Tetrahydromethanopterin, a carbon carrier in methanogenesis

Model Organisms To Study Methanogenesis, a Uniquely Archaeal Metabolism

Methanogenic archaea are the only organisms that produce CH4 as part of their energy-generating metabolism. They are ubiquitous in oxidant-depleted, anoxic environments such as aquatic sediments, anaerobic digesters, inundated agricultural fields, the rumen of cattle, and the hindgut of termites, where they catalyze the terminal reactions in the degradation of organic matter. Methanogenesis is the only metabolism that is restricted to members of the domain Archaea. Here, we discuss the importance of model organisms in the history of methanogen research, including their role in the discovery of the archaea and in the biochemical and genetic characterization of methanogenesis. We also discuss outstanding questions in the field and newly emerging model systems that will expand our understanding of this uniquely archaeal metabolism.

Highlighting the Unique Roles of Radical S-Adenosylmethionine Enzymes in Methanogenic Archaea

Radical S-adenosylmethionine (SAM) enzymes catalyze an impressive variety of difficult biochemical reactions in various pathways across all domains of life. These metalloenzymes employ a reduced [4Fe-4S] cluster and SAM to generate a highly reactive 5'-deoxyadenosyl radical that is capable of initiating catalysis on otherwise unreactive substrates. Interestingly, the genomes of methanogenic archaea encode many unique radical SAM enzymes with underexplored or completely unknown functions. These organisms are responsible for the yearly production of nearly 1 billion tons of methane, a potent greenhouse gas as well as a valuable energy source. Thus, understanding the details of methanogenic metabolism and elucidating the functions of essential enzymes in these organisms can provide insights into strategies to decrease greenhouse gas emissions as well as inform advances in bioenergy production processes. This minireview provides an overview of the current state of the field regarding the functions of radical SAM enzymes in methanogens and discusses gaps in knowledge that should be addressed.

Deconstructing Methanosarcina acetivorans into an acetogenic archaeon

The reductive acetyl-coenzyme A (acetyl-CoA) pathway is the only carbon fixation pathway that can also be used for energy conservation like it is known for acetogenic bacteria. In methanogenic archaea, this pathway is extended with one route toward acetyl-CoA formation for anabolism and another route toward methane formation for catabolism. Which of these traits is ancestral in evolution has not been resolved. By diverging virtually all substrate carbon from methanogenesis to flow through acetyl-CoA, Methanosarcina acetivorans can be converted to an acetogenic organism. Being able to deconstruct methanogenic into the seemingly simpler acetogenic energy metabolism provides compelling evidence that methanogens are not nearly as metabolically limited as previously thought and suggests that methanogenesis might have evolved from the acetyl-CoA pathway.

The reductive acetyl-coenzyme A (acetyl-CoA) pathway, whereby carbon dioxide is sequentially reduced to acetyl-CoA via coenzyme-bound C1 intermediates, is the only autotrophic pathway that can at the same time be the means for energy conservation. A conceptually similar metabolism and a key process in the global carbon cycle is methanogenesis, the biogenic formation of methane. All known methanogenic archaea depend on methanogenesis to sustain growth and use the reductive acetyl-CoA pathway for autotrophic carbon fixation. Here, we converted a methanogen into an acetogen and show that Methanosarcina acetivorans can dispense with methanogenesis for energy conservation completely. By targeted disruption of the methanogenic pathway, followed by adaptive evolution, a strain was created that sustained growth via carbon monoxide–dependent acetogenesis. A minute flux (less than 0.2% of the carbon monoxide consumed) through the methane-liberating reaction remained essential, indicating that currently living methanogens utilize metabolites of this reaction also for anabolic purposes. These results suggest that the metabolic flexibility of methanogenic archaea might be much greater than currently known. Also, our ability to deconstruct a methanogen into an acetogen by merely removing cellular functions provides experimental support for the notion that methanogenesis could have evolved from the reductive acetyl-coenzyme A pathway.

Methanogenic archaea use a bacteria-like methyltransferase system to demethoxylate aromatic compounds

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.

Substrate Specificity Analysis of Dihydrofolate/Dihydromethanopterin Reductase Homologs in Methylotrophic α-Proteobacteria

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 M. 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 Escherichia 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.

Hydrogenase Enzymes and Their Synthetic Models: The Role of Metal Hydrides

Hydrogenase enzymes efficiently process H2 and protons at organometallic FeFe, NiFe, or Fe active sites. Synthetic modeling of the many H2ase states has provided insight into H2ase structure and mechanism, as well as afforded catalysts for the H2 energy vector. Particularly important are hydride-bearing states, with synthetic hydride analogues now known for each hydrogenase class. These hydrides are typically prepared by protonation of low-valent cores. Examples of FeFe and NiFe hydrides derived from H2 have also been prepared. Such chemistry is more developed than mimicry of the redox-inactive monoFe enzyme, although functional models of the latter are now emerging. Advances in physical and theoretical characterization of H2ase enzymes and synthetic models have proven key to the study of hydrides in particular, and will guide modeling efforts toward more robust and active species optimized for practical applications.

Metabolic processes of Methanococcus maripaludis and potential applications

Methanococcus maripaludis is a rapidly growing, fully sequenced, genetically tractable model organism among hydrogenotrophic methanogens. It has the ability to convert CO2 and H2 into a useful cleaner energy fuel (CH4). In fact, this conversion enhances in the presence of free nitrogen as the sole nitrogen source due to prolonged cell growth. Given the global importance of GHG emissions and climate change, diazotrophy can be attractive for carbon capture and utilization applications from appropriately treated flue gases, where surplus hydrogen is available from renewable electricity sources. In addition, M. maripaludis can be engineered to produce other useful products such as terpenoids, hydrogen, methanol, etc. M. maripaludis with its unique abilities has the potential to be a workhorse like Escherichia coli and S. cerevisiae for fundamental and experimental biotechnology studies. More than 100 experimental studies have explored different specific aspects of the biochemistry and genetics of CO2 and N2 fixation by M. maripaludis. Its genome-scale metabolic model (iMM518) also exists to study genetic perturbations and complex biological interactions. However, a comprehensive review describing its cell structure, metabolic processes, and methanogenesis is still lacking in the literature. This review fills this crucial gap. Specifically, it integrates distributed information from the literature to provide a complete and detailed view for metabolic processes such as acetyl-CoA synthesis, pyruvate synthesis, glycolysis/gluconeogenesis, reductive tricarboxylic acid (RTCA) cycle, non-oxidative pentose phosphate pathway (NOPPP), nitrogen metabolism, amino acid metabolism, and nucleotide biosynthesis. It discusses energy production via methanogenesis and its relation to metabolism. Furthermore, it reviews taxonomy, cell structure, culture/storage conditions, molecular biology tools, genome-scale models, and potential industrial and environmental applications. Through the discussion, it develops new insights and hypotheses from experimental and modeling observations, and identifies opportunities for further research and applications.

Physiology, Biochemistry, and Applications of F420- and Fo-Dependent Redox Reactions

5-Deazaflavin cofactors enhance the metabolic flexibility of microorganisms by catalyzing a wide range of challenging enzymatic redox reactions. While structurally similar to riboflavin, 5-deazaflavins have distinctive and biologically useful electrochemical and photochemical properties as a result of the substitution of N-5 of the isoalloxazine ring for a carbon. 8-Hydroxy-5-deazaflavin (Fo) appears to be used for a single function: as a light-harvesting chromophore for DNA photolyases across the three domains of life. In contrast, its oligoglutamyl derivative F420 is a taxonomically restricted but functionally versatile cofactor that facilitates many low-potential two-electron redox reactions. It serves as an essential catabolic cofactor in methanogenic, sulfate-reducing, and likely methanotrophic archaea. It also transforms a wide range of exogenous substrates and endogenous metabolites in aerobic actinobacteria, for example mycobacteria and streptomycetes. In this review, we discuss the physiological roles of F420 in microorganisms and the biochemistry of the various oxidoreductases that mediate these roles. Particular focus is placed on the central roles of F420 in methanogenic archaea in processes such as substrate oxidation, C1 pathways, respiration, and oxygen detoxification. We also describe how two F420-dependent oxidoreductase superfamilies mediate many environmentally and medically important reactions in bacteria, including biosynthesis of tetracycline and pyrrolobenzodiazepine antibiotics by streptomycetes, activation of the prodrugs pretomanid and delamanid by Mycobacterium tuberculosis, and degradation of environmental contaminants such as picrate, aflatoxin, and malachite green. The biosynthesis pathways of Fo and F420 are also detailed. We conclude by considering opportunities to exploit deazaflavin-dependent processes in tuberculosis treatment, methane mitigation, bioremediation, and industrial biocatalysis.

The One-carbon Carrier Methylofuran from Methylobacterium extorquens AM1 Contains a Large Number of α- and γ-Linked Glutamic Acid Residues

Methylobacterium extorquens AM1 uses dedicated cofactors for one-carbon unit conversion. Based on the sequence identities of enzymes and activity determinations, a methanofuran analog was proposed to be involved in formaldehyde oxidation in Alphaproteobacteria. Here, we report the structure of the cofactor, which we termed methylofuran. Using an in vitro enzyme assay and LC-MS, methylofuran was identified in cell extracts and further purified. From the exact mass and MS-MS fragmentation pattern, the structure of the cofactor was determined to consist of a polyglutamic acid side chain linked to a core structure similar to the one present in archaeal methanofuran variants. NMR analyses showed that the core structure contains a furan ring. However, instead of the tyramine moiety that is present in methanofuran cofactors, a tyrosine residue is present in methylofuran, which was further confirmed by MS through the incorporation of a (13)C-labeled precursor. Methylofuran was present as a mixture of different species with varying numbers of glutamic acid residues in the side chain ranging from 12 to 24. Notably, the glutamic acid residues were not solely γ-linked, as is the case for all known methanofurans, but were identified by NMR as a mixture of α- and γ-linked amino acids. Considering the unusual peptide chain, the elucidation of the structure presented here sets the basis for further research on this cofactor, which is probably the largest cofactor known so far.

Auxiliary iron-sulfur cofactors in radical SAM enzymes

A vast number of enzymes are now known to belong to a superfamily known as radical SAM, which all contain a [4Fe-4S] cluster ligated by three cysteine residues. The remaining, unligated, iron ion of the cluster binds in contact with the α-amino and α-carboxylate groups of S-adenosyl-l-methionine (SAM). This binding mode facilitates inner-sphere electron transfer from the reduced form of the cluster into the sulfur atom of SAM, resulting in a reductive cleavage of SAM to methionine and a 5'-deoxyadenosyl radical. The 5'-deoxyadenosyl radical then abstracts a target substrate hydrogen atom, initiating a wide variety of radical-based transformations. A subset of radical SAM enzymes contains one or more additional iron-sulfur clusters that are required for the reactions they catalyze. However, outside of a subset of sulfur insertion reactions, very little is known about the roles of these additional clusters. This review will highlight the most recent advances in the identification and characterization of radical SAM enzymes that harbor auxiliary iron-sulfur clusters. This article is part of a Special Issue entitled: Fe/S proteins: Analysis, structure, function, biogenesis and diseases.

Role of a putative tungsten-dependent formylmethanofuran dehydrogenase in Methanosarcina acetivorans

Methanogenesis, the biological production of methane, is the sole means for energy conservation for methanogenic archaea. Among the few methanogens shown to grow on carbon monoxide (CO) is Methanosarcina acetivorans, which produces, beside methane, acetate and formate in the process. Since CO-dependent methanogenesis proceeds via formation of formylmethanofuran from CO2 and methanofuran, catalyzed by formylmethanofuran dehydrogenase, we were interested whether this activity could participate in the formate formation from CO. The genome of M. acetivorans encodes four putative formylmethanofuran dehydrogenases, two annotated as molybdenum-dependent and the remaining two as tungsten-dependent enzymes. A mutant lacking one of the putative tungsten enzymes grew very slowly on CO and only after a prolonged adaptation period, which suggests an important role for this isoform during growth on CO. Methanol- and CO-dependent growth of the mutant required the presence of molybdenum indicating an indispensable function of this metal in the remaining isoforms. CO-dependent formate formation could not be observed in the mutant indicating involvement of the respective isoform in the process. However, addition of formaldehyde, which spontaneously reacts with tetrahydrosarcinapterin (H4SPT) to methenyl-H4SPT, led to near-wild-type formate production rates, which argues for an alternative route of formate formation in this organism.

Methylobacterium extorquens: methylotrophy and biotechnological applications

Methylotrophy is the ability to use reduced one-carbon compounds, such as methanol, as a single source of carbon and energy. Methanol is, due to its availability and potential for production from renewable resources, a valuable feedstock for biotechnology. Nature offers a variety of methylotrophic microorganisms that differ in their metabolism and represent resources for engineering of value-added products from methanol. The most extensively studied methylotroph is the Alphaproteobacterium Methylobacterium extorquens. Over the past five decades, the metabolism of M. extorquens has been investigated physiologically, biochemically, and more recently, using complementary omics technologies such as transcriptomics, proteomics, metabolomics, and fluxomics. These approaches, together with a genome-scale metabolic model, facilitate system-wide studies and the development of rational strategies for the successful generation of desired products from methanol. This review summarizes the knowledge of methylotrophy in M. extorquens, as well as the available tools and biotechnological applications.

Identification of a unique radical S-adenosylmethionine methylase likely involved in methanopterin biosynthesis in Methanocaldococcus jannaschii

Methanopterin (MPT) and its analogs are coenzymes required for methanogenesis and methylotrophy in specialized microorganisms. The methyl groups at C-7 and C-9 of the pterin ring distinguish MPT from all other pterin-containing natural products. However, the enzyme(s) responsible for the addition of these methyl groups has yet to be identified. Here we demonstrate that a putative radical S-adenosyl-L-methionine (SAM) enzyme superfamily member encoded by the MJ0619 gene in the methanogen Methanocaldococcus jannaschii is likely this missing methylase. When MJ0619 was heterologously expressed in Escherichia coli, various methylated pterins were detected, consistent with MJ0619 catalyzing methylation at C-7 and C-9 of 7,8-dihydro-6-hydroxymethylpterin, a common intermediate in both folate and MPT biosynthesis. Site-directed mutagenesis of Cys77 present in the first of two canonical radical SAM CX₃CX₂C motifs present in MJ0619 did not inhibit C-7 methylation, while mutation of Cys102, found in the other radical SAM amino acid motif, resulted in the loss of C-7 methylation, suggesting that the first motif could be involved in C-9 methylation, while the second motif is required for C-7 methylation. Further experiments demonstrated that the C-7 methyl group is not derived from methionine and that methylation does not require cobalamin. When E. coli cells expressing MJ0619 were grown with deuterium-labeled acetate as the sole carbon source, the resulting methyl group on the pterin was predominantly labeled with three deuteriums. Based on these results, we propose that this archaeal radical SAM methylase employs a previously uncharacterized mechanism for methylation, using methylenetetrahydrofolate as a methyl group donor.

Biochemical fossils of the ancient transition from geoenergetics to bioenergetics in prokaryotic one carbon compound metabolism

The deep dichotomy of archaea and bacteria is evident in many basic traits including ribosomal protein composition, membrane lipid synthesis, cell wall constituents, and flagellar composition. Here we explore that deep dichotomy further by examining the distribution of genes for the synthesis of the central carriers of one carbon units, tetrahydrofolate (H4F) and tetrahydromethanopterin (H4MPT), in bacteria and archaea. The enzymes underlying those distinct biosynthetic routes are broadly unrelated across the bacterial-archaeal divide, indicating that the corresponding pathways arose independently. That deep divergence in one carbon metabolism is mirrored in the structurally unrelated enzymes and different organic cofactors that methanogens (archaea) and acetogens (bacteria) use to perform methyl synthesis in their H4F- and H4MPT-dependent versions, respectively, of the acetyl-CoA pathway. By contrast, acetyl synthesis in the acetyl-CoA pathway - from a methyl group, CO2 and reduced ferredoxin - is simpler, uniform and conserved across acetogens and methanogens, and involves only transition metals as catalysts. The data suggest that the acetyl-CoA pathway, while being the most ancient of known CO2 assimilation pathways, reflects two phases in early evolution: an ancient phase in a geochemically confined and non-free-living universal common ancestor, in which acetyl thioester synthesis proceeded spontaneously with the help of geochemically supplied methyl groups, and a later phase that reflects the primordial divergence of the bacterial and archaeal stem groups, which independently invented genetically-encoded means to synthesize methyl groups via enzymatic reactions. This article is part of a Special Issue entitled: 18th European Bioenergetic Conference.

Discovery and characterization of the first archaeal dihydromethanopterin reductase, an iron-sulfur flavoprotein from Methanosarcina mazei

The microbial production of methane by methanogenic archaea is dependent on the synthesis of the pterin-containing cofactor tetrahydromethanopterin (H4MPT). The enzyme catalyzing the last step of H4MPT biosynthesis (dihydromethanopterin reductase) has not previously been identified in methane-producing microorganisms. Previous complementation studies with the methylotrophic bacterium Methylobacterium extorquens have indicated that an uncharacterized archaeal-flavoprotein-like flavoprotein (AfpA) from Methylobacillus flagellatus or Burkholderia xenovorans can replace the activity of a phylogenetically unrelated bacterial dihydromethanopterin reductase (DmrA). We propose that MM1854, a homolog of AfpA from Methanosarcina mazei, catalyzes the last step of H4MPT biosynthesis in methane-producing microorganisms. To test this hypothesis, a six-histidine (His6)-tagged version of MM1854 was produced. Bioinformatic analysis revealed the presence of one flavin mononucleotide (FMN)-binding site and two iron-sulfur cluster sites, consistent with an oxidoreductase enzyme. Purified His6-MM1854 occurred as a homodimer of 29-kDa subunits, and the UV-visible spectrum of the purified protein showed absorbance peaks at 380 and 460 nm, characteristic of oxidized FMN. NAD(P)H was incapable of directly reducing the flavin cofactor, but dithionite eliminated the FMN peaks, indicating successful electron transfer to MM1854. An electron transfer system of NADPH, spinach NADPH-ferredoxin oxidoreductase, and ferredoxin could also reduce the FMN peaks. A newly developed assay indicated that dithiothreitol-reduced MM1854 could transfer electrons to dihydromethanopterin. This assay was also effective with a heat-stable DmrX analog from Methanocaldococcus jannaschii (MJ0208). These results provide the first biochemical evidence that MM1854 and MJ0208 function as archaeal dihydromethanopterin reductases (DmrX) and that ferredoxin may serve as an electron donor.

Beating the acetyl coenzyme A-pathway to the origin of life

Attempts to draft plausible scenarios for the origin of life have in the past mainly built upon palaeogeochemical boundary conditions while, as detailed in a companion article in this issue, frequently neglecting to comply with fundamental thermodynamic laws. Even if demands from both palaeogeochemistry and thermodynamics are respected, then a plethora of strongly differing models are still conceivable. Although we have no guarantee that life at its origin necessarily resembled biology in extant organisms, we consider that the only empirical way to deduce how life may have emerged is by taking the stance of assuming continuity of biology from its inception to the present day. Building upon this conviction, we have assessed extant types of energy and carbon metabolism for their appropriateness to conditions probably pertaining in those settings of the Hadean planet that fulfil the thermodynamic requirements for life to come into being. Wood-Ljungdahl (WL) pathways leading to acetyl CoA formation are excellent candidates for such primordial metabolism. Based on a review of our present understanding of the biochemistry and biophysics of acetogenic, methanogenic and methanotrophic pathways and on a phylogenetic analysis of involved enzymes, we propose that a variant of modern methanotrophy is more likely than traditional WL systems to date back to the origin of life. The proposed model furthermore better fits basic thermodynamic demands and palaeogeochemical conditions suggested by recent results from extant alkaline hydrothermal seeps.

Elucidation of the role of the methylene-tetrahydromethanopterin dehydrogenase MtdA in the tetrahydromethanopterin-dependent oxidation pathway in Methylobacterium extorquens AM1

The methylotroph Methylobacterium extorquens AM1 oxidizes methanol and methylamine to formaldehyde and subsequently to formate, an intermediate that serves as the branch point between assimilation (formation of biomass) and dissimilation (oxidation to CO₂). The oxidation of formaldehyde to formate is dephosphotetrahydromethanopterin (dH₄MPT) dependent, while the assimilation of carbon into biomass is tetrahydrofolate (H₄F) dependent. This bacterium contains two different enzymes, MtdA and MtdB, both of which are dehydrogenases able to use methylene-dH₄MPT, an intermediate in the oxidation of formaldehyde to formate. Unique to MtdA is a second enzymatic activity with methylene-H₄F. Since methylene-H₄F is the entry point into the biomass pathways, MtdA plays a key role in assimilatory metabolism. However, its role in oxidative metabolism via the dH₄MPT-dependent pathway and its apparent inability to replace MtdB in vivo on methanol growth are not understood. Here, we have shown that an mtdB mutant is able to grow on methylamine, providing a system to study the role of MtdA. We demonstrate that the absence of MtdB results in the accumulation of methenyl-dH₄MPT. Methenyl-dH₄MPT is shown to be a competitive inhibitor of the reduction of methenyl-H₄F to methylene-H₄F catalyzed by MtdA, with an estimated Ki of 10 μM. Thus, methenyl-dH₄MPT accumulation inhibits H₄F-dependent assimilation. Overexpression of mch in the mtdB mutant strain, predicted to reduce methenyl-dH₄MPT accumulation, enhances growth on methylamine. Our model proposes that MtdA regulates carbon flux due to differences in its kinetic properties for methylene-dH₄MPT and for methenyl-H₄F during growth on single-carbon compounds.

A survey of carbon fixation pathways through a quantitative lens

While the reductive pentose phosphate cycle is responsible for the fixation of most of the carbon in the biosphere, it has several natural substitutes. In fact, due to the characterization of three new carbon fixation pathways in the last decade, the diversity of known metabolic solutions for autotrophic growth has doubled. In this review, the different pathways are analysed and compared according to various criteria, trying to connect each of the different metabolic alternatives to suitable environments or metabolic goals. The different roles of carbon fixation are discussed; in addition to sustaining autotrophic growth it can also be used for energy conservation and as an electron sink for the recycling of reduced electron carriers. Our main focus in this review is on thermodynamic and kinetic aspects, including thermodynamically challenging reactions, the ATP requirement of each pathway, energetic constraints on carbon fixation, and factors that are expected to limit the rate of the pathways. Finally, possible metabolic structures of yet unknown carbon fixation pathways are suggested and discussed.

Structural basis of the hydride transfer mechanism in F(420)-dependent methylenetetrahydromethanopterin dehydrogenase

F(420)-dependent methylenetetrahydromethanopterin (methylene-H(4)MPT) dehydrogenase (Mtd) of Methanopyrus kandleri is an enzyme of the methanogenic energy metabolism that catalyzes the reversible hydride transfer between methenyl-H(4)MPT(+) and methylene-H(4)MPT using coenzyme F(420) as hydride carrier. We determined the structures of the Mtd-methylene-H(4)MPT, Mtd-methenyl-H(4)MPT(+), and the Mtd-methenyl-H(4)MPT(+)-F(420)H(2) complexes at 2.1, 2.0, and 1.8 A resolution, respectively. The pterin-imidazolidine-phenyl ring system is present in a new extended but not planar conformation which is virtually identical in methenyl-H(4)MPT(+) and methylene-H(4)MPT at the current resolution. Both substrates methenyl-H(4)MPT(+) and F(420)H(2) bind in a face to face arrangement to an active site cleft, thereby ensuring a direct hydride transfer between their C14a and C5 atoms, respectively. The polypeptide scaffold does not reveal any significant conformational change upon binding of the bulky substrates but in turn changes the conformations of the substrate rings either to avoid clashes between certain ring atoms or to adjust the rings involved in hydride transfer for providing an optimal catalytic efficiency.

Si-face stereospecificity at C5 of coenzyme F420 for F420H2 oxidase from methanogenic Archaea as determined by mass spectrometry

Coenzyme F420 is a 5-deazaflavin. Upon reduction, 1,5 dihydro-coenzyme F420 is formed with a prochiral centre at C5. All the coenzyme F420-dependent enzymes investigated to date have been shown to be Si-face stereospecific with respect to C5 of the deazaflavin, despite most F420-dependent enzymes being unrelated phylogenetically. In this study, we report that the recently discovered F420H2 oxidase from methanogenic Archaea is also Si-face stereospecific. The enzyme was found to catalyse the oxidation of (5S)-[5-2H1]F420H2 with O2 to [5-1H]F420 rather than to [5-2H]F420 as determined by MALDI-TOF MS. (5S)-[5-2H1]F420H2 was generated by stereospecific enzymatic reduction of F420 with (14a-2H2)-[14a-2H2] methylenetetrahydromethanopterin.

How an Enzyme Binds the C1 Carrier Tetrahydromethanopterin

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.

Carbon Monoxide as an Intrinsic Ligand to Iron in the Active Site of the Iron−Sulfur-Cluster-Free Hydrogenase H2-Forming Methylenetetrahydromethanopterin Dehydrogenase As Revealed by Infrared Spectroscopy

The iron-sulfur-cluster-free hydrogenase Hmd (H(2)-forming methylenetetrahydromethanopterin dehydrogenase) from methanogenic archaea has recently been found to contain one iron associated tightly with an extractable cofactor of yet unknown structure. We report here that Hmd contains intrinsic CO bound to the Fe. Chemical analysis of Hmd revealed the presence of 2.4 +/- 0.2 mol of CO/mol of iron. Fourier transform infrared spectra of the native enzyme showed two bands of almost equal intensity at 2011 and 1944 cm(-)(1), interpreted as the stretching frequencies of two CO molecules bound to the same iron in an angle of 90 degrees . We also report on the effect of extrinsic (12)CO, (13)CO, (12)CN(-), and (13)CN(-) on the IR spectrum of Hmd.

Generation of formate by the formyltransferase/hydrolase complex (Fhc) from Methylobacterium extorquens AM1

Methylobacterium extorquens AM1 possesses a formyltransferase (Ftr) complex that is essential for growth in the presence of methanol and involved in formaldehyde oxidation to CO(2). One of the subunits of the complex carries the catalytic site for transfer of the formyl group from tetrahydromethanopterin to methanofuran (MFR). We now found via nuclear magnetic resonance-based studies that the Ftr complex also catalyzes the hydrolysis of formyl-MFR and generates formate. The enzyme was therefore renamed Ftr/hydrolase complex (Fhc). FhcA shares a sequence pattern with amidohydrolases and is assumed to be the catalytic site where the hydrolysis takes place.

Genetic analysis of the archaeon Methanosarcina barkeri Fusaro reveals a central role for Ech hydrogenase and ferredoxin in methanogenesis and carbon fixation

Ech hydrogenase (Ech) from the methanogenic archaeon Methanosarcina barkeri catalyzes the reversible reduction of ferredoxin by H(2) and is a member of a distinct group of membrane-bound [NiFe] hydrogenases with sequence similarity to energy-conserving NADH:quinone oxidoreductase (complex I). To elucidate the physiological role(s) of Ech a mutant lacking this enzyme was constructed. The mutant was unable to grow on methanol/H(2)/CO(2), H(2)/CO(2), or acetate as carbon and energy sources but showed wild-type growth rates with methanol as sole substrate. Addition of pyruvate to the growth medium restored growth on methanol/H(2)/CO(2) but not on H(2)/CO(2) or acetate. Results obtained from growth experiments, cell suspension experiments, and enzyme activity measurements in cell extracts provide compelling evidence for essential functions of Ech and a 2[4Fe-4S] ferredoxin in the metabolism of M. barkeri. The following conclusions were made. (i) In acetoclastic methanogenesis, Ech catalyzes H(2) formation from reduced ferredoxin, generated by the oxidation of the carbonyl group of acetate to CO(2). (ii) Under autotrophic growth conditions, the enzyme catalyzes the energetically unfavorable reduction of ferredoxin by H(2), most probably driven by reversed electron transport, and the reduced ferredoxin thus generated functions as low potential electron donor for the synthesis of pyruvate in an anabolic pathway. (iii) Reduced ferredoxin in addition provides the reducing equivalents for the first step of methanogenesis from H(2)/CO(2), the reduction of CO(2) to formylmethanofuran. Thus, in vivo genetic analysis has led to the identification of the electron donor of this key initial step of methanogenesis.

Characterization of the formyltransferase from Methylobacterium extorquens AM1

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 microM; apparent Km for H4MPT = 30 microM). The enzyme is encoded by the ffsA gene and exhibits a sequence identity of approximately 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.

Re-face stereospecificity of NADP dependent methylenetetrahydromethanopterin dehydrogenase from Methylobacterium extorquens AM1 as determined by NMR spectroscopy

MtdA catalyzes the dehydrogenation of N(5),N(10)-methylenetetrahydromethanopterin (methylene-H4MPT) with NADP(+) as electron acceptor. In the reaction two prochiral centers are involved, C14a of methylene-H4MPT and C4 of NADP(+), between which a hydride is transferred. The two diastereotopic protons at C14a of methylene-H4MPT and at C4 of NADPH can be seen separately in 1H-NMR spectra. This fact was used to determine the stereospecificity of the enzyme. With (14aR)-[14a-2H(1)]-[14a-13C]methylene-H4MPT as the substrate, it was found that the pro-R hydrogen of methylene-H4MPT is transferred by MtdA into the pro-R position of NADPH.

Novel formaldehyde-activating enzyme in Methylobacterium extorquens AM1 required for growth on methanol

Formaldehyde is toxic for all organisms from bacteria to humans due to its reactivity with biological macromolecules. Organisms that grow aerobically on single-carbon compounds such as methanol and methane face a special challenge in this regard because formaldehyde is a central metabolic intermediate during methylotrophic growth. In the alpha-proteobacterium Methylobacterium extorquens AM1, we found a previously unknown enzyme that efficiently catalyzes the removal of formaldehyde: it catalyzes the condensation of formaldehyde and tetrahydromethanopterin to methylene tetrahydromethanopterin, a reaction which also proceeds spontaneously, but at a lower rate than that of the enzyme-catalyzed reaction. Formaldehyde-activating enzyme (Fae) was purified from M. extorquens AM1 and found to be one of the major proteins in the cytoplasm. The encoding gene is located within a cluster of genes for enzymes involved in the further oxidation of methylene tetrahydromethanopterin to CO(2). Mutants of M. extorquens AM1 defective in Fae were able to grow on succinate but not on methanol and were much more sensitive toward methanol and formaldehyde. Uncharacterized orthologs to this enzyme are predicted to be encoded by uncharacterized genes from archaea, indicating that this type of enzyme occurs outside the methylotrophic bacteria.

The metal-free hydrogenase from methanogenic archaea: evidence for a bound cofactor

The hmd gene, which encodes the metal-free hydrogenase in methanogenic archaea, was heterologously expressed in Escherichia coli. The overproduced enzyme was completely inactive. High activity could, however, be induced by the addition of ultrafiltrate from active enzyme denatured in 8 M urea. The active fraction in the ultrafiltrate was heat-labile and migrated on gel filtration columns with an apparent molecular mass well below 1000 Da.

The NADP-dependent methylene tetrahydromethanopterin dehydrogenase in Methylobacterium extorquens AM1

An NADP-dependent methylene tetrahydromethanopterin (H4MPT) dehydrogenase has recently been proposed to be involved in formaldehyde oxidation to CO2 in Methylobacterium extorquens AM1. We report here on the purification of this novel enzyme to apparent homogeneity. Via the N-terminal amino acid sequence, it was identified to be the mtdA gene product. The purified enzyme catalyzed the dehydrogenation of methylene H4MPT with NADP+ rather than with NAD+, with a specific activity of approximately 400 U/mg of protein. It also catalyzed the dehydrogenation of methylene tetrahydrofolate (methylene H4F) with NADP+. With methylene H4F as the substrate, however, the specific activity (26 U/mg) and the catalytic efficiency (Vmax/Km) were approximately 20-fold lower than with methylene H4MPT. Whereas the dehydrogenation of methylene H4MPT (E0 = -390 mV) with NADP+ (E0 = -320 mV) proceeded essentially irreversibly, the dehydrogenation of methylene H4F (E0 = -300 mV) was fully reversible. Comparison of the primary structure of the NADP-dependent dehydrogenase from M. extorquens AM1 with those of methylene H4F dehydrogenases from other bacteria and eucarya and with those of methylene H4MPT dehydrogenases from methanogenic archaea revealed only marginally significant similarity (<15%).

Biochemistry of methanogenesis: a tribute to Marjory Stephenson. 1998 Marjory Stephenson Prize Lecture

Max-Planck-Institut für terrestrische Mikrobiologie, Karl-von-Frisch-Straße, D-35043 Marburg, and Laboratorium für Mikrobiologie, Fachbereich Biologie, Philipps-Universität, Karl-von-Frisch-Straße, D-35032 Marburg, Germany

In 1933, Stephenson & Stickland (1933a) published that they had isolated from river mud, by the single cell technique, a methanogenic organism capable of growth in an inorganic medium with formate as the sole carbon source.

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.

Purine biosynthesis in the domain Archaea without folates or modified folates

The established pathway for the last two steps in purine biosynthesis, the conversion of 5-aminoimidazole-4-carboxamide ribonucleotide (ZMP) to IMP, is known to utilize 10-formyl-tetrahydrofolate as the required C1 donor cofactor. The biosynthetic conversion of ZMP to IMP in three members of the domain Archaea, Methanobacterium thermoautotrophicum deltaH, M. thermoautotrophicum Marburg, and Sulfolobus solfataricus, however, has been demonstrated to occur with only formate and ATP serving as cofactors. Thus, in these archaea, which use methanopterin (MPT) or another modified folate in place of folate as the C1 carrier coenzyme, neither folate nor a modified folate serves as a cofactor for this biosynthetic transformation. It is concluded that archaea, which function with modified folates such as MPT, are able to carry out purine biosynthesis without the involvement of folates or modified folates.

Si-face stereospecificity at C5 of coenzyme F420 for F420-dependent glucose-6-phosphate dehydrogenase from Mycobacterium smegmatis and F420-dependent alcohol dehydrogenase from Methanoculleus thermophilicus

Coenzyme F420 is a 5-deazaflavin. Upon reduction, 1,5-dihydro-coenzyme F420 is formed with a prochiral center at C5. In this study we report that the F420-dependent glucose-6-phosphate dehydrogenase from Mycobacterium smegmatis and the F420-dependent alcohol dehydrogenase from Methanoculleus thermophilicus are Si-face stereospecific with respect to C5 of the 5-deazaflavin. These results were obtained by following the stereochemical course of the reversible incorporation of 3H into F420 from tritium-labeled substrates. Our findings bring to eight the number of coenzyme-F420-dependent enzymes shown to be Si-face stereospecific. No F420-dependent enzyme with Re-face stereospecificity is known. This is noteworthy since coenzyme F420 is functionally similar to pyridine nucleotides for which both Si-face and Re-face specific enzymes have been found.

Purification, properties and primary structure of H2-forming N5 ,N10 -methylenetetrahydromethanopterin dehydrogenase from Methanococcus thermolithotrophicus

H2-Forming N5,N10 -methylenetetrahydromethanopterin dehydrogenase (Hmd) is a novel type of hydrogenase found in methanogenic Achaea that contains neither nickel nor iron-sulfur clusters. The enzyme has previously been characterized from Methanobacterium thermoautotrophicum and from Methanopyrus kandleri. We report here on the purification and properties of the enzyme from Methanococcus thermolithotrophicus. The hmd gene was cloned and sequenced. The results indicate that the enzyme from Mc. thermolithotrophicus is functionally and structurally closely related to the H2-forming methylene tetrahydromethanopterin dehydrogenase from Mb. thermoautotrophicum and Mp. kandleri. From amino acid sequence comparisons of the three enzymes, a phylogenetic tree was deduced that shows branching orders similar to those derived from sequence comparisons of the 16S rRNA of the orders Methanococcales, Methanobacteriales, and Methanopyrales.

dTMP biosynthesis in Archaea

The biosynthesis of dTMP has been studied in cell extracts of two different members of the domain Archaea, Methanosarcina thermophila and Sulfolobus solfataricus. In M. thermophila, the dTMP was formed from dUMP and [methylene-2H2]-5,10-methylenetetrahydrosarcinapterin generated in situ from added [methylene-2H2] formaldehyde and the tetrahydrosarcinapterin present in the cell extract. In S. solfataricus, the 5,10-methyl-enetetrahydro derivative of a synthetic fragment of sulfopterin, the modified folate present in these cells, served as the C1 donor. These data indicate that the Archaea thymidylate synthases carry out the same basic reaction which occurs in other organisms but use the 5,10-methylenetetrahydro derivatives of modified folates as C1 donors.

Oxidation–reduction of methanol, formaldehyde, serine, and formate inMethanosphaera stadtmanaeusing14C short- and long-term labelling

Methanosphaera stadtmanae derives its energy from the reduction by H2of CH3OH, but not CO2, indicating there is a block in the CO2methanogenesis pathway. Both14CH4and14CO2production were detected in whole cells using [14C]formaldehyde or [14C]serine as substrate.14CO2was also observed from [14C]formate in both whole cells and cofactor-depleted cell-free extracts, and NADP-dependent formate dehydrogenase activity was detected. Both formate and serine blocked the formation of14CO2from formaldehyde in whole cells. The results confirmed that enzymes involved in the reduction of carbon from the level of methylene-tetrahydromethanopterin in a common methanogenic pathway and a tetrahydromethanopterin-dependent serine hydroxymethyltransferase were present in this organism. However, the production of14CH4could not be observed from [14C]formate or14CO2plus H2. [14C]Formate was incorporated specifically into histidine and RNA. [14C]Methanol was also found to label rRNA and cytoplasmic proteins, especially corrinoid proteins.Key words: methanogenesis, formate dehydrogenase, formaldehyde oxidation, C1intermediates.

Hydrogen isotope effects in the reactions catalyzed by H2-forming N5,N10-methylenetetrahydromethanopterin dehydrogenase from methanogenic Archaea

H2-forming N5,N10-methylenetetrahydromethanopterin dehydrogenase from methanogenic Archaea, which is a novel hydrogenase containing neither nickel nor iron-sulfur clusters, catalyzes the reversible reduction of N5,N10-methenyltetrahydomethanopterin (CH identical to H4MPT+) with H2 to N5,N10-methylenetetrahydromethanopterin (CH2 = H4MPT) and a proton (delta G degree' = -5.5 kJ/mol). The enzyme also catalyzes a CH identical to H4MPT(+)-dependent H2/H+ exchange. We report here on kinetic deuterium isotope effects in these reactions. When CH identical to H4MPT+ reduction was performed with D2 instead of H2, Vmax and the Km did not change. A primary isotope effect of 1 was found at all pH and temperatures tested and independent of whether H2O or D2O was the solvent. The findings indicate that a step other than the activation of H2 was rate-determining in CH identical to H4MPT+ reduction with H2. This was substantiated by the observation that also the CH identical to H4MPT(+)-dependent H2/H+ exchange reaction did not exhibit an appreciable deuterium isotope effect. Vmax for CH2 = H4MPT dehydrogenation to CH identical to H4MPT+ and H2 was only 2-3 times higher than for CD2 = H4MPT dehydrogenation to CD identical to H4MPT+ and HD. Such a small primary isotope effect indicates that the breakage of the C-H bond in the methylene group of CH2 = H4MPT was only rate-limiting when hydrogen was substituted by a deuterium.

Coenzyme F420-dependent N5,N10-methylenetetrahydromethanopterin reductase (Mer) from Methanobacterium thermoautotrophicum strain Marburg. Cloning, sequencing, transcriptional analysis, and functional expression in Escherichia coli of the mer gene

The gene encoding the F420-dependent N5,N10-methylenetetrahydromethanopterin reductase (Mer), which catalyzes an intermediate step in methanogensis, was cloned and sequenced from the thermophilic Methanobacterium thermoautotrophicum strain Marburg. The gene was identified on a 3.8-kbp BamHI fragment of M. thermoautotrophicum genomic DNA using a homologous probe. The mer gene encoded an acidic protein of 321 amino acids, corresponding to a calculated molecular mass of 33,492 Da. Sequence analysis revealed the presence of a ribosome binding site, a putative promoter, and a possible terminator structure. The size of the mer mRNA was estimated as 1 kb indicating monocistronic transcription. The mer gene was expressed in Escherichia coli yielding an active enzyme of 36 kDa consistent with the apparent molecular mass described for the enzyme from M. thermoautotrophicum. Sequence comparisons revealed similarities between the F420-dependent N5,N10-methylenetetrahydromethanopterin reductase and a F420-dependent reductase involved in lincomycin biosynthesis in Streptomyces lincolnensis.

Re-face specificity at C14a of methylenetetrahydromethanopterin and Si-face specificity at C5 of coenzyme F420 for coenzyme F420-dependent methylenetetrahydromethanopterin dehydrogenase from methanogenic Archaea

Coenzyme F420-dependent methylenetetrahydromethanopterin dehydrogenase from methanogenic Archaea catalyzes the reversible transfer of a hydride ion from C14a of N5,N10-methylenetetrahydromethanopterin to C5 of coenzyme F420. In this study, we report that this hydride transfer proceeds stereospecifically from the Re face at C14a to the Si face at C5. The results were obtained by using chirally 3H-labelled N5,N10-methylenetetrahydromethanopterin generated via Re-face-specific H2-forming N5,N10-methylenetetrahydromethanopterin dehydrogenase and by analyzing reduced coenzyme F420 via Si-face-specific F420-reducing hydrogenase.

Purification and partial characterization of a putative thymidylate synthase from Methanobacterium thermoautotrophicum

A protein catalyzing the tritium exchange of [5-3H]deoxyuridine monophosphate ([5-3H]dUMP) for solvent protons and the dehalogenation of 5-bromo-deoxyuridine monophosphate (Br-dUMP) has been isolated from the methanogenic archaea Methanobacterium thermoautotrophicum. These two activities are well-established side reactions of thymidylate synthase and do not require cofactors. Sodium dodecylsulfate/polyacrylamide gel electrophoresis of the purified enzyme showed a single band with a molecular mass of 27 kDa. The suggested molecular mass of the native protein calculated from sedimentation equilibrium experiments was 33.5 kDa, indicating that the enzyme is a monomer. The pH optima were 9.0 and 7.0 for the exchange reaction and the dehalogenation, respectively. The effects of temperature, salt, reducing agent and inhibitors were determined. The apparent Km for the tritium exchange from [5-3H]dUMP was 7 microM and for the dehalogenation of Br-dUMP was 14 microM. However, thus far, the conditions for dTMP synthesis from dUMP have not yet been established. Incubation of the enzyme with dUMP, tetrahydromethanopterin, a folate analog present in methanogens, and formaldehyde did not yield dTMP. The first 30 amino acids of the amino terminus have been sequenced. However, there is no similarity with any of the thymidylate synthases. Surprisingly, the protein from M. thermoautotrophicum appears to be related to chitin synthases from several organisms.

Si-face stereospecificity at C5 of coenzyme F420 for F420-dependent N5,N10-methylenetetrahydromethanopterin dehydrogenase, F420-dependent N5,N10-methylenetetrahydromethanopterin reductase and F420H2:dimethylnaphthoquinone oxidoreductase

Coenzyme F420-dependent enzymes catalyze the reversible reduction of F420 by stereospecific hydride transfer to C5 of 5-deazaflavin. Two F420-dependent enzymes have been investigated with respect to the stereochemistry of hydride transfer, the F420-dependent NADP reductase and the F420-reducing hydrogenase. Both enzymes were found to be Si-face specific. In this study we report that three additional F420-dependent enzymes are also Si-face specific: N5,N10-methylenetetrahydromethanopterin dehydrogenase, N5,N10-methylenetetrahydromethanopterin reductase and coenzyme F420H2: dimethylnaphthoquinone oxidoreductase (F420H2 dehydrogenase). Thus, all five characterized F420-dependent enzymes are Si-face specific, which is noteworthy since coenzyme F420 is functionally similar to pyridine nucleotides and both Si-face specific and Re-face specific pyridine-nucleotide-dependent enzymes exist.