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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Autores principales: Jacob N. W. Howe, Alexander M. Piotrowski, Taryn L. Noble, Stefan Mulitza, Cristiano M. Chiessi, Germain Bayon
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2016
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Acceso en línea:https://doaj.org/article/5b843f02a4bf4ca696afd91c12917652
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