Thermodynamics of hydrogen metabolism in methanogenic cocultures degrading ethanol or lactate

Pure cultures of Desulfovibrio vulgaris or Pelobacter acetylenicus do not grow with lactate or ethanol, respectively, under obligately proton- reducing conditions. However, a small part of these substrates was oxidized and molecular hydrogen was produced up to 4.2 and 3.2 kPa, respectively. During growth in syntrophic methanogenic cocultures with Methanospirillum hungatei as partner, maximum hydrogen partial pressures were significantly lower (0.7 to 2.5 kPa) than in the corresponding pure cultures. Calculation of Gibbs free energies for the prevailing culture conditions showed that H₂ partial pressures were kept in a range at which both, H₂-producing and H₂-consuming reactions, were thermodynamically permissive in pure as well as in syntrophic mixed cultures.     

Characterization of populations of aerobic hydrogen-oxidizing soil bacteria

Abstract Freshly isolated soil bacteria were screened for different characteristics of the H₂ metabolism without prior selection for growth on H₂. The bacteria were isolated from different grain size fractions of a neutral meadow cambisol and an acidic forest cambisol, and then tested (1) for the ability to oxidize H₂, (2) for chemolithoautotrophic growth on H₂ as sole electron donor and energy source, (3) for DNA-DNA-hybridization with two hydrogenase gene fragments from Alcaligenes eutrophus and Rhizobium leguminosarum , and (4) for reduction of 2,3,5-triphenyl-2H-tetrazoliumchloride (TTC) in the presence of H₂. Many (65–90%) of the isolates were able to reduce TTC, but only 30–65% were actually able to oxidize H₂ indicating that the TTC test was not a specific characteristic for H₂ oxidation ability. The TTC test was only reliable in pure cultures of known bacteria with optimized test conditions, here shown for Alcaligenes eutrophus, Bradyrhizobium japonicum and Nocardia opaca , but not in mixed cultures of unknown bacteria. Still less (< 30%) of the isolates were able to grow chemolithoautotrophically indicating that culturable aerobic bacteria with the ability for H₂ oxidation are more abundant than bacteria with the ability for chemolithoautotrophic growth. The DNA-DNA-hybridization test failed to detect many of the bacteria with H₂ oxidation activity, probably since the hydrogenase genes present in the isolates were too diverse to be all detected by the DNA probes applied.     

Hydrogen-using bacteria in a methanogenic acetate enrichment culture

A rcher , D.B. 1984. Hydrogen-using bacteria in a methanogenic acetate enrichment culture. Journal of Applied Bacteriology 56 , 125–129.
In a study of the anaerobic utilization of acetate, an enrichment culture of sewage sludge organisms was initiated with calcium acetate as the sole carbon and energy source. A mixed bacterial population became established from which 14 anaerobic species were isolated. Two of the isolates were methanogenic bacteria but only one of these, Methanosarcina barkeri , utilised acetate as an energy source in axenic culture. The other methanogenic isolate, a Methanobacterium sp., utilised H₂/CO₂ but not acetate. A third methanogen, which was morphologically identical to Methanothrix soehngenii , was detected in the enrichment but was not obtained in monoculture. 2-Bromoethanesulphonate, a specific inhibitor of methanogenesis. completely inhibited the enrichment at a concentration of 10 μmol/1. Addition of H₂ formate or methanol to the enrichment did not affect the rate of methanogenesis. An H₂-utilizing Desulfovibrio sp. was also isolated from the enrichment.     

Breakdown of dimethyl sulphide by mixed cultures and by Thiobacillus thioparus

Abstract Dimethyl sulphide (DMS) was degraded by acclimatized activated sludge and by a mixed culture of Thiobacillus thioparus TK-1 and Pseudomonas sp. AK-2. While both these organisms persisted in stable co-culture on DMS, it was found that T. thioparus TK-1 and the derived strain TK-m grew in pure culture on DMS, and oxidized DMS with an apparent K _m of 4.5 × 10⁻⁵ M. During growth, all the DMS-sulphur was oxidized stoichiometrically to sulphate but no methanol was detected in pure cultures of TK-m. DMS-carbon was probably converted to CO₂, since the fixation of ¹⁴CO₂ was progressively diluted during growth of a culture on ¹⁴CO₂ and DMS. Growth yields were consistent with autotrophic growth, dependent on the oxidation of the methyl residues to CO₂ (probably with formaldehyde as a first intermediate) and the sulphide to sulphate. The organism thus appears to exhibit a mixture, from the one substrate, of chemolithotrophic and methylotrophic energy generation supporting autotrophic growth with CO₂ fixation.     

Thymidine incorporation into lake water bacterioplankton and pure cultures of chemolithotrophic (CO, H2) and methanotrophic bacteria

Abstract Incorporation of [³H]methyl thymidine into bacterial DNA was measured using samples of bacterioplankton from Lake Constance and pure cultures of CO, H₂ and CH₄-oxidizing bacteria. Thymidine was incorporated by Pseudomonas carboxydovorans, Paracoccus denitrificans, Methylosinus trichosporium, Methylomonas agile , and by various chemolithotropic or methylotrophic isolates from Lake Constance. Thymidine incorporation by bacterial cultures was stimulated by increasing concentrations of CO or H₂. Increased CH₄ concentrations stimulated thymidine incorporation by Ms. trichosporium only if the cells had been starved. In contrast to bacterial cultures, thymidine incorporation by bacterioplankton samples was not stimulated by increasing     

Aerotaxis in Desulfovibrio

Aerotaxis of two sulphate-reducing bacteria, the freshwater strain Desulfovibrio desulfuricans CSN (DSM 9104) and the marine strain Desulfovibrio oxyclinae N13 (DSM 11498), was studied using capillary microslides, microscopy and oxygen microsensors. The bacteria formed ring-shaped bands in oxygen diffusion gradients surrounding O₂ bubbles, which were placed into anoxic sulphate-free cell suspensions in capillary microslides. The radial expansion of the oxic volume by diffusion was stopped by aerobic respiration. Bands were formed by cells avoiding high O₂ levels near the O₂ bubble, as well as by cells entering from the surrounding anoxic zone. At the inner edge of the bands, O₂ levels of up to 20% air saturation (50 μM O₂) were found, while the outer edge always coincided with the oxic–anoxic interface. Ring diameters and O₂ concentrations at the inner edge of the band depended on the cell density and the strain used in the suspension. Band formation did not occur in the absence of an electron donor (5 mM lactate) or when N₂ gas bubbles were used. Both strains were highly motile with velocities of ≈ 32 μm s⁻¹ during forward runs, and 7 μm s⁻¹ during backward runs respectively. Within the bands, cells moved in circles of about 20 μm diameter, while cells outside the band exhibited straighter or only slightly bent traces. It is concluded that the capacity of respiration at high rates and the positive and negative aerotactical responses of Desulfovibrio provide an efficient strategy for removing O₂ from the habitat in situations where sufficient electron donors and high cell densities are present.     

Fixation of molecular nitrogen by Methanosarcina barkeri

Abstract Methanosarcina barkeri cells were observed in ammonia-free anaerobic acetate enrichments for sulfate-reducing bacteria. The capacity of Methanosarcina to grow diazotrophically was proved with a pure culture in mineral media with methanol. The cell yields with N₂ or NH₄⁺ ions as nitrogen source were 2.2 g and 6.1 g dry weight, respectively, per mol of methanol. Growth experiments with ¹⁵N₂ revealed that 84% of the cell nitrogen was derived from N₂. Acetylene was highly toxic to Methanosarcina and only reduced at concentrations lower than 100 μmol dissolved per 1 of medium. Assimilation of N₂ and reduction of acetylene were inhibited by NH₄⁺ ions. The experiments show that N₂ fixation occurs not only in eubacteria but also in archaebacteria. The ecological significance of diazotrophic growth of Methanosarcina is discussed.     

A note on the control of sulphate-reducing bacteria in seawater by u.v. irradiation

Continuous and batch cultures of marine sulphate-reducing bacteria (SRB) in North Sea water were irradiated with 110000 to 329500 μWs/cm² of ultraviolet radiation (wavelength 253.7 nm) with a commercial u.v. sterilizing unit. A 100% kill was obtained with logarithmic cultures of Desulfovibrio desulfuricans NCIMB 8400 at population densities of 10–10⁴/ml. A >99.99% kill was obtained with a mixture (ca 10⁵/ml) of batch grown Desulfovibrio spp. and oilfield SRB enrichments. Ultraviolet irradiation was less effective against the indigenous heterotrophic bacteria in the seawater ( ca 90% kill).     

Incorporation of [methyl-3H]thymidine by obligate and facultative anaerobic bacteria when grown under defined culture conditions

Abstract Incorporation of [ methyl -³H]thymidine into bacterial DNA was determined for a range of axenic anaerobic bacterial cultures: fermentative heterotrophs, sulphate-reducing bacteria, purple sulphur bacteria, acetogens and methanogens. Anaerobically growing Bacillus sp. and the obligate aerobe Thiobacillus ferrooxidans were also investigated. Actively growing cultures of sulphate-reducing bacteria belonging to the genera Desulfovibrio, Desulfotomaculum, Desulfobacter, Desulfobotulus and Desulfobulbus , purple sulphur bacteria ( Chromatium vinosum OP2 and Thiocapsa roseopersicina OP1), methanogens ( Methanococcus GS16 and Methanosarcina barkeri ) and an acetogen ( Acetobacterium woodii ) did not incorporate [ methyl -³H]thymidine into DNA. The only obligate anaerobes in which thymidine incorporation into DNA could be unequivocally demonstrated were members of the genus Clostridium . Anaerobically growing Bacillus sp. also incorporated thymidine. These data demonstrate that pure culture representatives of major groups of anaerobic bacteria involved in the terminal oxidation of organic carbon and anoxygenic phototrophs within sediments are unable to incorporate [ methyl -³H]thymidine into DNA, although some obligate and facultative anaerobes can. Variability in thymidine incorporation amongst pure culture isolates indicates that unless existing techniques can be calibrated to take this into consideration then productivity estimates in both aerobic and anaerobic environments may be greatly underestimated using the [ methyl -³H]thymidine technique.     

Metabolism of nitric oxide in soil and denitrifying bacteria

Abstract Production and consumption of NO was measured under anaerobic conditions in a slightly alkaline and an acidic soil as well as in pure cultures of denitrifying Pseudomonas aeruginosa, P. stutzeri, P. fluorescens, Paracoccus denitrificans, Azospirillum brasilense , and A. lipoferum . Growing bacterial cultures reduced nitrate and intermediately accumulated nitrite, NO, N₂O, but not NO₂. Addition of formaldehyde inhibited NO production and NO consumption. In the presence of acetylene NO was reduced to N₂O. Net NO release rates in denitrifying bacterial suspensions and in soil samples decreased hyperbolically with increasing NO up to mixing ratios of about 5 ppmv NO. This behaviour could be modelled by assuming a constant rate of NO production simultaneously with a NO consumption activity that increased with NO until V _max was reached. The data allowed calculation of the gross rates ( P ) of NO production, of the rate constants ( k ), V _max and K _m of NO consumption, and of the NO compensation mixing ratio ( m _c). In soil, P was larger than V _max resulting in net NO release even at high NO mixing ratios unless P was selectively inhibited by chlorate + chlorite or by aerobic incubation conditions. In bacteria, V _max was somewhat larger than P resulting in net NO uptake at high NO mixing ratios. Both P and V _max were dependent on the supply of electron donor (e.g. glucose). Both in soil (aerobic or anaerobic) and in pure culture, the K _m values of NO consumption were in a similar low range of about 0.5–6.0 nM. Anaerobic soil and denitrifying bacteria exhibited m _c values of 1.6–2.1 ppmv NO and 0.2–4.0 ppmv NO, respectively.     

Responses of lactic acid bacteria to oxygen

Abstract A small number of flavoprotein oxidase enzymes are responsible for the direct interaction of lactic acid bacteria (LAB) with oxygen; hydrogen peroxide or water are produced in these reactions. In some cultures exposed to oxygen, hydrogen peroxide accumulates to inhibitory levels.
Through these oxidase enzymes and NADH peroxidase, O₂ and H₂O₂ can accept electrons from sugar metabolism, and thus have a sparing effect on the use of metabolic intermediates, such as pyruvate or acetaldehyde, as electron acceptors. Consequently, sugar metabolism in aerated cultures of LAB can be substantially different from that in unaerated cultures. Energy and biomass yields, end-products of sugar metabolism and the range of substrates which can be metabolised are affected.
Lactic acid bacteria exhibit an inducible oxidative stress response when exposed to sublethal levels of H₂O₂. This response protects them if they are subsequently exposed to lethal concentrations of H₂O₂. The effect appears to be related to other stress responses such as heat-shock and is similar, in some but not all respects, to that previously reported for enteric bacteria.     

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.     

SULPHIDE PRODUCTION FROM SULPHATE-ENRICHED SEWAGE SLUDGES

SUMMARY: Sterilized raw sewage sludge enriched with sulphate and inoculated with pure strains of Desulphovibrio desulphuricans produced negligible sulphide. Unsterilized sludge supplemented with 7% (w/v) CaSO₄.2H₂O and inoculated with crude cultures of sulphate-reducing bacteria obtained from sewage yielded 1·0% S^2- (wt S^2- produced as H₂S/vol. of raw sludge) in 6 months at 30°. By repeated subculture more active cultures developed which produced 1% S^2- in 7 days and 1·2–1·9% in 28 days. Digested sludge yielded only 0·1% S^2-. In semicontinuous fermentations at 30°, raw sludge without added sulphate produced 20 times its own volume of gas containing 70% CH₄ and 30% CO₂. When 5% CaSO₄.2H₂O and an active crude culture of sulphate reducers were added, gas production decreased steadily to zero. There were no differences in pH, temperature and redox potential in sludges producing methane or sulphide. The chief cause of inhibition appeared to be the action of sulphide: 0·02% soluble sulphide (S^2-) totally inhibited methane formation; 0·01% S^2- initially decreased gas production by one-quarter but there was a slow recovery to normal, suggesting acclimatization of the methane-producing organisms to sulphide.
Linked fermentations, in which gas from a methane fermentation swept H₂S from a sulphide fermentation, gave a final gas mixture of about 60% CH₄, 30% CO₂ and 5–10% H₂S. The yield of sulphide depended on the rate of sweeping.     

H2 and CO2 production from methanol or formaldehyde by the methanogenic bacterium strain Gö1 treated with 2-bromoethanesulfonic acid

Abstract In cell suspensions of the methanogenic bacterium strain Gö1 or Methanosarcina barkeri H₂ formation from methanol in the presence of 2-bromoethanesulfonic acid (BES) was strictly dependent on sodium ions; apparent K _S for Na⁺, 1.3±0.3 mM.H₂ formation was inhibited by the uncoupler tetrachlorosalicylanilide (TCS), but this inhibition could be temporarily overcome, when a sodium pulse (100 mM) was given to the cell suspension. On the other hand, H₂ formation from formaldehyde in the presence of BES (rate: 300 nmol H₂/h·mg protein as compared to 25 nmol H₂/h·mg protein from methanol) was not sodium-dependent, not TCS-sensitive and not inhibited by addition of monensin. H₂ formation was accompanied by CO₂ formation in stoichiometric amounts, 3 H₂:1 CO₂ for methanol and 2 H₂:1 CO₂ for formaldehyde oxidation.     

Characterization of sulfate-reducing bacteria isolated from Senegal ricefields

Abstract Sulfate-reducing bacteria were enumerated in soils and water samples from Senegal ricefields using lactate and sulfate as substrates. When rice plants were severely injured by sulfides, maximum densities ranged from 10⁷ to 10⁹ bacteria g⁻¹ of dry spermosphere or rhizosphere soil. Seven non-sporulating, mesophilic strains were isolated. The strains had motile curved cells and stained Gram-negative. Lactate, pyruvate, H₂+ CO₂, malate, fumarate, or ethanol could serve as electron donors. Organic acids were incompletely oxidized to acetate. Alcohols were degraded to the corresponding fatty acids. Sulfate, sulfite, or thiosulfate could serve as electron acceptors and were reduced to sulfide. Vitamins, yeast extract, Biotrypcase, or additional NaCl were not required for growth. On the basis of morphological and physiological properties, and the G + C mol % of the DNA, six isolates were identified as Desulfovibrio vulgaris and one as Desulfovibrio desulfuricans . The comparison of their main physiological properties with the physico-chemical properties of sampling sites indicated that they were better adapted to conditions prevailing in the rice rhizosphere than to those prevailing in the bulk of soil.     

Inhibition of Methanosarcina barkeri strain 227 by cadmium

Abstract The effect of cadmium (Cd) on methane formation from methanol and/or H₂–CO₂ by Methanosarcina barkeri was examined in a defined growth medium and in a simplified buffer system containing 50 mM Tes with or without 2 mM dithiothreitol (DTT). No inhibition of methanogenesis by high concentrations of cadmium was observed in growth medium. Similarly, little inhibition of methanogenesis by whole cells in the Tes buffer system was observed in the presence of 430 μM Cd or 370 μM mercury (Hg) with 2 mM DTT. When the concentration of DTT was reduced to 0.4 mM, almost complete inhibition of methanogenesis from H₂–CO₂ and methanol by 600 μM Cd was observed. In the absence of DTT, 150 μM Cd inhibited methanogenesis from H₂–CO₂ completely and from methanol by 97%. Methanogenesis from H₂–CO₂ was more sensitive to Cd than that from methanol.     

Coexistence of aerobic chemotrophic and anaerobic phototrophic sulfur bacteria under oxygen limitation

Abstract: The aerobic chemotrophic sulfur bacterium Thiobacillus thioparus T5 and the anaerobic phototrophic sulfur bacterium Thiocapsa roseopersicina M1 were co-cultured in continuously illuminated chemostats at a dilution rate of 0.05 h⁻¹. Sulfide was the only externally supplied electron donor, and oxygen and carbon dioxide served as electron acceptor and carbon source, respectively. Steady states were obtained with oxygen supplies ranging from non-limiting amounts (1.6 mol O₂ per mol sulfide, resulting in sulfide limitation) to severe limitation (0.65 mol O₂ per mol sulfide). Under sulfide limitation Thiocapsa was competitively excluded by Thiobacillus and washed out. Oxygen/sulfide ratios between 0.65 and 1.6 resulted in stable coexistence. It could be deduced that virtually all sulfide was oxidized by Thiobacillus . The present experiments showed that Thiocapsa is able to grow phototrophically on the partially oxidized products of Thiobacillus . In pure Thiobacillus cultures in steady state extracellular zerovalent sulfur accumulated, in contrast to mixed cultures. This suggests that a soluble form of sulfur at the oxidation state of elemental sulfur is formed by Thiobacillus as intermediate. As a result, under oxygen limitation colorless sulfur bacteria and purple sulfur bacteria do not competitively exclude each other but can coexist. It was shown that its ability to use partially oxidized sulfur compounds, formed under oxygen limiting conditions by Thiobacillus , helps explain the bloom formation of Thiocapsa in marine microbial mats.     

Mitigation of adverse effects of rising CO2 on a planktonic herbivore by mixed algal diets

Putative future increase in atmospheric CO₂ is expected to adversely affect herbivore growth due to decrease in contents of key nutrients such as nitrogen and phosphorus (P) relative to carbon in primary producers including plant and algal species. However, as many herbivores are polyphagous and as the response of primary producers to elevated CO₂ is highly species-specific, effects of elevated CO₂ on herbivore growth may differ between feeding conditions with monospecific and multiproducer diets. To examine this possibility, we performed CO₂ manipulation experiments under a P-limited condition with a planktonic herbivore, Daphnia , and three algal species, Scenedesmus obliquus (green algae), Cyclotella sp. (diatoms) and Synechococcus sp. (cyanobacteria). Semibatch cultures with single algal species (monocultures) and multiple algal species (mixed cultures) were grown at ambient (360 ppm) and high CO₂ levels (2000 ppm) that were within the natural range in lakes. Both in the mono- and mixed cultures, algal steady state abundance increased but algal P : C and N : C ratios decreased when they were grown at high CO₂. As expected, Daphnia fed monospecific algae cultured at high CO₂ had decreased growth rates despite increased algal abundance. However, when fed mixed algae cultured at high CO₂, especially consisting of diatoms and cyanobacteria or the three algal species, Daphnia maintained high growth rates despite lowered P and N contents relative to C in the algal diets. These results imply that algal diets composed of multiple species can mitigate the adverse effects of elevated CO₂ on herbivore performance, although the magnitude of this mitigation depends on the composition of algal species involved in the diets.     

Sulfate-reducing bacteria in littoral sediment of Lake Constance

Abstract The viable population of sulfate-reducing bacteria (SRB) in littoral sediments of Lake Constance was investigated using enrichment and enumeration techniques. Enrichment studies established that most types of SRB grew best in media with low salt concentrations (max. 0.4 g Cl⁻/1), consistent with the low salinity of the freshwater habitat. Enumerations were based on an adequate medium with the following electron donors: H₂, lactate, acetate, propionate, butyrate, caprylate, succinate, benzoate, or S₂O₃²⁻ for thiosulfate-disproportionating bacteria. Cultures were incubated for 6 weeks to obtain maximum counts. A maximum cell density of 6.3 × 10⁶ cells per ml sediment was estimated, which is the highest number of SRB ever reported for anoxic sediments. A comparison with measured sulfate reduction rates showed that the enumeration techniques were about 10–100-fold more efficient than those previously used. The population of SRB had a characteristic structure consisting of 87.7% H₂-utilizing SRB (physiologically resembling the classical Desulfovibrio species); 12.0% propionate utilizers (tentatively identified as Desulfobulbus species); 0.3% long chain fatty acid-oxidizing Desulfovibrio sapovorans species. Acetate-utilizing SRB ( Desulfotomaculum acetoxidans ) constituted ≤ 0.05% of the total estimated population. Moreover, the latter species was only present as inactive spores. Benzoate-degrading SRB were not detected.     

ASYMMETRIC, BIMODAL TRADE-OFFS DURING ADAPTATION OF METHYLOBACTERIUM TO DISTINCT GROWTH SUBSTRATES

Trade-offs between selected and nonselected environments are often assumed to exist during adaptation. This phenomenon is prevalent in microbial metabolism, where many organisms have come to specialize on a narrow breadth of substrates. One well-studied example is methylotrophic bacteria that can use single-carbon (C₁) compounds as their sole source of carbon and energy, but generally use few, if any, multi-C compounds. Here, we use adaptation of experimental populations of the model methylotroph, Methylobacterium extorquens AM1, to C₁ (methanol) or multi-C (succinate) compounds to investigate specialization and trade-offs between these two metabolic lifestyles. We found a general trend toward trade-offs during adaptation to succinate, but this was neither universal nor showed a quantitative relationship with the extent of adaptation. After 1500 generations, succinate-evolved strains had a remarkably bimodal distribution of fitness values on methanol: either an improvement comparable to the strains adapted on methanol or the complete loss of the ability to grow on C₁ compounds. In contrast, adaptation to methanol resulted in no such trade-offs. Based on the substantial, asymmetric loss of C₁ growth during growth on succinate, we suggest that the long-term maintenance of C₁ metabolism across the genus Methylobacterium requires relatively frequent use of C₁ compounds to prevent rapid loss.