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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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Autors principals: Bjerrum, Christian J., Canfield, Donald E.
Format: Artigo
Idioma:Inglês
Publicat: National Academy of Sciences 2011
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Accés en línia: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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