Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation

The trigger, pace, and nature of the intensification of Northern Hemisphere Glaciation (iNHG) are uncertain, but can be probed by study of ODP Site 1208 North Pacific marine sediments. Herein, we present magnetic proxy data that indicate a 4-fold increase of dust between ~ 2.73 and ~ 2.72 Ma, with s...

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Published in:Nature Communications
Main Authors: Bridges, Joshua D., Tarduno, John A., Cottrell, Rory D., Herbert, Timothy D.
Format: Text
Language:English
Published: Nature Publishing Group UK 2023
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10318093/
http://www.ncbi.nlm.nih.gov/pubmed/37400450
https://doi.org/10.1038/s41467-023-39557-4
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spelling ftpubmed:oai:pubmedcentral.nih.gov:10318093 2023-07-30T04:04:13+02:00 Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation Bridges, Joshua D. Tarduno, John A. Cottrell, Rory D. Herbert, Timothy D. 2023-07-03 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10318093/ http://www.ncbi.nlm.nih.gov/pubmed/37400450 https://doi.org/10.1038/s41467-023-39557-4 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10318093/ http://www.ncbi.nlm.nih.gov/pubmed/37400450 http://dx.doi.org/10.1038/s41467-023-39557-4 © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . Nat Commun Article Text 2023 ftpubmed https://doi.org/10.1038/s41467-023-39557-4 2023-07-09T01:00:20Z The trigger, pace, and nature of the intensification of Northern Hemisphere Glaciation (iNHG) are uncertain, but can be probed by study of ODP Site 1208 North Pacific marine sediments. Herein, we present magnetic proxy data that indicate a 4-fold increase of dust between ~ 2.73 and ~ 2.72 Ma, with subsequent increases at the start of glacials thereafter, indicating a strengthening of the mid-latitude westerlies. Moreover, a permanent shift in dust composition after 2.72 Ma is observed, consistent with drier conditions in the source region and/or the incorporation of material which could not have been transported via the weaker Pliocene winds. The sudden increase in our dust proxy data, a coeval rapid rise in dust recorded by proxy dust data in the North Atlantic (Site U1313), and the Site 1208 shift in dust composition, suggest that the iNHG represents a permanent crossing of a climate threshold toward global cooling and ice sheet growth, ultimately driven by lower atmospheric CO(2). Text Ice Sheet North Atlantic PubMed Central (PMC) Pacific Nature Communications 14 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Bridges, Joshua D.
Tarduno, John A.
Cottrell, Rory D.
Herbert, Timothy D.
Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation
topic_facet Article
description The trigger, pace, and nature of the intensification of Northern Hemisphere Glaciation (iNHG) are uncertain, but can be probed by study of ODP Site 1208 North Pacific marine sediments. Herein, we present magnetic proxy data that indicate a 4-fold increase of dust between ~ 2.73 and ~ 2.72 Ma, with subsequent increases at the start of glacials thereafter, indicating a strengthening of the mid-latitude westerlies. Moreover, a permanent shift in dust composition after 2.72 Ma is observed, consistent with drier conditions in the source region and/or the incorporation of material which could not have been transported via the weaker Pliocene winds. The sudden increase in our dust proxy data, a coeval rapid rise in dust recorded by proxy dust data in the North Atlantic (Site U1313), and the Site 1208 shift in dust composition, suggest that the iNHG represents a permanent crossing of a climate threshold toward global cooling and ice sheet growth, ultimately driven by lower atmospheric CO(2).
format Text
author Bridges, Joshua D.
Tarduno, John A.
Cottrell, Rory D.
Herbert, Timothy D.
author_facet Bridges, Joshua D.
Tarduno, John A.
Cottrell, Rory D.
Herbert, Timothy D.
author_sort Bridges, Joshua D.
title Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation
title_short Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation
title_full Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation
title_fullStr Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation
title_full_unstemmed Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation
title_sort rapid strengthening of westerlies accompanied intensification of northern hemisphere glaciation
publisher Nature Publishing Group UK
publishDate 2023
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10318093/
http://www.ncbi.nlm.nih.gov/pubmed/37400450
https://doi.org/10.1038/s41467-023-39557-4
geographic Pacific
geographic_facet Pacific
genre Ice Sheet
North Atlantic
genre_facet Ice Sheet
North Atlantic
op_source Nat Commun
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10318093/
http://www.ncbi.nlm.nih.gov/pubmed/37400450
http://dx.doi.org/10.1038/s41467-023-39557-4
op_rights © The Author(s) 2023
https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
op_doi https://doi.org/10.1038/s41467-023-39557-4
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