Sea level fingerprinting of the Bering Strait flooding history detects the source of the Younger Dryas climate event

During the Last Glacial Maximum, expansive continental ice sheets lowered globally averaged sea level ~130 m, exposing a land bridge at the Bering Strait. During the subsequent deglaciation, sea level rose rapidly and ultimately flooded the Bering Strait, linking the Arctic and Pacific Oceans. Obser...

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Detalles Bibliográficos
Autores principales: Pico, T., Mitrovica, J. X., Mix, A. C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2020
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7043918/
https://www.ncbi.nlm.nih.gov/pubmed/32133400
http://dx.doi.org/10.1126/sciadv.aay2935

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7043918/
https://www.ncbi.nlm.nih.gov/pubmed/32133400
http://dx.doi.org/10.1126/sciadv.aay2935

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