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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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 |
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Article Bridges, Joshua D. Tarduno, John A. Cottrell, Rory D. Herbert, Timothy D. Rapid strengthening of westerlies accompanied intensification of Northern Hemisphere glaciation |
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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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Nature Communications |
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14 |
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1 |
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