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Carbon isotope evidence for a northern source of deep water in the glacial western North Atlantic

The prevailing view of western Atlantic hydrography during the Last Glacial Maximum (LGM) calls for transport and intermixing of deep southern and intermediate northern end members. However, δ(13)C and Δ(14)C results on foraminifera from a sediment core at 5.0 km in the northern subtropics show that...

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Detalhes bibliográficos
Publicado no:Proc Natl Acad Sci U S A
Main Authors: Keigwin, Lloyd D., Swift, Stephen A.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2017
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC5358345/
https://ncbi.nlm.nih.gov/pubmed/28193884
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1614693114
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