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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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| Formato: | Artigo |
| Idioma: | Inglês |
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The National Academy of Sciences of the USA
1997
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| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC33731/ https://ncbi.nlm.nih.gov/pubmed/11607737 |
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