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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Published in:Science
Main Authors: Yu, Jimin, Broecker, Wally S.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2010
Subjects:
Online Access:http://dx.doi.org/10.1126/science.1186544
https://www.science.org/doi/pdf/10.1126/science.1186544
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spelling 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
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id 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
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