1] State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, People's Republic of China [2] State Key Laboratory of Ocean Engineering, School of Naval Architecture, Ocean and Civil Engineering, Shanghai Jiao Tong University, Shanghai, People's Republic of China [3] Key Laboratory of Systems Biomedicine (Ministry of Education), School of Systems Biomedicine, Shanghai Jiao Tong University, Shanghai, People's Republic of China.
1] State Key Laboratory of Microbial Metabolism, School of Life Sciences and Biotechnology, Shanghai Jiao Tong University, Shanghai, People's Republic of China [2] State Key Laboratory of Ocean Engineering, School of Naval Architecture, Ocean and Civil Engineering, Shanghai Jiao Tong University, Shanghai, People's Republic of China [3] Laboratory of Microbial Ecology and Technology (LabMET), Ghent University, Gent, Belgium.
ISME J. 2014 May;8(5):1069-78. doi: 10.1038/ismej.2013.212. Epub 2013 Dec 12.
Anaerobic oxidation of methane (AOM) is a crucial process limiting the flux of methane from marine environments to the atmosphere. The process is thought to be mediated by three groups of uncultivated methane-oxidizing archaea (ANME-1, 2 and 3). Although the responsible microbes have been intensively studied for more than a decade, central mechanistic details remain unresolved. On the basis of an integrated analysis of both environmental metatranscriptome and single-aggregate genome of a highly active AOM enrichment dominated by ANME-2a, we provide evidence for a complete and functioning AOM pathway in ANME-2a. All genes required for performing the seven steps of methanogenesis from CO2 were found present and actively expressed. Meanwhile, genes for energy conservation and electron transportation including those encoding F420H2 dehydrogenase (Fpo), the cytoplasmic and membrane-associated Coenzyme B-Coenzyme M heterodisulfide (CoB-S-SCoM) reductase (HdrABC, HdrDE), cytochrome C and the Rhodobacter nitrogen fixation (Rnf) complex were identified and expressed, whereas genes encoding for hydrogenases were absent. Thus, ANME-2a is likely performing AOM through a complete reversal of methanogenesis from CO2 reduction without involvement of canonical hydrogenase. ANME-2a is demonstrated to possess versatile electron transfer pathways that would provide the organism with more flexibility in substrate utilization and capacity for rapid adjustment to fluctuating environments. This work lays the foundation for understanding the environmental niche differentiation, physiology and evolution of different ANME subgroups.
厌氧甲烷氧化 (AOM) 是限制海洋环境中甲烷向大气通量的关键过程。该过程被认为是由三组未培养的甲烷氧化古菌 (ANME-1、2 和 3) 介导的。尽管负责的微生物已经被深入研究了十多年,但核心机制细节仍未解决。基于对以 ANME-2a 为主导的高度活跃 AOM 富集的环境宏转录组和单个聚集体基因组的综合分析,我们为 ANME-2a 中完整的和功能齐全的 AOM 途径提供了证据。从 CO2 生成甲烷的七个步骤所需的所有基因都被发现存在并被积极表达。同时,发现并表达了用于能量守恒和电子传递的基因,包括 F420H2 脱氢酶 (Fpo)、细胞质和膜相关的辅酶 B-辅酶 M 异二硫化物 (CoB-S-SCoM) 还原酶 (HdrABC、HdrDE)、细胞色素 C 和 Rhodobacter 固氮 (Rnf) 复合物的编码基因,而编码氢化酶的基因则不存在。因此,ANME-2a 可能通过完整的逆转从 CO2 还原生成甲烷来进行 AOM,而不涉及典型的氢化酶。ANME-2a 被证明具有多种电子转移途径,这将为该生物体在底物利用和快速适应波动环境的能力方面提供更大的灵活性。这项工作为理解不同 ANME 亚群的环境生态位分化、生理学和进化奠定了基础。