Cryptic CH(4) cycling in the sulfate–methane transition of marine sediments apparently mediated by ANME-1 archaea

Methane in the seabed is mostly oxidized to CO(2) with sulfate as the oxidant before it reaches the overlying water column. This microbial oxidation takes place within the sulfate–methane transition (SMT), a sediment horizon where the downward diffusive flux of sulfate encounters an upward flux of m...

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Vydáno v:ISME J
Hlavní autoři: Beulig, F., Røy, H., McGlynn, S. E., Jørgensen, B. B.
Médium: Artigo
Jazyk:Inglês
Vydáno: Nature Publishing Group UK 2018
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Article
On-line přístup:https://ncbi.nlm.nih.gov/pmc/articles/PMC6331549/
https://ncbi.nlm.nih.gov/pubmed/30194429
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41396-018-0273-z
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