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Differentiating biotic from abiotic methane genesis in hydrothermally active planetary surfaces
Molecular hydrogen (H(2)) is derived from the hydrothermal alteration of olivine-rich planetary crust. Abiotic and biotic processes consume H(2) to produce methane (CH(4)); however, the extent of either process is unknown. Here, we assess the temporal dependence and limit of abiotic CH(4) related to...
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| Asıl Yazarlar: | , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
National Academy of Sciences
2012
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| Konular: | |
| Online Erişim: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3382529/ https://ncbi.nlm.nih.gov/pubmed/22679287 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1205223109 |
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