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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...

Ausführliche Beschreibung

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Bibliographische Detailangaben
Veröffentlicht in:Sci Rep
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: Artigo
Sprache:Inglês
Veröffentlicht: Nature Publishing Group UK 2018
Schlagworte:
Online Zugang:https://ncbi.nlm.nih.gov/pmc/articles/PMC6063862/
https://ncbi.nlm.nih.gov/pubmed/30054536
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-29718-7
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