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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Bibliographic Details
Main Authors: Sangiorgi, Francesca (Author) , Pross, Jörg (Author) , Brinkhuis, Henk (Author)
Format: Article (Journal)
Language:English
Published: 22 January 2018
In: Nature Communications
Year: 2018, Volume: 9
ISSN:2041-1723
DOI:10.1038/s41467-017-02609-7
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Author Notes:Francesca Sangiorgi, Peter K. Bijl, Sandra Passchier, Ulrich Salzmann, Stefan Schouten, Robert McKay, Rosemary D. Cody, Jörg Pross, Tina Flierdt, Steven M. Bohaty, Richard Levy, Trevor Williams, Carlota Escutia, Henk Brinkhuis
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Summary: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.
Item Description:Gesehen am 14.02.2018
Physical Description:Online Resource
ISSN:2041-1723
DOI:10.1038/s41467-017-02609-7