No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum
The Southern Ocean plays a key role in glacial-interglacial transitions and today, Weddell Sea derived Antarctic Bottom Water is one of the most important deep water masses. New records show that in contrast to today, no Weddell Sea water was exported during the last two glacial maxima, providing ne...
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Format: | Article |
Language: | English |
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Nature Portfolio
2020-01-01
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Series: | Nature Communications |
Online Access: | https://doi.org/10.1038/s41467-020-14302-3 |
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author | Huang Huang Marcus Gutjahr Anton Eisenhauer Gerhard Kuhn |
author_facet | Huang Huang Marcus Gutjahr Anton Eisenhauer Gerhard Kuhn |
author_sort | Huang Huang |
collection | DOAJ |
description | The Southern Ocean plays a key role in glacial-interglacial transitions and today, Weddell Sea derived Antarctic Bottom Water is one of the most important deep water masses. New records show that in contrast to today, no Weddell Sea water was exported during the last two glacial maxima, providing new insights towards the condition of Antarctic Bottom Water formation in extreme climate states. |
first_indexed | 2024-12-19T04:26:06Z |
format | Article |
id | doaj.art-1235d436c3e7432f8f740f597e51f90c |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-12-19T04:26:06Z |
publishDate | 2020-01-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
spelling | doaj.art-1235d436c3e7432f8f740f597e51f90c2022-12-21T20:36:00ZengNature PortfolioNature Communications2041-17232020-01-0111111010.1038/s41467-020-14302-3No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial MaximumHuang Huang0Marcus Gutjahr1Anton Eisenhauer2Gerhard Kuhn3GEOMAR Helmholtz Centre for Ocean Research KielGEOMAR Helmholtz Centre for Ocean Research KielGEOMAR Helmholtz Centre for Ocean Research KielAlfred-Wegener-Institut Helmholtz-Zentrum für Polar- und MeeresforschungThe Southern Ocean plays a key role in glacial-interglacial transitions and today, Weddell Sea derived Antarctic Bottom Water is one of the most important deep water masses. New records show that in contrast to today, no Weddell Sea water was exported during the last two glacial maxima, providing new insights towards the condition of Antarctic Bottom Water formation in extreme climate states.https://doi.org/10.1038/s41467-020-14302-3 |
spellingShingle | Huang Huang Marcus Gutjahr Anton Eisenhauer Gerhard Kuhn No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum Nature Communications |
title | No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum |
title_full | No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum |
title_fullStr | No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum |
title_full_unstemmed | No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum |
title_short | No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum |
title_sort | no detectable weddell sea antarctic bottom water export during the last and penultimate glacial maximum |
url | https://doi.org/10.1038/s41467-020-14302-3 |
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