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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American Association for the Advancement of Science (AAAS)
2010
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Online Access: | http://dx.doi.org/10.1126/science.1186768 https://www.science.org/doi/pdf/10.1126/science.1186768 |
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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 |
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AAAS Resource Center (American Association for the Advancement of Science) |
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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 |
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328 |
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5985 |
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1480 |
op_container_end_page |
1480 |
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1801379527895547904 |