Freshwater influx to the Eastern Mediterranean Sea from the melting of the Fennoscandian ice sheet d...
Freshwater influx to the Eastern Mediterranean Sea from the melting of the Fennoscandian ice sheet during the last deglaciation
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London: Nature Publishing Group UK
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Language
English
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Publisher
London: Nature Publishing Group UK
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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 long preconditioning period of a few thousand years...
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Freshwater influx to the Eastern Mediterranean Sea from the melting of the Fennoscandian ice sheet during the last deglaciation
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TN_cdi_doaj_primary_oai_doaj_org_article_01279c7f67a0471ea8a0d91e7ff9e262
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_01279c7f67a0471ea8a0d91e7ff9e262
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ISSN
2045-2322
E-ISSN
2045-2322
DOI
10.1038/s41598-022-12055-1
