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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Bibliographic Details
Published in:Science
Main Authors: Sosdian, Sindia, Rosenthal, Yair
Format: Article in Journal/Newspaper
Language:unknown
Published: AAAS 2010
Subjects:
QE Geology
North Atlantic
Online Access:https://orca.cardiff.ac.uk/id/eprint/9555/
https://doi.org/10.1126/science.1186768
id ftunivcardiff:oai:https://orca.cardiff.ac.uk:9555
record_format openpolar
spelling ftunivcardiff:oai:https://orca.cardiff.ac.uk:9555 2023-05-15T17:27:29+02:00 Response to comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions" Sosdian, Sindia Rosenthal, Yair 2010-06 https://orca.cardiff.ac.uk/id/eprint/9555/ https://doi.org/10.1126/science.1186768 unknown AAAS Sosdian, Sindia https://orca.cardiff.ac.uk/view/cardiffauthors/A185665E.html orcid:0000-0002-4599-5529 orcid: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 https://doi.org/10.1126/science.1186768 doi:10.1126/science.1186768 QE Geology Article PeerReviewed 2010 ftunivcardiff https://doi.org/10.1126/science.1186768 2022-10-20T22:34:04Z 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 Cardiff University: ORCA (Online Research @ Cardiff) Science 328 5985 1480 1480
institution Open Polar
collection Cardiff University: ORCA (Online Research @ Cardiff)
op_collection_id ftunivcardiff
language unknown
topic QE Geology
spellingShingle QE Geology
Sosdian, Sindia
Rosenthal, Yair
Response to comment on "Deep-Sea Temperature and Ice Volume Changes Across the Pliocene-Pleistocene Climate Transitions"
topic_facet QE Geology
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, Sindia
Rosenthal, Yair
author_facet Sosdian, Sindia
Rosenthal, Yair
author_sort Sosdian, Sindia
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 AAAS
publishDate 2010
url https://orca.cardiff.ac.uk/id/eprint/9555/
https://doi.org/10.1126/science.1186768
genre North Atlantic
genre_facet North Atlantic
op_relation Sosdian, Sindia https://orca.cardiff.ac.uk/view/cardiffauthors/A185665E.html orcid:0000-0002-4599-5529 orcid: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 https://doi.org/10.1126/science.1186768
doi:10.1126/science.1186768
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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