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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Detalhes bibliográficos
Publicado no:Sci Rep
Main Authors: 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
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
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Article
Acesso em linha: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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