Anaerobic oxidation of ethane by archaea from a marine hydrocarbon seep

被引:122
|
作者
Chen, Song-Can [1 ,2 ]
Musat, Niculina [1 ]
Lechtenfeld, Oliver J. [3 ]
Paschke, Heidrun [3 ]
Schmidt, Matthias [1 ]
Said, Nedal [1 ]
Popp, Denny [4 ]
Calabrese, Federica [1 ]
Stryhanyuk, Hryhoriy [1 ]
Jaekel, Ulrike [5 ,8 ]
Zhu, Yong-Guan [2 ,6 ]
Joye, Samantha B. [7 ]
Richnow, Hans-Hermann [1 ]
Widdel, Friedrich [5 ]
Musat, Florin [1 ,5 ]
机构
[1] UFZ Helmholtz Ctr Environm Res, Dept Isotope Biogeochem, Leipzig, Germany
[2] Chinese Acad Sci, State Key Lab Urban & Reg Ecol, Ecoenvironm Sci Res Ctr, Beijing, Peoples R China
[3] UFZ Helmholtz Ctr Environm Res, Dept Analyt Chem, Leipzig, Germany
[4] UFZ Helmholtz Ctr Environm Res, Dept Environm Microbiol, Leipzig, Germany
[5] Max Planck Inst Marine Microbiol, Bremen, Germany
[6] Chinese Acad Sci, Inst Urban Environm, Key Lab Urban Environm & Hlth, Xiamen, Peoples R China
[7] Univ Georgia, Dept Marine Sci, Athens, GA 30602 USA
[8] Res Council Norway, Dept Res Infrastruct, Oslo, Norway
基金
美国国家科学基金会;
关键词
MULTIPLE SEQUENCE ALIGNMENT; METHYL-COENZYME M; GAS HYDRATE; ELECTRON-TRANSFER; RAPID ANNOTATION; GUAYMAS BASIN; METHANE; SULFATE; GULF; COMMUNITY;
D O I
10.1038/s41586-019-1063-0
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Ethane is the second most abundant component of natural gas in addition to methane, and-similar to methane-is chemically unreactive. The biological consumption of ethane under anoxic conditions was suggested by geochemical profiles at marine hydrocarbon seeps(1-3), and through ethane-dependent sulfate reduction in slurries(4-7). Nevertheless, the microorganisms and reactions that catalyse this process have to date remained unknown(8). Here we describe ethane-oxidizing archaea that were obtained by specific enrichment over ten years, and analyse these archaea using phylogeny-based fluorescence analyses, proteogenomics and metabolite studies. The co-culture, which oxidized ethane completely while reducing sulfate to sulfide, was dominated by an archaeon that we name ` Candidatus Argoarchaeum ethanivorans'; other members were sulfate-reducing Deltaproteobacteria. The genome of Ca. Argoarchaeum contains all of the genes that are necessary for a functional methyl-coenzyme M reductase, and all subunits were detected in protein extracts. Accordingly, ethylcoenzyme M (ethyl-CoM) was identified as an intermediate by liquid chromatography-tandem mass spectrometry. This indicated that Ca. Argoarchaeum initiates ethane oxidation by ethyl-CoM formation, analogous to the recently described butane activation by 'Candidatus Syntrophoarchaeum('9). Proteogenomics further suggests that oxidation of intermediary acetyl-CoA to CO2 occurs through the oxidative Wood-Ljungdahl pathway. The identification of an archaeon that uses ethane (C2H6) fills a gap in our knowledge of microorganisms that specifically oxidize members of the homologous alkane series (CnH(2n+2)) without oxygen. Detection of phylogenetic and functional gene markers related to those of Ca. Argoarchaeum at deep-sea gas seeps(10-12) suggests that archaea that are able to oxidize ethane through ethyl-CoM are widespread members of the local communities fostered by venting gaseous alkanes around these seeps.
引用
收藏
页码:108 / +
页数:19
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