The paradox of a long grounding during West Antarctic Ice Sheet retreat in Ross Sea

Marine geological data show that the West Antarctic Ice Sheet (WAIS) advanced to the eastern Ross Sea shelf edge during the Last Glacial Maximum (LGM) and eventually retreated ~1000 km to the current grounding-line position on the inner shelf. During the early deglacial, the WAIS deposited a volumin...

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Detalles Bibliográficos
Autores principales: Bart, Philip J., Krogmeier, Benjamin J., Bart, Manon P., Tulaczyk, Slawek
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5430838/
https://www.ncbi.nlm.nih.gov/pubmed/28455508
http://dx.doi.org/10.1038/s41598-017-01329-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5430838/
https://www.ncbi.nlm.nih.gov/pubmed/28455508
http://dx.doi.org/10.1038/s41598-017-01329-8

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