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
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
相关论文
共 50 条
  • [41] Mapping methane emissions from a marine geological seep source using imaging spectrometry
    Roberts, Dar A.
    Bradley, Eliza S.
    Cheung, Ross
    Leifer, Ira
    Dennison, Philip E.
    Margolis, Jack S.
    REMOTE SENSING OF ENVIRONMENT, 2010, 114 (03) : 592 - 606
  • [42] Lithium isotope geochemistry of marine pore waters - Insights from cold seep fluids
    Scholz, Florian
    Hensen, Christian
    De Lange, Gert J.
    Haeckel, Matthias
    Liebetrau, Volker
    Meixner, Anette
    Reitz, Anja
    Romer, Rolf L.
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2010, 74 (12) : 3459 - 3475
  • [43] Paleozoic bedded barite deposits from Sonora (NW Mexico): Evidence for a hydrocarbon seep environment of formation
    Canet, Caries
    Anadon, Pere
    Gonzalez-Partida, Eduardo
    Alfonso, Pura
    Rajabi, Abdorrahman
    Perez-Segura, Efren
    Alba-Aldave, Leticia A.
    ORE GEOLOGY REVIEWS, 2014, 56 : 292 - 300
  • [44] Diversity and Metabolic Potential of the Terrestrial Mud Volcano Microbial Community with a High Abundance of Archaea Mediating the Anaerobic Oxidation of Methane
    Merkel, Alexander Y.
    Chernyh, Nikolay A.
    Pimenov, Nikolai V.
    Bonch-Osmolovskaya, Elizaveta A.
    Slobodkin, Alexander I.
    LIFE-BASEL, 2021, 11 (09):
  • [45] A novel exoelectrogen from microbial fuel cell: Bioremediation of marine petroleum hydrocarbon pollutants
    Li, Xiaoling
    Zheng, Ruiyu
    Zhang, Xuwu
    Liu, Zhiwei
    Zhu, Ruiyan
    Zhang, Xiaoyu
    Gao, Dawei
    JOURNAL OF ENVIRONMENTAL MANAGEMENT, 2019, 235 : 70 - 76
  • [46] Mineralogical and stable isotopic characterization of authigenic carbonate from a hydrocarbon seep site, Gulf of Mexico slope: Possible relation to crude oil degradation
    Mansour, Ahmed S.
    Sassen, Roger
    MARINE GEOLOGY, 2011, 281 (1-4) : 59 - 69
  • [47] High Diversity of Anaerobic Alkane-Degrading Microbial Communities in Marine Seep Sediments Based on (1-methylalkyl)succinate Synthase Genes
    Stagars, Marion H.
    Ruff, S. Emil
    Amann, Rudolf
    Knittel, Katrin
    FRONTIERS IN MICROBIOLOGY, 2016, 6
  • [48] Algal and archaeal polyisoprenoids in a recent marine sediment: Molecular isotopic evidence for anaerobic oxidation of methane
    Bian, LQ
    Hinrichs, KU
    Xie, TM
    Brassell, SC
    Iversen, H
    Fossing, H
    Jorgensen, BB
    Hayes, JM
    GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2001, 2
  • [49] Differential aerobic and anaerobic oxidation of hydrocarbon gases discharged at mud volcanoes in the Nile deep-sea fan
    Mastalerz, Vincent
    de Lange, Gert J.
    Dahlmann, Anke
    GEOCHIMICA ET COSMOCHIMICA ACTA, 2009, 73 (13) : 3849 - 3863
  • [50] Anaerobic oxidation of methane in a cold-water coral carbonate mound from the Gulf of Cadiz
    Maignien, L.
    Depreiter, D.
    Foubert, A.
    Reveillaud, J.
    De Mol, L.
    Boeckx, P.
    Blamart, D.
    Henriet, J. -P.
    Boon, N.
    INTERNATIONAL JOURNAL OF EARTH SCIENCES, 2011, 100 (06) : 1413 - 1422