Past continental shelf evolution increased Antarctic ice sheet sensitivity to climatic conditions

Over the past 34 Million years, the Antarctic continental shelf has gradually deepened due to ice sheet loading, thermal subsidence, and erosion from repeated glaciations. The deepening that is recorded in the sedimentary deposits around the Antarctic margin indicates that after the mid-Miocene Clim...

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Veröffentlicht in:	Scientific reports Jg. 8; H. 1; S. 11323
Hauptverfasser:	Colleoni, Florence, De Santis, Laura, Montoli, Enea, Olivo, Elisabetta, Sorlien, Christopher C., Bart, Philip J., Gasson, Edward G. W., Bergamasco, Andrea, Sauli, Chiara, Wardell, Nigel, Prato, Stefano
Format:	Journal Article
Sprache:	Englisch
Veröffentlicht:	London Nature Publishing Group UK 27.07.2018 Nature Publishing Group
Schlagworte:	639/705/1042 704/106/413 Atmospheric forcing Climatic conditions Continental shelves Evolution Glaciation Humanities and Social Sciences Ice Miocene multidisciplinary Pleistocene Science Science (multidisciplinary) Sea level
ISSN:	2045-2322, 2045-2322
Online-Zugang:	Volltext
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