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Anaerobic oxidation of methane at different temperature regimes in Guaymas Basin hydrothermal sediments

Anaerobic oxidation of methane (AOM) was investigated in hydrothermal sediments of Guaymas Basin based on δ(13)C signatures of CH(4), dissolved inorganic carbon and porewater concentration profiles of CH(4) and sulfate. Cool, warm and hot in-situ temperature regimes (15–20 °C, 30–35 °C and 70–95 °C)...

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Detalhes bibliográficos
Main Authors: Biddle, Jennifer F, Cardman, Zena, Mendlovitz, Howard, Albert, Daniel B, Lloyd, Karen G, Boetius, Antje, Teske, Andreas
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group 2012
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Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC3329104/
https://ncbi.nlm.nih.gov/pubmed/22094346
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ismej.2011.164
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