Effect of 2,4-dinitrophenol and ionophores on growth and methanogenesis inMethanobacterium thermoautotrophicum

2,4-Dinitrophenol and gramicidin D completely inhibited growth and methanogenesis inMethanobacterium thermoautotrophicum. At low K⁺ concentrations valinomycin inhibited growth and methanogenesis relatively slightly, at high K⁺ concentrations (0.1m KCl) growth was inhibited completely and methanogenesis by about 50%. Monensin and nigericin inhibited growth completely; methanogenesis was inhibited like with valinomycin at high K⁺ concentrations. The results can be interpreted in terms of Mitchell’s chemiosmotic theory as follows. The protonmotive force inM. thermoautotrophicum is the basic source of energy for endergonic processes. Dissipation of the electrical component of protonmotive force may probably be compensated by an increased generation of the proton gradient. However, the osmotic component is essential for growth ofM. thermoautotrophicum.     

Methanogenesis in McLean Bog,an Acidic Peat Bog in Upstate New York: Stimulation by H2/CO2 in the Presence of Rifampicin,or by Low Concentrations of Acetate

Acidic peat bog soils produce CH₄ and although molecular biological studies have demonstrated the presence of diverse methano-genic populations in them, few studies have sustained methanogenesis by adding the CH₄ precursors H₂/CO₂ or acetate, and few indigenous methanogens have been cultured. McLean Bog is a small (ca. 70 m across), acidic (pH 3.4–4.3) Sphagnum -dominated bog in upstate New York. Although addition of H₂/CO₂ or 10 mM acetate stimulated methanogenesis in soils from a nearby circumneutral-pH fen, neither of these substrates led to sustained methanogenesis in McLean Bog soil slurries. After a brief period of stimulation by H₂/CO₂, methanogenesis in McLean Bog soil declined, which could be attributed to buildup of large amounts of acetic acid produced from the H₂/CO₂ by acetogens. Addition of the antibiotic rifampicin inhibited acetogenesis (carried out by Bacteria) and allowed methanogenesis (carried out by Archaea) to continue. Using rifampicin, we were able to study effects of temperature, pH, and salts on methanogenesis from H₂/CO₂ in McLean Bog soil samples. The enriched H₂/CO₂-utilizing methanogens showed an optimum for activity near pH 5, and a temperature optimum near 35°C. Methanogenesis was not stimulated by addition of 10 mM acetate, but it was stimulated by 1 mM acetate, and multiple additions were consumed at increasing rates and nearly stoichiometrically converted to CH₄. In conclusion, we have found that both hydrogentrophic and aceticlastic methanogens are present in McLean Bog soils, and that methanogenic activity can be stimulated using H₂/CO₂ in the presence of rifampicin, or using low concentrations of acetate.     

Phosphate Inhibits Acetotrophic Methanogenesis on Rice Roots

The contribution of acetate- and H₂/CO₂-dependent methanogenesis to total CH₄ production was determined in excised washed rice roots by radiolabeling, methyl fluoride inhibition, and stable carbon isotope fractionation. Addition of ≥20 mM phosphate inhibited methanogenesis, which then was exclusively from H₂/CO₂. Otherwise, acetate contributed about 50 to 60% of the total methanogenesis, demonstrating that phosphate specifically inhibited acetotrophic methanogens on rice roots.     

Valinomycin inhibited methane synthesis in Methanobacteriumthermoautotrophicum

$\text{Methanobacterium}\text{thermoautotrophicum}$ cells, incubated anaerobically under H₂ in 0.1 M KCl or 0.1 M NaCl, above pH 7.5, are interior acid with respect to the incubation medium. The pH gradient thus established can be discharged by either carbonyl cyanide m-chlorophenylhydrazone or valinomycin at high concentration (17μM). In these cells, which actively synthesize CH₄ from CO₂ and H₂, methanogenesis is strongly inhibited when the pH gradient is discharged.     

Trophic links between fermenters and methanogens in a moderately acidic fen soil

Trophic links between fermentation and methanogenesis of soil derived from a methane‐emitting, moderately acidic temperate fen (pH 4.5) were investigated. Initial CO₂:CH₄ production ratios in anoxic microcosms indicated that methanogenesis was concomitant to other terminal anaerobic processes. Methane production in anoxic microcosms at in situ pH was stimulated by supplemental H₂–CO₂, formate or methanol; supplemental acetate did not stimulate methanogenesis. Supplemental H₂–CO₂, formate or methanol also stimulated the formation of acetate, indicating that the fen harbours moderately acid‐tolerant acetogens. Supplemental monosaccharides (glucose, N‐acetylglucosamine and xylose) stimulated the production of CO₂, H₂, acetate and other fermentation products when methanogenesis was inhibited with 2‐bromoethane sulfonate 20 mM. Glucose stimulated methanogenesis in the absence of BES. Upper soil depths yielded higher anaerobic activities and also higher numbers of cells. Detected archaeal 16S rRNA genes were indicative of H₂–CO₂‐ and formate‐consuming methanogens (Methanomicrobiaceae), obligate acetoclastic methanogens (Methanosaetaceae) and crenarchaeotes (groups I.1a, I.1c and I.3). Molecular analyses of partial sequences of 16S rRNA genes revealed the presence of Acidobacteria, Nitrospirales, Clamydiales, Clostridiales, Alpha‐, Gamma‐, Deltaproteobacteria and Cyanobacteria. These collective results suggest that this moderately acidic fen harbours phylogenetically diverse, moderately acid tolerant fermenters (both facultative aerobes and obligate anaerobes) that are trophically linked to methanogenesis.     

Fate of Immediate Methane Precursors in Low-Sulfate, Hot-Spring Algal-Bacterial Mats

The fates of acetate and carbon dioxide were examined in several experiments designed to indicate their relative contributions to methane production at various temperatures in two low-sulfate, hot-spring algal-bacterial mats. [2-¹⁴C]acetate was predominantly incorporated into cell material, although some ¹⁴CH₄ and ¹⁴CO₂ was produced. Acetate incorporation was reduced by dark incubation in short-term experiments and severely depressed by a 2-day preincubation in darkness. Autoradiograms showed that acetate was incorporated by long filaments resembling phototrophic microorganisms of the mat communities. [³H]acetate was not converted to C³H₄ in samples from Octopus Spring collected at the optimum temperature for methanogenesis. NaH¹⁴CO₃ was readily converted to ¹⁴CH₄ at temperatures at which methanogenesis was active in both mats. Comparisons of the specific activities of methane and carbon dioxide suggested that of the methane produced, 80 ± 6% in Octopus Spring and 71 ± 21% in Wiegert Channel were derived from carbon dioxide. Addition of acetate to 1 mM did not reduce the relative importance of carbon dioxide as a methane precursor in samples from Octopus Spring. Experiments with pure cultures of Methanobacterium thermoautotrophicum suggested that the measured ratio of specific activities might underestimate the true contribution of carbon dioxide in methanogenesis.     

Microbial Methanogenesis and Acetate Metabolism in a Meromictic Lake

Methanogenesis and the anaerobic metabolism of acetate were examined in the sediment and water column of Knaack Lake, a small biogenic meromictic lake located in central Wisconsin. The lake was sharply stratified during the summer and was anaerobic below a depth of 3 m. Large concentrations (4,000 μmol/liter) of dissolved methane were detected in the bottom waters. A methane concentration maximum occurred at 4 m above the sediment. The production of ¹⁴CH₄ from ¹⁴C-labeled HCOOH, HCO₃⁻, and CH₃OH and [2-¹⁴C]acetate demonstrated microbial methanogenesis in the water column of the lake. The maximum rate of methanogenesis calculated from reduction of H¹⁴CO₃⁻ by endogenous electron donors in the surface sediment (depth, 22 m) was 7.6 nmol/h per 10 ml and in the water column (depth, 21 m) was 0.6 nmol/h per 10 ml. The methyl group of acetate was simultaneously metabolized to CH₄ and CO₂ in the anaerobic portions of the lake. Acetate oxidation was greatest in surface waters and decreased with water depth. Acetate was metabolized primarily to methane in the sediments and water immediately above the sediment. Sulfide inhibition studies and temperature activity profiles demonstrated that acetate metabolism was performed by several microbial populations. Sulfide additions (less than 5 μg/ml) to water from 21.5 m stimulated methanogenesis from acetate, but inhibited CO₂ production. Sulfate addition (1 mM) had no significant effect on acetate metabolism in water from 21.5 m, whereas nitrate additions (10 to 14,000 μg/liter) completely inhibited methanogenesis and stimulated CO₂ formation.     

Molecular weight and quaternary structure of ribulose bisphosphate carboxylase from the cyanobacterium,Synechococcus sp.

Inhibition of photosynthetic growth of Rhodopseudomonas capsulata by metronidazole was dependent on the nitrogen supply in culture solutions. Cultures fixing dinitrogen were more susceptible to inhibition by low concentrations than those supplied with NH ₄ ⁺ . Light-dependent C₂H₂ reduction and H₂ production by washed cells were inhibited by 80% and 60% respectively by 1 mM metronidazole. When this compound was first reduced with H₂-palladised asbestos prior to assay, it only partially restricted C₂H₂ reduction in washed cells (33%) compared with unreduced inhibitor (68%). Metronidazole was without effect on other metabolic functions. Thus, even at 40 mM it did not inhibit either (a) dark or light respiration in cells grown under photo- and chemo-heterotrophic conditions; (b) H₂-dependent photoreduction of ¹⁴CO₂; (c) -glutamyltransferase activity of glutamine synthetase in cell-free extracts (25 mM inhibitor).Metronidazole (1 mM) completely inhibited C₂H₂ reduction by washed cells of Azotobacter vinelandii. The dithionite-dependent C₂H₂ reduction of a partially purified nitrogenase was only partially inhibited (30%) by 1 mM metronidazole.     

Formate production and utilization by methanogens and by sewage sludge consortia — interference with the concept of interspecies formate transfer

Pure cultures of H₂/CO₂- and formate-utilizing methanogens or mixed consortia of sewage sludge generated some formate from H₂/CO₂ at H₂ partial pressure in the gas phase above 200 kPa. At decreasing H₂ partial pressure the formate was taken up again and converted to methane. If methanogenesis was inhibited by bromoethanesulphonic acid (BESA) or a high redox potential (–180 to –200 mV), formate-utilizing methanogens produced high amounts of formate from H₂/CO₂. No formate was excreted by the species, which could only utilize H₂/CO₂ for methanogenesis. In contrast, H₂ formation from formate was observed in cultures of Methanobacterium thermoformicicum and M. formicicum. Measurable amounts were, however, only formed if its immediate utilization for methane production was inhibited by BESA. In the light of the data on formate formation from H₂/CO₂ and its re-utilization by all formate-utilizing methanogens, the concept of interspecies formate transfer of Thiele and Zeikus should be reconsidered. In pure cultures of methanogens or complex ecosystems with excess H₂, formate formation seemed to serve more as a means of disposal of surplus reducing power than for H₂ transfer. Correspondence to: J. Winter     

Monensin and gramicidin stimulate CH4 formation from H2 and CO2 in Methanobacterium thermoautotrophicum at low external Na+ concentration

Methane formation from H₂ and CO₂ in methanogenic bacteria is a Na⁺-dependent process. In this communication the effects of Na⁺ ionophores, of uncouplers, and of Na⁺/H⁺ antiporter inhibitors on methane formation from H₂ and CO₂ were studied with Methanobacterium thermoautotrophicum.

1. Na⁺ ionophores (the Na⁺/H⁺ antiporters monensin and lasalocid and the Na⁺ uniporter gramicidin) stimulated methanogenesis at lwo external Na⁺ concentrations when the K⁺ concentration was high. The ionophores had no effect at high external Na⁺ concentrations and were inhibitory at low external K⁺ concentrations.
2. Uncouplers (protonophores and valinomycin plus K⁺) inhibited methanogenesis at low external Na⁺ concentration at both low and high external K⁺ concentrations. Inhibition by uncouplers was relieved by the addition of either Na⁺ or Na⁺ ionophores.
3. Na⁺/H⁺ antiporter inhibitors (harmaline, amiloride, and NH ₄ ⁺ ) inhibited methanogenesis at low external Na⁺ concentration. Inhibition was relieved by the addition of either Na⁺ or of the Na⁺ ionophores.

The results are discussed with respect to the role of Na transport across the cytoplasmic membrane in methanogenesis from H₂ and CO₂.     

Nutrition and factors limiting the growth of a methanogenic bacterium (Methanobacterium thermoautotrophicum)

The purification of Methanobacterium thermoautotrophicum from a culture contaminated with a heterotrophic organism is described. A defined inorganic medium under H₂/CO₂ (80:20 v/v) has been developed to support growth of M. thermoautotrophicum up to a concentration of at least 1.7 g dry weight/l. In a conventional medium iron and nitrogen sources were found to be growth-limiting factors. Throughout most of the culture period the rate of transfer of hydrogen or carbon dioxide from gas to liquid was the factor which controlled the growth rate.The growth yields of bacteria were in the range 0.6–1.6 g dry weight/mole CH₄.Abbreviation TGP thioglycollate peptone medium     

Carbon and Electron Flow in Mud and Sandflat Intertidal Sediments at Delaware Inlet, Nelson, New Zealand

An investigation of carbon and electron flow in mud and sandflat intertidal sediments showed that the terminal electron acceptor was principally sulfate and that the carbon flow was mainly to CO₂. Studies with thin layers of sediment exposed to H₂ showed that methane production accounted for virtually none of the H₂ utilized, whereas sulfate reduction accounted for a major proportion of the gas uptake. At all sampling sites except one (site B7), rates of methanogenesis were low but sulfate concentrations in the interstitial water were high (>18 mM). At site B7, the sulfate concentrations declined with depth from 32 mM at 2 cm to <1 mM at 10 cm or below, and active methanogenesis occurred in the low-sulfate zone. Sulfate-reducing activity at this site initially decreased and then increased with depth so that elevated rates occurred in both the active and nonactive methanogenic zones. The respiratory index (RI) [RI = ¹⁴CO₂/(¹⁴CO₂ + ¹⁴CH₄)] for [2-¹⁴C]acetate catabolism at site B7 ranged from 0.98 to 0.2 in the depth range of 2 to 14 cm. Addition of sulfate to sediment from the low-sulfate zone resulted in an increase in RI and a decrease in methanogenesis. At all other sites examined, RI ranged from 0.97 to 0.99 and was constant with depth. The results suggested that although methanogenesis was inhibited by sulfate (presumably through the activity of sulfate-reducing bacteria), it was not always limited by sulfate reduction.     

Anaerobic Degradation of Lactate by Syntrophic Associations of Methanosarcina barkeri and Desulfovibrio Species and Effect of H2 on Acetate Degradation

When grown in the absence of added sulfate, cocultures of Desulfovibrio desulfuricans or Desulfovibrio vulgaris with Methanobrevibacter smithii (Methanobacterium ruminantium), which uses H₂ and CO₂ for methanogenesis, degraded lactate, with the production of acetate and CH₄. When D. desulfuricans or D. vulgaris was grown in the absence of added sulfate in coculture with Methanosarcina barkeri (type strain), which uses both H₂-CO₂ and acetate for methanogenesis, lactate was stoichiometrically degraded to CH₄ and presumably to CO₂. During the first 12 days of incubation of the D. desulfuricans-M. barkeri coculture, lactate was completely degraded, with almost stoichiometric production of acetate and CH₄. Later, acetate was degraded to CH₄ and presumably to CO₂. In experiments in which 20 mM acetate and 0 to 20 mM lactate were added to D. desulfuricans-M. barkeri cocultures, no detectable degradation of acetate occurred until the lactate was catabolized. The ultimate rate of acetate utilization for methanogenesis was greater for those cocultures receiving the highest levels of lactate. A small amount of H₂ was detected in cocultures which contained D. desulfuricans and M. barkeri until after all lactate was degraded. The addition of H₂, but not of lactate, to the growth medium inhibited acetate degradation by pure cultures of M. barkeri. Pure cultures of M. barkeri produced CH₄ from acetate at a rate equivalent to that observed for cocultures containing M. barkeri. Inocula of M. barkeri grown with H₂-CO₂ as the methanogenic substrate produced CH₄ from acetate at a rate equivalent to that observed for acetate-grown inocula when grown in a rumen fluid-vitamin-based medium but not when grown in a yeast extract-based medium. The results suggest that H₂ produced by the Desulfovibrio species during growth with lactate inhibited acetate degradation by M. barkeri.     

Presence of a Na+/H+ antiporter in Methanobacterium thermoautotrophicum and its role in Na+ dependent methanogenesis

Methane formation from H₂/CO₂ by methanogenic bacteria is dependent on Na⁺ ions. In this communication it is shown with Methanobacterium thermoautotrophicum that a Na⁺/H⁺ antiporter plays a role in methane formation from H₂ and CO₂ and in the regulation of the ΔpH. This is based on the following findings:

1. Li⁺ ions, an alternative substrate of Na⁺/H⁺ antiporters, could replace Na⁺ in stimulating methanogenesis from H₂ and CO₂.
2. Harmaline, amiloride, and NH ₄ ⁺ , which are inhibitors of Na⁺/H⁺ antiporters, inhibited methanogenesis; inhibition was competitive to Na⁺ or Li⁺.
3. Addition of Na⁺ or Li⁺ rather than of other cations to cell suspensions resulted in an acidification of the suspension medium. The rate and extent of acidification was affected by those inhibitors, which inhibited methanogenesis competitively to Na⁺ or Li.
4. During methane formation from H₂ and CO₂ the generation of a ΔpH (inside alkaline) was dependent on the presence of Na⁺ or Li⁺. However, methanogenesis was also dependent on Na⁺ or Li⁺ under conditions where ΔpH was zero.
5. ATP synthesis driven by an electrogenic potassium efflux was significantly enhanced in the presence of Na⁺ or Li⁺. Na⁺ or Li⁺ were shown to prevent acidification of the cytoplasm under these conditions.

     

Acetate assimilation and the synthesis of alanine,aspartate and glutamate inMethanobacterium thermoautotrophicum

Cultures of the autotrophic bacteriumMethanobacterium thermoautotrophicum were shown to assimilate acetate when grown on CO₂ and H₂ in the presence of acetate. At 1 mM acetate 10% of the cell carbon came from acetate, the rest from CO₂. At higher concentrations the percentage increased to reach a maximum of 65%at acetate concentrations higher than 20 mM. The data suggest that acetate may be an important carbon source under physiological conditions.The incorporation of acetate into alanine, aspartate and glutamate was studied in more detail. The cells were grown on CO₂ and H₂ in the presence of 1 mM U-¹⁴C-acetate. The three amino acids were isolated from the labelled cells by a simplified procedure. Alanine, aspartate and glutamate were found to have the same specific radioactivity. Degradation studies showed that C₁ of alanine C₁ and C₄ of aspartate, and C₁ and C₅ of glutamate were exclusively derived from CO₂, whereas C₂ and C₃ alamine and aspartate, and C₃ and C₄ of glutamate were partially derived from acetate. These findings and the presence of pyruvate synthase, phosphoenolpyruvate carboxylase and -ketoglutarate synthase inM. thermoautotrophicum indicate that CO₂ is assimilated into the three amino acids via acetyl CoA carboxylation to pyruvate, phosphoenolpyruvate carboxylation to oxaloacetate, and succinyl CoA carboxylation to -ketoglutarate.     

Microbial community structure in a biofilm anode fed with a fermentable substrate: The significance of hydrogen scavengers

We compared the microbial community structures that developed in the biofilm anode of two microbial electrolysis cells fed with ethanol, a fermentable substrate—one where methanogenesis was allowed and another in which it was completely inhibited with 2‐bromoethane sulfonate. We observed a three‐way syntrophy among ethanol fermenters, acetate‐oxidizing anode‐respiring bacteria (ARB), and a H₂ scavenger. When methanogenesis was allowed, H₂‐oxidizing methanogens were the H₂ scavengers, but when methanogenesis was inhibited, homo‐acetogens became a channel for electron flow from H₂ to current through acetate. We established the presence of homo‐acetogens by two independent molecular techniques: 16S rRNA gene based pyrosequencing and a clone library from a highly conserved region in the functional gene encoding formyltetrahydrofolate synthetase in homo‐acetogens. Both methods documented the presence of the homo‐acetogenic genus, Acetobacterium, only with methanogenic inhibition. Pyrosequencing also showed a predominance of ethanol‐fermenting bacteria, primarily represented by the genus Pelobacter. The next most abundant group was a diverse community of ARB, and they were followed by H₂‐scavenging syntrophic partners that were either H₂‐oxidizing methanogens or homo‐acetogens when methanogenesis was suppressed. Thus, the community structure in the biofilm anode and suspension reflected the electron‐flow distribution and H₂‐scavenging mechanism. Biotechnol. Bioeng. 2010;105: 69–78. © 2009 Wiley Periodicals, Inc.     

Adaptation of methane formation and enzyme contents during growth of Methanobacterium thermoautotrophicum (strain ΔH) in a fed-batch fermentor

During growth of Methanobacterium thermoautotrophicum in a fed-batch fermentor, the cells are confronted with a steady decrease in the concentration of the hydrogen energy supply. In order to investigate how the organism responds to these changes, cells collected during different growth phases were examined for their methanogenic properties. Cellular levels of the various methanogenic isoenzymes and functionally equivalent enzymes were also determined. Cells were found to maintain the rates of methanogenesis by lowering their affinity for hydrogen: the apparent K _m ^H2 decreased in going from the exponential to the stationary phase. Simultaneously, the maximal specific methane production rate changed. Levels of H₂-dependent methenyl-tetrahydromethanopterin dehydrogenase (H₂-MDH) and methyl coenzyme M reductase isoenzyme II (MCR II) decreased upon entry of the stationary phase. Cells grown under conditions that favored MCR II expression had higher levels of MCR II and H₂-MDH, whereas in cells grown under conditions favoring MCR I, levels of MCR II were much lower and the cells had an increased affinity for hydrogen throughout the growth cycle. The use of thiosulfate as a medium reductant was found to have a negative effect on levels of MCR II and H₂-MDH. From these results it was concluded that M. thermoautotrophicum responds to variations in hydrogen availability and other environmental conditions (pH, growth temperature, medium reductant) by altering its physiology. The adaptation includes, among others, the differential expression of the MDH and MCR isoenzymes.     

Function of H2-forming methylenetetrahydromethanopterin dehydrogenase from Methanobacterium thermoautotrophicum in coenzyme F420 reduction with H2

Summary In most methanogenic archaea, two hydrogenase systems that can catalyze the reduction of coenzyme F₄₂₀ (F₄₂₀) with H₂ are present: (1) the F₄₂₀-reducing hydrogenase, which is a nickel iron-sulfur flavoprotein composed of three different subunits, and (2) the N ⁵, N¹⁰-methylenetetrahydromethanopterin dehydrogenase system, which is composed of H₂-forming methylenetetrahydromethanopterin dehydrogenase and F₄₂₀-dependent methylenetetrahydromethanopterin dehydrogenase, both metal-free proteins without an apparent prosthetic group. We report here that in nickel-limited chemostat cultures of Methanobacterium thermoautotrophicum, the specific activity of the F₄₂₀-reducing Ni/Fe-hydrogenase was essentially zero, whereas that of the H₂-forming methylenetetrahydromethanopterin dehydrogenase was six times higher, and that of the F₄₂₀-dependent methylenetetrahydromethanopterin dehydrogenase was four times higher than in cells grown under non-nickel-limited conditions. This evidence supports the hypothesis that when M. thermoautotrophicum grows under conditions of nickel limitation, the reduction of F₄₂₀ with H₂ is catalyzed by the metal-free methylenetetrahydromethanopterin dehydrogenase system. Received: 9 September 1997 / Accepted: 30 October 1997     

Function of fumarate reductase in methanogenic bacteria (Methanobacterium)

Methanogenic bacteria contain high activities of fumarate reductase. An interesting hypothesis has recently been advanced that this enzyme, in cooperation with a succinate dehydrogenase, functions in a fumarate-succinate cycle for ATP synthesis. This hypothesis was tested by determining whether [2, 3-³H] succinate loses³H when taken up by growing cells.Methanobacterium thermoautotrophicum was grown on H₂ plus CO₂ in the presence of [U-¹⁴C, 2,3-³H] succinate. The double labelled dicarboxylic acid was found to be incorporated into cell material with the loss of only 30% of tritium. Neither was³H released into H₂O in significant amounts. This finding excludes a catabolic oxidation of succinate to fumarate in the growing cells and thus the operation of a fumaratesuccinate cycle. It is shown that the function of fumarate reductase inM. thermoautotrophicum is to provide the cells with succinate for the synthesis of -ketoglutarate, an intermediate in glutamate, arginine and proline synthesis.     

Autotrophic synthesis of activated acetic acid from two CO2 in Methanobacterium thermoautotrophicum

In a previous study with Methanobacterium thermoautotrophicum evidence was presented that methanogenesis and autotrophic synthesis of activated acetic acid from CO₂ are linked processes. In this study one-carbon metabolism was investigated with growing cultures and in vitro.Serine was shown to be converted into glycine and activated formaldehyde, but only traces of label from [¹⁴C-3] of serine appeared in biosynthetic one-carbon positions. This seeming discrepancy could be explained if the same activated formaldehyde is an intermediate in biosynthesis and in methanogenesis from CO₂. This hypothesis was supported by demonstrating that [¹⁴C-3] of serine and [¹⁴C] formaldehyde were rapidly converted into methane, but a small portion of the label was also specifically incorporated into the methyl group of acetate. Methane and acetate synthesis in vitro were similarly stimulated by various compounds. These experiments indicate that the methyl of acetate and methane share common one-carbon precursor(s), i.e. methylene tetrahydromethanopterin, which can also be formed enzymatically from C-3 of serine or chemically from formaldehyde.Propyl iodide 20–40 M) and methyl iodide (1–3 M) completely inhibited growth in the dark. This effect was abolished by light. Methane formation was hardly affected. When ¹⁴CH₃I was applied at an only slightly inhibitory concentration, ¹⁴C was incorporated into the methyl of acetate. In vitro, similar effects on [¹⁴C] acetate formation from ¹⁴CO₂ or from [¹⁴C-3] of serine were observed, except that methyl iodide did not inhibit, but even stimulated acetate synthesis. These experiments indicate that a corrinoid is involved in acetate synthesis and probably not in methanogenesis from CO₂; the metal is light-reversibly alkylated and functions in methyl transfer to the acetate methyl.