North Atlantic Deep Water Production during the Last Glacial Maximum
The nature of the overturning circulation in the Atlantic Ocean during the Last Glacial Maximum remains a topic of contention. Here, using neodymium isotope measurements, the authors demonstrate that North Atlantic Deep Water was produced under glacial climate conditions.
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| Autors principals: | , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Portfolio
2016-06-01
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| Col·lecció: | Nature Communications |
| Accés en línia: | https://doi.org/10.1038/ncomms11765 |
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