Freshwater influx to the Eastern Mediterranean Sea from the melting of the Fennoscandian ice sheet during the last deglaciation

Between the Last Glacial Maximum and the mid-Holocene, the Mediterranean Sea experienced major hydrological changes. The deposition of the last sapropel, S1, during the Early Holocene is a consequence of these changes. In order to cause anoxia in the Eastern Mediterranean Sea (EMS) bottom water, a l...

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Detalles Bibliográficos
Autores principales: Vadsaria, Tristan, Zaragosi, Sébastien, Ramstein, Gilles, Dutay, Jean-Claude, Li, Laurent, Siani, Giuseppe, Revel, Marie, Obase, Takashi, Abe-Ouchi, Ayako
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2022
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9120512/
https://www.ncbi.nlm.nih.gov/pubmed/35589756
http://dx.doi.org/10.1038/s41598-022-12055-1

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9120512/
https://www.ncbi.nlm.nih.gov/pubmed/35589756
http://dx.doi.org/10.1038/s41598-022-12055-1

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