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Towards a quantitative understanding of the late Neoproterozoic carbon cycle
The cycles of carbon and oxygen at the Earth surface are intimately linked, where the burial of organic carbon into sediments represents a source of oxygen to the surface environment. This coupling is typically quantified through the isotope records of organic and inorganic carbon. Yet, the late Neo...
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| Autori principali: | , |
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| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
National Academy of Sciences
2011
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3078370/ https://ncbi.nlm.nih.gov/pubmed/21422280 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1101755108 |
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