Asynchronous warming and δ(18)O evolution of deep Atlantic water masses during the last deglaciation

The large-scale reorganization of deep ocean circulation in the Atlantic involving changes in North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW) played a critical role in regulating hemispheric and global climate during the last deglaciation. However, changes in the relative contribu...

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Détails bibliographiques
Publié dans:Proc Natl Acad Sci U S A
Auteurs principaux: Zhang, Jiaxu, Liu, Zhengyu, Brady, Esther C., Oppo, Delia W., Clark, Peter U., Jahn, Alexandra, Marcott, Shaun A., Lindsay, Keith
Format: Artigo
Langue:Inglês
Publié: National Academy of Sciences 2017
Sujets:
Physical Sciences
Accès en ligne:https://ncbi.nlm.nih.gov/pmc/articles/PMC5651742/
https://ncbi.nlm.nih.gov/pubmed/28973944
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1704512114
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