Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions”
Sosdian and Rosenthal (Reports, 17 July 2009, p. 306) used magnesium/calcium ratios in benthic foraminifera from the North Atlantic to reconstruct past bottom-water temperatures. They suggested that both ice volume change and ice-sheet dynamics played important roles during the late Pliocene and mid...
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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.1186544 https://www.science.org/doi/pdf/10.1126/science.1186544 |
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craaas:10.1126/science.1186544 2024-09-15T18:12:17+00:00 Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” Yu, Jimin Broecker, Wally S. 2010 http://dx.doi.org/10.1126/science.1186544 https://www.science.org/doi/pdf/10.1126/science.1186544 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.1186544 2024-06-27T04:01:33Z Sosdian and Rosenthal (Reports, 17 July 2009, p. 306) used magnesium/calcium ratios in benthic foraminifera from the North Atlantic to reconstruct past bottom-water temperatures. They suggested that both ice volume change and ice-sheet dynamics played important roles during the late Pliocene and mid-Pleistocene climate transitions. We present evidence that their record of deep ocean temperature is not reliable, thus raising doubts about their conclusions. Article in Journal/Newspaper Ice Sheet North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 328 5985 1480 1480 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
Sosdian and Rosenthal (Reports, 17 July 2009, p. 306) used magnesium/calcium ratios in benthic foraminifera from the North Atlantic to reconstruct past bottom-water temperatures. They suggested that both ice volume change and ice-sheet dynamics played important roles during the late Pliocene and mid-Pleistocene climate transitions. We present evidence that their record of deep ocean temperature is not reliable, thus raising doubts about their conclusions. |
format |
Article in Journal/Newspaper |
author |
Yu, Jimin Broecker, Wally S. |
spellingShingle |
Yu, Jimin Broecker, Wally S. Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” |
author_facet |
Yu, Jimin Broecker, Wally S. |
author_sort |
Yu, Jimin |
title |
Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” |
title_short |
Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” |
title_full |
Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” |
title_fullStr |
Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” |
title_full_unstemmed |
Comment on “Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions” |
title_sort |
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.1186544 https://www.science.org/doi/pdf/10.1126/science.1186544 |
genre |
Ice Sheet North Atlantic |
genre_facet |
Ice Sheet 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.1186544 |
container_title |
Science |
container_volume |
328 |
container_issue |
5985 |
container_start_page |
1480 |
op_container_end_page |
1480 |
_version_ |
1810449877002354688 |