Deep-branching ANME-1c archaea grow at the upper temperature limit of anaerobic oxidation of methane
In seafloor sediments, the anaerobic oxidation of methane (AOM) consumes most of the methane formed in anoxic layers, preventing this greenhouse gas from reaching the water column and finally the atmosphere. AOM is performed by syntrophic consortia of specific anaerobic methane-oxidizing archaea (AN...
| Hlavní autoři: | , , , |
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| Médium: | Článek |
| Jazyk: | English |
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Frontiers Media S.A.
2022-09-01
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| Edice: | Frontiers in Microbiology |
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| On-line přístup: | https://www.frontiersin.org/articles/10.3389/fmicb.2022.988871/full |