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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Detalles Bibliográficos
Autores principales: 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: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6063862/
https://www.ncbi.nlm.nih.gov/pubmed/30054536
http://dx.doi.org/10.1038/s41598-018-29718-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6063862/
https://www.ncbi.nlm.nih.gov/pubmed/30054536
http://dx.doi.org/10.1038/s41598-018-29718-7

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