre North Atlantic
genre_facet North Atlantic
op_source Science
volume 328, issue 5985, page 1480-1480
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.1186768
container_title Science
container_volume 328
container_issue 5985
container_start_page 1480
op_container_end_page 1480
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