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Global synchronous changes in the carbon isotopic composition of carbonate sediments unrelated to changes in the global carbon cycle
The carbon isotopic (δ(13)C) composition of bulk carbonate sediments deposited off the margins of four carbonate platforms/ramp systems (Bahamas, Maldives, Queensland Plateau, and Great Australian Bight) show synchronous changes over the past 0 to 10 million years. However, these variations are diff...
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2008
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| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC2544524/ https://ncbi.nlm.nih.gov/pubmed/18772393 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0802841105 |
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