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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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| Publicado en: | Proc Natl Acad Sci U S A |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado: |
National Academy of Sciences
2017
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| Assuntos: | |
| Acceso en liña: | 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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