Characteristics of the deep ocean carbon system during the past 150,000 years: ΣCO(2) distributions, deep water flow patterns, and abrupt climate change
Studies of carbon isotopes and cadmium in bottom-dwelling foraminifera from ocean sediment cores have advanced our knowledge of ocean chemical distributions during the late Pleistocene. Last Glacial Maximum data are consistent with a persistent high-ΣCO(2) state for eastern Pacific deep water. Both...
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| Publié dans: | Proc Natl Acad Sci U S A |
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| Auteur principal: | |
| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
National Academy of Sciences
1997
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| Accès en ligne: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC33731/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11607737/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.94.16.8300 |
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