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Limited role for methane in the mid-Proterozoic greenhouse

Pervasive anoxia in the subsurface ocean during the Proterozoic may have allowed large fluxes of biogenic CH(4) to the atmosphere, enhancing the climatic significance of CH(4) early in Earth’s history. Indeed, the assumption of elevated pCH(4) during the Proterozoic underlies most models for both an...

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Bibliografski detalji
Izdano u:Proc Natl Acad Sci U S A
Glavni autori: Olson, Stephanie L., Reinhard, Christopher T., Lyons, Timothy W.
Format: Artigo
Jezik:Inglês
Izdano: National Academy of Sciences 2016
Teme:
Online pristup:https://ncbi.nlm.nih.gov/pmc/articles/PMC5068276/
https://ncbi.nlm.nih.gov/pubmed/27671638
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1608549113
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