Detection of acetyl coenzyme A as an early CO2 assimilation intermediate in Methanobacterium

Serpentinization as the source of energy, electrons, organics, catalysts, nutrients and pH gradients for the origin of LUCA and life

Serpentinization in hydrothermal vents is central to some autotrophic theories for the origin of life because it generates compartments, reductants, catalysts and gradients. During the process of serpentinization, water circulates through hydrothermal systems in the crust where it oxidizes Fe (II) in ultramafic minerals to generate Fe (III) minerals and H2. Molecular hydrogen can, in turn, serve as a freely diffusible source of electrons for the reduction of CO2 to organic compounds, provided that suitable catalysts are present. Using catalysts that are naturally synthesized in hydrothermal vents during serpentinization H2 reduces CO2 to formate, acetate, pyruvate, and methane. These compounds represent the backbone of microbial carbon and energy metabolism in acetogens and methanogens, strictly anaerobic chemolithoautotrophs that use the acetyl-CoA pathway of CO2 fixation and that inhabit serpentinizing environments today. Serpentinization generates reduced carbon, nitrogen and - as newer findings suggest - reduced phosphorous compounds that were likely conducive to the origins process. In addition, it gives rise to inorganic microcompartments and proton gradients of the right polarity and of sufficient magnitude to support chemiosmotic ATP synthesis by the rotor-stator ATP synthase. This would help to explain why the principle of chemiosmotic energy harnessing is more conserved (older) than the machinery to generate ion gradients via pumping coupled to exergonic chemical reactions, which in the case of acetogens and methanogens involve H2-dependent CO2 reduction. Serpentinizing systems exist in terrestrial and deep ocean environments. On the early Earth they were probably more abundant than today. There is evidence that serpentinization once occurred on Mars and is likely still occurring on Saturn's icy moon Enceladus, providing a perspective on serpentinization as a source of reductants, catalysts and chemical disequilibrium for life on other worlds.

Effects of set cathode potentials on microbial electrosynthesis system performance and biocathode methanogen function at a metatranscriptional level

Microbial electrosynthesis exploits the catalytic activity of microorganisms to utilize a cathode as an electron donor for reducing waste CO2 to valuable fuels and chemicals. Electromethanogenesis is the process of CO2 reduction to CH4 catalyzed by methanogens using the cathode directly as a source of electrons or indirectly via H2. Understanding the effects of different set cathode potentials on the functional dynamics of electromethanogenic communities is crucial for the rational design of cathode materials. Replicate enriched electromethanogenic communities were subjected to different potentials (- 1.0 V and - 0.7 V vs. Ag/AgCl) and the potential-induced changes were analyzed using a metagenomic and metatranscriptomic approach. The most abundant and transcriptionally active organism on the biocathodes was a novel species of Methanobacterium sp. strain 34x. The cathode potential-induced changes limited electron donor availability and negatively affected the overall performance of the reactors in terms of CH4 production. Although high expression of key genes within the methane and carbon metabolism pathways was evident, there was no significant difference in transcriptional response to the different set potentials. The acetyl-CoA decarbonylase/synthase (ACDS) complex were the most highly expressed genes, highlighting the significance of carbon assimilation under limited electron donor conditions and its link to the methanogenesis pathway.

β-alanine biosynthesis in Methanocaldococcus jannaschii

One efficient approach to assigning function to unannotated genes is to establish the enzymes that are missing in known biosynthetic pathways. One group of such pathways is those involved in coenzyme biosynthesis. In the case of the methanogenic archaeon Methanocaldococcus jannaschii as well as most methanogens, none of the expected enzymes for the biosynthesis of the β-alanine and pantoic acid moieties required for coenzyme A are annotated. To identify the gene(s) for β-alanine biosynthesis, we have established the pathway for the formation of β-alanine in this organism after experimentally eliminating other known and proposed pathways to β-alanine from malonate semialdehyde, l-alanine, spermine, dihydrouracil, and acryloyl-coenzyme A (CoA). Our data showed that the decarboxylation of aspartate was the only source of β-alanine in cell extracts of M. jannaschii. Unlike other prokaryotes where the enzyme producing β-alanine from l-aspartate is a pyruvoyl-containing l-aspartate decarboxylase (PanD), the enzyme in M. jannaschii is a pyridoxal phosphate (PLP)-dependent l-aspartate decarboxylase encoded by MJ0050, the same enzyme that was found to decarboxylate tyrosine for methanofuran biosynthesis. A Km of ∼0.80 mM for l-aspartate with a specific activity of 0.09 μmol min(-1) mg(-1) at 70°C for the decarboxylation of l-aspartate was measured for the recombinant enzyme. The MJ0050 gene was also demonstrated to complement the Escherichia coli panD deletion mutant cells, in which panD encoding aspartate decarboxylase in E. coli had been knocked out, thus confirming the function of this gene in vivo.

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.

Acetate Production by Methanogenic Bacteria

Methanosarcina barkeri MS and 227 and Methanosarcina mazei S-6 produced acetate when grown on H 2 -CO 2 , methanol, or trimethylamine. Marked differences in acetate production by the two bacterial species were found, even though methane and cell yields were nearly the same. M. barkeri produced 30 to 75 μmol of acetate per mmol of CH 4 formed, but M. mazei produced only 8 to 9 μmol of acetate per mmol of CH 4 .

Vitamin contents of archaebacteria

The levels of six water-soluble vitamins of seven archaebacterial species were determined and compared with the levels found in a eubacterium, Escherichia coli. Biotin, riboflavin, pantothenic acid, nicotinic acid, pyridoxine, and lipoic acid contents of Halobacterium volcanii, Methanobacterium thermoautotrophicum delta H, "Archaeoglobus fulgidus" VC-16, Thermococcus celer, Pyrodictium occultum, Thermoproteus tenax, and Sulfolobus solfataricus were measured by using bioassays. The archaebacteria examined were found to contain these vitamins at levels similar to or significantly below the levels found in in E. coli. Riboflavin was found at levels comparable to those in E. coli. Pyridoxine was as abundant among the archaebacteria of the methanogenhalophile branch as in E. coli. It was only one-half as abundant in the sulfur-metabolizing branch. "A. fulgidus," however, contained only 4% as much pyridoxine as E. coli. Nicotinic and pantothenic acids were approximately 10-fold less abundant (except for a 200-fold-lower nicotinic acid level in "A. fulgidus"). Nicotinic acid may be replaced by an 8-hydroxy-5-deazaflavin coenzyme (factor F420) in some archaebacteria (such as "A. fulgidus"). Compared with the level in E. coli, biotin was equally as abundant in Thermococcus celer and Methanobacterium thermoautotrophicum, about one-fourth less abundant in P. occultum and "A. fulgidus," and 25 to over 100 times less abundant in the others. The level of lipoic acid was up to 20 times lower in H. volcanii, Methanobacterium thermoautotrophicum, and Thermococcus celer. It was over two orders of magnitude lower among the remaining organisms. With the exception of "A. fulgidus," lipoic acid, pantothenic acid, and pyridoxine were more abundant in the members of the methanogen-halophile branch of the archaebacteria than in the sulfur-metabolizing branch.

Autotrophic acetyl coenzyme A biosynthesis in Methanococcus maripaludis

To detect autotrophic CO2 assimilation in cell extracts of Methanococcus maripaludis, lactate dehydrogenase and NADH were added to convert pyruvate formed from autotrophically synthesized acetyl coenzyme A to lactate. The lactate produced was determined spectrophotometrically. When CO2 fixation was pulled in the direction of lactate synthesis, CO2 reduction to methane was inhibited. Bromoethanesulfonate (BES), a potent inhibitor of methanogenesis, enhanced lactate synthesis, and methyl coenzyme M inhibited it in the absence of BES. Lactate synthesis was dependent on CO2 and H2, but H2 + CO2-independent synthesis was also observed. In cell extracts, the rate of lactate synthesis was about 1.2 nmol min-1 mg of protein-1. When BES was added, the rate of lactate synthesis increased to 2.3 nmol min-1 mg of protein-1. Because acetyl coenzyme A did not stimulate lactate synthesis, pyruvate synthase may have been the limiting activity in these assays. Radiolabel from 14CO2 was incorporated into lactate. The percentages of radiolabel in the C-1, C-2, and C-3 positions of lactate were 73, 33, and 11%, respectively. Both carbon monoxide and formaldehyde stimulated lactate synthesis. 14CH2O was specifically incorporated into the C-3 of lactate, and 14CO was incorporated into the C-1 and C-2 positions. Low concentrations of cyanide also inhibited autotrophic growth, CO dehydrogenase activity, and autotrophic lactate synthesis. These observations are in agreement with the acetogenic pathway of autotrophic CO2 assimilation.

Autotrophic synthesis of activated acetic acid from CO2 in Methanobacterium thermoautotrophicum. Synthesis from tetrahydromethanopterin-bound C1 units and carbon monoxide

The synthesis of acetyl-CoA from CO2, H2, and various C1 compounds was studied in vitro with extracts and with protein fractions of Methanobacterium thermoautotrophicum. Acetyl-CoA synthesis from CO2 and H2 by extracts required CO2 reduction to CH4 to proceed. Both processes were highly stimulated by formaldehyde which served as the carbon precursor of both CH4 and the CH3 group of acetate. Carbon monoxide in combination with formaldehyde dramatically stimulated the acetyl-CoA synthesis up to 150-fold. In this system, which did not require CO2 reduction to the formaldehyde and CO level, acetyl-CoA synthesis was no longer dependent on CH4 formation. The soluble (100,000 X g supernatant) cell protein was resolved into a protein fraction [45-60% (NH4)2SO4-fraction] which catalyzed acetyl-CoA synthesis at a specific rate of 15 nmol X min-1 X (equivalent of mg cell protein)-1 (60 degrees C). This oxygen-sensitive enzyme reaction required dithioerythritol for activity and was strictly dependent on coenzyme A, CO, and N5,N10-methylene tetrahydromethanopterin, N5-methyl tetrahydromethanopterin or formaldehyde plus tetrahydromethanopterin. The incorporation of formaldehyde is explained by the spontaneous formation of methylene tetrahydromethanopterin. The product of the reaction, acetyl-CoA, was quantitatively derived from CO (carboxyl of acetate) and a C1 derivative of tetrahydromethanopterin (methyl of acetate). The C1 derivative of tetrahydromethanopterin could not be replaced by a C1 derivative of tetrahydrofolate or by methyl-coenzyme M; ATP was not required. The active protein fraction contained CO dehydrogenase and at least on corrinoid protein. These results provide strong biochemical arguments for the proposed mechanism of autotrophic acetyl-CoA synthesis in Methanobacterium.

Indirect observation by 13C NMR spectroscopy of a novel CO2 fixation pathway in methanogens

High-field carbon-13 nuclear magnetic resonance (NMR) spectroscopy has been used to monitor the isotopic dilution of doubly carbon-13-labeled precursors for 2,3-cyclopyrophosphoglycerate, a novel primary metabolite that occurs in certain methanogens. A unique carbon dioxide fixation pathway that gives rise to asymmetric labeling of acetyl coenzyme A has been demonstrated in Methanobacterium thermoautotrophicum. The effect of selected metabolic inhibitors on the labeled species in the pathway has been examined by NMR. These techniques establish a general, sensitive method for the delineation of convergent biosynthetic pathways.