Acetogenesis and acetotrophy in a hexanoate-catabolizing microbial association isolated from anoxic landfill

Metabolism of the key intermediates, acetate and hydrogen, in anaerobic hexanoate catabolism by an interacting microbial association isolated from a landfill was examined in the presence of sulphate. Hydrogen (the β-oxidation product of hexanoate and butyrate), was competitively utilized by the component sulphate-reducing bacteria whereas in the absence of sulphate an interaction between H₂-utilizing acetogenic and methanogenic bacteria facilitated H₂ removal, with acetate catabolism restricted to methanogenic bacteria. A possible mechanism for energy conservation was suggested in which excess electrons were stored as acetate for subsequent usage as an energy source.     

Most probable number enumeration of H2-utilizing acetogenic bacteria from the digestive tract of animals and man

Abstract A method is proposed that allows the enrichment and most probable number estimation of H₂/CO₂-utilizing acetogenic bacteria. It is based on the difference in acetate production for serial dilutions incubated under either a test H₂/CO₂ (4:1), or a control N₂/CO₂ (4:1) headspace atmosphere. A nutritionally non-selective medium was used, containing bromoethane-sulfonic acid as inhibitor of methanogenic archaea and 10% pre-incubated clarified rumen fluid. Acetogenic bacteria were enumerated in rumen and hindgut contents of animals and in human feces. They ranged from below 10² to above 10⁸ per gram wet weight gut content and their population levels were the highest in the absence of methanogenesis. The method described therein should prove useful to better understand the diversity and ecological importance of dominant gut acetogens.     

Temporal change of gas metabolism by hydrogen-syntrophic methanogenic bacterial associations in anoxic paddy soil

Abstract Interspecies H₂ transfer within methanogenic bacterial associations (MBA) accounted for 95–97% of the conversion of ¹⁴CO₂ to ¹⁴CH₄ in anoxic paddy soil. Only 3–5% of the ¹⁴CH₄ were produced from the turnover of dissolved H₂. The H₂-syntrophic MBA developed within 5 days after the paddy soil had been submerged and placed under anoxic atmosphere. Afterwards, both the contribution of MBA to H₂-dependent methanogenesis and the turnover of dissolved H₂ did not change significantly for up to 7 months of incubation. However, while the rates of H₂-dependent methanogenesis stayed relatively constant, the rates of total methanogenesis decreased. The contribution of MBA to H₂-dependent methanogenesis was further enhanced to 99% when the temperature was shifted from 30°C to 17°C, or when the soil had been planted with rice. This enhancement was partially due to an increased utilization of dissolved H₂ by chloroform-insensitive non-methanogenic bacteria, most probably homoacetogens, so that CH₄ production was almost completely restricted to H₂-syntrophic MBA. The activity of MBA, as measured by the conversion of ¹⁴CO₂ to ¹⁴CH₄, was stimulated by glucose, lactate, and ethanol to a similar or greater extent than by exogenous H₂. Propionate and acetate had no effect.     

Isolation and characterization of a thermophilic, acetate-utilizing methanogenic bacterium

Abstract A thermophilic acetate-decarboxylating methanogenic bacterium was isolated from a laboratory-scale 60°C sludge digestor. Cells form straight filaments with flat to blunted ends normally consisting of 2–3 cells held together by a sheath-like outer cell wall. The organism uses acetate, H₂-CO₂ and formate for methanogenesis and growth. With acetate as the sole methanogenic substrate, almost all of the radioactivity from methyl-labelled acetate appeared as methane. Acetate was converted to methane in equimolar amounts with a doubling time of 3 days.     

Hydrogen turnover by psychrotrophic homoacetogenic and mesophilic methanogenic bacteria in anoxic paddy soil and lake sediment

Abstract The effect of temperature on CH₄ production, turnover of dissolved H₂, and enrichment of H₂-utilizing anaerobic bacteria was studied in anoxic paddy soil and sediment of Lake Constance. When anoxic paddy soil was incubated under an atmosphere of H₂/CO₂, rates of CH₄ production increased 25°C, but decreased at temperatures lower than 20°C. Chloroform completely inhibited methano-genesis in anoxic paddy soil and lake sediment, but did not or only partially inhibit the turnover of dissolved H₂, especially at low incubation temperatures. Cultures with H₂ as energy source resulted in the enrichment of chemolithotrophic homoacetogenic bacteria whenever incubation temperatures were lower than 20°C. Hydrogenotrophic methanogens could only be enriched at 30°C from anoxic paddy soil. A homoacetogen     

Hydrogen-dependent control of the continuous thermophilic anaerobic digestion process using membrane inlet mass spectrometry

The control of a thermophilic continuous anaerobic digestion system when subjected to potential inhibitory shock loadings was achieved through the regulation of dissolved H₂, monitored using membrane inlet mass spectrometry, by the controlled addition of carbon source. At a feed pump switching threshold equivalent to 1 μmol/1 H₂ a steady state rate of methanogenesis of approximately 40 μmol/1/min was obtained. Higher H₂ thresholds resulted in an inhibition of methanogenesis, but precise control of H₂ concentration was demonstrated with an oscillatory response of period 2·5–5·0 min.     

Methanogenesis in the hypersaline Solar Lake (Sinai)

Abstract Enrichment studies on microbial mat sediments (potential stromatolites) from the hypersaline Solar Lake (Sinai) indicated high numbers of methanogenic bacteria (up to 10⁵ ml⁻¹ sediment) in spite of the high sulfate reduction rate, sulfate concentration and salinity. Among H₂/CO₂, acetate and monomethylamine, the methylated amine was the preferred substrate. The predominant species enriched was a Methanosarcina sp. The findings indicate that methanogenic bacteria play an important role in hypersaline sulfate-enriched anoxic sediments and stromatolithic microbial mats.     

Hydrogen cycling in a three-tiered food web growing on the methanogenic conversion of 3-chlorobenzoate

Abstract A defined 3-chlorobenzoate-degrading methanogenic consortium was constructed by recombining key organisms isolated from a 3-chlorobenzoate-degrading methanogenic sludge enrichment. The organisms comprise a three-tiered food chain which includes: (1) reductive dechlorination of 3-chlorobenzoate; (2) oxidation of benzoate to acetate, H₂ and CO₂; (3) removal of H₂ plus CO₂ by conversion into methane. The defined consortium, consisting of a dechlorinating organism (DCB-1), a benzoate degrader (BZ-1) and a lithotrophic methanogen ( Methanospirillum strain PM-1) grew well in a basal salts medium supplemented with 3-chlorobenzoate (3.2 mM) as the sole energy source. The chlorine released from the aromatic ringe was recovered in stoichiometric amounts as the chloride ion. The reducing power required for reductive dechlorination was obtained from the hydrogen produced in the acetogenic oxidation of benzoate. One-third of the benzoate-derived hydrogen was recycled via the reductive dechlorination of 3-chlorobenzoate, indicating that the consortium operated as a food web rather than a food chain.     

Thermodynamics of H2-consuming and H2-producing metabolic reactions in diverse methanogenic environments under in situ conditions

Abstract In situ concentrations of hydrogen and other metabolites involved in H₂-consuming and H₂-producing reactions were measured in anoxic methanogenic lake sediments, sewage sludge and fetid liquid of cottonwood. The data were used to calculate the Gibbs free energies of the metabolic reactions under the conditions prevailing in situ. The thermodynamics of most of the reactions studied were exergonic with Gibbs free energies being more negative for H₂-dependent sulfate reduction methanogenesis acetogenesis and for H₂-producing lactate fermentation ethanol fermentation. Butyrate and propionate fermentation, on the other hand, were endergonic under in situ conditions. This observation is interpreted by suggesting that butyrate and propionate is degraded within microbial clusters which shield the fermentating bacteria from the outside H₂ (and acetate) pool.     

Competition between reductive acetogenesis and methanogenesis in the pig large-intestinal flora

Washed bacterial suspensions obtained from the pig hindgut were incubated under ¹³CO₂ in a buffer containing NaH¹³CO₃ and carbohydrates. Incorporation of ¹³C into short chain fatty acids was assayed by quantitative nuclear magnetic resonance. The effects of different levels of H₂ added to the gas phase (0, 20 and 80% v/v) and of the specific methanogenesis inhibitor 2-bromoethane-sulphonic acid (BES) were determined. In control incubations increasing the concentration of H₂ markedly increased methane production. Single- and double-labelled acetate and butyrate were formed in all incubations. In the absence of BES, increasing H₂ significantly increased the incorporation of ¹³CO² into butyrate and the proportion of double-labelled acetate in total labelled acetate. The addition of BES proved to be very successful as a methane inhibitor and greatly enhanced the amount of mono- and double-labelled acetate, especially at the highest H₂ partial pressure. The results suggest that methanogenesis inhibited both routes of reductive acetogenesis, i.e. the homoacetate fermentation of hexose (represented for the most part by single labelling) and the synthesis of acetate from external CO₂ and H₂ (represented mostly by double labelling). A highly significant interaction between BES and H₂ concentration was observed. At the highest pH2 BES increased the proportion of labelled acetate in total acetate from 17.1% for the control to 50.9%. It was concluded that although acetogenesis and methanogenesis can occur simultaneously in the pig hindgut, reductive acetogenesis may become a significant pathway of acetate formation in the absence of methanogenesis.     

Involvement of a corrinoid enzyme in methanogenesis from acetate in Methanosarcina barkeri

Abstract Extracts of acetate-grown Methanosarcina barkeri strain Fusaro formed methane from acetate plus ATP and form acetyl phosphate under H₂. Coenzyme A (CoA) is stimulatory. Inhibitors of methanogenesis are cyanide, propyliodide and bromoethanesulfonic acid. In cofactor-free extracts methanogenic activity from acetate was restored by addition of ATP, CoA, coenzyme M and 7-mercaptoheptanoylthreonine phosphate.
An enzyme-bound corrinoid was found to be involved in methanogenesis from acetate.     

Aerobic and anaerobic microbial consumption of hydrogen in geothermal spring water

Abstract Hydrogen consumption was measured in hot geothermal water from two ponds of the San Federigo solfatara, Tuscany, Italy, where emanation gases contained approx. 4% H₂. H₂ consumption was completely inhibited by NaOH and partially by HgCl₂ indicating microbial utilization. Aerobic and anaerobic H₂ consumption activities coexisted in the same water with aerobic activity being higher in one pond and anaerobic activity in the other. The kinetics of H₂ consumption were consistent with those of 'Knallgas', methanogenic or sulfidogenic bacteria.     

Energy transduction in vesicles of the methanogenic strain Gö1

Abstract Everted vesicles of the methanogenic strain Gö1 synthesized ATP in response to methanogenesis from methyl-coenzyme M and H₂. Simultaneously, a transmembrane pH gradient (ΔpH) was generated as evident from fluorescence quenching of acridine orange. Protonophorous uncouplers prevented ΔpH generation and ATP synthesis, but did not affect methanogenesis. The ATP synthase inhibitor diethylstilbestrol (DES) inhibited ATP synthesis but had no effect on methanogenesis and on ΔpH formation, indicating the essential role of the transmembrane proton potential in ATP synthesis. Progress has also been made in assigning specific functions to membrane components in methanogenesis from methyl-CoM and H₂. Separation of cell extracts into cytoplasmic and membrane fraction revealed an essential role of membrane-bound components in electron transfer: methanogenesis catalyzed by the cytoplasmic fraction from strain Gö1 was stimulated several fold by membranes from various methanogens. This stimulation was prevented if the membranes had been treated with oxidants (O₂, K₃[Fe(CN)₆]) or SH reagents (Ag⁺, p -chloromercuribenzoate, iodoacetamide) pointing to the involvement of functional SH groups in methanogenesis from methyl-CoM and H₂.     

Sodium bioenergetics in methanogens and acetogens

Abstract Recent investigations with Methanosarcina barkeri elucidated the role of sodium ions in the energy metabolism of methanogenic bacteria and provided evidence for a novel mechanism of energy transduction with Na⁺ as the coupling ion. During methanogenesis from methanol, an eletrochemical sodium gradient generated by a Na⁺/H⁺ antiporter is used as the driving force for the thermodynamically unfavourable oxidation of methanol to the formal redox level of formaldehyde. During methanogenesis from H₂+ CO₂, the reverse reaction, the reduction of formaldehyde to the level of methanol, is accompanied by a primary, electron transport-driven sodium extrusion. Acetogenesis from H₂+ CO₂ as carried out by Acetobacterium woodii is a sodium-dependent process and is accompanied by the generation of a transmembrane sodium gradient with the reduction of formaldehyde to the level of methanol as the sodium-dependent step.     

Electron transfer reactions in methanogens

Abstract Methanogenic bacteria comprise a specialized group of obligately anaerobic microorganisms able to reduce a limited number of substrates to CH₄. The intermediates involved in this reduction process remain bound to a series of typical C₁-carriers. Reducing equivalents are either obtained from the oxidation of H₂ or from oxidation of carbon substrates to CO₂. Electron transfer reactions thus constitute the very essence of the process of methanogenesis.
In recent years much progress has been made in the elucidation of the special metabolic pathways and the nature of the C₁-carriers involved in methanogenic bacteria. The energy generated at the oxidoreduction reactions, notably at the methylreductase step, is conserved by ATP synthesis. The energy is used for cell carbon synthesis and, in catalytic amounts, for the reductive activation of some methanogenic enzymes. Before the condensing reaction resulting in the formation of acetyl-CoA takes place, 2 C₁-units are reduced or oxidized depending on the substrate to a carbonyl and a -CH₃ group. Formation of the latter proceeds via the methanogenic route. Intermediary cell carbon synthesis starting from acetyl-CoA involves reductive carboxylations and oxidoreductions by the participation of the enzymes of the tricarboxylic acid cycle.     

Isolation and characterization of methanogenic bacteria from rice paddies

Abstract Enrichment cultures for H₂-CO₂, methanol- or acetate-utilizing methanogens were prepared from two rice field soil samples. All the cultures except one acetate enrichment showed significant methane production. Pure cultures of Methanobacterium - and Methanosarcina -like organisms were isolated from H₂-CO₂ and methanol enrichment cultures, respectively, and were characterized for various nutritional and growth conditions. The organisms had an optimal pH range of 6.4–6.6 and a temperature optimum of 37°C. The Methanobacterium isolates were able to utilize H₂-CO₂ but no other substrates as sole energy source, while the Methanosarcina isolates were able to utilize methanol, methylamines or H₂-CO₂ as sole energy sources. Both Methanobacterium isolates and one isolate of Methanosarcina were able to use dinitrogen as the sole source of nitrogen for growth. The isolates used several sulfur compounds as sole sources of sulfur.     

Kinetics of two complementary hydrogen sink reactions in a defined 3-chlorobenzoate degrading methanogenic co-culture

Abstract The interrelationships between an obligate hydrogen-producing and two different hydrogen-scavenging populations grown as synthrophic members of a 3-chlorobenzoate degrading methanogenic consortium were studied. The hydrogen producer was a benzoate degrader (strain BZ-2), and the hydrogen consumers were a 3-chlorobenzoate dechlorinating bacterium ( Desulfomonile tiedjei ) and a hydrogenotropic methanogen ( Methanospirillum strain PM-1). When a mixture of 3-chlorobenzoate plus benzoate was added to this consortium, the rate of benzoate degradation was 50% higher, at slightly lower H₂ concentrations, than when benzoate alone was added. The enhanced benzoate degradation rate was apparantly triggered by the lower H₂ concentration, as the rate of benzoate degradation was shown to be a function of the H₂ concentration. By offering a hydrogen sink, in addition to methanogenesis, the dechlorinating hydrogen-scavenging population stimulated the rate of benzoate degradation. The lowering of the H₂ concentration was very small, which was in agreement with the observation that the rate of methanogenesis was hardly affected by this lower hydrogen concentration. Thus there was no significant competition for H₂ between the two hydrogen-scavenging populations in the consortium, as they practically complemented each other's hydrogen-scavenging potential at in situ hydrogen concentrations during the degradation of 3-chlorobenzoate. The H₂ concentrations at which hydrogen driven methanogenesis by Methanospirillum occurred in the consortium were well below the threshold concentration extrapolated for this methanogen after growth at high H₂ concentrations.     

A strict anaerobic extreme thermophilic hydrogen-producing culture enriched from digested household waste

Aims:  The aim of this study was to enrich, characterize and identify strict anaerobic extreme thermophilic hydrogen (H₂) producers from digested household solid wastes.
Methods and Results:  A strict anaerobic extreme thermophilic H₂ producing bacterial culture was enriched from a lab-scale digester treating household wastes at 70°C. The enriched mixed culture consisted of two rod-shaped bacterial members growing at an optimal temperature of 80°C and an optimal pH 8·1. The culture was able to utilize glucose, galactose, mannose, xylose, arabinose, maltose, sucrose, pyruvate and glycerol as carbon sources. Growth on glucose produced acetate, H₂ and carbon dioxide. Maximal H₂ production rate on glucose was 1·1 mmol l⁻¹ h⁻¹ with a maximum H₂ yield of 1·9 mole H₂ per mole glucose. 16S ribosomal DNA clone library analyses showed that the culture members were phylogenetically affiliated to the genera Bacillus and Clostridium. Relative abundance of the culture members, assessed by fluorescence in situ hybridization, were 87 ± 5% and 13 ± 5% for Bacillus and Clostridium , respectively.
Conclusions:  An extreme thermophilic, strict anaerobic, mixed microbial culture with H₂-producing potential was enriched from digested household wastes.
Significance and Impact of the Study:  This study provided a culture with a potential to be applied in reactor systems for extreme thermophilic H₂ production from complex organic wastes.     

Effect of dilution on methanogenesis, hydrogen turnover and interspecies hydrogen transfer in anoxic paddy soil

Abstract Dilution of anoxic slurries of paddy soil resulted in a proportional decrease of the rates of total methanogenesis and the rate constants of H₂ turnover per gram soil. Dilution did not affect the fraction of H₂/CO₂-dependent methanogenesis which made up 22% of total CH₄ production. However, dilution resulted in a ten fold decrease of the H₂ steady state partial pressure from approximately 4 to 0.4 Pa indicating that H₂/CO₂-dependent methanogenesis was more or less independent of the H₂ pool. The rates of H₂ production calculated from the H₂ turnover rate constants and the H₂ steady state partial pressures accounted for only < 5% of H₂/CO₂-dependent methanogenesis in undiluted soil slurries and for even less after dilution. Upon dilution, the Gibbs free energy available for H₂/CO₂-dependent methanogenesis decreased from −28.4 to only −5.6 kJ per mol. The results indicate that methane was mainly produced from interspecies H₂ transfer within syntrophic bacterial associations and was not significantly affected by the outside H₂ pool.     

Acetogenesis from H2 and CO2 by methane- and non-methane-producing human colonic bacterial communities

Abstract: The purpose of the study was to define the potential for reductive acetogenesis of colonic microflora from six non-methane- and four methane-excreting human subjects in relation to numbers of the different H₂-utilizing microorganisms. Faecal bacterial suspensions were incubated in the presence of NaH¹³CO₃ and under a gas phase composed of either 100% N₂ (control) or 80% H₂–20% N₂. The effects of a specific methanogenesis inhibitor or of sulfate supplementation were also determined. Quantitative nuclear magnetic resonance showed the presence of both single- and double-labelled acetate in all incubations under hydrogen. H₂/CO₂-acetogenesis appears to be a quantitatively important activity only in the presence of very low numbers of methanogens. Inhibition of methanogenesis induced a large increase in ¹³CO₂ incorporation into acetate in CH₄-producing samples. These results showed that methanogens can efficiently outcompete acetogens in human colonic contents. In contrast, no clear-cut competition for H₂ between acetogenesis and dissimilatory sulfate-reduction could be demonstrated. A slight reduction of the acetogenic activity was only observed at the highest sulfate addition (100 mM).