Coenzyme F420-dependent sulfite reductase-enabled sulfite detoxification and use of sulfite as a sole sulfur source by Methanococcus maripaludis

Coenzyme F(420)-dependent sulfite reductase (Fsr) of Methanocaldococcus jannaschii, a sulfite-tolerant methanogen, was expressed with activity in Methanococcus maripaludis, a sulfite-sensitive methanogen. The recombinant organism reduced sulfite to sulfide and grew with sulfite as the sole sulfur source, indicating that Fsr is a sulfite detoxification and assimilation enzyme for methanogens and that M. maripaludis synthesizes siroheme.     

An Intertwined Evolutionary History of Methanogenic Archaea and Sulfate Reduction

Hydrogenotrophic methanogenesis and dissimilatory sulfate reduction, two of the oldest energy conserving respiratory systems on Earth, apparently could not have evolved in the same host, as sulfite, an intermediate of sulfate reduction, inhibits methanogenesis. However, certain methanogenic archaea metabolize sulfite employing a deazaflavin cofactor (F₄₂₀)-dependent sulfite reductase (Fsr) where N- and C-terminal halves (Fsr-N and Fsr-C) are homologs of F₄₂₀H₂ dehydrogenase and dissimilatory sulfite reductase (Dsr), respectively. From genome analysis we found that Fsr was likely assembled from freestanding Fsr-N homologs and Dsr-like proteins (Dsr-LP), both being abundant in methanogens. Dsr-LPs fell into two groups defined by following sequence features: Group I (simplest), carrying a coupled siroheme-[Fe₄-S₄] cluster and sulfite-binding Arg/Lys residues; Group III (most complex), with group I features, a Dsr-type peripheral [Fe₄-S₄] cluster and an additional [Fe₄-S₄] cluster. Group II Dsr-LPs with group I features and a Dsr-type peripheral [Fe₄-S₄] cluster were proposed as evolutionary intermediates. Group III is the precursor of Fsr-C. The freestanding Fsr-N homologs serve as F₄₂₀H₂ dehydrogenase unit of a putative novel glutamate synthase, previously described membrane-bound electron transport system in methanogens and of assimilatory type sulfite reductases in certain haloarchaea. Among archaea, only methanogens carried Dsr-LPs. They also possessed homologs of sulfate activation and reduction enzymes. This suggested a shared evolutionary history for methanogenesis and sulfate reduction, and Dsr-LPs could have been the source of the oldest (3.47-Gyr ago) biologically produced sulfide deposit.     

Comparative proteomic analysis of Methanothermobacter themautotrophicus ΔH in pure culture and in co-culture with a butyrate-oxidizing bacterium

To understand the physiological basis of methanogenic archaea living on interspecies H(2) transfer, the protein expression of a hydrogenotrophic methanogen, Methanothermobacter thermautotrophicus strain ΔH, was investigated in both pure culture and syntrophic coculture with an anaerobic butyrate oxidizer Syntrophothermus lipocalidus strain TGB-C1 as an H(2) supplier. Comparative proteomic analysis showed that global protein expression of methanogen cells in the model coculture was substantially different from that of pure cultured cells. In brief, in syntrophic coculture, although methanogenesis-driven energy generation appeared to be maintained by shifting the pathway to the alternative methyl coenzyme M reductase isozyme I and cofactor F(420)-dependent process, the machinery proteins involved in carbon fixation, amino acid synthesis, and RNA/DNA metabolisms tended to be down-regulated, indicating restrained cell growth rather than vigorous proliferation. In addition, our proteome analysis revealed that α subunits of proteasome were differentially acetylated between the two culture conditions. Since the relevant modification has been suspected to regulate proteolytic activity of the proteasome, the global protein turnover rate could be controlled under syntrophic growth conditions. To our knowledge, the present study is the first report on N-acetylation of proteasome subunits in methanogenic archaea. These results clearly indicated that physiological adaptation of hydrogenotrophic methanogens to syntrophic growth is more complicated than that of hitherto proposed.     

Novel reactions involved in energy conservation by methanogenic archaea.

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

Function of coenzyme F420 in aerobic catabolism of 2,4, 6-trinitrophenol and 2,4-dinitrophenol by Nocardioides simplex FJ2-1A

2,4,6-Trinitrophenol (picric acid) and 2,4-dinitrophenol were readily biodegraded by the strain Nocardioides simplex FJ2-1A. Aerobic bacterial degradation of these pi-electron-deficient aromatic compounds is initiated by hydrogenation at the aromatic ring. A two-component enzyme system was identified which catalyzes hydride transfer to picric acid and 2,4-dinitrophenol. Enzymatic activity was dependent on NADPH and coenzyme F420. The latter could be replaced by an authentic preparation of coenzyme F420 from Methanobacterium thermoautotrophicum. One of the protein components functions as a NADPH-dependent F420 reductase. A second component is a hydride transferase which transfers hydride from reduced coenzyme F420 to the aromatic system of the nitrophenols. The N-terminal sequence of the F420 reductase showed high homology with an F420-dependent NADP reductase found in archaea. In contrast, no N-terminal similarity to any known protein was found for the hydride-transferring enzyme.     

Distribution of coenzyme F420 and properties of its hydrolytic fragments.

The ability of hydrolytic products of coenzyme F420 to substitute for F420 in the hydrogenase and nicotinamide adenine dinucleotide phosphate-liniked hydrogenase systems of Methanobacterium strain M.o.H. was kinetically determined. The nicotinamide adenine dinucleotide phosphate-linked hydrogenase system was employed to quantitate the levels of F420 in a number of methanogenic bacteria as well as in some nonmethanogens. Methanobacterium ruminantium and Methanosarcina barkeri contained low levels of F420, whereas other methanogens tested contained high levels (100 to 400 mg/kg of cells). F420 from six of the seven methanogens was tested by thin-layer electrophoresis and was found to be electrophoretically identical to that purified from Methanobacterium strain M.o.H. The only exception was M. barkeri, which contained a more electronegative derivative of F420. Acetobacterium woodii, Escherichia coli, and yeast extract contained no compounds able to substitute for F420 in the nicotinamide adenine dinucleotide phosphate-linked hydrogenase system.     

Relationship of Intracellular Coenzyme F(420) Content to Growth and Metabolic Activity of Methanobacterium bryantii and Methanosarcina barkeri

The use of F(420) as a parameter for growth or metabolic activity of methanogenic bacteria was investigated. Two representative species of methanogens were grown in batch culture: Methanobacterium bryantii (strain M.o.H.G.) on H(2) and CO(2), and Methanosarcina barkeri (strain Fusaro) on methanol or acetate. The total intracellular content of coenzyme F(420) was followed by high-resolution fluorescence spectroscopy. F(420) concentration in M. bryantii ranged from 1.84 to 3.65 mumol . g of protein; and in M. barkeri grown with methanol it ranged from 0.84 to 1.54 mumol . g depending on growth conditions. The content of F(420) in M. barkeri was influenced by a factor of 2 depending on the composition of the medium (minimal or complex) and by a factor of 3 to 4 depending on whether methanol or acetate was used as the carbon source. A comparison of F(420) content with protein, cell dry weight, optical density, and specific methane production rate showed that the intracellular content of F(420) approximately followed the increase in biomass in both strains. In contrast, no correlation was found between specific methane production rate and intracellular F(420) content. However, qCH(4)(F(420)), calculated by dividing the methane production rate by the coenzyme F(420) concentration, almost paralleled qCH(4)(protein). These results suggest that F(420) may be used as a specific parameter for estimating the biomass, but not the metabolic activity, of methanogens; hence qCH(4)(F(420)) determined in mixed populations with complex carbon substrates must be considered as measure of the actual methanogenic activity and not as a measure of potential activity.     

Biosynthesis of the phosphodiester bond in coenzyme F(420) in the methanoarchaea

The biochemical route for the formation of the phosphodiester bond in coenzyme F(420), one of the methanogenic coenzymes, has been established in the methanoarchaea Methanosarcina thermophila and Methanococcus jannaschii. The first step in the formation of this portion of the F(420) structure is the GTP-dependent phosphorylation of L-lactate to 2-phospho-L-lactate and GDP. The 2-phospho-L-lactate represents a new natural product that was chemically identified in Methanobacterium thermoautotrophicum, M. thermophila, and Mc. jannaschii. Incubation of cell extracts of both M. thermophila and Mc. jannaschii with [hydroxy-(18)O, carboxyl-(18)O(2)]lactate and GTP produced 2-phospho-L-lactate with the same (18)O distribution as found in both the starting lactate and the lactate recovered from the incubation. These results indicate that the carboxyl oxygens are not involved in the phosphorylation reaction. Incubation of Sephadex G-25 purified cell extracts of M. thermophila or Mc. jannaschii with 7,8-didemethyl-8-hydroxy-5-deazariboflavin (Fo), 2-phospho-L-lactate, and GTP or ATP lead to the formation of F(420)-0 (F(420) with no glutamic acids). This transformation was shown to involve two steps: (i) the GTP- or ATP-dependent activation of 2-phospho-L-lactate to either lactyl(2)diphospho-(5')guanosine (LPPG) or lactyl(2)diphospho-(5')adenosine (LPPA) and (ii) the reaction of the resulting LPPG or LPPA with Fo to form F(420)-0 with release of GMP or AMP. Attempts to identify LPPG or LPPA intermediates by incubation of cell extracts with L-[U-(14)C]lactate, [U-(14)C]2-phospho-L-lactate, or [8-(3)H]GTP were not successful owing to the instability of these compounds toward hydrolysis. Synthetically prepared LPPG and LPPA had half-lives of 10 min at 50 degrees C (at pH 7.0) and decomposed into GMP or AMP and 2-phospho-L-lactate via cyclic 2-phospho-L-lactate. No evidence for the functioning of the cyclic 2-phospho-L-lactate in the in vitro biosynthesis could be demonstrated. Incubation of cell extracts of M. thermophila or Mc. jannaschii with either LPPG or LPPA and Fo generated F(420)-0. In summary, this study demonstrates that the formation of the phosphodiester bond in coenzyme F(420) follows a reaction scheme like that found in one of the steps of the DNA ligase reaction and in the biosynthesis of coenzyme B(12) and phospholipids.     

2,5-diamino-6-ribitylamino-4(3H)-pyrimidinone 5'-phosphate synthases of fungi and archaea

The pathway of riboflavin (vitamin B2) biosynthesis is significantly different in archaea, eubacteria, fungi and plants. Specifically, the first committed intermediate, 2,5-diamino-6-ribosylamino-4(3H)-pyrimidinone 5'-phosphate, can either undergo hydrolytic cleavage of the position 2 amino group by a deaminase (in plants and most eubacteria) or reduction of the ribose side chain by a reductase (in fungi and archaea). We compare 2,5-diamino-6-ribitylamino-4(3H)-pyrimidinone 5'-phosphate synthases from the yeast Candida glabrata, the archaeaon Methanocaldococcus jannaschii and the eubacterium Aquifex aeolicus. All three enzymes convert 2,5-diamino-6-ribosylamino-4(3H)-pyrimidinone 5'-phosphate into 2,5-diamino-6-ribitylamino-4(3H)-pyrimidinone 5'-phosphate, as shown by 13C-NMR spectroscopy using [2,1',2',3',4',5'-13C6]2,5-diamino-6-ribosylamino-4(3H)-pyrimidinone 5'-phosphate as substrate. The beta anomer was found to be the authentic substrate, and the alpha anomer could serve as substrate subsequent to spontaneous anomerisation. The M. jannaschii and C. glabrata enzymes were shown to be A-type reductases catalysing the transfer of deuterium from the 4(R) position of NADPH to the 1' (S) position of the substrate. These results are in agreement with the known three-dimensional structure of the M. jannaschii enzyme.     

Bioenergetics and anaerobic respiratory chains of aceticlastic methanogens

Methane-forming archaea are strictly anaerobic microbes and are essential for global carbon fluxes since they perform the terminal step in breakdown of organic matter in the absence of oxygen. Major part of methane produced in nature derives from the methyl group of acetate. Only members of the genera Methanosarcina and Methanosaeta are able to use this substrate for methane formation and growth. Since the free energy change coupled to methanogenesis from acetate is only − 36 kJ/mol CH₄, aceticlastic methanogens developed efficient energy-conserving systems to handle this thermodynamic limitation. The membrane bound electron transport system of aceticlastic methanogens is a complex branched respiratory chain that can accept electrons from hydrogen, reduced coenzyme F₄₂₀ or reduced ferredoxin. The terminal electron acceptor of this anaerobic respiration is a mixed disulfide composed of coenzyme M and coenzyme B. Reduced ferredoxin has an important function under aceticlastic growth conditions and novel and well-established membrane complexes oxidizing ferredoxin will be discussed in depth. Membrane bound electron transport is connected to energy conservation by proton or sodium ion translocating enzymes (F₄₂₀H₂ dehydrogenase, Rnf complex, Ech hydrogenase, methanophenazine-reducing hydrogenase and heterodisulfide reductase). The resulting electrochemical ion gradient constitutes the driving force for adenosine triphosphate synthesis. Methanogenesis, electron transport, and the structure of key enzymes are discussed in this review leading to a concept of how aceticlastic methanogens make a living. This article is part of a Special Issue entitled: 18th European Bioenergetic Conference.     

Biochemical origins of lactaldehyde and hydroxyacetone in Methanocaldococcus jannaschii

The biochemical routes for the metabolism of methylglyoxal and the formation of lactaldehyde and hydroxyacetone in Methanocaldococcus jannaschii have been established. The addition of methylglyoxal and NADH, NADPH, F 420H 2, or DTT to a M. jannaschii cell extract stimulated the production of both lactaldehyde and hydroxyacetone. Using appropriately labeled NADH, NADPH, and F 420H 2, hydride transfer was only observed from F 420H 2 to lactaldehyde. It was shown that cell extracts of this Archaea readily catalyzed the F 420H 2-dependent reduction of methylglyoxal to lactaldehyde, a precursor of the lactate found in coenzyme F 420. This conversion was established by measuring the incorporation of deuterium from (5 RS)[5- (2)H 1]F 420H 2 into the C-2 position of the formed lactaldehyde. In vivo generated (5 R)[5- (2)H 1]F 420H 2 was also found to incorporate deuterium into lactaldehyde. The experimental data indicated that the pro- R hydrogen of F 420H 2 was transferred during the reduction. The stereochemistry of this transfer was opposite from that observed for all other known enzyme-catalyzed hydride-transfer reactions involving F 420. [1,3,3,3- (2)H 4]-Methylglyoxal was incorporated into lactaldehyde and hydroxyacetone as an intact unit during this reduction with the occurrence of some deuterium exchange. The exchange observed during this incorporation into lactaldehyde was substantially more than the exchange observed during the incorporation into the hydroxyacetone. The hydroxyacetone was derived directly from methylglyoxal, with the hydrogen for the reduction being derived from water. Hydroxyacetone was also readily formed by the condensation of pyruvate with formaldehyde. The product of the MJ0663 gene was shown to catalyze this condensation reaction.     

Changes in concentrations of coenzyme F420 analogs during batch growth of Methanosarcina barkeri and Methanosarcina mazei

Coenzyme F420 has been assayed by high-performance liquid chromatography with fluorimetric detection; this permits quantification of individual coenzyme F420 analogs whilst avoiding the inclusion of interfering material. The total intracellular coenzyme F420 content of Methanosarcina barkeri MS cultivated on methanol and on H2-CO2 and of Methanosarcina mazei S-6 cultured on methanol remained relatively constant during batch growth. The most abundant analogs in M. barkeri were coenzymes F420-2 and F420-4, whilst in M. mazei coenzymes F420-2 and F420-3 predominated. Significant changes in the relative proportions of the coenzyme F420 analogs were noted during batch growth, with coenzymes F420-2 and F420-4 showing opposite responses to each other and the same being also true for coenzymes F420-3 and F420-5. This suggests that an enzyme responsible for transferring pairs of glutamic acid residues may be active. The degradation fragment FO was also detected in cells in late exponential and stationary phase. Coenzyme F420 analogs were present in the culture supernatant of both methanogens, in similar proportions to that in the cells, except for FO which was principally located in the supernatant.     

Changes in concentrations of coenzyme F420 analogs during batch growth of Methanosarcina barkeri and Methanosarcina mazei.

Coenzyme F420 has been assayed by high-performance liquid chromatography with fluorimetric detection; this permits quantification of individual coenzyme F420 analogs whilst avoiding the inclusion of interfering material. The total intracellular coenzyme F420 content of Methanosarcina barkeri MS cultivated on methanol and on H2-CO2 and of Methanosarcina mazei S-6 cultured on methanol remained relatively constant during batch growth. The most abundant analogs in M. barkeri were coenzymes F420-2 and F420-4, whilst in M. mazei coenzymes F420-2 and F420-3 predominated. Significant changes in the relative proportions of the coenzyme F420 analogs were noted during batch growth, with coenzymes F420-2 and F420-4 showing opposite responses to each other and the same being also true for coenzymes F420-3 and F420-5. This suggests that an enzyme responsible for transferring pairs of glutamic acid residues may be active. The degradation fragment FO was also detected in cells in late exponential and stationary phase. Coenzyme F420 analogs were present in the culture supernatant of both methanogens, in similar proportions to that in the cells, except for FO which was principally located in the supernatant.     

The genome characteristics and predicted function of methyl-group oxidation pathway in the obligate aceticlastic methanogens, Methanosaeta spp

In this work, we report the complete genome sequence of an obligate aceticlastic methanogen, Methanosaeta harundinacea 6Ac. Genome comparison indicated that the three cultured Methanosaeta spp., M. thermophila, M. concilii and M. harundinacea 6Ac, each carry an entire suite of genes encoding the proteins involved in the methyl-group oxidation pathway, a pathway whose function is not well documented in the obligately aceticlastic methanogens. Phylogenetic analysis showed that the methyl-group oxidation-involving proteins, Fwd, Mtd, Mch, and Mer from Methanosaeta strains cluster with the methylotrophic methanogens, and were not closely related to those from the hydrogenotrophic methanogens. Quantitative PCR detected the expression of all genes for this pathway, albeit ten times lower than the genes for aceticlastic methanogenesis in strain 6Ac. Western blots also revealed the expression of fwd and mch, genes involved in methyl-group oxidation. Moreover, (13)C-labeling experiments suggested that the Methanosaeta strains might use the pathway as a methyl oxidation shunt during the aceticlastic metabolism. Because the mch mutants of Methanosarcina barkeri or M. acetivorans failed to grow on acetate, we suggest that Methanosaeta may use methyl-group oxidation pathway to generate reducing equivalents, possibly for biomass synthesis. An fpo operon, which encodes an electron transport complex for the reduction of CoM-CoB heterodisulfide, was found in the three genomes of the Methanosaeta strains. However, an incomplete protein complex lacking the FpoF subunit was predicted, as the gene for this protein was absent. Thus, F(420)H(2) was predicted not to serve as the electron donor. In addition, two gene clusters encoding the two types of heterodisulfide reductase (Hdr), hdrABC, and hdrED, respectively, were found in the three Methanosaeta genomes. Quantitative PCR determined that the expression of hdrED was about ten times higher than hdrABC, suggesting that hdrED plays a major role in aceticlastic methanogenesis.     

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

The membrane-associated coenzyme F420-reducing hydrogenase of Methanobacterium formicicum was purified 87-fold to electrophoretic homogeneity. The enzyme contained alpha, beta, and gamma subunits (molecular weights of 43,000, 36,700, and 28,800, respectively) and formed aggregates (molecular weight, 1,020,000) of a coenzyme F420-active alpha 1 beta 1 gamma 1 trimer (molecular weight, 109,000). The hydrogenase contained 1 mol of flavin adenine dinucleotide (FAD), 1 mol of nickel, 12 to 14 mol of iron, and 11 mol of acid-labile sulfide per mol of the 109,000-molecular-weight species, but no selenium. The isoelectric point was 5.6. The amino acid sequence I-N3-P-N2-R-N1-EGH-N6-V (where N is any amino acid) was conserved in the N-termini of the alpha subunits of the F420-hydrogenases from M. formicicum and Methanobacterium thermoautotrophicum and of the largest subunits of nickel-containing hydrogenases from Desulfovibrio baculatus, Desulfovibrio gigas, and Rhodobacter capsulatus. The purified F420-hydrogenase required reductive reactivation before assay. FAD dissociated from the enzyme during reactivation unless potassium salts were present, yielding deflavoenzyme that was unable to reduce coenzyme F420. Maximal coenzyme F420-reducing activity was obtained at 55 degrees C and pH 7.0 to 7.5, and with 0.2 to 0.8 M KCl in the reaction mixture. The enzyme catalyzed H2 production at a rate threefold lower than that for H2 uptake and reduced coenzyme F420, methyl viologen, flavins, and 7,8-didemethyl-8-hydroxy-5-deazariboflavin. Specific antiserum inhibited the coenzyme F420-dependent but not the methyl viologen-dependent activity of the purified enzyme.     

Post-translational modifications in the active site region of methyl-coenzyme M reductase from methanogenic and methanotrophic archaea

Methyl-coenzyme M reductase (MCR) catalyzes the methane-forming step in methanogenic archaea. Isoenzyme I from Methanothermobacter marburgensiswas shown to contain a thioxo peptide bond and four methylated amino acids in the active site region. We report here that MCRs from all methanogens investigated contain the thioxo peptide bond, but that the enzymes differ in their post-translational methylations. The MS analysis included MCR I and MCR II from Methanothermobacter marburgensis, MCR I from Methanocaldococcus jannaschii and Methanoculleus thermophilus, and MCR from Methanococcus voltae, Methanopyrus kandleri and Methanosarcina barkeri. Two MCRs isolated from Black Sea mats containing mainly methanotrophic archaea of the ANME-1 cluster were also analyzed.     

Purification and properties of 5,10-methylenetetrahydromethanopterin reductase, a coenzyme F420-dependent enzyme, from Methanobacterium thermoautotrophicum strain delta H

5,10-Methylenetetrahydromethanopterin reductase was purified 22-fold to apparent homogeneity from the methanogenic bacterium Methanobacterium thermoautotrophicum. The enzyme catalyzes the reduction of 5,10-methylene- to 5-methyltetrahydromethanopterin. The electron carrier coenzyme F420 is specifically used as the cosubstrate. The reductase reaction may proceed in both directions, methylene reduction is, however, thermodynamically favored. In addition, the velocity of the reaction in this direction exceeds the reverse reaction by a factor of 26. The reductase is composed of a single subunit with an estimated Mr = 35,000. The active enzyme does not contain a flavin prosthetic group or iron-sulfur clusters, in contrast to 5,10-methylenetetrahydrofolate reductases purified from eukaryotic and eubacterial sources, which catalyze an analogous reaction as the methanogenic reductase.     

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.     

Identification of lactaldehyde dehydrogenase in Methanocaldococcus jannaschii and its involvement in production of lactate for F420 biosynthesis

One of the early steps in the biosynthesis of coenzyme F(420) in Methanocaldococcus jannaschii requires generation of 2-phospho-L-lactate, which is formed by the phosphorylation of L-lactate. Preliminary studies had shown that L-lactate in M. jannaschii is not derived from pyruvate, and thus an alternate pathway(s) for its formation was examined. Here we report that L-lactate is formed by the NAD(+)-dependent oxidation of l-lactaldehyde by the MJ1411 gene product. The lactaldehyde, in turn, was found to be generated either by the NAD(P)H reduction of methylglyoxal or by the aldol cleavage of fuculose-1-phosphate by fuculose-1-phosphate aldolase, the MJ1418 gene product.     

Distribution of anaerobic methane-oxidizing and sulfate-reducing communities in the G11 Nyegga pockmark,Norwegian Sea

Pockmarks are seabed geological structures sustaining methane seepage in cold seeps. Based on RNA-derived sequences the active fraction of the archaeal community was analysed in sediments associated with the G11 pockmark, in the Nyegga region of the Norwegian Sea. The anaerobic methanotrophic Archaea (ANME) and sulfate-reducing bacteria (SRB) communities were studied as well. The vertical distribution of the archaeal community assessed by PCR-DGGE highlighted the presence of ANME-2 in surface sediments, and ANME-1 in deeper sediments. Enrichments of methanogens showed the presence of hydrogenotrophic methanogens of the Methanogenium genus in surface sediment layers as well. The active fraction of the archaeal community was uniquely composed of ANME-2 in the shallow sulfate-rich sediments. Functional methyl coenzyme M reductase gene libraries showed that sequences affiliated with the ANME-1 and ANME-3 groups appeared in the deeper sediments but ANME-2 dominated both surface and deeper layers. Finally, dissimilatory sulfite reductase gene libraries revealed a high SRB diversity (i.e. Desulfobacteraceae, Desulfobulbaceae, Syntrophobacteraceae and Firmicutes) in the shallow sulfate-rich sediments. The SRB diversity was much lower in the deeper section. Overall, these results show that the microbial community in sediments associated with a pockmark harbour classical cold seep ANME and SRB communities.