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Anaerobic oxidation of ethane by archaea from a marine hydrocarbon seep
被引:123
|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
来源:
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.
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页码:108 / +
页数:19
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