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Asgard is an archaeal superphylum that might hold the key to understand the origin of eukaryotes, but its diversity and ecological roles remain poorly understood. Here, we reconstructed 15 metagenomic-assembled genomes from coastal sediments covering most known Asgard archaea and a novel group, which is proposed as a new Asgard phylum named as the “Gerdarchaeota”. Genomic analyses predict that Gerdarchaeota are facultative anaerobes in utilizing both organic and inorganic carbon. Unlike their closest relatives Heimdallarchaeota, Gerdarchaeota have genes encoding for cellulase and enzymes involved in the tetrahydromethanopterin-based Wood–Ljungdahl pathway. Transcriptomics showed that most of our identified Asgard archaea are capable of degrading organic matter, including peptides, amino acids and fatty acids, occupying ecological niches in different depths of layers of the sediments. Overall, this study broadens the diversity of the mysterious Asgard archaea and provides evidence for their ecological roles in coastal sediments.

Methane production by archaea depends on tetrahydromethanopterin (H4MPT), a pterin-containing cofactor that carries one-carbon units. Two redox reactions within the nine steps of H4MPT side chain biosynthesis have been hypothesized. Biochemical assays have demonstrated that the archaeal iron-sulfur flavoprotein dihydromethanopterin reductase X (DmrX or MM1854) catalyzes the final reaction of the pathway, the reduction of dihydromethanopterin to H4MPT, using dithiothreitol (DTT) as an artificial electron donor. The crystal structure of DmrB, a bacterial DmrX homolog that lacks iron-sulfur clusters, has led to a proposed ping-pong mechanism of electron transfer between FMNH2 and the FMN prosthetic group of DmrB. However, an enzymatic assay to test the hypothetical DmrB mechanism is lacking because a suitable electron donor has not previously been identified. Furthermore, a second uncharacterized archaeal flavoprotein (MM1853) has been hypothesized to function in H4MPT side chain biosynthesis. In this work, to facilitate the development of assays to elucidate the functions of DmrB and MM1853, we tested a variety of electron donors, including dithiothreitol, ferredoxin, and a system consisting of NADH and an NADH-dependent flavin-reducing enzyme (Fre). Reduction of the DmrB prosthetic group (FMN) was measured as a decrease in absorbance at 460 nm. NADPH, NADH, and DTT were unable to reduce DmrB. However, NADH/Fre was able to reduce DmrB within 70 min (initial rate of 1.3 μM/min), providing the basis for a future DmrB activity assay. Carbon monoxide (CO)/CO dehydrogenase/ferredoxin reduced DmrB more rapidly within 6 min. Both electron transfer systems reduced a second flavin-containing archaeal protein MM1853, which is predicted to catalyze the third step of H4MPT biosynthesis. While NADH and NADPH were incapable of directly reducing the FMN cofactor of MM1853, DTT or NADH/Fre could eliminate the FMN peaks. These results establish the basis for new oxidoreductase assays that will facilitate testing several proposed DmrB mechanisms and defining the specific function of MM1853 in methanogen cofactor biosynthesis.

Methane-generating archaea drive the final step in anaerobic organic compound mineralization and dictate the carbon flow of Earth’s diverse anoxic ecosystems in the absence of inorganic electron acceptors. Although such Archaea were presumed to be restricted to life on simple compounds like hydrogen (H2), acetate or methanol, an archaeon, Methermicoccus shengliensis, was recently found to convert methoxylated aromatic compounds to methane. Methoxylated aromatic compounds are important components of lignin and coal, and are present in most subsurface sediments. Despite the novelty of such a methoxydotrophic archaeon its metabolism has not yet been explored. In this study, transcriptomics and proteomics reveal that under methoxydotrophic growth M. shengliensis expresses an O-demethylation/methyltransferase system related to the one used by acetogenic bacteria. Enzymatic assays provide evidence for a two step-mechanisms in which the methyl-group from the methoxy compound is (1) transferred on cobalamin and (2) further transferred on the C1-carrier tetrahydromethanopterin, a mechanism distinct from conventional methanogenic methyl-transfer systems which use coenzyme M as final acceptor. We further hypothesize that this likely leads to an atypical use of the methanogenesis pathway that derives cellular energy from methyl transfer (Mtr) rather than electron transfer (F420H2 re-oxidation) as found for methylotrophic methanogenesis.

Nitrogen-fixing bacterial strain, designated B2T, was isolated from methane-oxidation enrichment originating from a Sphagnum-dominated raised peatland in Tver region, Russia, and its phenotypic, chemotaxonomic and genomic characteristics were investigated. Cells of isolate were Gram-negative, aerobic, rod or spiral-shaped, with motility provided by a single polar flagellum in liquid media and peritrichous flagella on solid media. Strain was able to grow at 15–40 °C, pH 5.5–8.5 and tolerated NaCl to 2.0 % (w/v). Strain B2T gave positive amplification for dinitrogen reductase (nifH gene) and acetylene reduction activity was recorded up to 1250 nmol ethylene h–1 (mg protein)–1. Analysis of 16S rRNA showed that B2T represents a member of the genus Azospirillum and had the highest sequence similarity with A. humicireducens SgZ-5T (97.92 %). The predominant quinone system was ubiquinone Q-10 and the major fatty acids were C18 : 1ω7, C16 : 1ω7 and C16 : 0. The strain was facultative methylotrophic and used methanol and formate for the growth. Genome sequencing revealed a genome size of 8.0 Mbp and a G+C content of 67.8 mol%. The mxaFI genes encoding methanol dehydrogenase were absent, but a homologous xoxF gene was detected. The genes encoding enzymes involved in the biosynthesis of tetrahydromethanopterin (H4MPT) (formaldehyde oxidation) and NAD-linked formate dehydrogenase (fdsABG) were identified. Pairwise determined whole genome average nucleotide identity (gANI) values confirmed that strain B2T represents a novel species, for which we propose the name Azospirillum palustre sp. nov. with the type strain B2T (VKM B-3233T, КСТС 62613Т).

Symbiotic digestion of lignocellulose in the hindgut of higher termites is mediated by a diverse assemblage of bacteria and archaea. During a large-scale metagenomic study, we reconstructed 15 metagenome-assembled genomes of Bathyarchaeia that represent two distinct lineages in subgroup 6 (formerly MCG-6) unique to termite guts. One lineage (TB2; Candidatus Termitimicrobium) encodes all enzymes required for reductive acetogenesis from CO2 via an archaeal variant of the Wood–Ljungdahl pathway, involving tetrahydromethanopterin as C1 carrier and an (ADP-forming) acetyl-CoA synthase. This includes a novel 11-subunit hydrogenase, which possesses the genomic architecture of the respiratory Fpo-complex of other archaea but whose catalytic subunit is phylogenetically related to and shares the conserved [NiFe] cofactor-binding motif with [NiFe] hydrogenases of subgroup 4 g. We propose that this novel Fpo-like hydrogenase provides part of the reduced ferredoxin required for CO2 reduction and is driven by the electrochemical membrane potential generated from the ATP conserved by substrate-level phosphorylation; the other part may require the oxidation of organic electron donors, which would make members of TB2 mixotrophic acetogens. Members of the other lineage (TB1; Candidatus Termiticorpusculum) are definitely organotrophic because they consistently lack hydrogenases and/or methylene-tetrahydromethanopterin reductase, a key enzyme of the archaeal Wood–Ljungdahl pathway. Both lineages have the genomic capacity to reduce ferredoxin by oxidizing amino acids and might conduct methylotrophic acetogenesis using unidentified methylated compound(s). Our results indicate that Bathyarchaeia of subgroup 6 contribute to acetate formation in the guts of higher termites and substantiate the genomic evidence for reductive acetogenesis from organic substrates, possibly including methylated compounds, in other uncultured representatives of the phylum.

Methane (CH(4)) emissions from Arctic lakes are a large and growing source of greenhouse gas to the atmosphere with critical implications for global climate. Because Arctic lakes are ice covered for much of the year, understanding the metabolic flexibility of methanotrophs under anoxic conditions would aid in characterizing the mechanisms responsible for limiting CH(4) emissions from high-latitude regions. Using sediments from an active CH(4) seep in Lake Qalluuraq, Alaska, we conducted DNA-based stable isotope probing (SIP) in anoxic mesocosms and found that aerobic Gammaproteobacterial methanotrophs dominated in assimilating CH(4). Aerobic methanotrophs were also detected down to 70 cm deep in sediments at the seep site, where anoxic conditions persist. Metagenomic analyses of the heavy DNA from (13)CH(4)-SIP incubations showed that these aerobic methanotrophs had the capacity to generate intermediates such as methanol, formaldehyde, and formate from CH(4) oxidation and to oxidize formaldehyde in the tetrahydromethanopterin (H(4)MPT)-dependent pathway under anoxic conditions. The high levels of Fe present in sediments, combined with Fe and CH(4) profiles in the persistent CH(4) seep site, suggested that oxidation of CH(4), or, more specifically, its intermediates such as methanol and formaldehyde might be coupled to iron reduction. Aerobic methanotrophs also possessed genes associated with nitrogen and hydrogen metabolism, which might provide potentially alternative energy conservation options under anoxic conditions. These results expand the known metabolic spectrum of aerobic methanotrophs under anoxic conditions and necessitate the re-assessment of the mechanisms underlying CH(4) oxidation in the Arctic, especially under lakes that experience extended O(2) limitations during ice cover.

Most methanogenic archaea use the rudimentary hydrogenotrophic pathway—from CO2and H2to methane—as the terminal step of microbial biomass degradation in anoxic habitats. The barely exergonic process that just conserves sufficient energy for a modest lifestyle involves chemically challenging reactions catalyzed by complex enzyme machineries with unique metal-containing cofactors. The basic strategy of the methanogenic energy metabolism is to covalently bind C1species to the C1carriers methanofuran, tetrahydromethanopterin, and coenzyme M at different oxidation states. The four reduction reactions from CO2to methane involve one molybdopterin-based two-electron reduction, two coenzyme F420–based hydride transfers, and one coenzyme F430–based radical process. For energy conservation, one ion-gradient-forming methyl transfer reaction is sufficient, albeit supported by a sophisticated energy-coupling process termed flavin-based electron bifurcation for driving the endergonic CO2reduction and fixation. Here, we review the knowledge about the structure-based catalytic mechanism of each enzyme of hydrogenotrophic methanogenesis.

Methanogens are considered as one of the earliest life forms on Earth, and together with anaerobic methane-oxidizing archaea, they have crucial effects on climate stability. Yet, the origin and evolution of anaerobic alkane metabolism in the domain Archaea remain controversial. Here, we show that methanogenesis was already present in the common ancestor of Euryarchaeota, TACK archaea, and Asgard archaea likely in the late Hadean or early Archean eon and that the ancestral methanogen was dependent on methylated compounds and hydrogen. Carbon dioxide-reducing methanogenesis developed later through the evolution of tetrahydromethanopterin S-methyltransferase, which linked methanogenesis to the Wood-Ljungdahl pathway for energy conservation. Multicarbon alkane metabolisms in Archaea also originated early, with genes coding for the activation of short- or even long-chain alkanes likely evolving from an ethane-metabolizing ancestor. These genes were likely horizontally transferred to multiple archaeal clades including Candidatus (Ca) Bathyarchaeota, Ca. Helarchaeota, Ca Hadesarchaeota, and the methanogenic Ca. Methanoliparia.

The sulfate-dependent, anaerobic oxidation of methane (AOM) is an important sink for methane in marine environments. It is carried out between anaerobic methanotrophic archaea (ANME) and sulfate-reducing bacteria (SRB) living in syntrophic partnership. In this study, we compared the genomes, gene expression patterns and ultrastructures of three phylogenetically different microbial consortia found in hydrocarbon-rich environments under different temperature regimes: ANME-1a/HotSeep-1 (60°C), ANME-1a/Seep-SRB2 (37°C) and ANME-2c/Seep-SRB2 (20°C). All three ANME encode a reverse methanogenesis pathway: ANME-2c encodes all enzymes, while ANME-1a lacks the gene for N5,N10-methylene tetrahydromethanopterin reductase (mer) and encodes a methylenetetrahydrofolate reductase (Met). The bacterial partners contain the genes encoding the canonical dissimilatory sulfate reduction pathway. During AOM, all three consortia types highly expressed genes encoding for the formation of flagella or type IV pili and/or c-type cytochromes, some predicted to be extracellular. ANME-2c expressed potentially extracellular cytochromes with up to 32 hemes, whereas ANME-1a and SRB expressed less complex cytochromes (≤ 8 and ≤ 12 heme respectively). The intercellular space of all consortia showed nanowire-like structures and heme-rich areas. These features are proposed to enable interspecies electron exchange, hence suggesting that direct electron transfer is a common mechanism to sulfate-dependent AOM, and that both partners synthesize molecules to enable it.

Methylotrophy, the ability of microorganisms to grow on reduced one-carbon substrates such as methane or methanol, is a feature of various bacterial species. The prevailing oxidation pathway depends on tetrahydromethanopterin (H4MPT) and methylofuran (MYFR), an analog of methanofuran from methanogenic archaea. Formyltransferase/hydrolase complex (Fhc) generates formate from formyl-H4MPT in two consecutive reactions where MYFR acts as a carrier of one-carbon units. Recently, we chemically characterized MYFR from the model methylotroph Methylorubrum extorquens and identified an unusually long polyglutamate side chain of up to 24 glutamates. Here, we report on the crystal structure of Fhc to investigate the function of the polyglutamate side chain in MYFR and the relatedness of the enzyme complex with the orthologous enzymes in archaea. We identified MYFR as a prosthetic group that is tightly, but noncovalently, bound to Fhc. Surprisingly, the structure of Fhc together with MYFR revealed that the polyglutamate side chain of MYFR is branched and contains glutamates with amide bonds at both their α- and γ-carboxyl groups. This negatively charged and branched polyglutamate side chain interacts with a cluster of conserved positively charged residues of Fhc, allowing for strong interactions. The MYFR binding site is located equidistantly from the active site of the formyltransferase (FhcD) and metallo-hydrolase (FhcA). The polyglutamate serves therefore an additional function as a swinging linker to shuttle the one-carbon carrying amine between the two active sites, thereby likely increasing overall catalysis while decreasing the need for high intracellular MYFR concentrations., Proceedings of the National Academy of Sciences of the United States of America, 116 (51), ISSN:0027-8424, ISSN:1091-6490

Dimethylsulfide is a volatile organic sulfur compound that provides the largest input of biogenic sulfur from the oceans to the atmosphere, and thence back to land, constituting an important link in the global sulfur cycle. Microorganisms degrading DMS affect fluxes of DMS in the environment, but the underlying metabolic pathways are still poorly understood. Methylophaga thiooxydans is a marine methylotrophic bacterium capable of growth on DMS as sole source of carbon and energy. Using proteomics and transcriptomics we identified genes expressed during growth on dimethylsulfide and methanol to refine our knowledge of the metabolic pathways that are involved in DMS and methanol degradation in this strain. Amongst the most highly expressed genes on DMS were the two methanethiol oxidases driving the oxidation of this reactive and toxic intermediate of DMS metabolism. Growth on DMS also increased expression of the enzymes of the tetrahydrofolate linked pathway of formaldehyde oxidation, in addition to the tetrahydromethanopterin linked pathway. Key enzymes of the inorganic sulfur oxidation pathway included flavocytochrome c sulfide dehydrogenase, sulfide quinone oxidoreductase, and persulfide dioxygenases. A sulP permease was also expressed during growth on DMS. Proteomics and transcriptomics also identified a number of highly expressed proteins and gene products whose function is currently not understood. As the identity of some enzymes of organic and inorganic sulfur metabolism previously detected in Methylophaga has not been characterized at the genetic level yet, highly expressed uncharacterized genes provide new targets for further biochemical and genetic analysis. A pan-genome analysis of six available Methylophaga genomes showed that only two of the six investigated strains, M. thiooxydans and M. sulfidovorans have the gene encoding methanethiol oxidase, suggesting that growth on methylated sulfur compounds of M. aminisulfidivorans is likely to involve different enzymes and metabolic intermediates. Hence, the pathways of DMS-utilization and subsequent C1 and sulfur oxidation are not conserved across Methylophaga isolates that degrade methylated sulfur compounds.

The effect of different bioaugmentation strategies on anaerobic digestion related to the alleviation of ammonia inhibition was investigated in a long-term operation. The long-term operation confirmed that bioaugmentation is a stable method. A 35% increase in methane production (MP) was observed in bottles bioaugmented with Methanosarcina barkeri (MSB) or Syntrophaceticu schinkii (SS) + Methanobrevibacter smithii (MBS), and a 49% increment was obtained from the bottles bioaugmented with Methanosaeta harundinacea (MSH) + SS + MBS. Results suggest that the enhancement in both aceticlastic and hydrogenotrophic methanogenic pathways should be considered, and bioaugmentation strain should be properly selected to achieve a synergistic effect. The microbial community analysis indicated Methanosarcina spp. was the dominant archaea. Combined with specific methanogenic activity and carbon isotope fractionation analysis, it was suggested that Methanosarcina spp. performed differently in methanogenic pathways in different bottles. The abundance of COG and total enzymes in the bottles with high MP (MSB and MSH + SS + MBS) was higher than that in the other bottles. The ratio of the functional enzyme tetrahydromethanopterin S-methyltransferase subunit H (EC 2.1.1.86) to formylmethanofuran dehydrogenase subunit E (EC 1.2.99.5) and the relative abundance of enolase (EC 1.2.1.2) confirmed the aceticlastic methanogenic pathway of MSB in Group 1 and the pathway enhancement balance in MSH + SS + MBS. The modified Anaerobic Digestion Model No.1 including syntrophic acetate oxidation was used for simulation with R2 > 0.96. Simulated contribution rate data indicated that the hydrogenotrophic methanogenic pathway was dominant while both two pathways got strengthened, which is consistent with the findings of the microbial analysis.

Lanthanides (Ln) are an essential cofactor for XoxF-type methanol dehydrogenases (MDHs) in Gram-negative methylotrophs. The Ln3+ dependency of XoxF has expanded knowledge and raised new questions in methylotrophy, including the differences in characteristics of XoxF-type MDHs, their regulation, and the methylotrophic metabolism including formaldehyde oxidation. In this study, we genetically identified one set of Ln3+- and Ca2+-dependent MDHs (XoxF1 and MxaFI), that are involved in methylotrophy, and an ExaF-type Ln3+-dependent ethanol dehydrogenase, among six MDH-like genes in Methylobacterium aquaticum strain 22A. We also identified the causative mutations in MxbD, a sensor kinase necessary for mxaF expression and xoxF1 repression, for suppressive phenotypes in xoxF1 mutants defective in methanol growth even in the absence of Ln3+. Furthermore, we examined the phenotypes of a series of formaldehyde oxidation-pathway mutants (fae1, fae2, mch in the tetrahydromethanopterin (H4MPT) pathway and hgd in the glutathione-dependent formaldehyde dehydrogenase (GSH) pathway). We found that MxaF produces formaldehyde to a toxic level in the absence of the formaldehyde oxidation pathways and that either XoxF1 or ExaF can oxidize formaldehyde to alleviate formaldehyde toxicity in vivo. Furthermore, the GSH pathway has a supportive role for the net formaldehyde oxidation in addition to the H4MPT pathway that has primary importance. Studies on methylotrophy in Methylobacterium species have a long history, and this study provides further insights into genetic and physiological diversity and the differences in methylotrophy within the plant-colonizing methylotrophs.

Methane-producing archaea and methylotrophic bacteria use tetrahydromethanopterin (H4MPT) and/or tetrahydrofolate (H4F) as coenzymes in one-carbon (C1) transfer pathways. The α-proteobacterium Methylobacterium extorquens AM1 contains a dihydromethanopterin reductase (DmrA) and two annotated dihydrofolate reductases (DfrA and DfrB). DmrA has been shown to catalyze the final step of H4MPT biosynthesis; however, the functions of DfrA and DfrB have not been examined biochemically. Moreover, sequence alignment (BLAST) searches have recognized scores of proteins that share up to 99% identity with DmrA but are annotated as diacylglycerol kinases (DAGK). In this work, we used bioinformatics and enzyme assays to provide insight into the phylogeny and substrate specificity of selected Dfr and DmrA homologs. In a phylogenetic tree, DmrA and homologs annotated as DAGKs grouped together in one clade. Purified histidine-tagged versions of the annotated DAGKs from Hyphomicrobium nitrativorans and Methylobacterium nodulans (respectively, sharing 69% and 84% identity with DmrA) showed only low activity in phosphorylating 1,2-dihexanoyl-sn-glycerol when compared with a commercial DAGK from E. coli. However, the annotated DAGKs successfully reduced a dihydromethanopterin analog (dihydrosarcinapterin, H2SPT) with kinetic values similar to those determined for M. extorquens AM1 DmrA. DfrA and DfrB showed little or no ability to reduce H2SPT under the conditions studied; however, both catalyzed the NADPH-dependent reduction of dihydrofolate. These results provide the first evidence that DfrA and DfrB function as authentic dihydrofolate reductases, while DAGKs with greater than 69% identity to DmrA may be misannotated and are likely to function in H4MPT biosynthesis.

Asgard is a newly proposed archaeal superphylum. Phylogenetic position of Asgard archaea and its relationships to the origin of eukaryotes is attracting increasingly research interest. However, in-depth knowledge of their diversity, distribution, and activity of Asgard archaea remains limited. Here, we used phylogenetic analysis to cluster the publicly available Asgard archaeal 16S rRNA gene sequences into 13 subgroups, including five previously unknown subgroups. These lineages were widely distributed in anaerobic environments, with the majority of 16S rRNA gene sequences (92%) originating from sediment habitats. Co-occurrence analysis revealed potential relationships between Asgard, Bathyarchaeota, and Marine Benthic Group D archaea. Genomic analysis suggested that Asgard archaea are potentially mixotrophic microbes with divergent metabolic capabilities. Importantly, metatranscriptomics confirmed the versatile lifestyles of Lokiarchaeota and Thorarchaeota, which can fix CO2using the tetrahydromethanopterin Wood-Ljungdahl pathway, perform acetogenesis, and degrade organic matters. Overall, this study broadens the understandings of Asgard archaea ecology, and also provides the first evidence to support a transcriptionally active mixotrophic lifestyle of Asgard archaea, shedding light on the potential roles of these microorganisms in the global biogeochemical cycling.

The metabolic pathways of one-carbon compounds utilized by colorless sulfur bacterium Beggiatoa leptomitoformis D-402 were revealed based on comprehensive analysis of its genomic organization, together with physiological, biochemical and molecular biological approaches. Strain D-402 was capable of aerobic methylotrophic growth with methanol as a sole source of carbon and energy and was not capable of methanotrophic growth because of the absence of genes of methane monooxygenases. It was established that methanol can be oxidized to CO(2) in three consecutive stages. On the first stage methanol was oxidized to formaldehyde by the two PQQ (pyrroloquinolinequinone)-dependent methanol dehydrogenases (MDH): XoxF and Mdh2. Formaldehyde was further oxidized to formate via the tetrahydromethanopterin (H(4)MPT) pathway. And on the third stage formate was converted to CO(2) by NAD(+)-dependent formate dehydrogenase Fdh2. Finally, it was established that endogenous CO(2), formed as a result of methanol oxidation, was subsequently assimilated for anabolism through the Calvin–Benson–Bassham cycle. The similar way of one-carbon compounds utilization also exists in representatives of another freshwater Beggiatoa species—B. alba. ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (10.1007/s12088-018-0737-x) contains supplementary material, which is available to authorized users.

We sequenced the genomes of 19 methylotrophic isolates from Lake Washington, which belong to nine genera within eight families of the Alphaproteobacteria, two of the families being the newly proposed families. Comparative genomic analysis with a focus on methylotrophy metabolism classifies these strains into heterotrophic and obligately or facultatively autotrophic methylotrophs. The most persistent metabolic modules enabling methylotrophy within this group are the N-methylglutamate pathway, the two types of methanol dehydrogenase (MxaFI and XoxF), the tetrahydromethanopterin pathway for formaldehyde oxidation, the serine cycle and the ethylmalonyl-CoA pathway. At the same time, a great potential for metabolic flexibility within this group is uncovered, with different combinations of these modules present. Phylogenetic analysis of key methylotrophy functions reveals that the serine cycle must have evolved independently in at least four lineages of Alphaproteobacteria and that all methylotrophy modules seem to be prone to lateral transfers as well as deletions.

Prior studies have indicated that MJ1099 fromMethanocaldococcus jannaschiihas roles in the biosynthesis of tetrahydromethanopterin and methanofuran, two key cofactors of one-carbon (C1) metabolism in diverse organisms including the methanogenic archaea. Here, the structure of MJ1099 has been solved to 1.7 Å resolution using anomalous scattering methods. The results indicate that MJ1099 is a member of the TIM-barrel superfamily and that it is a homohexamer. Bioinformatic analyses identified a potential active site that is highly conserved among MJ1099 homologs and the key amino acids involved were identified. The results presented here should guide further studies of MJ1099 including mechanistic studies and possibly the development of inhibitors that target the methanogenic archaea in the digestive tracts of humans and that are a source of the greenhouse gas methane.

Dihydromethanopterin reductase (Dmr) is a redox enzyme that plays a key role in generating tetrahydromethanopterin (H4MPT) for use in one-carbon metabolism by archaea and some bacteria. DmrB is a bacterial enzyme understood to reduce dihydromethanopterin (H2MPT) to H4MPT using flavins as the source of reducing equivalents, but the mechanistic details have not been elucidated previously. Here we report the crystal structure of DmrB from Burkholderia xenovorans at a resolution of 1.9 Å. Unexpectedly, the biological unit is a 24-mer composed of eight homotrimers located at the corners of a cubic cage-like structure. Within a homotrimer, each monomer-monomer interface exhibits an active site with two adjacently bound flavin mononucleotide (FMN) ligands, one deeply buried and tightly bound and one more peripheral, for a total of 48 ligands in the biological unit. Computational docking suggested that the peripheral site could bind either the observed FMN (the electron donor for the overall reaction) or the pterin, H2MPT (the electron acceptor for the overall reaction), in configurations ideal for electron transfer to and from the tightly bound FMN. On this basis, we propose that DmrB uses a ping-pong mechanism to transfer reducing equivalents from FMN to the pterin substrate. Sequence comparisons suggested that the catalytic mechanism is conserved among the bacterial homologs of DmrB and partially conserved in archaeal homologs, where an alternate electron donor is likely used. In addition to the mechanistic revelations, the structure of DmrB could help guide the development of anti-obesity drugs based on modification of the ecology of the human gut.

Metabolic Origins Methyl groups, including those derived from or ending up in methane, are managed through a dizzying array of metabolic pathways. Some of these originated early in life's history, and their evolution paralleled and contributed to Earth's chemistry. Adam et al. analyzed a set of bacterial and archaeal genomes, looking for patterns in the presence and divergence of enzymes in the tetrahydromethanopterin methyl branch of the Wood–Ljungdahl pathway, which is involved in carbon redox reactions. Expanding previous analyses narrowed the distance between bacterial and archaeal sequences, making horizontal transfer more plausible relative to an origin in the last universal common ancestor. An origin of this branch in Archaea is likely given wide distribution therein and enzyme phylogenies consistent with those of the organisms. Nat. Microbiol. 10.1038/s41564-019-0534-2 (2019).

In this opinion article, I wish to highlight the fact that reactions linked to tetrahydromethanopterin (H4MPT) and methanofuran (MF), the ones involved in methanogenesis as well as in methylotrophy, are much more widespread among both Bacteria and Archaea than originally thought. While, over the past two decades, databases of the respective genes have been steadily growing and expanding to include novel, divergent sequences, belonging to a variety of taxa, somehow a view still prevails of the limited distribution of these genes, along with an evolutionary scenario in which genes for the methanogenesis pathway were horizontally transferred from Euryarchaea into Proteobacteria (Graham et al., 2000; Gogarten et al., 2002; Boucher et al., 2003; Braakman and Smith, 2012; Arnold, 2015). The two main arguments originally used to support this scenario were (1) the limited distribution of the H4MPT/MF-dependent pathway in the bacterial domain of life, and (2) the low probability of the respective genes being lost in most bacterial lineages (Boucher et al., 2003). However, these arguments can be easily refuted in the light of the current knowledge. In Figure ​Figure1,1, I utilize the recently constructed universal tree of life (Hug et al., 2016), to map the taxa in which at least some of the genes for the H4MPT/MF-dependent C1 transfers are recognized. Among the Archaea, these include, in addition to the well-characterized methanonogens or methane oxidizers, members of Euryarchaeota not known for a methanogenic life style (Thermoplasmatales, Hadesarchaea; Baker et al., 2016), members of Crenarchaeota (Thermoproteales, Ignisphaera, Ingnispaeroid; Goker et al., 2010; Jay et al., 2016), Bathyarchaeota (Evans et al., 2015; Lazar et al., 2016), and Thorarchaeota (Seitz et al., 2016). Among the Bacteria, genes for the H4MPT/MF-dependent reactions have been identified, beside Alpha-, Beta-, and Gammaproteobacteria (Vorholt et al., 1999), in the genomes of Planctomycetes (Chistoserdova et al., 2004; Chistoserdova, 2013), Deltaproteobacteria, Firmicutes, Actinomycetes, Synergistetes, Chloroflexi (Brown et al., 2011 and unpublished genomes available through the NCBI), as well as in the Candidate phylum NC10 (Ettwig et al., 2010). This wide distribution across the tree of life (Figure ​(Figure1),1), along with great sequence divergence for the genes in question (Chistoserdova, 2013; Evans et al., 2015; Spang et al., 2015) support a scenario of a long evolution within both Archaea and Bacteria, and point to the emergence of these reactions in early life, before Bacteria and Archaea have branched apart.

Methanogenic archaea share one ion gradient forming reaction in their energy metabolism catalyzed by the membrane-spanning multisubunit complex N(5)-methyl-tetrahydromethanopterin: coenzyme M methyltransferase (MtrABCDEFGH or simply Mtr). In this reaction the methyl group transfer from methyl-tetrahydromethanopterin to coenzyme M mediated by cobalamin is coupled with the vectorial translocation of Na(+) across the cytoplasmic membrane. No detailed structural and mechanistic data are reported about this process. In the present work we describe a procedure to provide a highly pure and homogenous Mtr complex on the basis of a selective removal of the only soluble subunit MtrH with the membrane perturbing agent dimethyl maleic anhydride and a subsequent two-step chromatographic purification. A molecular mass determination of the Mtr complex by laser induced liquid bead ion desorption mass spectrometry (LILBID-MS) and size exclusion chromatography coupled with multi-angle light scattering (SEC-MALS) resulted in a (MtrABCDEFG)3 heterotrimeric complex of ca. 430kDa with both techniques. Taking into account that the membrane protein complex contains various firmly bound small molecules, predominantly detergent molecules, the stoichiometry of the subunits is most likely 1:1. A schematic model for the subunit arrangement within the MtrABCDEFG protomer was deduced from the mass of Mtr subcomplexes obtained by harsh IR-laser LILBID-MS.

Microbial methane oxidizers play a crucial role in the oxidation of methane in marine ecosystems, as such preventing the escape of excessive methane to the atmosphere. Despite the important role of methanotrophs in marine ecosystems, only a limited number of isolates are described, with only four genomes available. Here, we report on two genomes of gammaproteobacterial methanotroph cultures, affiliated with the deep-sea cluster 2, obtained from North Sea sediment. Initial enrichments using methane as sole source of carbon and energy and mimicking the in situ conditions followed by serial subcultivations and multiple extinction culturing events over a period of 3 years resulted in a highly enriched culture. The draft genomes of the methane oxidizer in both cultures showed the presence of genes typically found in type I methanotrophs, including genes encoding particulate methane monooxygenase (pmoCAB), genes for tetrahydromethanopterin (H4MPT)- and tetrahydrofolate (H4F)-dependent C1-transfer pathways, and genes of the ribulose monophosphate (RuMP) pathway. The most distinctive feature, when compared to other available gammaproteobacterial genomes, is the absence of a calcium-dependent methanol dehydrogenase. Both genomes reported here only have a xoxF gene encoding a lanthanide-dependent XoxF5-type methanol dehydrogenase. Thus, these genomes offer novel insight in the genomic landscape of uncultured diversity of marine methanotrophs.

C-1 carriers are essential cofactors in all domains of life, and in Archaea, these can be derivatives of tetrahydromethanopterin (H(4)-MPT) or tetrahydrofolate (H(4)-folate). Their synthesis requires 6-hydroxymethyl-7,8-dihydropterin diphosphate (6-HMDP) as the precursor, but the nature of pathways that lead to its formation were unknown until the recent discovery of the GTP cyclohydrolase IB/MptA family that catalyzes the first step, the conversion of GTP to dihydroneopterin 2',3'-cyclic phosphate or 7,8-dihydroneopterin triphosphate [El Yacoubi, B.; et al. (2006) J. Biol. Chem., 281, 37586-37593 and Grochowski, L. L.; et al. (2007) Biochemistry46, 6658-6667]. Using a combination of comparative genomics analyses, heterologous complementation tests, and in vitro assays, we show that the archaeal protein families COG2098 and COG1634 specify two of the missing 6-HMDP synthesis enzymes. Members of the COG2098 family catalyze the formation of 6-hydroxymethyl-7,8-dihydropterin from 7,8-dihydroneopterin, while members of the COG1634 family catalyze the formation of 6-HMDP from 6-hydroxymethyl-7,8-dihydropterin. The discovery of these missing genes solves a long-standing mystery and provides novel examples of convergent evolutions where proteins of dissimilar architectures perform the same biochemical function.

The non-methane-utilizing methylotroph, Methylophilus sp. TWE2, was isolated from tap-water during the enrichment of methanotrophs with methane. The complete genome sequence of strain TWE2 showed that this bacterium may convert methanol to formaldehyde via catalysis of methanol dehydrogenase (MDH), after which formaldehyde would be assimilated to biomass through the ribulose monophosphate (RuMP) pathway or dissimilated via the tetrahydromethanopterin (H4MPT) pathway. The deficiency of glycolysis and the TCA cycle indicate that strain TWE2 may be an obligate methylotroph. This is the first complete genome sequence of the genus Methylophilus.

Tetrahydromethanopterin (H4 MPT) is a tetrahydrofolate analogue involved as a C1 carrier in the metabolism of various groups of microorganisms. How H4MPT is bound to the respective C1 unit converting enzymes remained elusive. We describe here the structure of the homopentameric formaldehyde-activating enzyme (Fae) from Methylobacterium extorquens AM1 established at 2.0 angstrom without and at 1.9 angstrom with methylene-H4MPT bound. Methylene-H4MPT is bound in an "S"-shaped conformation into the cleft formed between two adjacent subunits. Coenzyme binding is accompanied by side chain rearrangements up to 5 angstrom and leads to a rigidification of the C-terminal arm, a formation of a new hydrophobic cluster, and an inversion of the amide side chain of Gln88. Methylene-H4MPT in Fae shows a characteristic kink between the tetrahydropyrazine and the imidazolidine rings of 70 degrees that is more pronounced than that reported for free methylene-H4MPT in solution (50 degrees). Fae is an essential enzyme for energy metabolism and formaldehyde detoxification of this bacterium and catalyzes the formation of methylene-H4MPT from H4MPT and formaldehyde. The molecular mechanism ofthis reaction involving His22 as acid catalyst is discussed.

During growth on one-carbon (C 1 ) compounds, the aerobic α-proteobacterium Methylobacterium extorquens AM1 synthesizes the tetrahydromethanopterin (H 4 MPT) derivative dephospho-H 4 MPT as a C 1 carrier in addition to tetrahydrofolate. The enzymes involved in dephospho-H 4 MPT biosynthesis have not been identified in bacteria. In archaea, the final step in the proposed pathway of H 4 MPT biosynthesis is the reduction of dihydromethanopterin (H 2 MPT) to H 4 MPT, a reaction analogous to the reaction of the bacterial dihydrofolate reductase. A gene encoding a dihydrofolate reductase homolog has previously been reported for M. extorquens and assigned as the putative H 2 MPT reductase gene ( dmrA ). In the present work, we describe the biochemical characterization of H 2 MPT reductase (DmrA), which is encoded by dmrA . The gene was expressed with a six-histidine tag in Escherichia coli , and the recombinant protein was purified by nickel affinity chromatography and gel filtration. Purified DmrA catalyzed the NAD(P)H-dependent reduction of H 2 MPT with a specific activity of 2.8 μmol of NADPH oxidized per min per mg of protein at 30°C and pH 5.3. Dihydrofolate was not a substrate for DmrA at the physiological pH of 6.8. While the existence of an H 2 MPT reductase has been proposed previously, this is the first biochemical evidence for such an enzyme in any organism, including archaea. Curiously, no DmrA homologs have been identified in the genomes of known methanogenic archaea, suggesting that bacteria and archaea produce two evolutionarily distinct forms of dihydromethanopterin reductase. This may be a consequence of different electron donors, NAD(P)H versus reduced F 420 , used, respectively, in bacteria and methanogenic archaea.

An enzymatic assay was developed to measure tetrahydromethanopterin (H 4 MPT) levels in wild-type and mutant cells of Methylobacterium extorquens AM1. H 4 MPT was detectable in wild-type cells but not in strains with a mutation of either the orf4 or the dmrA gene, suggesting a role for these two genes in H 4 MPT biosynthesis. The protein encoded by orf4 catalyzed the reaction of ribofuranosylaminobenzene 5′-phosphate synthase, the first committed step of H 4 MPT biosynthesis. These results provide the first biochemical evidence for H 4 MPT biosynthesis genes in bacteria.

In methylotrophic bacteria, formaldehyde is an important but potentially toxic metabolic intermediate that can be assimilated into biomass or oxidized to yield energy. Previously reported was the purification of an NAD(P)(+)-dependent formaldehyde dehydrogenase (FDH) from the obligate methane-oxidizing methylotroph Methylococcus capsulatus (Bath), presumably important in formaldehyde oxidation, which required a heat-stable factor (known as the modifin) for FDH activity. Here, the major protein component of this FDH preparation was shown by biophysical techniques to comprise subunits of 64 and 8 kDa in an alpha(2)beta(2) arrangement. N-terminal sequencing of the subunits of FDH, together with enzymological characterization, showed that the alpha(2)beta(2) tetramer was a quinoprotein methanol dehydrogenase of the type found in other methylotrophs. The FDH preparations were shown to contain a highly active NAD(P)(+)-dependent methylene tetrahydromethanopterin dehydrogenase that was the probable source of the NAD(P)(+)-dependent formaldehyde oxidation activity. These results support previous findings that methylotrophs possess multiple pathways for formaldehyde dissimilation.

The classic scheme of energy metabolism during methylotrophic growth involves a formate oxidation step except in strains in which all formaldehyde is oxidized in the cyclic ribulose monophosphate cycle (1). Formate dehydrogenase (FDH) activity has been detected in most methylotrophs (3, 10, 13, 15, 22, 42), and a few FDHs have been purified and analyzed (reviewed in reference 39). In the methylotrophic yeast Candida boidinii, the FDH step was shown not to be essential for methylotrophic growth, but FDH mutants showed reduced growth on methanol (32). However, as the complete C. boidinii genome sequence is not available, the presence of other FDHs is not excluded. Mutant-based analysis of the role of the FDH step in C1 oxidation has not yet been attempted in methylotrophic bacteria. M. extorquens AM1 offers a convenient model to study this question. It possesses two pathways in which formaldehyde can be oxidized to formate (Fig. ​(Fig.1),1), one linked to tetrahydromethanopterin (H4MPT) and another linked to tetrahydrofolate (H4F) (5, 6). The enzymes involved in the two pathways have been studied in detail, and current evidence suggests that the main pathway for oxidizing formaldehyde is the H4MPT-linked pathway (reviewed in reference 37). It has been demonstrated recently that this pathway produces formate as an intermediate, a result of a formylmethanofuran transferase/hydrolase reaction (29), and thus in this pathway one molecule of formate is formed in M. extorquens AM1 per oxidized molecule of a C1 substrate, such as methanol or methylamine. This formate is subsequently oxidized to CO2, presumably by FDH (Fig. ​(Fig.11). FIG. 1. C1 metabolism of M. extorquens AM1. H4MPT, tetrahydromethanopterin; H4F, tetrahydrofolate; Fae, H4MPT-dependent formaldehyde activating enzyme (39); MtdA, NADP-dependent methylene-H4MPT dehydrogenase (8, 38); MtdB, NAD(P)-dependent methylene-H4MPT dehydrogenase ... An FDH from M. extorquens AM1 has recently been purified and characterized and shown to be a novel, tungsten-containing FDH encoded by two genes, fdh1AB (20). In this study we identified two new regions in the M. extorquens AM1 chromosome coding for two additional FDH enzymes. Using mutation analysis, we demonstrate that all three enzymes are expressed during growth on C1 compounds but none is essential for growth on methanol, providing new insight into the energetics of C1 metabolism in serine cycle methylotrophs.

The serine cycle methylotroph Methylobacterium extorquens AM1 contains two pterin-dependent pathways for C 1 transfers, the tetrahydrofolate (H 4 F) pathway and the tetrahydromethanopterin (H 4 MPT) pathway, and both are required for growth on C 1 compounds. With the exception of formate-tetrahydrofolate ligase (FtfL, alternatively termed formyl-H 4 F synthetase), all of the genes encoding the enzymes comprising these two pathways have been identified, and the corresponding gene products have been purified and characterized. We present here the purification and characterization of FtfL from M. extorquens AM1 and the confirmation that this enzyme is encoded by an ftfL homolog identified previously through transposon mutagenesis. Phenotypic analyses of the ftfL mutant strain demonstrated that FtfL activity is required for growth on C 1 compounds. Unlike mutants defective for the H 4 MPT pathway, the ftfL mutant strain does not exhibit phenotypes indicative of defective formaldehyde oxidation. Furthermore, the ftfL mutant strain remained competent for wild-type conversion of [ 14 C]methanol to [ 14 C]CO 2 . Collectively, these data confirm our previous presumptions that the H 4 F pathway is not the key formaldehyde oxidation pathway in M. extorquens AM1. Rather, our data suggest an alternative model for the role of the H 4 F pathway in this organism in which it functions to convert formate to methylene H 4 F for assimilatory metabolism.

The facultative methylotroph Methylobacterium extorquens AM1 possesses two pterin-dependent pathways for C 1 transfer between formaldehyde and formate, the tetrahydrofolate (H 4 F)-linked pathway and the tetrahydromethanopterin (H 4 MPT)-linked pathway. Both pathways are required for growth on C 1 substrates; however, mutants defective for the H 4 MPT pathway reveal a unique phenotype of being inhibited by methanol during growth on multicarbon compounds such as succinate. It has been previously proposed that this methanol-sensitive phenotype is due to the inability to effectively detoxify formaldehyde produced from methanol. Here we present a comparative physiological characterization of four mutants defective in the H 4 MPT pathway and place them into three different phenotypic classes that are concordant with the biochemical roles of the respective enzymes. We demonstrate that the analogous H 4 F pathway present in M. extorquens AM1 cannot fulfill the formaldehyde detoxification function, while a heterologously expressed pathway linked to glutathione and NAD + can successfully substitute for the H 4 MPT pathway. Additionally, null mutants were generated in genes previously thought to be essential, indicating that the H 4 MPT pathway is not absolutely required during growth on multicarbon compounds. These results define the role of the H 4 MPT pathway as the primary formaldehyde oxidation and detoxification pathway in M. extorquens AM1.

Proteins in the ATP-grasp superfamily of amide bond-forming ligases have evolved to function in a number of unrelated biosynthetic pathways. Previously identified homologs encoding glutathione synthetase, d -alanine: d -alanine ligase and the bacterial ribosomal protein S6:glutamate ligase have been vertically inherited within certain organismal lineages. Although members of this specificity-diverse superfamily share a common reaction mechanism, the nonoverlapping set of amino acid and peptide substrates recognized by each family provided few clues as to their evolutionary history. Two members of this family have been identified in the hyperthermophilic marine archaeon Methanococcus jannaschii and shown to catalyze the final reactions in two coenzyme biosynthetic pathways. The MJ0620 ( mptN ) locus encodes a tetrahydromethanopterin:α- l -glutamate ligase that forms tetrahydrosarcinapterin, a single carbon-carrying coenzyme. The MJ1001 ( cofF ) locus encodes a γ-F 420 -2:α- l -glutamate ligase, which caps the γ-glutamyl tail of the hydride carrier coenzyme F 420 . These two genes share a common ancestor with the ribosomal protein S6:glutamate ligase and a putative α-aminoadipate ligase, defining the first group of ATP-grasp enzymes with a shared amino acid substrate specificity. As in glutathione biosynthesis, two unrelated amino acid ligases catalyze sequential reactions in coenzyme F 420 polyglutamate formation: a γ-glutamyl ligase adds 1–3 l -glutamate residues and the ATP-grasp-type ligase described here caps the chain with a single α-linked l -glutamate residue. The analogous pathways for glutathione, F 420 , folate, and murein peptide biosyntheses illustrate convergent evolution of nonribosomal peptide biosynthesis through the recruitment of single-step amino acid ligases.

Ten novel methylotrophy genes of the facultative methylotroph Methylobacterium extorquens AM1 were identified from a transposon mutagenesis screen. One of these genes encodes a product having identity with dihydrofolate reductase (DHFR). This mutant has a C 1 -defective and methanol-sensitive phenotype that has previously only been observed for strains defective in tetrahydromethanopterin (H 4 MPT)-dependent formaldehyde oxidation. These results suggest that this gene, dmrA , may encode dihydromethanopterin reductase, an activity analogous to that of DHFR that is required for the final step of H 4 MPT biosynthesis.

Tetrahydromethanopterin (H4MPT) is a tetrahydrofolate analog originally discovered in methanogenic archaea, but later found in other archaea and bacteria. The extent to which H4MPT occurs among living organisms is unknown. The key enzyme which distinguishes the biosynthetic pathways of H4MPT and tetrahydrofolate is ribofuranosylaminobenzene 5'-phosphate synthase (RFAP synthase). Given the importance of RFAP synthase in H4MPT biosynthesis, the identification of putative RFAP synthase genes and measurement of RFAP synthase activity would provide an indication of the presence of H4MPT in untested microorganisms. Investigation of putative archaeal RFAP synthase genes has been hampered by the tendency of the resulting proteins to form inactive inclusion bodies in Escherichia coli. The current work describes a colorimetric assay for measuring RFAP synthase activity, and two modified procedures for expressing recombinant RFAP synthase genes to produce soluble, active enzyme. By lowering the incubation temperature during expression, RFAP synthase from Archaeoglobus fulgidus was produced in E. coli and purified to homogeneity. The production of active RFAP synthase from Methanothermobacter thermautotrophicus was achieved by coexpression of the gene MTH0830 with a molecular chaperone. This is the first direct biochemical identification of a methanogen gene that codes for an active RFAP synthase.

NADP-dependent methylene-H 4 MPT dehydrogenase, MtdA, from Methylobacterium extorquens AM1 catalyzes the dehydrogenation of methylene-tetrahydromethanopterin and methylene-tetrahydrofolate with NADP + as cosubstrate. The X-ray structure of MtdA with and without NADP bound was established at 1.9 A resolution. The enzyme is present as a homotrimer. The α,β fold of the monomer is related to that of methylene-H 4 F dehydrogenases, suggesting a common evolutionary origin. The position of the active site is located within a large crevice built up by the two domains of one subunit and one domain of a second subunit. Methylene-H 4 MPT could be modeled into the cleft, and crucial active site residues such as Phe18, Lys256, His260, and Thr102 were identified. The molecular basis of the different substrate specificities and different catalytic demands of MtdA compared to methylene-H 4 F dehydrogenases are discussed.

Biogenic methane production is dominated by methanoarchaea of the genera Methanosarcina (Ms.) and Methanosaeta (Mt.) that grow on acetate (6). Interestingly, Methanosaeta species can use only acetate as a substrate and are therefore obligate aceticlastic methanogens. Members of this genus are of special importance for the productivity of biogas plants, especially for reactor performance and stability at low acetate concentrations. To optimize biomethanation, it is necessary to acquire a comprehensive understanding of the biochemistry of acetate-dependent methanogenesis. Energy conservation in Methanosaeta species is not well understood, and even the sequencing of the Methanosaeta thermophila genome (13) did not unravel its mechanism. Comparative genomics indicated that the core methanogenic pathway, the breakdown of acetylcoenzyme A (CoA) to methane, is obviously well conserved in Mt. thermophila. It can be concluded that acetate is activated by acetyl-CoA synthetases and the resulting acetyl-CoA serves as a substrate for a CO dehydrogenase/acetyl-CoA synthase (CODH/ACS) that oxidizes the carbonyl group to CO 2 and reduces ferredoxin. The methyl group is first transferred to tetrahydromethanopterin and then to coenzyme M (CoM) (2

Methylotrophs grow on reduced single-carbon compounds like methylamine as the sole source of carbon and energy. In Methylobacterium extorquens AM1, the best-studied aerobic methylotroph, a periplasmic methylamine dehydrogenase that catalyzes the primary oxidation of methylamine to formaldehyde has been examined in great detail. However, recent metagenomic data from natural ecosystems are revealing the abundance and importance of lesser-known routes, such as the N -methylglutamate pathway, for methylamine oxidation. In this study, we used M. extorquens PA1, a strain that is closely related to M. extorquens AM1 but is lacking methylamine dehydrogenase, to dissect the genetics and physiology of the ecologically relevant N -methylglutamate pathway for methylamine oxidation. Phenotypic analyses of mutants with null mutations in genes encoding enzymes of the N -methylglutamate pathway suggested that γ-glutamylmethylamide synthetase is essential for growth on methylamine as a carbon source but not as a nitrogen source. Furthermore, analysis of M. extorquens PA1 mutants with defects in methylotrophy-specific dissimilatory and assimilatory modules suggested that methylamine use via the N -methylglutamate pathway requires the tetrahydromethanopterin (H 4 MPT)-dependent formaldehyde oxidation pathway but not a complete tetrahydrofolate (H 4 F)-dependent formate assimilation pathway. Additionally, we present genetic evidence that formaldehyde-activating enzyme (FAE) homologs might be involved in methylotrophy. Null mutants of FAE and homologs revealed that FAE and FAE2 influence the growth rate and FAE3 influences the yield during the growth of M. extorquens PA1 on methylamine.

The availability of thousands of sequenced genomes has revealed the diversity of biochemical solutions to similar chemical problems. Even for molecules at the heart of metabolism, such as cofactors, the pathway enzymes first discovered in model organisms like Escherichia coli or Saccharomyces cerevisiae are often not universally conserved. Tetrahydrofolate (THF) (or its close relative tetrahydromethanopterin) is a universal and essential C1-carrier that most microbes and plants synthesize de novo. The THF biosynthesis pathway and enzymes are, however, not universal and alternate solutions are found for most steps, making this pathway a challenge to annotate automatically in many genomes. Comparing THF pathway reconstructions and functional annotations of a chosen set of folate synthesis genes in specific prokaryotes revealed the strengths and weaknesses of different microbial annotation platforms. This analysis revealed that most current platforms fail in metabolic reconstruction of variant pathways. However, all the pieces are in place to quickly correct these deficiencies if the different databases were built on each other's strengths.

1 Methylobacterium extorquens AM1 possesses a formaldehyde-oxidation pathway that involves enzymes with high sequence identity with enzymes from methanogenic and sulfate-reducing archaea. Here we describe the purification and characterization of formylmethanofuran–tetrahydromethanopterin formyltransferase (Ftr), which catalyzes the reversible formation of formylmethanofuran (formylMFR) and tetrahydromethanopterin (H4MPT) from N5-formylH4MPT and methanofuran (MFR). Formyltransferase from M. extorquens AM1 showed activity with MFR and H4MPT isolated from the methanogenic archaeon Methanothermobacter marburgensis (apparent Km for formylMFR = 50 µm; apparent Km for H4MPT = 30 µm). The enzyme is encoded by the ffsA gene and exhibits a sequence identity of ≈ 40% with Ftr from methanogenic and sulfate-reducing archaea. The 32-kDa Ftr protein from M. extorquens AM1 copurified in a complex with three other polypeptides of 60 kDa, 37 kDa and 29 kDa. Interestingly, these are encoded by the genes orf1, orf2 and orf3 which show sequence identity with the formylMFR dehydrogenase subunits FmdA, FmdB and FmdC, respectively. The clustering of the genes orf2, orf1, ffsA, and orf3 in the chromosome of M. extorquens AM1 indicates that, in the bacterium, the respective polypeptides form a functional unit. Expression studies in Escherichia coli indicate that Ftr requires the other subunits of the complex for stability. Despite the fact that three of the polypeptides of the complex showed sequence similarity to subunits of Fmd from methanogens, the complex was not found to catalyze the oxidation of formylMFR. Detailed comparison of the primary structure revealed that Orf2, the homolog of the active site harboring subunit FmdB, lacks the binding motifs for the active-site cofactors molybdenum, molybdopterin and a [4Fe−4S] cluster. Cytochrome c was found to be spontaneously reduced by H4MPT. On the basis of this property, a novel assay for Ftr activity and MFR is described.