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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Detaylı Bibliyografya
Asıl Yazarlar: Biddle, Jennifer F, Cardman, Zena, Mendlovitz, Howard, Albert, Daniel B, Lloyd, Karen G, Boetius, Antje, Teske, Andreas
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Nature Publishing Group 2012
Konular:
Original Article
Online Erişim: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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