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PubMed2026

An integrated culturomic and genomic database and analysis platform for methanogenic archaea.

Methanogenic archaea research is challenged by limited strain resources, fragmented genomic data, inconsistent genome quality, substantial uncultured lineages, and difficulties in laboratory culturing, hindering advances in biogas production, climate mitigation, and microbial ecology. These archaea play crucial roles in global carbon cycling and anaerobic environments, yet scattered data and unculturable strains limit systematic studies and applications. To address this, we created MethArDB (Methanogenic Archaeal Genome Database), a specialized database for methanogenic archaea, compiling 3919 genomes, 87 host-associated plasmids, and 42 phages, with standardized quality classifications (complete, scaffold, draft), protein sequences, and metadata on geography, habitats, metabolism, and inheritable elements. Integrated MethArCT (Methanogenic Archaeal Culturomics Toolkit) employs a dual-threshold orthologous/paralogous protein analysis to evaluate metabolic pathway completeness, predicting cultivation parameters and suggesting candidate cultivation strategies, including potential medium formulations and conditions, to support strain isolation. Overall, MethArDB and MethArCT form an integrated platform combining genomics and culturomics to facilitate methanogenic archaea research. Database URL:  http://methardb.cn.

Genome, Archaeal↗

PubMed1998

An Escherichia coli hydrogenase-3-type hydrogenase in methanogenic archaea.

Methanogenic archaea are known to contain two types of [NiFe] hydrogenases designated F420-reducing hydrogenase and F420-non-reducing hydrogenase. We report here that they additionally contain Escherichia coli hydrogenase-3-type [NiFe] hydrogenases. The evidence is based on biochemical studies and analysis of the subunit primary structure of this hydrogenase (designated Ech) purified from membranes of acetate-grown cells of Methanosarcina barkeri. The subunits EchE and EchC of the EchABCDEF complex showed 34% and 45% sequence identity to the nickel-containing large subunit HycE and to the iron-sulfur cluster containing small subunit HycG, respectively, of the hydrogenase in the formate hydrogen lyase complex from E. coli. Analysis of the totally sequenced genomes of Methanococcus jannaschii and Methanobacterium thermoautotrophicum strain deltaH revealed that these organisms contain similar open reading frames, indicating the presence of an E. coli hydrogenase-3-type hydrogenase also in these methanogenic archaea.

Amino Acid Sequence↗

PubMed2002

Redox-driven proton translocation in methanogenic Archaea.

Methanogenic archaea of the genus Methanosarcina are able to utilize H2 + CO2, methylated C1 compounds or acetate as energy and carbon source, thereby producing methane as the major end product. The methanogenic pathways lead to the formation of a mixed disulfide derived from coenzyme M and coenzyme B. This disulfide is of major importance for methanogens because it is the terminal electron acceptor of a branched respiratory chain. Molecular hydrogen, reduced coenzyme F420 or reduced ferredoxin are used as electron donors. Four enzymes are involved in the membrane-bound electron transport system of Methanosarcina species, all of which are involved in the generation of an electrochemical proton gradient that is used for ATP synthesis. This review focuses on the membrane-bound electron transport chains of Methanosarcina species with respect to the biochemical and genetic characteristics of the unusual energy transducing enzymes. Furthermore, the review addresses questions concerning the relationship between methanogenic proteins and components of respiratory chains found in bacteria and eukarya.

Amino Acid Sequence↗

PubMed1999

Novel reactions involved in energy conservation by methanogenic archaea.

Methanogenic archaea of the order Methanosarcinales which utilize C(1) compounds such as methanol, methylamines or H(2)+CO(2), employ two novel membrane-bound electron transport systems generating an electrochemical proton gradient: the H(2):heterodisulfide oxidoreductase and the F(420)H(2):heterodisulfide oxidoreductase. The systems are composed of the heterodisulfide reductase and either a membrane-bound hydrogenase or a F(420)H(2) dehydrogenase which is functionally homologous to the proton-translocating NADH dehydrogenase. Cytochromes and the novel electron carrier methanophenazine are also involved. In addition, the methyl-H(4)MPT:HS-CoM methyltransferase is bioenergetically relevant. The enzyme couples methyl group transfer with the translocation of sodium ions and seems to be present in all methanogens. The proton-translocating systems with the participation of cytochromes and methanophenazine have been found so far only in the Methanosarcinales.

Cytochromes↗

PubMed2001

The Na(+)-translocating methyltransferase complex from methanogenic archaea.

Methanogenic archaea are dependent on sodium ions for methane formation. A sodium ion-dependent step has been shown to be methyl transfer from N(5)-methyltetrahydromethanopterin to coenzyme M. This exergonic reaction (DeltaG degrees '=-30 kJ/mol) is catalyzed by a Na(+)-translocating membrane-associated multienzyme complex composed of eight different subunits, MtrA-H. Subunit MtrA harbors a cob(I)amide prosthetic group which is methylated and demethylated in the catalytic cycle, demethylation being sodium ion-dependent. Based on the finding that in the cob(II)amide oxidation state the corrinoid is bound in a base-off/His-on configuration it is proposed that methyl transfer from MtrA to coenzyme M is associated with a conformational change of the protein and that this change drives the electrogenic translocation of the sodium ions.

Amino Acid Sequence↗

PubMed1998

C1 transfer enzymes and coenzymes linking methylotrophic bacteria and methanogenic Archaea.

Methanogenic and sulfate-reducing Archaea are considered to have an energy metabolism involving C1 transfer coenzymes and enzymes unique for this group of strictly anaerobic microorganisms. An aerobic methylotrophic bacterium, Methylobacterium extorquens AM1, was found to contain a cluster of genes that are predicted to encode some of these enzymes and was shown to contain two of the enzyme activities and one of the methanogenic coenzymes. Insertion mutants were all unable to grow on C1 compounds, suggesting that the archaeal enzymes function in aerobic C1 metabolism. Thus, methylotrophy and methanogenesis involve common genes that cross the bacterial/archaeal boundaries.

Amino Acid Sequence↗

PubMed2001

A comprehensive study into the molecular methodology and molecular biology of methanogenic Archaea.

Methanogens belong to the kingdom of Euryarchaeota in the domain of Archaea. The Archaea differ from Bacteria in many aspects important to molecular work. Among these are cell wall composition, their sensitivity to antibiotics, their translation and transcription machinery, and their very strict demands to anaerobic culture conditions. These differences may, at least partly, be responsible for the delay in availability of genetic research tools for methanogens. At present, however, the research within genetics of methanogens and their gene regulation and expression is in rapid progress. Two complete methanogenic genomes have been sequenced and published and more are underway. Besides, sequences are known from a multitude of individual genes from methanogens. Standard methods for simple DNA and RNA work can normally be employed, but permeabilization of the cell wall may demand special procedures. Efficient genetic manipulation systems, including shuttle and integration vector systems, have appeared for mesophilic, but not for thermophilic species within the last few years and will have a major impact on future investigations of methanogenic molecular biology.

Euryarchaeota↗

PubMed2006

Survival of methanogenic archaea from Siberian permafrost under simulated Martian thermal conditions.

Methanogenic archaea from Siberian permafrost complementary to the already well-studied methanogens from non-permafrost habitats were exposed to simulated Martian conditions. After 22 days of exposure to thermo-physical conditions at Martian low- and mid-latitudes up to 90% of methanogenic archaea from Siberian permafrost survived in pure cultures as well as in environmental samples. In contrast, only 0.3%-5.8% of reference organisms from non-permafrost habitats survived at these conditions. This suggests that methanogens from terrestrial permafrost seem to be remarkably resistant to Martian conditions. Our data also suggest that in scenario of subsurface lithoautotrophic life on Mars, methanogenic archaea from Siberian permafrost could be used as appropriate candidates for the microbial life on Mars.

Archaea↗

PubMed1997

The active species of 'CO2' utilized by formylmethanofuran dehydrogenase from methanogenic Archaea.

Formylmethanofuran dehydrogenase from methanogenic Archaea catalyzes the reversible conversion of CO2 and methanofuran to formylmethanofuran, which is an intermediate in methanogenesis from CO2, a biological process yielding approximately 0.3 billion tons of CH4 per year. With the enzyme from Methanosarcina barkeri, it is shown that CO2 rather than HCO3- is the active species of 'CO2' utilized by the dehydrogenase. Evidence is also presented that the enzyme catalyzes a methanofuran-dependent exchange between CO2 and the formyl group of formylmethanofuran. The results are consistent with N-carboxymethanofuran being an intermediate in CO2 reduction to formylmethanofuran.

Aldehyde Oxidoreductases↗

PubMed1992

Interrelations between populations of methanogenic archaea and sulfate-reducing bacteria in the human colon.

In humans, CH4 is produced in the colon by methanogenic archaea and is detected in breath samples from approximately 50% of healthy adults, identified as CH4-excretors. Methanogenesis and sulfate reduction have been described as two mutually exclusive processes, potentially regulated by sulfate availability. To determine whether microbial population balances reflected these apparently co-regulated activities, we compared sulfate-reducing bacteria, methanogenic archaea, sulfate and sulfide concentrations in faeces of 10 CH4-excretors (CH4+) and 9 non-CH4-excretors (CH4-). The mean +/- SE of the logarithm of methanogenic archaea per gram wet weight were 9.0 +/- 0.2 and 4.0 +/- 0.7 for CH4+ and CH4-, respectively (P < 0.001). Sulfate-reducing bacterial counts were 6.5 +/- 0.1 and 7.3 +/- 0.2, respectively (P < 0.001). Fecal sulfate and sulfide concentrations did not differ between groups. These results suggest that a competitive interrelation between methanogenic archaea and sulfate-reducing bacteria occurs in the human colon. However, it does not lead to a complete exclusion of the two populations.

Adolescent↗

PubMed2001

A paramagnetic species with unique EPR characteristics in the active site of heterodisulfide reductase from methanogenic archaea.

Heterodisulfide reductase (Hdr) from methanogenic archaea is an iron-sulfur protein that catalyses the reversible reduction of the heterodisulfide (CoM-S-S-CoB) of the methanogenic thiol coenzymes, coenzyme M (H-S-CoM) and coenzyme B (H-S-CoB). In EPR spectroscopic studies with the enzyme from Methanothermobacter marburgensis, we have identified a unique paramagnetic species that is formed upon reaction of the oxidized enzyme with H-S-CoM in the absence of H-S-CoB. This paramagnetic species can be reduced in a one-electron step with a midpoint-potential of -185 mV but not further oxidized. A broadening of the EPR signal in the 57Fe-enriched enzyme indicates that it is at least partially iron based. The g values (gxyz = 2.013, 1.991 and 1.938) and the midpoint potential argue against a conventional [2Fe-2S]+, [3Fe-4S]+, [4Fe-4S]+ or [4Fe-4S]3+ cluster. This species reacts with H-S-CoB to form an EPR silent form. Hence, we propose that only a half reaction is catalysed in the presence of H-S-CoM and that a reaction intermediate is trapped. This reaction intermediate is thought to be a [4Fe-4S]3+ cluster that is coordinated by one of the cysteines of a nearby active-site disulfide or by the sulfur of H-S-CoM. A paramagnetic species with similar EPR properties was also identified in Hdr from Methanosarcina barkeri.

Alkylating Agents↗

PubMed2006

Methane and sulfate profiles within the subsurface of a tidal flat are reflected by the distribution of sulfate-reducing bacteria and methanogenic archaea.

The anoxic layers of marine sediments are dominated by sulfate reduction and methanogenesis as the main terminal oxidation processes. The aim of this study was to analyze the vertical succession of microbial populations involved in these processes along the first 4.5 m of a tidal-flat sediment. Therefore, a quantitative PCR approach was applied using primers targeting the domains of Bacteria and Archaea, and key functional genes for sulfate reduction (dsrA) and methanogenesis (mcrA). The sampling site was characterized by an unusual sulfate peak at 250 cm depth resulting in separate sulfate-methane transition zones. Methane and sulfate profiles were diametrically opposed, with a methane maximum in the sulfate-depleted zone showing high numbers of archaea and methanogens. The methane-sulfate interfaces harbored elevated numbers of sulfate reducers, and revealed a slight increase in mcrA and archaeal 16S rRNA genes, suggesting sulfate-dependent anaerobic oxidation of methane. A diversity analysis of both functional genes by PCR-denaturing gradient gel electrophoresis revealed a vertical succession of subpopulations that were governed by geochemical and sedimentologic conditions. Along the upper 200 cm, sulfate-reducing populations appeared quite uniform and were dominated by the Deltaproteobacteria. In the layers beneath, an apparent increase in diversity and a shift to the Firmicutes as the predominant group was observed.

Anaerobiosis↗

PubMed2006

Effects of insufficient air injection on methanogenic Archaea in landfill bioreactor.

In this study, methanogenic Archaea diversity in an aerated landfill bioreactor filled with co-disposed incineration bottom ashes and shredded incombustible wastes was monitored and analyzed as a function of time using molecular techniques. Besides, the effects of insufficient air injection on the bioreactor performance and methanogenic diversity were evaluated thoroughly. Results indicated that rapid bio-stabilization of solid waste are possible with aerated landfill bioreactor at various oxygen and oxidation reduction potential levels. Slot-blot hybridization results of leachate samples collected from aerated landfill bioreactor showed that archaeal and bacterial activities increased as stabilization accelerated and bacterial populations constituted almost 95% of all microorganisms. The results of slot-blot hybridization and phylogenetic analysis based on 16S rRNA gene revealed that Methanobacteriales and Methanomicrobiales were dominant species at the beginning while substituted by Methanosarcina-related methanogens close to the end of the operation of bioreactor.

Air↗

PubMed2006

Shuffling of discrete tRNASer regions reveals differently utilized identity elements in yeast and methanogenic archaea.

Seryl-tRNA synthetases (SerRSs) from methanogenic archaea possess distinct evolutionary origin and show minimal sequence similarity with counterparts from bacteria, eukaryotes and other archaea. Here we show that SerRS from yeast Saccharomyces cerevisiae and archaeon Methanococcus maripaludis (ScSerRS and MmSerRS, respectively) display significantly different ability to serylate heterologous tRNA(Ser). Recognition in yeast was shown to be more stringent than in archaeon. While cross-aminoacylation of M. maripaludis tRNA(Ser) (MmtRNA(Ser)) by yeast SerRS barely occurs, yeast tRNA(Ser) (SctRNA(Ser)) was shown to be a good substrate for heterologous MmSerRS. To investigate the contribution of different tRNA regions for the recognition by yeast and archaeal SerRS, chimeric tRNAs bearing separated domains of SctRNA(Ser) in MmtRNA(Ser) framework were produced by in vitro transcription and subjected to kinetic and gel mobility shift analysis with both enzymes. Generally, the recognition in M. maripaludis seems to be relatively relaxed toward tertiary elements of tRNA(Ser) structure and relies on the direct recognition of identity nucleotides. On the other hand, expression of tRNA(Ser) identity elements in yeast seems to be more sensitive toward surrounding sequence context. In both systems variable arm of tRNA was recognized as a major identity region with a strong influence on SerRS:tRNA binding. Acceptor domain of SctRNA(Ser) was also shown to be important for serylation in yeast. We propose that cognate interactions between N-terminal domain of yeast SerRS and variable region of SctRNA(Ser) place the acceptor stem into the enzyme's active site and lead to increased affinity toward serine and efficient serylation of tRNA. The same effect was not observed in M. maripaludis. Unlike its yeast counterpart, MmSerRS forms only one type of covalent complex with MmtRNA(Ser), regardless of the tRNA/SerRS molar ratio. Stoichiometry of the complex, one tRNA per dimeric SerRS, was revealed by mass spectrometry. Our studies indicate that different SerRS:tRNA recognition mode is utilized by these two systems.

Base Sequence↗

PubMed1999

The energy conserving methyltetrahydromethanopterin:coenzyme M methyltransferase complex from methanogenic archaea: function of the subunit MtrH.

In methanogenic archaea the transfer of the methyl group of N5-methyltetrahydromethanopterin to coenzyme M is coupled with energy conservation. The reaction is catalyzed by a membrane associated multienzyme complex composed of eight different subunits MtrA-H. The 23 kDa subunit MtrA harbors a corrinoid prosthetic group which is methylated and demethylated in the catalytic cycle. We report here that the 34 kDa subunit MtrH catalyzes the methylation reaction. MtrH was purified and shown to exhibit methyltetrahydromethanopterin:cob(I)alamin methyltransferase activity. Sequence comparison revealed similarity of MtrH with MetH from Escherichia coli and AcsE from Clostridium thermoaceticum: both enzymes exhibit methyltetrahydrofolate:cob(I)alamin methyltransferase activity.

Amino Acid Sequence↗

PubMed1996

Quantitative determination of H2-utilizing acetogenic and sulfate-reducing bacteria and methanogenic archaea from digestive tract of different mammals.

Total number of bacteria, cellulolytic bacteria, and H2-utilizing microbial populations (methanogenic archaea, acetogenic and sulfate-reducing bacteria) were enumerated in fresh rumen samples from sheep, cattle, buffaloes, deer, llamas, and caecal samples from horses. Methanogens and sulfate reducers were found in all samples, whereas acetogenes were not detected in some samples of each animal. Archaea methanogens were the largest H2-utilizing populations in all animals, and a correlation was observed between the numbers of methanogens and those of cellulolytic microorganisms. Higher counts of acetogens were found in horses and llamas (1 x 10(4) and 4 x 10(4) cells ml-1 respectively).

Acetates↗

PubMed1993

Formylmethanofuran: tetrahydromethanopterin formyltransferase and N5,N10-methylenetetrahydromethanopterin dehydrogenase from the sulfate-reducing Archaeoglobus fulgidus: similarities with the enzymes from methanogenic Archaea.

The sulfate-reducing Archaeoglobus fulgidus contains a number of enzymes previously thought to be unique for methanogenic Archaea. The purification and properties of two of these enzymes, of formylmethanofuran: tetrahydromethanopterin formyltransferase and of N5,N10-methylenetetrahydromethanopterin dehydrogenase (coenzyme F420 dependent) are described here. A comparison of the N-terminal amino acid sequences and of other molecular properties with those of the respective enzymes from three methanogenic Archaea revealed a high degree of similarity.

Amino Acid Sequence↗

PubMed1997

Function of coenzyme F420-dependent NADP reductase in methanogenic archaea containing an NADP-dependent alcohol dehydrogenase.

Methanogenic archaea growing on ethanol or isopropanol as the electron donor for CO2 reduction to CH4 contain either an NADP-dependent or a coenzyme F420-dependent alcohol dehydrogenase. We report here that in both groups of methanogens, the N5, N10-methylenetetrahydromethanopterin dehydrogenase and the N5, N10-methylenetetrahydromethanopterin reductase, two enzymes involved in CO2 reduction to CH4, are specific for F420. This raised the question how F420H2 is regenerated in the methanogens with an NADP-dependent alcohol dehydrogenase. We found that these organisms contain catabolic activities of an enzyme catalyzing the reduction of F420 with NADPH. The F420-dependent NADP reductase from Methanogenium organophilum was purified and characterized. The N-terminal amino acid sequence showed 42% sequence identity to a putative gene product in Methanococcus jannaschii, the total genome of which has recently been sequenced.

Alcohol Oxidoreductases↗