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Synchronous deglacial thermocline and deep-water ventilation in the eastern equatorial Pacific

The deep ocean is most likely the primary source of the radiocarbon-depleted CO(2) released to the atmosphere during the last deglaciation. While there are well-documented millennial scale Δ(14)C changes during the most recent deglaciation, most marine records lack the resolution needed to identify...

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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: Umling, Natalie E., Thunell, Robert C.
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2017
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5264251/
https://ncbi.nlm.nih.gov/pubmed/28112161
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms14203
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