The biological oxidation of methane by anaerobic microorganisms is a significant sink for methane in the marine environment. Although there is convincing biogeochemical evidence for anaerobic oxidation of methane (AOM) by methanotrophic archaea and sulfate-reducing bacteria, the identity of these uncultured microorganisms is only now being described. In this study, we examined the diversity archaeal and bacterial assemblages involved in AOM using directly coupled isotopic and phylogenetic analyses at the level of single cells. The combined application of fluorescent in situ hybridization and secondary ion mass spectrometry (FISHSIMS) identified two phylogenetically distinct groups of archaea (ANME-1 and ANME-2) from marine metha...
Convergent lines of molecular, carbon-isotopic, and phylogenetic evidence have previously indicated ...
Convergent lines of molecular, carbon-isotopic, and phylogenetic evidence have previously indicated ...
The anaerobic oxidation of methane (AOM) with sulfate as the final electron acceptor according to (C...
No microorganism capable of anaerobic growth on methane as the sole carbon source has yet been culti...
A large fraction of globally produced methane is converted to CO2 by anaerobic oxidation in marine s...
The anaerobic oxidation of methane (AOM) is a globally important process estimated to consume over 3...
The anaerobic oxidation of methane (AOM) is a globally important process estimated to consume over 3...
Summary Anaerobic oxidation of methane (AOM) is an important methane sink in the ocean but the micro...
Summary Anaerobic oxidation of methane (AOM) is an important methane sink in the ocean but the micro...
Microorganisms living in anoxic marine sediments consume more than 80% of the methane produced in th...
Microorganisms living in anoxic marine sediments consume more than 80% of the methane produced in th...
The anaerobic oxidation of methane (AOM) in the marine subsurface is a significant sink for methane ...
© 2020 Elsevier Ltd Methane is abundant in marine subsurface sediments, sourced from microbial or th...
Methane is abundant in marine subsurface sediments, sourced from microbial or thermocatalytic produc...
The microbially mediated anaerobic oxidation of methane (AOM) is the major biological sink of the gr...
Convergent lines of molecular, carbon-isotopic, and phylogenetic evidence have previously indicated ...
Convergent lines of molecular, carbon-isotopic, and phylogenetic evidence have previously indicated ...
The anaerobic oxidation of methane (AOM) with sulfate as the final electron acceptor according to (C...
No microorganism capable of anaerobic growth on methane as the sole carbon source has yet been culti...
A large fraction of globally produced methane is converted to CO2 by anaerobic oxidation in marine s...
The anaerobic oxidation of methane (AOM) is a globally important process estimated to consume over 3...
The anaerobic oxidation of methane (AOM) is a globally important process estimated to consume over 3...
Summary Anaerobic oxidation of methane (AOM) is an important methane sink in the ocean but the micro...
Summary Anaerobic oxidation of methane (AOM) is an important methane sink in the ocean but the micro...
Microorganisms living in anoxic marine sediments consume more than 80% of the methane produced in th...
Microorganisms living in anoxic marine sediments consume more than 80% of the methane produced in th...
The anaerobic oxidation of methane (AOM) in the marine subsurface is a significant sink for methane ...
© 2020 Elsevier Ltd Methane is abundant in marine subsurface sediments, sourced from microbial or th...
Methane is abundant in marine subsurface sediments, sourced from microbial or thermocatalytic produc...
The microbially mediated anaerobic oxidation of methane (AOM) is the major biological sink of the gr...
Convergent lines of molecular, carbon-isotopic, and phylogenetic evidence have previously indicated ...
Convergent lines of molecular, carbon-isotopic, and phylogenetic evidence have previously indicated ...
The anaerobic oxidation of methane (AOM) with sulfate as the final electron acceptor according to (C...