Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene

Ocean heat is important in forcing ice sheet retreat, yet past ocean temperature data from proximal ice sheet locations are sparse. Here, the authors present temperature reconstructions from the Wilkes Land subglacial basin during the mid-Miocene, and show that warm waters sustained ice sheet retrea...

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Autores principales: Francesca Sangiorgi, Peter K. Bijl, Sandra Passchier, Ulrich Salzmann, Stefan Schouten, Robert McKay, Rosemary D. Cody, Jörg Pross, Tina van de Flierdt, Steven M. Bohaty, Richard Levy, Trevor Williams, Carlota Escutia, Henk Brinkhuis
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Lenguaje:EN
Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/5d1d8a15101a4010af35615aec6ac5b9
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spelling oai:doaj.org-article:5d1d8a15101a4010af35615aec6ac5b92021-12-02T16:56:59ZSouthern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene10.1038/s41467-017-02609-72041-1723https://doaj.org/article/5d1d8a15101a4010af35615aec6ac5b92018-01-01T00:00:00Zhttps://doi.org/10.1038/s41467-017-02609-7https://doaj.org/toc/2041-1723Ocean heat is important in forcing ice sheet retreat, yet past ocean temperature data from proximal ice sheet locations are sparse. Here, the authors present temperature reconstructions from the Wilkes Land subglacial basin during the mid-Miocene, and show that warm waters sustained ice sheet retreat 17–14.8 Ma.Francesca SangiorgiPeter K. BijlSandra PasschierUlrich SalzmannStefan SchoutenRobert McKayRosemary D. CodyJörg ProssTina van de FlierdtSteven M. BohatyRichard LevyTrevor WilliamsCarlota EscutiaHenk BrinkhuisNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-11 (2018)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Francesca Sangiorgi
Peter K. Bijl
Sandra Passchier
Ulrich Salzmann
Stefan Schouten
Robert McKay
Rosemary D. Cody
Jörg Pross
Tina van de Flierdt
Steven M. Bohaty
Richard Levy
Trevor Williams
Carlota Escutia
Henk Brinkhuis
Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
description Ocean heat is important in forcing ice sheet retreat, yet past ocean temperature data from proximal ice sheet locations are sparse. Here, the authors present temperature reconstructions from the Wilkes Land subglacial basin during the mid-Miocene, and show that warm waters sustained ice sheet retreat 17–14.8 Ma.
format article
author Francesca Sangiorgi
Peter K. Bijl
Sandra Passchier
Ulrich Salzmann
Stefan Schouten
Robert McKay
Rosemary D. Cody
Jörg Pross
Tina van de Flierdt
Steven M. Bohaty
Richard Levy
Trevor Williams
Carlota Escutia
Henk Brinkhuis
author_facet Francesca Sangiorgi
Peter K. Bijl
Sandra Passchier
Ulrich Salzmann
Stefan Schouten
Robert McKay
Rosemary D. Cody
Jörg Pross
Tina van de Flierdt
Steven M. Bohaty
Richard Levy
Trevor Williams
Carlota Escutia
Henk Brinkhuis
author_sort Francesca Sangiorgi
title Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
title_short Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
title_full Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
title_fullStr Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
title_full_unstemmed Southern Ocean warming and Wilkes Land ice sheet retreat during the mid-Miocene
title_sort southern ocean warming and wilkes land ice sheet retreat during the mid-miocene
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/5d1d8a15101a4010af35615aec6ac5b9
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