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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Autores principales:	Huang Huang, Marcus Gutjahr, Anton Eisenhauer, Gerhard Kuhn
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2020
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/1235d436c3e7432f8f740f597e51f90c
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spelling	oai:doaj.org-article:1235d436c3e7432f8f740f597e51f90c2021-12-02T17:31:56ZNo detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum10.1038/s41467-020-14302-32041-1723https://doaj.org/article/1235d436c3e7432f8f740f597e51f90c2020-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-14302-3https://doaj.org/toc/2041-1723The 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.Huang HuangMarcus GutjahrAnton EisenhauerGerhard KuhnNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Huang Huang Marcus Gutjahr Anton Eisenhauer Gerhard Kuhn No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum
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.
format	article
author	Huang Huang Marcus Gutjahr Anton Eisenhauer Gerhard Kuhn
author_facet	Huang Huang Marcus Gutjahr Anton Eisenhauer Gerhard Kuhn
author_sort	Huang Huang
title	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_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_sort	no detectable weddell sea antarctic bottom water export during the last and penultimate glacial maximum
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/1235d436c3e7432f8f740f597e51f90c
work_keys_str_mv	AT huanghuang nodetectableweddellseaantarcticbottomwaterexportduringthelastandpenultimateglacialmaximum AT marcusgutjahr nodetectableweddellseaantarcticbottomwaterexportduringthelastandpenultimateglacialmaximum AT antoneisenhauer nodetectableweddellseaantarcticbottomwaterexportduringthelastandpenultimateglacialmaximum AT gerhardkuhn nodetectableweddellseaantarcticbottomwaterexportduringthelastandpenultimateglacialmaximum
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No detectable Weddell Sea Antarctic Bottom Water export during the Last and Penultimate Glacial Maximum

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