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Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum

Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_987d5132d86f4a4eb951c9a1a7b4b410

Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum

About this item

Full title

Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum

Publisher

London: Nature Publishing Group UK

Journal title

Scientific reports, 2021-03, Vol.11 (1), p.6788-14, Article 6788

Language

English

Formats

Publication information

Publisher

London: Nature Publishing Group UK

More information

Scope and Contents

Contents

The Last Glacial Maximum (LGM, 23–19,000 year BP) designates a period of extensive glacial extent and very cold conditions on the Northern Hemisphere. The strength of ocean circulation during this period has been highly debated. Based on investigations of two marine sediment cores from the Davis Strait (1033 m water depth) and the northern Labrador...

Alternative Titles

Full title

Evidence for influx of Atlantic water masses to the Labrador Sea during the Last Glacial Maximum

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_987d5132d86f4a4eb951c9a1a7b4b410

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_987d5132d86f4a4eb951c9a1a7b4b410

Other Identifiers

ISSN

2045-2322

E-ISSN

2045-2322

DOI

10.1038/s41598-021-86224-z

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