Purification and properties of the membrane-associated coenzyme F420-reducing hydrogenase from Methanobacterium formicicum

The Fluorescence-Activating and Absorption-Shifting Tag (FAST) Enables Live-Cell Fluorescence Imaging of Methanococcus maripaludis

Live-cell fluorescence imaging of methanogenic archaea has been limited due to the strictly anoxic conditions required for growth and issues with autofluorescence associated with electron carriers in central metabolism. Here, we show that the fluorescence-activating and absorption-shifting tag (FAST) complexed with the fluorogenic ligand 4-hydroxy-3-methylbenzylidene-rhodanine (HMBR) overcomes these issues and displays robust fluorescence in Methanococcus maripaludis. We also describe a mechanism to visualize cells under anoxic conditions using a fluorescence microscope. Derivatives of FAST were successfully applied for protein abundance analysis, subcellular localization analysis, and determination of protein-protein interactions. FAST fusions to both formate dehydrogenase (Fdh) and F₄₂₀-reducing hydrogenase (Fru) displayed increased fluorescence in cells grown on formate-containing medium, consistent with previous studies suggesting the increased abundance of these proteins in the absence of H₂. Additionally, FAST fusions to both Fru and the ATPase associated with the archaellum (FlaI) showed a membrane localization in single cells observed using anoxic fluorescence microscopy. Finally, a split reporter translationally fused to the alpha and beta subunits of Fdh reconstituted a functionally fluorescent molecule in vivo via bimolecular fluorescence complementation. Together, these observations demonstrate the utility of FAST as a tool for studying members of the methanogenic archaea. IMPORTANCE Methanogenic archaea are important members of anaerobic microbial communities where they catalyze essential reactions in the degradation of organic matter. Developing additional tools for studying the cell biology of these organisms is essential to understanding them at a mechanistic level. Here, we show that FAST, in combination with the fluorogenic ligand HMBR, can be used to monitor protein dynamics in live cells of M. maripaludis. The application of FAST holds promise for future studies focused on the metabolism and physiology of methanogenic archaea.

Energy Conservation and Hydrogenase Function in Methanogenic Archaea, in Particular the Genus Methanosarcina

The biological production of methane is vital to the global carbon cycle and accounts for ca. 74% of total methane emissions. The organisms that facilitate this process, methanogenic archaea, belong to a large and phylogenetically diverse group that thrives in a wide range of anaerobic environments. Two main subgroups exist within methanogenic archaea: those with and those without cytochromes. Although a variety of metabolisms exist within this group, the reduction of growth substrates to methane using electrons from molecular hydrogen is, in a phylogenetic sense, the most widespread methanogenic pathway. Methanogens without cytochromes typically generate methane by the reduction of CO₂ with electrons derived from H₂, formate, or secondary alcohols, generating a transmembrane ion gradient for ATP production via an Na⁺-translocating methyltransferase (Mtr). These organisms also conserve energy with a novel flavin-based electron bifurcation mechanism, wherein the endergonic reduction of ferredoxin is facilitated by the exergonic reduction of a disulfide terminal electron acceptor coupled to either H₂ or formate oxidation. Methanogens that utilize cytochromes have a broader substrate range, and can convert acetate and methylated compounds to methane, in addition to the ability to reduce CO₂ Cytochrome-containing methanogens are able to supplement the ion motive force generated by Mtr with an H⁺-translocating electron transport system. In both groups, enzymes known as hydrogenases, which reversibly interconvert protons and electrons to molecular hydrogen, play a central role in the methanogenic process. This review discusses recent insight into methanogen metabolism and energy conservation mechanisms with a particular focus on the genus Methanosarcina.

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.

Characterization of the frhAGB-encoding hydrogenase from a non-methanogenic hyperthermophilic archaeon

The F420-reducing hydrogenase has been known as a key enzyme in methanogenesis. Its homologs have been identified in non-methanogenic hyperthermophilic archaea, including Thermococcus onnurineus NA1, but neither physiological function nor biochemical properties have been reported to date. The enzyme of T. onnurineus NA1 was distinguished from those of other methanogens and the members of the family Desulfurobacteriaceae with respect to the phylogenetic distribution of the α and β subunits, organization of frhAGB genes and conservation of F420-coordinating residues. RT-qPCR and Western blot analyses revealed frhA gene is not silent but is expressed in T. onnurineus NA1 grown in the presence of sulfur, carbon monoxide, or formate. The trimeric enzyme complex was purified to homogeneity via affinity chromatography from T. onnurineus NA1 and exhibited catalytic activity toward the electron acceptors such as viologens and flavins but not the deazaflavin coenzyme F420. This is the first biochemical study on the function of the frhAGB-encoding enzyme from a non-methanogenic archaea.

Proteome analyses of hydrogen-producing hyperthermophilic archaeon Thermococcus onnurineus NA1 in different one-carbon substrate culture conditions

Thermococcus onnurineus NA1, a sulfur-reducing hyperthermophilic archaeon, is capable of H(2)-producing growth, considered to be hydrogenogenic carboxydotrophy. Utilization of formate as a sole energy source has been well studied in T. onnurineus NA1. However, whether formate can be used as its carbon source remains unknown. To obtain a global view of the metabolic characteristics of H(2)-producing growth, a quantitative proteome analysis of T. onnurineus NA1 grown on formate, CO, and starch was performed by combining one-dimensional SDS-PAGE with nano UPLC-MS(E). A total of 587 proteins corresponding to 29.7% of the encoding genes were identified, and the major metabolic pathways (especially energy metabolism) were characterized at the protein level. Expression of glycolytic enzymes was common but more highly induced in starch-grown cells. In contrast, enzymes involved in key steps of the gluconeogenesis and pentose phosphate pathways were strongly up-regulated in formate-grown cells, suggesting that formate could be utilized as a carbon source by T. onnurineus NA1. In accordance with the genomic analysis, comprehensive proteomic analysis also revealed a number of hydrogenase clusters apparently associated with formate metabolism. On the other hand, CODH and CO-induced hydrogenases belonging to the Hyg4-II cluster, as well as sulfhydrogenase-I and Mbx, were prominently expressed during CO culture. Our data suggest that CO can be utilized as a sole energy source for H(2) production via an electron transport mechanism and that CO(2) produced from catabolism or CO oxidation by CODH and CO-induced hydrogenases may subsequently be assimilated into the organic carbon. Overall, proteomic comparison of formate- and CO-grown cells with starch-grown cells revealed that a single carbon compound, such as formate and CO, can be utilized as an efficient substrate to provide cellular carbon and/or energy by T. onnurineus NA1.

How to make a living by exhaling methane

Methane produced in the biosphere is derived from two major pathways. Conversion of the methyl group of acetate to CH(4) in the aceticlastic pathway accounts for at least two-thirds, and reduction of CO(2) with electrons derived from H(2), formate, or CO accounts for approximately one-third. Although both pathways have terminal steps in common, they diverge considerably in the initial steps and energy conservation mechanisms. Steps and enzymes unique to the CO(2) reduction pathway are confined to methanogens and the domain Archaea. On the other hand, steps and enzymes unique to the aceticlastic pathway are widely distributed in the domain Bacteria, the understanding of which has contributed to a broader understanding of prokaryotic biology.

Geochemical constraints on the diversity and activity of H2 -oxidizing microorganisms in diffuse hydrothermal fluids from a basalt- and an ultramafic-hosted vent

Mixing processes of reduced hydrothermal fluids with oxygenated seawater and fluid-rock reactions contribute to the chemical signatures of diffuse venting and likely determine the geochemical constraints on microbial life. We examined the influence of fluid chemistry on microbial diversity and activity by sampling diffuse fluids emanating through mussel beds at two contrasting hydrothermal vents. The H(2) concentration was very low at the basalt-hosted Clueless site, and mixing models suggest O(2) availability throughout much of the habitat. In contrast, effluents from the ultramafic-hosted Quest site were considerably enriched in H(2) , while O(2) is likely limited to the mussel layer. Only two different hydrogenase genes were identified in clone libraries from the H(2) -poor Clueless fluids, but these fluids exhibited the highest H(2) uptake rates in H(2) -spiked incubations (oxic conditions, at 18 °C). In contrast, a phylogenetically diverse H(2) -oxidizing potential was associated with distinct thermal conditions in the H(2) -rich Quest fluids, but under oxic conditions, H(2) uptake rates were extremely low. Significant stimulation of CO(2) fixation rates by H(2) addition was solely illustrated in Quest incubations (P-value <0.02), but only in conjunction with anoxic conditions (at 18 °C). We conclude that the factors contributing toward differences in the diversity and activity of H(2) oxidizers at these sites include H(2) and O(2) availability.

Genome analysis and genome-wide proteomics of Thermococcus gammatolerans, the most radioresistant organism known amongst the Archaea

The genome sequence of Thermococcus gammatolerans, a radioresistant archaeon, is described; a proteomic analysis reveals that radioresistance may be due to unknown DNA repair enzymes.

Background

Thermococcus gammatolerans was isolated from samples collected from hydrothermal chimneys. It is one of the most radioresistant organisms known amongst the Archaea. We report the determination and annotation of its complete genome sequence, its comparison with other Thermococcales genomes, and a proteomic analysis.

Results

T. gammatolerans has a circular chromosome of 2.045 Mbp without any extra-chromosomal elements, coding for 2,157 proteins. A thorough comparative genomics analysis revealed important but unsuspected genome plasticity differences between sequenced Thermococcus and Pyrococcus species that could not be attributed to the presence of specific mobile elements. Two virus-related regions, tgv1 and tgv2, are the only mobile elements identified in this genome. A proteogenome analysis was performed by a shotgun liquid chromatography-tandem mass spectrometry approach, allowing the identification of 10,931 unique peptides corresponding to 951 proteins. This information concurrently validates the accuracy of the genome annotation. Semi-quantification of proteins by spectral count was done on exponential- and stationary-phase cells. Insights into general catabolism, hydrogenase complexes, detoxification systems, and the DNA repair toolbox of this archaeon are revealed through this genome and proteome analysis.

Conclusions

This work is the first archaeal proteome investigation done at the stage of primary genome annotation. This archaeon is shown to use a large variety of metabolic pathways even under a rich medium growth condition. This proteogenomic study also indicates that the high radiotolerance of T. gammatolerans is probably due to proteins that remain to be characterized rather than a larger arsenal of known DNA repair enzymes.

A Methanocaldococcus jannaschii archaeal signature gene encodes for a 5-formaminoimidazole-4-carboxamide-1-beta-D-ribofuranosyl 5'-monophosphate synthetase. A new enzyme in purine biosynthesis

We have identified and characterized a new member of the ATP-grasp enzyme family that catalyzes the ATP- and formate-dependent formylation of 5-aminoimidazole-4-carboxamide-1-beta-D-ribofuranosyl 5'-monophosphate (AICAR) to 5-formaminoimidazole-4-carboxamide-1-beta-D-ribofuranosyl 5'-monophosphate (FAICAR) in the absence of folates. The enzyme, which we designate as PurP, is the product of the Methanocaldococcus jannaschii purP gene (MJ0136), which is a signature gene for Archaea. As is characteristic of reactions catalyzed by this family of enzymes, the other products of the reaction, ADP and P(i), were produced stoichiometrically with the amount of ATP, formate, and AICAR used. Formyl phosphate was found to substitute for ATP and formate in the reaction, yet the methylene analog, phosphonoacetaldehyde, was not an inhibitor or substrate for the reaction. The enzyme, along with PurO, which catalyzes the cyclization of FAICAR to inosine 5'-monophosphate, catalyzes the same overall transformation in purine biosynthesis as is accomplished by PurH in bacteria and eukaryotes. No homology exists between PurH and either PurO or PurP. 1H NMR and gas chromatography-mass spectrometry analysis of an M. jannaschii cell extract showed the presence of free formate that can be used by the enzyme for purine biosynthesis. This formate arises by the reduction of CO2 with hydrogen; this was demonstrated by incorporating 13C into the formate when M. jannaschii cell extracts were incubated with H13CO3- and hydrogen gas. The presence of this signature gene in all of the Archaea indicates the presence of a purine biosynthetic pathway proceeding in the absence of folate coenzymes.

The anabolic pyruvate oxidoreductase from Methanococcus maripaludis

In autotrophic methanogens, pyruvate oxidoreductase (POR) plays a key role in the assimilation of CO(2) and the biosynthesis of organic carbon. This enzyme has been purified to homogeneity, and the genes from Methanococcus maripaludis were sequenced. The purified POR contained five polypeptides with molecular masses of 47, 33, 25, 21.5 and 13 kDa. The N-terminal sequences of four of the polypeptides had high similarity to the subunits commonly associated with this enzyme from other archaea. However, the 21.5-kDa polypeptide had not been previously observed in PORs. Nucleotide sequencing of the gene cluster encoding the POR revealed six open reading frames ( porABCDEF). The genes porABCD corresponded to the subunits previously identified in PORs. On the basis of the N-terminal amino acid sequence, porE encoded the 21.5-kDa polypeptide and contained a high cysteinyl residue content and a motif indicative of a [Fe-S] cluster. porF also had a high sequence similarity to porE, a high cysteinyl residue content, and two [Fe-S] cluster motifs. Homologs to porE were also present in the genomic sequences of the autotrophic methanogens Methanocaldococcus jannaschii and Methanothermobacter thermautotrophicus. Based upon these results, it is proposed that PorE and PorF are components of a specialized system required to transfer low-potential electrons for pyruvate biosynthesis. Some biochemical properties of the purified methanococcal POR were also determined. This unstable enzyme was very sensitive to O(2 )and demonstrated high activity with pyruvate, oxaloacetate, and alpha-ketobutyrate. Methyl viologen, rubredoxin, FMN, and FAD were readily reduced. Activity was also observed with spinach and clostridial ferredoxins and cytochrome c. Coenzyme F(420) was not an electron acceptor for the purified enzyme.

The hyperthermophilic bacterium, Thermotoga maritima, contains an unusually complex iron-hydrogenase: amino acid sequence analyses versus biochemical characterization

The hyperthermophilic bacterium, Thermotoga maritima, grows up to 90 degrees C by fermenting carbohydrates and it disposes of excess reductant by H(2) production. The H(2)-evolving cytoplasmic hydrogenase of this organism was shown to consist of three different subunits of masses 73 (alpha), 68 (beta) and 19 (gamma) kDa and to contain iron as the only metal. The genes encoding the subunits were clustered in a single operon in the order hydC (gamma), hydB (beta), and hydA (alpha). Sequence analyses indicated that: (a) the enzyme is an Fe-S-cluster-containing flavoprotein which uses NADH as an electron donor; and (b) the catalytic Fe-S cluster resides within the alpha-subunit, which is equivalent to the single subunit that constitutes most mesophilic Fe-hydrogenases. The alpha- and beta-subunits of the purified enzyme were separated by chromatography in the presence of 4 M urea. As predicted, the H(2)-dependent methyl viologen reduction activity of the holoenzyme (45-70 U mg(-1)) was retained in the alpha-subunit (130-160 U mg(-1)) after subunit separation. However, the holoenzyme did not contain flavin and neither it nor the alpha-subunit used NAD(P)(H) or T. maritima ferredoxin as an electron carrier. The holoenzyme, but not the alpha-subunit, reduced anthraquinone-2,6-disulfonate (apparent K(m), 690 microM) with H(2). The EPR properties of the reduced holoenzyme, when compared with those of the separated and reduced subunits, indicate the presence of a catalytic 'H-cluster' and three [4Fe-4S] and one [2Fe-2S] cluster in the alpha-subunit, together with one [4Fe-4S] and two [2Fe-2S] clusters in the beta-subunit. Sequence analyses predict that the alpha-subunit should contain an additional [2Fe-2S] cluster, while the beta-subunit should contain one [2Fe-2S] and three [4Fe-4S] clusters. The latter cluster contents are consistent with the measured Fe contents of about 32, 20 and 14 Fe mol(-1) for the holoenzyme and the alpha- and beta-subunits, respectively. The T. maritima enzyme is the first 'complex' Fe-hydrogenase to be purified and characterized, although the reason for its complexity remains unclear.

Electrochemical and spectroscopic properties of the iron-sulfur flavoprotein from Methanosarcina thermophila

An iron-sulfur flavoprotein (Isf) from the methanoarchaeaon Methanosarcina thermophila, which participates in electron transfer reactions required for the fermentation of acetate to methane, was characterized by electrochemistry and EPR and Mössbauer spectroscopy. The midpoint potential (Em) of the FMN/FMNH2 couple was -0.277 V. No flavin semiquinone was observed during potentiometric titrations; however, low amounts of the radical were observed when Isf was quickly frozen after reaction with CO and the CO dehydrogenase/acetyl-CoA synthase complex from M. thermophila. Isf contained a [4Fe-4S]2+/1+ cluster with g values of 2.06 and 1.93 and an unusual split signal with g values at 1.86 and 1.82. The unusual morphology was attributed to microheterogeneity among Isf molecules. The Em value for the 2+/1+ redox couple of the cluster was -0.394 V. Extracts from H2-CO2-grown Methanobacterium thermoautotrophicum cells catalyzed either the H2- or CO-dependent reduction of M. thermophila Isf. In addition, Isf homologs were found in the genomic sequences of the CO2-reducing methanoarchaea M. thermoautotrophicum and Methanococcus jannaschii. These results support a general role for Isf in electron transfer reactions of both acetate-fermenting and CO2-reducing methanoarchaea. It is suggested that Isf functions to couple electron transfer from ferredoxin to membrane-bound electron carriers, such as methanophenazine and/or b-type cytochromes.

Characterization of an iron-sulfur flavoprotein from Methanosarcina thermophila

A gene (isf) encoding an iron-sulfur flavoprotein (Isf) from Methanosarcina thermophila was cloned and sequenced. The gene was located directly upstream of the genes (pta and ack) encoding phosphotransacetylase and acetate kinase and is transcribed in the opposite direction. The amino acid sequence deduced from isf contained a cluster of cysteine residues reminiscent of proteins that accommodate either a [4Fe-4S] or [3Fe-4S] center. The protein was heterologously produced in Escherichia coli and purified to apparent homogeneity. The 29-kDa subunit molecular mass of heterologously produced Isf (determined by SDS-polyacrylamide gel electrophoresis) corresponded to the molecular mass of 30,451 Da calculated from the amino acid composition deduced from isf. Gel filtration estimated a molecular mass of 65 kDa for the native Isf indicating an alpha2 homodimer. The UV-visible absorption spectrum was characteristic of iron-sulfur flavoproteins with maxima at 484, 452, 430, 378, and 280 nm. Analyses identified 2 FMN, 7-8 non-heme iron atoms, and 6-7 acid-labile sulfur atoms per alpha2 homodimer. Comparisons of the deduced Isf sequence with sequences in available protein data bases suggested Isf is a novel iron-sulfur flavoprotein. Western blot analysis indicated the presence of Isf in extracts of acetate-grown M. thermophila. Ferredoxin stimulated the CO-dependant reduction of Isf by the CO dehydrogenase middle dotacetyl-CoA synthase complex that suggested ferredoxin is a physiological electron donor to Isf.

Biochemical characterization of the 8-hydroxy-5-deazaflavin-reactive hydrogenase from Methanosarcina barkeri Fusaro

The membrane-associated coenzyme F420-reactive hydrogenase of the anaerobic methanogenic archaeon Methanosarcina barkeri Fusaro has been purified 95-fold to apparent homogeneity. A new purification procedure and altered storage conditions gave substantially higher yield (13.4% versus 4.3%) and specific coenzyme F420-reducing activity (82.8 mumol.min-1.mg protein-1 versus 11.5 mumol.min-1.mg protein-1) than reported previously [Fiebig, K. & Friedrich, B. (1989) Eur. J. Biochem. 184, 79-88]. The predominant coenzyme F420-reactive form of the hydrogenase has an apparent molecular mass of 198 kDa and is composed of three non-identical subunits with apparent molecular masses of 48 (alpha), 33 (beta), and 30 kDa (gamma), apparently in a stoichiometry of alpha 2 beta 2 gamma 1. This minimal coenzyme F420-reducing hydrogenase formed aggregates with apparent molecular masses of approximately 845 kDa. 1 mol of the 198-kDa form of hydrogenase contained 2 mol FAD, 2 mol nickel, 28-32 mol non-heme iron, and 34 mol acid-labile sulfur; in addition, 0.2 mol selenium was detected. The isoelectric point was 5.30. The amino acid sequence PXXRXEGH, where X is any amino acid, was found to be conserved in the N-termini of the putative nickel-binding subunits of most [NiFe]- and [NiFeSe]hydrogenases of methanogenic Archaea and Bacteria. However, this motif was not detected in the protein sequences of [Fe]hydrogenases. Maximal coenzyme F420-reducing activity was obtained with reductively reactivated enzyme at 55 degrees C in the pH range 6.5-7.25. The Km values of the purified enzyme for H2 with coenzyme F420 or methylviologen as electron acceptor were extremely low, namely 3 microM and 4 microM. The catalytic efficiency coefficients (kcat/Km) for H2 with both reducible cosubstrates were high: 2.5 x 10(7) M-1.s-1 with coenzyme F420 and 6.9 x 10(7) M-1.s-1 with methylviologen.

Structural aspects and immunolocalization of the F420-reducing and non-F420-reducing hydrogenases from Methanobacterium thermoautotrophicum Marburg

The F420-reducing hydrogenase and the non-F420-reducing hydrogenase (EC 1.12.99.1.) were isolated from a crude extract of Methanobacterium thermoautotrophicum Marburg. Electron microscopy of the negatively stained F420-reducing hydrogenase revealed that the enzyme is a complex with a diameter of 15.6 nm. It consists of two ring-like, stacked, parallel layers each composed of three major protein masses arranged in rotational symmetry. Each of these masses appeared to be subdivided into smaller protein masses. Electron microscopy of negatively stained samples taken from intermediate steps of the purification process revealed the presence of enzyme particles bound to inside-out membrane vesicles. Linker particles of 10 to 20 kDa which mediate the attachment of the hydrogenase to the cytoplasmic membrane were seen. Immunogold labelling confirmed that the F420-reducing hydrogenase is a membrane-bound enzyme. Electron microscopy of the negatively stained purified non-F420-reducing hydrogenase revealed that the enzyme is composed of three subunits exhibiting different diameters (5, 4, and 2 to 3 nm). According to immunogold labelling experiments, approximately 70% of the non-F420-reducing hydrogenase protein molecules were located at the cell periphery; the remaining 30% were cytoplasmic. No linker particles were observed for this enzyme.

Characterization of a CO: heterodisulfide oxidoreductase system from acetate-grown Methanosarcina thermophila

During the methanogenic fermentation of acetate by Methanosarcina thermophila, the CO dehydrogenase complex cleaves acetyl coenzyme A and oxidizes the carbonyl group (or CO) to CO2, followed by electron transfer to coenzyme M (CoM)-S-S-coenzyme B (CoB) and reduction of this heterodisulfide to HS-CoM and HS-CoB (A. P. Clements, R. H. White, and J. G. Ferry, Arch. Microbiol. 159:296-300, 1993). The majority of heterodisulfide reductase activity was present in the soluble protein fraction after French pressure cell lysis. A CO:CoM-S-S-CoB oxidoreductase system from acetate-grown cells was reconstituted with purified CO dehydrogenase enzyme complex, ferredoxin, membranes, and partially purified heterodisulfide reductase. Coenzyme F420 (F420) was not required, and CO:F420 oxidoreductase activity was not detected in cell extracts. The membranes contained cytochrome b that was reduced with CO and oxidized with CoM-S-S-CoB. The results suggest that a novel CoM-S-S-CoB reducing system operates during acetate conversion to CH4 and CO2. In this system, ferredoxin transfers electrons from the CO dehydrogenase complex to membrane-bound electron carriers, including cytochrome b, that are required for electron transfer to the heterodisulfide reductase. The cytochrome b was purified from solubilized membrane proteins in a complex with six other polypeptides. The cytochrome was not reduced when the complex was incubated with H2 or CO, and H2 uptake hydrogenase activity was not detected; however, the addition of CO dehydrogenase enzyme complex and ferredoxin enabled the CO-dependent reduction of cytochrome b.

Metabolism of methanogens

Methanogenic archaea convert a few simple compounds such as H2 + CO2, formate, methanol, methylamines, and acetate to methane. Methanogenesis from all these substrates requires a number of unique coenzymes, some of which are exclusively found in methanogens. H2-dependent CO2 reduction proceeds via carrier-bound C1 intermediates which become stepwise reduced to methane. Methane formation from methanol and methylamines involves the disproportionation of the methyl groups. Part of the methyl groups are oxidized to CO2, and the reducing equivalents thereby gained are subsequently used to reduce other methyl groups to methane. This process involves the same C1 intermediates that are formed during methanogenesis from CO2. Conversion of acetate to methane and carbon dioxide is preceded by its activation to acetyl-CoA. Cleavage of the latter compound yields a coenzyme-bound methyl moiety and an enzyme-bound carbonyl group. The reducing equivalents gained by oxidation of the carbonyl group to carbon dioxide are subsequently used to reduce the methyl moiety to methane. All these processes lead to the generation of transmembrane ion gradients which fuel ATP synthesis via one or two types of ATP synthases. The synthesis of cellular building blocks starts with the central anabolic intermediate acetyl-CoA which, in autotrophic methanogens, is synthesized from two molecules of CO2 in a linear pathway.

Isolation, characterization and N-terminal amino acid sequence of hydrogenase from the green alga Chlamydomonas reinhardtii

Hydrogenase from Chlamydomonas reinhardtii was purified to homogeneity by five column-chromatography steps under strict anaerobic conditions. The cells were disrupted by mild treatment with detergent. The enzyme was purified 6100-fold, resulting in a specific activity for H2 evolution of 935 mumol.min-1.mg protein-1 at 25 degrees C, using reduced methyl viologen as electron donor. The optimal temperature for hydrogen evolution is 60 degrees C, the optimal pH value is 6.9. The Km value for methyl viologen is 0.83 mM, for ferredoxin, 35 microM. From SDS/PAGE gels, the protein was judged to be pure. On non-denaturing gels, run under nitrogen, a single band was detected after activity staining. This band corresponded to the single band observed on denaturing SDS gels, which had an apparent molecular mass of 48 kDa. If the band was cut out of the native gel and incubated with reduced methyl viologen, hydrogen evolution could be measured. The purified enzyme contains 4 Fe atoms/mol. The amino acid composition and the N-terminal amino acid sequence (24 residues) of the protein were determined. No significant amino acid sequence homologies could be found to any sequences from prokaryotic hydrogenases.

N5-methyltetrahydromethanopterin: coenzyme M methyltransferase in methanogenic archaebacteria is a membrane protein

An assay is described that allows the direct measurement of the enzyme activity catalyzing the transfer of the methyl group from N5-methyltetrahydromethanopterin (CH3-H4MPT) to coenzyme M (H-S-CoM) in methanogenic archaebacteria. With this method the topology, the partial purification, and the catalytic properties of the methyltransferase in methanol- and acetate-grown Methanosarcina barkeri and in H2/CO(2)-grown Methanobacterium thermoautotrophicum were studied. The enzyme activity was found to be associated almost completely with the membrane fraction and to require detergents for solubilization. The transferase activity in methanol-grown M. barkeri was studied in detail. The membrane fraction exhibited a specific activity of CH3-S-CoM formation from CH3-H4MPT (apparent Km = 50 microM) and H-S-CoM (apparent Km = 250 microM) of approximately 0.6 mumol.min-1.mg protein-1. For activity the presence of Ti(III) citrate (apparent Km = 15 microM) and of ATP (apparent Km = 30 microM) were required in catalytic amounts. Ti(III) could be substituted by reduced ferredoxin. ATP could not be substituted by AMP, CTP, GTP, S-adenosylmethionine, or by ATP analogues. The membrane fraction was methylated by CH3-H4MPT in the absence of H-S-CoM. This methylation was dependent on Ti(III) and ATP. The methylated membrane fraction catalyzed the methyltransfer from CH3-H4MPT to H-S-CoM in the absence of ATP and Ti(III). Demethylation in the presence of H-S-CoM also did not require Ti(III) or ATP. Based on these findings a mechanism for the methyltransfer reaction and for the activation of the enzyme is proposed.

Purification and properties of a F420-nonreactive, membrane-bound hydrogenase from Methanosarcina strain Gö1

The distribution of the F420-reactive and F420-nonreactive hydrogenases from the methylotrophic Methanosarcina strain Gö1 indicated a membrane association of the F420-nonreactive enzyme. The membrane-bound F420-nonreactive hydrogenase was purified 42-fold to electrophoretic homogeneity with a yield of 26.7%. The enzyme had a specific activity of 359 mumol H2 oxidized.min-1.mg protein-1. The purification procedure involved dispersion of the membrane fraction with the detergent Chaps followed by anion exchange, hydrophobic and hydroxylapatite chromatography. The aerobically prepared enzyme had to be reactivated anaerobically. Maximal activity was observed at 80 degrees C. The molecular mass as determined by native gel electrophoresis and gel filtration was 77,000 and 79,000, respectively. SDS gel electrophoresis revealed two polypeptides with molecular masses of 60,000 and 40,000 indicating a 1:1 stoichiometry. The purified enzyme contained 13.3 mol S2-, 15.1 mol Fe and 0.8 mol Ni/mol enzyme. Flavins were not detected. The amino acid sequence of the N-termini of the subunits showed a higher degree of homology to eubacterial uptake-hydrogenases than to F420-dependent hydrogenases from other methanogenic bacteria. The physiological function of the F420-nonreactive hydrogenase from Methanosarcina strain Göl is discussed.

Biochemistry of methanogenesis

Methane is a product of the energy-yielding pathways of the largest and most phylogenetically diverse group in the Archaea. These organisms have evolved three pathways that entail a novel and remarkable biochemistry. All of the pathways have in common a reduction of the methyl group of methyl-coenzyme M (CH3-S-CoM) to CH4. Seminal studies on the CO2-reduction pathway have revealed new cofactors and enzymes that catalyze the reduction of CO2 to the methyl level (CH3-S-CoM) with electrons from H2 or formate. Most of the methane produced in nature originates from the methyl group of acetate. CO dehydrogenase is a key enzyme catalyzing the decarbonylation of acetyl-CoA; the resulting methyl group is transferred to CH3-S-CoM, followed by reduction to methane using electrons derived from oxidation of the carbonyl group to CO2 by the CO dehydrogenase. Some organisms transfer the methyl group of methanol and methylamines to CH3-S-CoM; electrons for reduction of CH3-S-CoM to CH4 are provided by the oxidation of methyl groups to CO2.

N5, N10-methylenetetrahydromethanopterin dehydrogenase (H2-forming) from the extreme thermophile Methanopyrus kandleri

Methanopyrus kandleri is a novel abyssal methanogenic archaebacterium growing at 110 degrees C on H2 and CO2. The N5, N10-methylenetetrahydromethanopterin dehydrogenase, an enzyme involved in methanogenesis from CO2 and H2, was purified from this hyperthermophile and characterized. The dehydrogenase was found to be composed of only one polypeptide of apparent molecular mass 44 kDa. The UV/Vis spectrum was similar to that of albumin. The protein catalyzed the reversible dehydrogenation of N5, N10-methylenetetrahydromethanopterin (CH2 = H4MPT) to N5, N10-methenyltetrahydromethanopterin (CH identical to H4MPT+) and molecular hydrogen: CH2 = H4MPT H+ in equilibrium CH identical to H4MPT+ +H2. The rate of CH2 = H4MPT dehydrogenation (apparent Vmax) at 65 degrees C and pH 5.8 was 1500 U/mg, the apparent Km for CH2 = H4MPT was 50 microM, the Arrhenius activation energy was 52 kJ/mol, and the Q10 between 30 degrees C and 70 degrees C was 2.0. The specific activity increased hyperbolically with the proton concentration between pH 7 and pH 4.5. The purified dehydrogenase did not catalyze the reduction of viologen dyes, of coenzyme F420, and of pyridine nucleotides with either CH2 = H4MPT or H2. For activity the CH2 = H4MPT dehydrogenase required the presence of salts. Fifty percent of maximal activity was reached at salt concentrations of 100 mM, potassium phosphate, potassium chloride, and sodium chloride being almost equally effective in stimulating the enzyme activity. Cell extracts of M. kandleri did not loose CH2 = H4MPT dehydrogenase activity when incubated at 90 degrees C for 60 min. The purified enzyme, however, proved very thermolabile. The purified enzyme, however, proved very thermolabile.(ABSTRACT TRUNCATED AT 250 WORDS)

Purification and characterization of the hydrogen uptake hydrogenase from the hyperthermophilic archaebacterium Pyrodictium brockii

Pyrodictium brockii is a hyperthermophilic archaebacterium with an optimal growth temperature of 105 degrees C. P. brockii is also a chemolithotroph, requiring H2 and CO2 for growth. We have purified the hydrogen uptake hydrogenase from membranes of P. brockii by reactive red affinity chromatography and sucrose gradient centrifugation. The molecular mass of the holoenzyme was 118,000 +/- 19,000 Da in sucrose gradients. The holoenzyme consisted of two subunits by sodium dodecyl sulfate-polyacrylamide gel electrophoresis. The large subunit had a molecular mass of 66,000 Da, and the small subunit had a molecular mass of 45,000 Da. Colorometric analysis of Fe and S content in reactive red-purified hydrogenase revealed 8.7 +/- 0.6 mol of Fe and 6.2 +/- 1.2 mol of S per mol of hydrogenase. Growth of cells in 63NiCl2 resulted in label incorporation into reactive red-purified hydrogenase. Growth of cells in 63NiCl2 resulted in label incorporation into reactive red-purified hydrogenase. Temperature stability studies indicated that the membrane-bound form of the enzyme was more stable than the solubilized purified form over a period of minutes with respect to temperature. However, the membranes were not able to protect the enzyme from thermal inactivation over a period of hours. The artificial electron acceptor specificity of the pure enzyme was similar to that of the membrane-bound form, but the purified enzyme was able to evolve H2 in the presence of reduced methyl viologen. The Km of membrane-bound hydrogenase for H2 was approximately 19 microM with methylene blue as the electron acceptor, whereas the purified enzyme had a higher Km value.

Conservation of primary structure in prokaryotic hydrogenases

All prokaryotic (NiFe)-hydrogenases so far studied at the primary sequence level appear to have evolved from a common ancestral sequence. Highly conserved cysteinyl and histidinyl residues indicate regions likely to be essential for enzyme activity, ligand and co-factor binding. There is a very highly conserved sequence over 100 basepairs (bp) in length within the intergenic region upstream of the methyl-viologen hydrogenase encoding genes in several different strains of Methanobacterium thermoautotrophicum, indicating that a sequence of this length is needed to direct and regulate the expression of these genes.

The structure and mechanism of iron-hydrogenases

Hydrogenases devoid of nickel and containing only Fe-S clusters have been found so far only in some strictly anaerobic bacteria. Four Fe-hydrogenases have been characterized: from Megasphaera elsdenii, Desulfovibrio vulgaris (strain Hildenborough), and two from Clostridium pasteurianum. All contain two or more [4Fe-4S]1+,2+ or F clusters and a unique type of Fe-S center termed the H cluster. The H cluster appears to be remarkably similar in all the hydrogenases, and is proposed as the site of H2 oxidation and H2 production. The F clusters serve to transfer electrons between the H cluster and the external electron carrier. In all of the hydrogenases the H cluster is comprised of at least three Fe atoms, and possibly six. In the oxidized state it contains two types of magnetically distinct Fe atoms, has an S = 1/2 spin state, and exhibits a novel rhombic EPR signal. The reduced cluster is diamagnetic (S = 0). The oxidized H cluster appears to undergo a conformation change upon reduction with H2 with an increase in Fe-Fe distances of about 0.5 A. Studies using resonance Raman, magnetic circular dichroism and electron spin echo spectroscopies suggest that the H cluster has significant non-sulfur coordination. The H cluster has two binding sites for CO, at least one of which can also bind O2. Binding to one site changes the EPR properties of the cluster and gives a photosensitive adduct, but does not affect catalytic activity. Binding to the other site, which only becomes exposed during the catalytic cycle, leads to loss of catalytic activity. Mechanisms of H2 activation and electron transfer are proposed to explain the effects of CO binding and the ability of one of the hydrogenases to preferentially catalyze H2 oxidation.

Formate dehydrogenase from the methane oxidizer Methylosinus trichosporium OB3b

Formate dehydrogenase (NAD+ dependent) was isolated from the obligate methanotroph Methylosinus trichosporium OB3b. When the enzyme was isolated anaerobically, two forms of the enzyme were seen on native polyacrylamide gels, DE-52 cellulose and Sephacryl S-300 columns; they were approximately 315,000 and 155,000 daltons. The enzyme showed two subunits on sodium dodecyl sulfate-polyacrylamide gels. The Mr of the alpha-subunit was 53,800 +/- 2,800, and that of the beta-subunit was 102,600 +/- 3,900. The enzyme (Mr 315,000) was composed of these subunits in an apparent alpha 2 beta 2 arrangement. Nonheme iron was present at a concentration ranging from 11 to 18 g-atoms per mol of enzyme (Mr 315,000). Similar levels of acid-labile sulfide were detected. No other metals were found in stoichiometric amounts. When the enzyme was isolated aerobically, there was no cofactor requirement for NAD reduction; however, when isolated anaerobically, activity was 80 to 90% dependent on the addition of flavin mononucleotide (FMN) to the reaction mixture. Furthermore, the addition of formate to an active, anoxic solution of formate dehydrogenase rapidly inactivated it in the absence of an electron acceptor; this activity could be reconstituted approximately 85% by 50 nM FMN. Flavin adenine dinucleotide could not replace FMN in reconstituting enzyme activity. The Kms of formate dehydrogenase for formate, NAD, and FMN were 146, 200, and 0.02 microM, respectively. "Pseudomonas oxalaticus" formate dehydrogenase, which has physical characteristics nearly identical to those of the M. trichosporium enzyme, was also shown to be inactivated under anoxic conditions by formate and reactivated by FMN. The evolutionary significance of this similarity is discussed.

Reconstitution and properties of a coenzyme F420-mediated formate hydrogenlyase system in Methanobacterium formicicum

Formate hydrogenlyase activity in a cell extract of Methanobacterium formicicum was abolished by removal of coenzyme F420; addition of purified coenzyme F420 restored activity. Formate hydrogenlyase activity was reconstituted with three purified components from M. formicicum: coenzyme F420-reducing hydrogenase, coenzyme F420-reducing formate dehydrogenase, and coenzyme F420. The reconstituted system required added flavin adenine dinucleotide (FAD) for maximal activity. Without FAD, the formate dehydrogenase and hydrogenase rapidly lost coenzyme F420-dependent activity relative to methyl viologen-dependent activity. Immunoadsorption of formate dehydrogenase or coenzyme F420-reducing hydrogenase from the cell extract greatly reduced formate hydrogenlyase activity; addition of the purified enzymes restored activity. The formate hydrogenlyase activity was reversible, since both the cell extract and the reconstituted system produced formate from H2 plus CO2 and HCO3-.