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Identification of methyl coenzyme M reductase A (mcrA) genes associated with methane-oxidizing archaea.

ABSTRACT: Phylogenetic and stable-isotope analyses implicated two methanogen-like archaeal groups, ANME-1 and ANME-2, as key participants in the process of anaerobic methane oxidation. Although nothing is known about anaerobic methane oxidation at the molecular level, the evolutionary relationship between methane-oxidizing archaea (MOA) and methanogenic archaea raises the possibility that MOA have co-opted key elements of the methanogenic pathway, reversing many of its steps to oxidize methane anaerobically. In order to explore this hypothesis, the existence and genomic conservation of methyl coenzyme M reductase (MCR), the enzyme catalyzing the terminal step in methanogenesis, was studied in ANME-1 and ANME-2 archaea isolated from various marine environments. Clone libraries targeting a conserved region of the alpha subunit of MCR (mcrA) were generated and compared from environmental samples, laboratory-incubated microcosms, and fosmid libraries. Four out of five novel mcrA types identified from these sources were associated with ANME-1 or ANME-2 group members. Assignment of mcrA types to specific phylogenetic groups was based on environmental clone recoveries, selective enrichment of specific MOA and mcrA types in a microcosm, phylogenetic congruence between mcrA and small-subunit rRNA tree topologies, and genomic context derived from fosmid sequences. Analysis of the ANME-1 and ANME-2 mcrA sequences suggested the potential for catalytic activity based on conservation of active-site amino acids. These results provide a basis for identifying methanotrophic archaea with mcrA sequences and define a functional genomic link between methanogenic and methanotrophic archaea.

SUBMITTER: Hallam SJ

PROVIDER: S-EPMC194966 | biostudies-literature | 2003 Sep

REPOSITORIES: biostudies-literature

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Identification of methyl coenzyme M reductase A (mcrA) genes associated with methane-oxidizing archaea.

Hallam Steven J SJ Girguis Peter R PR Preston Christina M CM Richardson Paul M PM DeLong Edward F EF

Applied and environmental microbiology 20030901 9

Phylogenetic and stable-isotope analyses implicated two methanogen-like archaeal groups, ANME-1 and ANME-2, as key participants in the process of anaerobic methane oxidation. Although nothing is known about anaerobic methane oxidation at the molecular level, the evolutionary relationship between methane-oxidizing archaea (MOA) and methanogenic archaea raises the possibility that MOA have co-opted key elements of the methanogenic pathway, reversing many of its steps to oxidize methane anaerobical ...[more]

PMID: 12957937

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Project description:Methyl-coenzyme M reductase (MCR) catalyzes the final and rate-limiting step in methane biogenesis: the reduction of methyl-coenzyme M (methyl-SCoM) by coenzyme B (CoBSH) to methane and a heterodisulfide (CoBS-SCoM). Crystallographic studies show that the active site is deeply buried within the enzyme and contains a highly reduced nickel-tetrapyrrole, coenzyme F(430). Methyl-SCoM must enter the active site prior to CoBSH, as species derived from methyl-SCoM are always observed bound to the F(430) nickel in the deepest part of the 30 A long substrate channel that leads from the protein surface to the active site. The seven-carbon mercaptoalkanoyl chain of CoBSH binds within a 16 A predominantly hydrophobic part of the channel close to F(430), with the CoBSH thiolate lying closest to the nickel at a distance of 8.8 A. It has previously been suggested that binding of CoBSH initiates catalysis by inducing a conformational change that moves methyl-SCoM closer to the nickel promoting cleavage of the C-S bond of methyl-SCoM. In order to better understand the structural role of CoBSH early in the MCR mechanism, we have determined crystal structures of MCR in complex with four different CoBSH analogues: pentanoyl, hexanoyl, octanoyl, and nonanoyl derivatives of CoBSH (CoB(5)SH, CoB(6)SH, CoB(8)SH, and CoB(9)SH, respectively). The data presented here reveal that the shorter CoB(5)SH mercaptoalkanoyl chain overlays with that of CoBSH but terminates two units short of the CoBSH thiolate position. In contrast, the mercaptoalkanoyl chain of CoB(6)SH adopts a different conformation, such that its thiolate is coincident with the position of the CoBSH thiolate. This is consistent with the observation that CoB(6)SH is a slow substrate. A labile water in the substrate channel was found to be a sensitive indicator for the presence of CoBSH and HSCoM. The longer CoB(8)SH and CoB(9)SH analogues can be accommodated in the active site through exclusion of this water. These analogues react with Ni(III)-methyl, a proposed MCR catalytic intermediate of methanogenesis. The CoB(8)SH thiolate is 2.6 A closer to the nickel than that of CoBSH, but the additional carbon of CoB(9)SH only decreases the nickel thiolate distance a further 0.3 A. Although the analogues do not induce any structural changes in the substrate channel, the thiolates appear to preferentially bind at two distinct positions in the channel, one being the previously observed CoBSH thiolate position and the other being at a hydrophobic annulus of residues that lines the channel proximal to the nickel.

Dataset Information

Identification of methyl coenzyme M reductase A (mcrA) genes associated with methane-oxidizing archaea.

Publications

Identification of methyl coenzyme M reductase A (mcrA) genes associated with methane-oxidizing archaea.

Similar Datasets

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