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...
Published in: | Science |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
AAAS
2010
|
Subjects: | |
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 |
_version_ |
1766119589893111808 |