Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth

Ocean circulation likely played a major role in past episodes of global warming. Here the authors show that converging neodymium isotope values indicate intensification of the Atlantic overturning circulation at 59 million years ago, which may have contributed to a more efficient distribution of hea...

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Main Authors:	S. J. Batenburg, S. Voigt, O. Friedrich, A. H. Osborne, A. Bornemann, T. Klein, L. Pérez-Díaz, M. Frank
Format:	article
Language:	EN
Published:	Nature Portfolio 2018
Subjects:	Science Q
Online Access:	https://doaj.org/article/bb59178d7edb47f6bbde604f5d972aac
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spelling	oai:doaj.org-article:bb59178d7edb47f6bbde604f5d972aac2021-12-02T17:32:14ZMajor intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth10.1038/s41467-018-07457-72041-1723https://doaj.org/article/bb59178d7edb47f6bbde604f5d972aac2018-11-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-07457-7https://doaj.org/toc/2041-1723Ocean circulation likely played a major role in past episodes of global warming. Here the authors show that converging neodymium isotope values indicate intensification of the Atlantic overturning circulation at 59 million years ago, which may have contributed to a more efficient distribution of heat over the planet.S. J. BatenburgS. VoigtO. FriedrichA. H. OsborneA. BornemannT. KleinL. Pérez-DíazM. FrankNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q S. J. Batenburg S. Voigt O. Friedrich A. H. Osborne A. Bornemann T. Klein L. Pérez-Díaz M. Frank Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
description	Ocean circulation likely played a major role in past episodes of global warming. Here the authors show that converging neodymium isotope values indicate intensification of the Atlantic overturning circulation at 59 million years ago, which may have contributed to a more efficient distribution of heat over the planet.
format	article
author	S. J. Batenburg S. Voigt O. Friedrich A. H. Osborne A. Bornemann T. Klein L. Pérez-Díaz M. Frank
author_facet	S. J. Batenburg S. Voigt O. Friedrich A. H. Osborne A. Bornemann T. Klein L. Pérez-Díaz M. Frank
author_sort	S. J. Batenburg
title	Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
title_short	Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
title_full	Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
title_fullStr	Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
title_full_unstemmed	Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth
title_sort	major intensification of atlantic overturning circulation at the onset of paleogene greenhouse warmth
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/bb59178d7edb47f6bbde604f5d972aac
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Major intensification of Atlantic overturning circulation at the onset of Paleogene greenhouse warmth

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