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A long marine history of carbon cycle modulation by orbital-climatic changes
Pacing of the marine carbon cycle by orbital forcing during the Pliocene and Pleistocene Ice Ages [past 2.5 million years (Myr)] is well known. As older deep-sea sediment records are being studied at greater temporal resolution, it is becoming clear that similar fluctuations in the marine carbon sys...
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
The National Academy of Sciences of the USA
1997
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| Accès en ligne: | https://ncbi.nlm.nih.gov/pmc/articles/PMC33754/ https://ncbi.nlm.nih.gov/pubmed/11607746 |
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