Methanofuran (carbon dioxide reduction factor), a formyl carrier in methane production from carbon dioxide in Methanobacterium

Methanofuran (carbon dioxide reduction factor) became labeled when incubated in cell extracts of Methanobacterium under hydrogen and 14CO2 in the absence of methanopterin. Proton NMR spectroscopy revealed that a formyl group was bound to the primary amine of methanofuran. [14C]Formylmethanofuran was enzymically converted to 14CH4 in the presence of CH3-S-CoM [2-(methylthio)ethanesulfonic acid], hydrogen, and methanopterin, establishing the formyl moiety as an intermediate in methanogenesis. In the absence of methanopterin, a substantial portion of the formyl label was oxidized to 14CO2 rather than reduced to 14CH4, consistent with a model in which the C1 intermediate is first bound to methanofuran and then to methanopterin, during its reduction. When CH3-S-CoM was replaced by HS-CoM (2-mercaptoethanesulfonic acid), most of the formyl label was oxidized to 14CO2, indicating that methyl group reduction by the CH3-S-CoM methylreductase is required for the conversion of formylmethanofuran to methane.     

Analysis of gene islands involved in methanopterin-linked C1 transfer reactions reveals new functions and provides evolutionary insights

In this study, the occurrence and chromosomal clustering of genes encoding C(1) transfer reactions linked to tetrahydromethanopterin (H(4)MPT) were analyzed in a variety of proteobacteria and in representatives of the Planctomycetes via genomic analysis or via partial sequencing by cosmid walking. Although a tendency for clustering was found common for the genes of interest, significant variations in gene order and the degree of clustering were uncovered both between and within different groups of Proteobacteria and between Proteobacteria and Planctomycetes. Phylogenetic analyses suggested that the evolution of genes encoding H(4)MPT-linked reactions in Proteobacteria involved lateral transfers within Proteobacteria and possibly between Proteobacteria and other phyla. Gene cluster comparisons revealed a number of novel genes potentially involved in the C(1) transfer reactions, and these were analyzed by mutation and expression analyses. Four genes, a homolog of pabB, and three genes conserved between methanogenic Archaea and Bacteria possessing H(4)MPT-linked functions, orfY, orf1, and afpA were shown to be involved in formaldehyde oxidation/detoxification, as judged by specific mutant phenotypes. In particular, pabB contributes to the biosynthesis of para-aminobenzoic acid, a precursor of both tetrahydrofolate and H(4)MPT, and afpA apparently encodes a novel dihydromethanopterin reductase, based on mutant complementation experiments.     

Identification of an archaeal 2-hydroxy acid dehydrogenase catalyzing reactions involved in coenzyme biosynthesis in methanoarchaea

Two putative malate dehydrogenase genes, MJ1425 and MJ0490, from Methanococcus jannaschii and one from Methanothermus fervidus were cloned and overexpressed in Escherichia coli, and their gene products were tested for the ability to catalyze pyridine nucleotide-dependent oxidation and reduction reactions of the following alpha-hydroxy-alpha-keto acid pairs: (S)-sulfolactic acid and sulfopyruvic acid; (S)-alpha-hydroxyglutaric acid and alpha-ketoglutaric acid; (S)-lactic acid and pyruvic acid; and 1-hydroxy-1,3,4,6-hexanetetracarboxylic acid and 1-oxo-1,3,4, 6-hexanetetracarboxylic acid. Each of these reactions is involved in the formation of coenzyme M, methanopterin, coenzyme F(420), and methanofuran, respectively. Both the MJ1425-encoded enzyme and the MJ0490-encoded enzyme were found to function to different degrees as malate dehydrogenases, reducing oxalacetate to (S)-malate using either NADH or NADPH as a reductant. Both enzymes were found to use either NADH or NADPH to reduce sulfopyruvate to (S)-sulfolactate, but the V(max)/K(m) value for the reduction of sulfopyruvate by NADH using the MJ1425-encoded enzyme was 20 times greater than any other combination of enzymes and pyridine nucleotides. Both the M. fervidus and the MJ1425-encoded enzyme catalyzed the NAD(+)-dependent oxidation of (S)-sulfolactate to sulfopyruvate. The MJ1425-encoded enzyme also catalyzed the NADH-dependent reduction of alpha-ketoglutaric acid to (S)-hydroxyglutaric acid, a component of methanopterin. Neither of the enzymes reduced pyruvate to (S)-lactate, a component of coenzyme F(420). Only the MJ1425-encoded enzyme was found to reduce 1-oxo-1,3,4,6-hexanetetracarboxylic acid, and this reduction occurred only to a small extent and produced an isomer of 1-hydroxy-1,3,4,6-hexanetetracarboxylic acid that is not involved in the biosynthesis of methanofuran c. We conclude that the MJ1425-encoded enzyme is likely to be involved in the biosynthesis of both coenzyme M and methanopterin.     

Methanopterin and methanogenic bacteria

Methanogenic bacteria comprise a selected group of microorganisms that derive their energy for growth from the hydrogen-dependent reduction of CO2 to methane or the disproportionation of reduced one-carbon compounds and acetate to CO2 and methane. In the reduction and oxidation steps at the formyl, hydroxymethyl and methyl level the one-carbon unit remains bound to the reduced form of methanopterin, a pterin derivative typical of methanogenic bacteria. In addition, the reduced methanopterin, 5,6,7,8-tetrahydromethanopterin, is involved in a number of anabolic reactions. Methanopterin is structurally and functionally the counterpart of folic acid found in other organisms. In this review the occurrence and properties of methanopterin and its derivatives, as well as the biosynthesis and the role in the different catabolic and anabolic reactions are discussed against the background of folic acid biochemistry.     

Carbon dioxide reduction factor and methanopterin, two coenzymes required for CO2 reduction to methane by extracts of Methanobacterium

Carbon dioxide reduction (CDR) factor is contained in a low molecular weight fraction of cell extract that is required for methane production from CO2 by resolved cell extracts. This fraction has been separated into two components both of which have been highly purified. One component is methanopterin, and for the other component the name CDR factor is retained. No known coenzymes tested substitute in the methane-producing assay for CDR factor and methanopterin, both of which are stable to boiling and exposure to air. The ultraviolet-visible spectrum of CDR factor has a peak at 273 nm, a shoulder at 280 nm, and at pH 1, a peak at 219 nm. The ultraviolet-visible spectrum of methanopterin isolated from the CDR fraction is similar to the spectrum previously reported for this compound (Keltjens, J. T., and Vogels, G. D. (1981) in Microbial Growth on C1 Compounds (Dalton, H., ed) pp. 152-158, Heyden and Son, Ltd., London). The addition of CDR factor (0.8 micrograms) and methanopterin (50 micrograms) to the assay mixture increased by 12-fold the amount of methane formed from CO2.     

Electron transfer reactions in the soluble methane monooxygenase of Methylococcus capsulatus (Bath)

Aerobic stopped-flow experiments have confirmed that component C is the methane monooxygenase component responsible for interaction with NADH. Reduction of component C by NADH is not the rate-limiting step for component C in the methane monooxygenase reaction. Removal and reconstitution of the redox centres of component C suggest a correlation between the presence of the FAD and Fe2S2 redox centres and NADH: acceptor reductase activity and methane monooxygenase activity respectively, consistent with the order of electron flow: NADH----FAD----Fe2S2----component A. This order suggests that component C functions as a 2e-1/1e-1 transformase, splitting electron pairs from NADH for transfer to component A via the one-electron-carrying Fe2S2 centre. Electron transfer has been demonstrated between the reductase component, component C and the oxygenase component, component A, of the methane monooxygenase complex from Methylococcus capsulatus (Bath) by three separate methods. This intermolecular electron transfer step is not rate-determining for the methane monooxygenase reaction. Intermolecular electron transfer was independent of component B, the third component of the methane monooxygenase. Component B is required to switch the oxidase activity of component A to methane mono-oxygenase activity, suggesting that the role of component B is to couple substrate oxidation to electron transfer, via the methane monooxygenase components.     

Structural characteristics of methanogenic cofactors in the non-methanogenic archaebacterium Archaeoglobus fulgidus

Archaeoglobus fulgidus is an extremely thermophilic, sulphate reducing archaebacterium thought to represent a biochemical missing-link between sulphur-metabolizing bacteria and methanogenic bacteria. Whereas the phylogenetic position of A.fulgidus is closer to the sulphur-metabolizing bacteria, there is a partial overlap in the biochemical machinery of A.fulgidus with both groups of bacteria. In particular, the presence of a number of aberrant cofactors up to now thought to be involved exclusively in the process of methanogenesis in methanogenic archaebacteria, i.e. coenzyme F420, methanofuran and methanopterin, has been indicated by previous studies. Here we present evidence for the structural identity of the methanopterin cofactor of A.fulgidus with the methanopterin isolated from Methanobacterium thermoautotrophicum and show that this non-methanogenic bacterium contains two as yet unknown analogues of coenzyme F420. The levels of the various cofactors were determined in cultures grown either on formate or lactate as the carbon source and sulphate or thiosulphate as the sulphur source.     

Evidence of a common pathway of carbon dioxide reduction to methane in methanogens.

The roles of methanofuran and tetrahydromethanopterin as carriers of C1 moieties in the reduction of carbon dioxide to methane were studied in representatives of diverse groups of methanogens, confirming that these roles, first reported for Methanobacterium thermoautotrophicum, are common for methanogenesis in general. Extracts of the methanogens tested converted formyl-methanofuran and methyl-tetrahydromethanopterin to methane; the extractable cofactors derived from the same methanogens, with one exception, complemented a methanofuran- and tetrahydromethanopterin-deficient enzyme system from M. thermoautotrophicum. The amounts of extractable methanofuran and tetrahydromethanopterin were determined for each representative methanogen.     

Highly divergent genes for methanopterin-linked C1 transfer reactions in Lake Washington, assessed via metagenomic analysis and mRNA detection

The origins and the evolutionary history of tetrahydromethanopterin-linked C1 transfer reactions that are part of two environmentally important biotransformations, methylotrophy and methanogenesis, are still not well understood. In previous studies, we have expanded the known phylogenetic diversity of these reactions by identifying genes highly diverging from the ones associated with cultivated Proteobacteria, Planctomycetes, or Archaea (M. G. Kalyuzhnaya, M. E. Lidstrom, and L. Chistoserdova, Microb. Ecol. 48:463-472, 2004; M. G. Kalyuzhnaya, O. Nercessian, M. E. Lidstrom, and L. Chistoserdova, Environ. Microbiol. 7:1269-1274, 2005). Here we used a metagenomic approach to demonstrate that these divergent genes are present with high abundance in the microbial community inhabiting Lake Washington sediment. We also gained preliminary insights into the genomic composition of the organisms possessing these genes by sequencing genomic fragments from three uncultured microbes possessing the genes of interest. Phylogenetic analyses suggested that, although distantly related to each other, these organisms deeply diverge from known Bacteria and Archaea, with more relation to the former, suggesting their affiliation with a new bacterial phylum. We also demonstrate, via specific mRNA detection, that these divergent genes are expressed in the environment, pointing toward their potential role in local carbon cycling.     

The bioenergetics of methanogenesis

The reduction of CO2 or any other methanogenic substrate to methane serves the same function as the reduction of oxygen, nitrate or sulfate to more reduced products. These exergonic reactions are coupled to the production of usable energy generated through a charge separation and a protonmotive-force-driven ATPase. For the understanding of how methanogens derive energy from C-1 unit reduction one must study the biochemistry of the chemical reactions involved and how these are coupled to the production of a charge separation and subsequent electron transport phosphorylation. Data on methanogenesis by a variety of organisms indicates ubiquitous use of CH3-S-CoM as the final electron acceptor in the production of methane through the methyl CoM reductase and of 5-deazaflavin as a primary source of reducing equivalents. Three known enzymes serve as catalysts in the production of reduced 5-deazaflavin: hydrogenase, formate dehydrogenase and CO dehydrogenase. All three are potential candidates for proton pumps. In the organisms that must oxidize some of their substrate to obtain electrons for the reduction of another portion of the substrate to methane (e.g., those using formate, methanol or acetate), the latter two enzymes may operate in the oxidizing direction. CO2 is the most frequent substrate for methanogenesis but is the only substrate that obligately requires the presence of H2 and hydrogenase. Growth on methanol requires a B12-containing methanol-CoM methyl transferase and does not necessarily need any other methanogenic enzymes besides the methyl-CoM reductase system when hydrogenase is present. When bacteria grow on methanol alone it is not yet clear if they get their reducing equivalents from a reversal of methanogenic enzymes, thus oxidizing methyl groups to CO2. An alternative (since these and acetate-catabolizing methanogens possess cytochrome b) is electron transport and possible proton pumping via a cytochrome-containing electron transport chain. Several of the actual components of the methanogenic pathway from CO2 have been characterized. Methanofuran is apparently the first carbon-carrying cofactor in the pathway, forming carboxy-methanofuran. Formyl-FAF or formyl-methanopterin (YFC, a very rapidly labelled compound during 14C pulse labeling) has been implicated as an obligate intermediate in methanogenesis, since methanopterin or FAF is an essential component of the carbon dioxide reducing factor in dialyzed extract methanogenesis. FAF also carries the carbon at the methylene and methyl oxidation levels.(ABSTRACT TRUNCATED AT 400 WORDS)     

Development and application of polymerase chain reaction primers based on fhcD for environmental detection of methanopterin-linked C1-metabolism in bacteria

In this work we describe development and testing of a novel pair of environmental primers targeting fhcD, a conserved gene in the H4MTP-linked C1-transfer pathway, and demonstrate that these primers enable confident detection of a broad variety of fhcD genes originating from phylogenetically diverse bacteria. The new primer pair was employed to analyse fhcD diversity in Lake Washington sediment, uncovering the presence of 40 fhcD phylotypes. Based on phylogenetic analyses, the phylotypes identified were affiliated with alpha-, beta- and gamma-proteobacteria, and Planctomycetes, while a number of sequences formed deep branches suggesting the presence of unknown groups of microorganisms. To assess the physiological potential and the possible substrate repertoire of the fhcD-containing species in Lake Washington, we conducted enrichments of natural populations on a variety of C1 substrates, and observed specific shifts in community structure in response to different C1 substrates. A specific shift in community structure was also observed in the presence of humic acids suggesting that C1 transfer metabolism linked to H4MPT may be part of the degradation pathway for this natural polymer, possibly involving formaldehyde production. Overall, our data suggest that C1 oxidation reactions linked to H4MPT are much more widespread in natural environments than previously thought.     

Purification,overproduction, and partial characterization of beta-RFAP synthase,a key enzyme in the methanopterin biosynthesis pathway

Methanopterin is a folate analog involved in the C1 metabolism of methanogenic archaea, sulfate-reducing archaea, and methylotrophic bacteria. Although a pathway for methanopterin biosynthesis has been described in methanogens, little is known about the enzymes and genes involved in the biosynthetic pathway. The enzyme beta-ribofuranosylaminobenzene 5'-phosphate synthase (beta-RFAP synthase) catalyzes the first unique step to be identified in the pathway of methanopterin biosynthesis, namely, the condensation of p-aminobenzoic acid with phosphoribosylpyrophosphate to form beta-RFAP, CO2, and inorganic pyrophosphate. The enzyme catalyzing this reaction has not been purified to homogeneity, and the gene encoding beta-RFAP synthase has not yet been identified. In the present work, we report on the purification to homogeneity of beta-RFAP synthase. The enzyme was purified from the methane-producing archaeon Methanosarcina thermophila, and the N-terminal sequence of the protein was used to identify corresponding genes from several archaea, including the methanogen Methanococcus jannaschii and the sulfate-reducing archaeon Archaeoglobus fulgidus. The putative beta-RFAP synthase gene from A. fulgidus was expressed in Escherichia coli, and the enzymatic activity of the recombinant gene product was verified. A BLAST search using the deduced amino acid sequence of the beta-RFAP synthase gene identified homologs in additional archaea and in a gene cluster required for C1 metabolism by the bacterium Methylobacterium extorquens. The identification of a gene encoding a potential beta-RFAP synthase in M. extorquens is the first report of a putative methanopterin biosynthetic gene found in the Bacteria and provides evidence that the pathways of methanopterin biosynthesis in Bacteria and Archaea are similar.     

Biogeochemistry and microbial ecology of methane oxidation in anoxic environments: a review

Evidence supporting a key role for anaerobic methane oxidation in the global methane cycle is reviewed. Emphasis is on recent microbiological advances. The driving force for research on this process continues to be the fact that microbial communities intercept and consume methane from anoxic environments, methane that would otherwise enter the atmosphere. Anaerobic methane oxidation is biogeochemically important because methane is a potent greenhouse gas in the atmosphere and is abundant in anoxic environments. Geochemical evidence for this process has been observed in numerous marine sediments along the continental margins, in methane seeps and vents, around methane hydrate deposits, and in anoxic waters. The anaerobic oxidation of methane is performed by at least two phylogenetically distinct groups of archaea, the ANME-1 and ANME-2. These archaea are frequently observed as consortia with sulfate-reducing bacteria, and the metabolism of these consortia presumably involves a syntrophic association based on interspecies electron transfer. The archaeal member of a consortium apparently oxidizes methane and shuttles reduced compounds to the sulfate-reducing bacteria. Despite recent advances in understanding anaerobic methane oxidation, uncertainties still remain regarding the nature and necessity of the syntrophic association, the biochemical pathway of methane oxidation, and the interaction of the process with the local chemical and physical environment. This review will consider the microbial ecology and biogeochemistry of anaerobic methane oxidation with a special emphasis on the interactions between the responsible organisms and their environment. This revised version was published online in August 2006 with corrections to the Cover Date.     

Targeting methanopterin biosynthesis to inhibit methanogenesis

This paper describes the design, synthesis, and successful employment of inhibitors of 4-(beta-D-ribofuranosyl)aminobenzene-5'-phosphate (RFA-P) synthase, which catalyzes the first committed step in the biosynthesis of methanopterin, to specifically halt the growth of methane-producing microbes. RFA-P synthase catalyzes the first step in the synthesis of tetrahydromethanopterin, a key cofactor required for methane formation and for one-carbon transformations in methanogens. A number of inhibitors, which are N-substituted derivatives of p-aminobenzoic acid (pABA), have been synthesized and their inhibition constants with RFA-P synthase have been determined. Based on comparisons of the inhibition constants among various inhibitors, we propose that the pABA binding site in RFA-P synthase has a relatively large hydrophobic pocket near the amino group. These enzyme-targeted inhibitors arrest the methanogenesis and growth of pure cultures of methanogens. Supplying pABA to the culture relieves the inhibition, indicating a competitive interaction between pABA and the inhibitor at the cellular target, which is most likely RFAP synthase. The inhibitors do not adversely affect the growth of pure cultures of the bacteria (acetogens) that play a beneficial role in the rumen. Inhibitors added to dense ruminal fluid cultures (artificial rumena) halt methanogenesis; however, they do not inhibit volatile fatty acid (VFA) production and, in some cases, VFA levels are slightly elevated in the methanogenesis-inhibited cultures. We suggest that inhibiting methanopterin biosynthesis could be considered in strategies to decrease anthropogenic methane emissions, which could have an environmental benefit since methane is a potent greenhouse gas.     

Phylogeny of β-xylanases from Planctomycetes

Here, we present the results of a computational analysis of a group of hypothetical GH10 endo-β-xylanases from the Planctomycetes, a bacterial phylum with poorly characterized functional capabilities. These proteins are encoded in all analyzed genomes of heterotrophic Planctomycetes and form a phylogenetically distinct and tight cluster. In addition, we determined nucleotide sequences for endo-β-xylanase genes from five strains of Isosphaera-Singulisphaera group of the Planctomycetes. The trees constructed for the 16S rRNA genes and the inferred amino acid sequences of endo-β-xylanases were highly congruent, thus suggesting the vertical transfer of endo-β-xylanase genes and their functional importance in Planctomycetes.     

Cyanobacterial contribution to algal nuclear genomes is primarily limited to plastid functions

A single cyanobacterial primary endosymbiosis that occurred approximately 1.5 billion years ago is believed to have given rise to the plastid in the common ancestor of the Plantae or Archaeplastida--the eukaryotic supergroup comprising red, green (including land plants), and glaucophyte algae. Critical to plastid establishment was the transfer of endosymbiont genes to the host nucleus (i.e., endosymbiotic gene transfer [EGT]). It has been postulated that plastid-derived EGT played a significant role in plant nuclear-genome evolution, with 18% (or 4,500) of all nuclear genes in Arabidopsis thaliana having a cyanobacterial origin with about one-half of these recruited for nonplastid functions. Here, we determine whether the level of cyanobacterial gene recruitment proposed for Arabidopsis is of the same magnitude in the algal sisters of plants by analyzing expressed-sequence tag (EST) data from the glaucophyte alga Cyanophora paradoxa. Bioinformatic analysis of 3,576 Cyanophora nuclear genes shows that 10.8% of these with significant database hits are of cyanobacterial origin and one-ninth of these have nonplastid functions. Our data indicate that unlike plants, early-diverging algal groups appear to retain a smaller number of endosymbiont genes in their nucleus, with only a minor proportion of these recruited for nonplastid functions.     

Derivatives of methanopterin, a coenzyme involved in methanogenesis

Degradational studies of methanopterin, a coenzyme involved in methanogenesis, are reported. The results of these studies are in full accordance with the proposed structure of methanopterin as N-[1'-(2'-amino-4'-hydroxy-7' -methyl-6'-pteridinyl)ethyl]-4-[2', 3', 4', 5'-tetrahydroxypent-1'-yl(5'-1' )O-alpha-ribofuranosyl-5'-phosphoric acid] aniline in which the phosphate group is esterified with alpha-hydroxyglutaric acid. Acid hydrolysis of methanopterin cleaved the 5'----1' glycosidic bond and yielded a 'hydrolytic product' which was identified as N-[1'-(2'-amino-4'-hydroxy-7' -methyl-6'-pteridinyl)ethyl]-4-[2', 3', 4', 5'-tetrahydroxypent-1'-yl]aniline. Alkaline permanganate oxidation of methanopterin yielded 7-methylpterin-6-carboxylic acid. Catalytic (or enzymatic) hydrogenation of methanopterin gave a mixture of 6-ethyl-7-methyl-7,8-dihydropterin, 6-ethyl-7-methylpterin and a third compound, named methaniline which was identified as 4-[2', 3', 4', 5'-tetrahydroxypent-1'-yl(5'----1')O-alpha -ribofuranosyl-5'-phosphoric acid]aniline, in which the phosphate group is esterified with alpha-hydroxyglutaric acid. Methanosarcina barkeri contains a closely related coenzyme called sarcinapterin, which was identified as a L-glutamyl derivative of methanopterin, where the glutamate moiety is attached to the alpha-carboxylic acid group of the alpha-hydroxyglutaric acid moiety of methanopterin via an amide linkage.     

Fishing for biodiversity: novel methanopterin-linked C transfer genes deduced from the Sargasso Sea metagenome

The recently generated database of microbial genes from an oligotrophic environment populated by a calculated 1800 major phylotypes (the Sargasso Sea metagenome-SSM) presents a great source for expanding local databases of genes indicative of a specific function. In this article we analyse the SSM for the presence of methanopterin-linked C1 transfer genes that are signature for methylotrophy. We conclude that more than 10 phylotypes possessing genes of interest are present in this environment. The sequences representative of these major phylotypes do not appear to belong to any known microbial group capable of methanopterin-linked C1 transfer. Instead, these sequences separate from all known sequences on phylogenetic trees, pointing toward their affiliation with novel microbial phyla. These data imply a broader distribution of methanopterin-linked functions in the microbial world than has been previously known.