Migration of the subtropical front as a modulator of glacial climate.
Ice cores extracted from the Antarctic ice sheet suggest that glacial conditions, and the relationship between isotopically derived temperatures and atmospheric PCO(2) have been constant over the last 800,000 years of the Late Pleistocene epoch. But independent lines of evidence, such as the extent...
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ftuloxford:oai:ora.ox.ac.uk:uuid:9bfdd9cd-1692-4adb-98f1-1b5694c960f6 2023-05-15T13:49:19+02:00 Migration of the subtropical front as a modulator of glacial climate. Bard, E Rickaby, R 2016-07-28 https://doi.org/10.1038/nature08189 https://ora.ox.ac.uk/objects/uuid:9bfdd9cd-1692-4adb-98f1-1b5694c960f6 eng eng doi:10.1038/nature08189 https://ora.ox.ac.uk/objects/uuid:9bfdd9cd-1692-4adb-98f1-1b5694c960f6 https://doi.org/10.1038/nature08189 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1038/nature08189 2022-06-28T20:19:22Z Ice cores extracted from the Antarctic ice sheet suggest that glacial conditions, and the relationship between isotopically derived temperatures and atmospheric PCO(2) have been constant over the last 800,000 years of the Late Pleistocene epoch. But independent lines of evidence, such as the extent of Northern Hemisphere ice sheets, sea level and other temperature records, point towards a fluctuating severity of glacial periods, particularly during the more extreme glacial stadials centred around 340,000 and 420,000 years ago (marine isotope stages 10 and 12). Previously unidentified mechanisms therefore appear to have mediated the relationship between insolation, CO(2) and climate. Here we test whether northward migration of the subtropical front (STF) off the southeastern coast of South Africa acts as a gatekeeper for the Agulhas current, which controls the transport of heat and salt from the Indo-Pacific Ocean to the Atlantic Ocean. Using a new 800,000-year record of sea surface temperature and ocean productivity from ocean sediment core MD962077, we demonstrate that during cold stadials (particularly marine isotope stages 10 and 12), productivity peaked and sea surface temperature was up to 6 degrees C cooler than modern temperatures. This suggests that during these cooler stadials, the STF moved northward by up to 7 degrees latitude, nearly shutting off the Agulhas current. Our results, combined with faunal assemblages from the south Atlantic show that variable northwards migration of the Southern Hemisphere STF can modulate the severity of each glacial period by altering the strength of the Agulhas current carrying heat and salt to the Atlantic meridional overturning circulation. We show hence that the degree of northwards migration of the STF can partially decouple global climate from atmospheric partial pressure of carbon dioxide, P CO(2), and help to resolve the long-standing puzzle of differing glacial amplitudes within a consistent range of atmospheric PCO(2). Article in Journal/Newspaper Antarc* Antarctic Ice Sheet ORA - Oxford University Research Archive Antarctic Pacific The Antarctic Nature 460 7253 380 383 |
institution |
Open Polar |
collection |
ORA - Oxford University Research Archive |
op_collection_id |
ftuloxford |
language |
English |
description |
Ice cores extracted from the Antarctic ice sheet suggest that glacial conditions, and the relationship between isotopically derived temperatures and atmospheric PCO(2) have been constant over the last 800,000 years of the Late Pleistocene epoch. But independent lines of evidence, such as the extent of Northern Hemisphere ice sheets, sea level and other temperature records, point towards a fluctuating severity of glacial periods, particularly during the more extreme glacial stadials centred around 340,000 and 420,000 years ago (marine isotope stages 10 and 12). Previously unidentified mechanisms therefore appear to have mediated the relationship between insolation, CO(2) and climate. Here we test whether northward migration of the subtropical front (STF) off the southeastern coast of South Africa acts as a gatekeeper for the Agulhas current, which controls the transport of heat and salt from the Indo-Pacific Ocean to the Atlantic Ocean. Using a new 800,000-year record of sea surface temperature and ocean productivity from ocean sediment core MD962077, we demonstrate that during cold stadials (particularly marine isotope stages 10 and 12), productivity peaked and sea surface temperature was up to 6 degrees C cooler than modern temperatures. This suggests that during these cooler stadials, the STF moved northward by up to 7 degrees latitude, nearly shutting off the Agulhas current. Our results, combined with faunal assemblages from the south Atlantic show that variable northwards migration of the Southern Hemisphere STF can modulate the severity of each glacial period by altering the strength of the Agulhas current carrying heat and salt to the Atlantic meridional overturning circulation. We show hence that the degree of northwards migration of the STF can partially decouple global climate from atmospheric partial pressure of carbon dioxide, P CO(2), and help to resolve the long-standing puzzle of differing glacial amplitudes within a consistent range of atmospheric PCO(2). |
format |
Article in Journal/Newspaper |
author |
Bard, E Rickaby, R |
spellingShingle |
Bard, E Rickaby, R Migration of the subtropical front as a modulator of glacial climate. |
author_facet |
Bard, E Rickaby, R |
author_sort |
Bard, E |
title |
Migration of the subtropical front as a modulator of glacial climate. |
title_short |
Migration of the subtropical front as a modulator of glacial climate. |
title_full |
Migration of the subtropical front as a modulator of glacial climate. |
title_fullStr |
Migration of the subtropical front as a modulator of glacial climate. |
title_full_unstemmed |
Migration of the subtropical front as a modulator of glacial climate. |
title_sort |
migration of the subtropical front as a modulator of glacial climate. |
publishDate |
2016 |
url |
https://doi.org/10.1038/nature08189 https://ora.ox.ac.uk/objects/uuid:9bfdd9cd-1692-4adb-98f1-1b5694c960f6 |
geographic |
Antarctic Pacific The Antarctic |
geographic_facet |
Antarctic Pacific The Antarctic |
genre |
Antarc* Antarctic Ice Sheet |
genre_facet |
Antarc* Antarctic Ice Sheet |
op_relation |
doi:10.1038/nature08189 https://ora.ox.ac.uk/objects/uuid:9bfdd9cd-1692-4adb-98f1-1b5694c960f6 https://doi.org/10.1038/nature08189 |
op_rights |
info:eu-repo/semantics/embargoedAccess |
op_doi |
https://doi.org/10.1038/nature08189 |
container_title |
Nature |
container_volume |
460 |
container_issue |
7253 |
container_start_page |
380 |
op_container_end_page |
383 |
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1766251163385069568 |