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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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Bibliografske podrobnosti
izdano v:Proc Natl Acad Sci U S A
Main Authors: Keigwin, Lloyd D., Swift, Stephen A.
Format: Artigo
Jezik:Inglês
Izdano: National Academy of Sciences 2017
Teme:
Online dostop: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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