Dataset Information

Divergent methyl-coenzyme M reductase genes in a deep-subseafloor Archaeoglobi.

ABSTRACT: The methyl-coenzyme M reductase (MCR) complex is a key enzyme in archaeal methane generation and has recently been proposed to also be involved in the oxidation of short-chain hydrocarbons including methane, butane, and potentially propane. The number of archaeal clades encoding the MCR continues to grow, suggesting that this complex was inherited from an ancient ancestor, or has undergone extensive horizontal gene transfer. Expanding the representation of MCR-encoding lineages through metagenomic approaches will help resolve the evolutionary history of this complex. Here, a near-complete Archaeoglobi metagenome-assembled genome (MAG; Ca. Polytropus marinifundus gen. nov. sp. nov.) was recovered from the deep subseafloor along the Juan de Fuca Ridge flank that encodes two divergent McrABG operons similar to those found in Ca. Bathyarchaeota and Ca. Syntrophoarchaeum MAGs. Ca. P. marinifundus is basal to members of the class Archaeoglobi, and encodes the genes for ?-oxidation, potentially allowing an alkanotrophic metabolism similar to that proposed for Ca. Syntrophoarchaeum. Ca. P. marinifundus also encodes a respiratory electron transport chain that can potentially utilize nitrate, iron, and sulfur compounds as electron acceptors. Phylogenetic analysis suggests that the Ca. P. marinifundus MCR operons were horizontally transferred, changing our understanding of the evolution and distribution of this complex in the Archaea.

SUBMITTER: Boyd JA

PROVIDER: S-EPMC6474303 | biostudies-literature | 2019 May

REPOSITORIES: biostudies-literature

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Divergent methyl-coenzyme M reductase genes in a deep-subseafloor Archaeoglobi.

Boyd Joel A JA Jungbluth Sean P SP Leu Andy O AO Evans Paul N PN Woodcroft Ben J BJ Chadwick Grayson L GL Orphan Victoria J VJ Amend Jan P JP Rappé Michael S MS Tyson Gene W GW

The ISME journal 20190116 5

The methyl-coenzyme M reductase (MCR) complex is a key enzyme in archaeal methane generation and has recently been proposed to also be involved in the oxidation of short-chain hydrocarbons including methane, butane, and potentially propane. The number of archaeal clades encoding the MCR continues to grow, suggesting that this complex was inherited from an ancient ancestor, or has undergone extensive horizontal gene transfer. Expanding the representation of MCR-encoding lineages through metagenom ...[more]

PMID: 30651609

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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

Divergent methyl-coenzyme M reductase genes in a deep-subseafloor Archaeoglobi.

Publications

Divergent methyl-coenzyme M reductase genes in a deep-subseafloor Archaeoglobi.

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