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