Heavy metal inhibition of methanogenesis by Methanospirillum hungatei GP1

Abstract Washed whole cells of Methanospirillum hungatei incubated in TES buffer retained methanogenic activity in the absence of any reducing agents. Washed cells grown with 80% H₂-20% CO₂ and acetate produced methane from H₂/CO₂ and 50 mM formate at 1.1 to 1.8 and 15 μmol methane · h⁻¹· mg⁻¹ protein, respectively. Cadmium at a concentration of 15 μM and 50 μM mercury, copper or zinc completely inhibited methane production from H₂/CO₂ by M. hungatei . The chelating agent, EDTA, protected the cells from inhibition by cadmium but acetate and citrate did not. The activity of formate dehydrogenase and hydrogenase remaining in cells after incubation with copper, mercury, zinc or cadmium was reduced with formate dehydrogenase being the more sensitive.     

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.     

Methyl sulfides as intermediates in the anaerobic oxidation of methane

While it is clear that microbial consortia containing Archaea and sulfate-reducing bacteria (SRB) can mediate the anaerobic oxidation of methane (AOM), the interplay between these microorganisms remains unknown. The leading explanation of the AOM metabolism is 'reverse methanogenesis' by which a methanogenesis substrate is produced and transferred between species. Conceptually, the reversal of methanogenesis requires low H₂ concentrations for energetic favourability. We used ¹³C-labelled CH₄ as a tracer to test the effects of elevated H₂ pressures on incubations of active AOM sediments from both the Eel River basin and Hydrate Ridge. In the presence of H₂, we observed a minimal reduction in the rate of CH₄ oxidation, and conclude H₂ does not play an interspecies role in AOM. Based on these results, as well as previous work, we propose a new model for substrate transfer in AOM. In this model, methyl sulfides produced by the Archaea from both CH₄ oxidation and CO₂ reduction are transferred to the SRB. Metabolically, CH₄ oxidation provides electrons for the energy-yielding reduction of CO₂ to a methyl group ('methylogenesis'). Methylogenesis is a dominantly reductive pathway utilizing most methanogenesis enzymes in their forward direction. Incubations of seep sediments demonstrate, as would be expected from this model, that methanethiol inhibits AOM and that CO can be substituted for CH₄ as the electron donor for methylogenesis.     

Fermentation characteristics of Clostridium pasteurianum LMG 3285 grown on glucose and mannitol

Clostridium pasteurianum fermented glucose to acetate, butyrate, CO₂ and H₂. In batch cultures the fermentation pattern was only slightly affected by culture pH over the range 8·0 to 5·5. The acetate/butyrate ratio was always higher than or equal to one. Between 2·14 and 2·33 mol H₂ was produced per mol glucose fermented. At unregulated pH, more butanol and less butyrate was formed. In a carbon-limited chemostat, the steady-state acetate/butyrate ratio was always lower than one. H₂ production was approximately 1·70 mol per mol glucose consumed. Substantial amounts of extracellular protein were formed. With decreasing pH, acetate and formate production decreased, while H₂ production was highest at pH 6.0. With increasing dilution rate ( D ), the product spectrum hardly changed, but more biomass was formed. Y _glucose^max and Y _ATP^max were 55·97 and 31·48 g dry weight per mol glucose or ATP respectively. With increasing glucose input the formation of fatty acids and H₂ slightly decreased.
Continuous cultures fermented mannitol to acetate, butyrate, butanol, CO₂ and H₂. With acetate as co-substrate, butanol production and molar growth yields, Y _mannitol and Y _ATP, markedly decreased, while the butyrate and H₂ production increased. The latter reached a value of 2·21 mol H₂ per mol mannitol consumed.     

Combined monitoring of changes in δ13CH4 and archaeal community structure during mesophilic methanization of municipal solid waste

Reconstituted municipal solid waste (MSW) with varying contents of putrescible and cellulosic waste was incubated anaerobically under mesophilic conditions. Standard physicochemical parameters were monitored, together with stable isotopic signatures of produced CH₄ and CO₂. δ¹³C values for CH₄ indicated a change of methanogenic metabolism with time. CH₄ was predominantly produced from H₂/CO₂ at the beginning of the incubations. This period was associated with important shifts in archaeal communities monitored by automated ribosomal intergenic spacer analysis (ARISA) and FISH of oligonucleotidic probes targeting specifically 16S rRNA gene of various methanogenic groups. The onset of the active methane generation phase was characterized by an increase of CH₄δ¹³C, indicating a progressive shift toward an aceticlastic metabolism. When the methane production levelled off, a decrease in the isotopic signature was observed toward values characteristics of hydrogenotrophic metabolism. ARISA profiles were, however, found to be stable from the beginning of the active methane generation phase until the end of the experiment. FISH observation indicated that members of the family Methanosarcinaceae were predominant in the archaeal community during this period, suggesting that these methanogens might exhibit a high metabolic versatility during methanization of waste.     

Growth, CO2 consumption and H2 production of Anabaena variabilis ATCC 29413-U under different irradiances and CO2 concentrations

Aims:  The objective of this study is to develop kinetic models based on batch experiments describing the growth, CO₂ consumption, and H₂ production of Anabaena variabilis ATCC 29413-U^TM as functions of irradiance and CO₂ concentration.
Methods and Results:  A parametric experimental study is performed for irradiances from 1120 to 16100 lux and for initial CO₂ mole fractions from 0·03 to 0·20 in argon at pH 7·0 ± 0·4 with nitrate in the medium. Kinetic models are successfully developed based on the Monod model and on a novel scaling analysis employing the CO₂ consumption half-time as the time scale.
Conclusions:  Monod models predict the growth, CO₂ consumption and O₂ production within 30%. Moreover, the CO₂ consumption half-time is an appropriate time scale for analysing all experimental data. In addition, the optimum initial CO₂ mole fraction is 0·05 for maximum growth and CO₂ consumption rates. Finally, the saturation irradiance is determined to be 5170 lux for CO₂ consumption and growth whereas, the maximum H₂ production rate occurs around 10 000 lux.
Significance and Impact of the Study:  The study presents kinetic models predicting the growth, CO₂ consumption and H₂ production of A. variabilis . The experimental and scaling analysis methods can be generalized to other micro-organisms.     

Protonmotive force-driven synthesis of ATP during methane formation from molecular hydrogen and formaldehyde or carbon dioxide in Methanosarcina barkeri

Abstract Methane formation from formaldehyde and H₂ or from carbon dioxide and H₂, as performed by cell suspensions of Methanosarcina barkeri , was coupled to ATP synthesis. In correspondence with this, methane formation was inhibited by N , N '-dicyclohexylcarbodiimide (DCCD), which at the same time, caused a decrease of the intracellular ATP concentration but only a slow decrease of the membrane potential. Addition of the uncoupler tetrachlorosalicylanilide (TCS) led to a relief of the inhibition of methane formation from CH₂O + H₂, but not from CO₂+ H₂.     

A Chromatographic Method for Analysis of the Gaseous Phase in Shake Flask Cultures and its Application to the Study of Methane Utilization

A simple gas chromatograph with a katharometer detector is described to determine O₂, N₂, methane and CO₂ in gas samples of 0·01–2·0 ml. The apparatus is inexpensive, and can be modified to determine other gases. The sensitivity to oxygen is 3 × 10⁻⁶ g. The use of the instrument is illustrated by a study of the growth kinetics of Methylococcus capsulatus grown on methane in shake flask experiments. The ratio of O₂ uptake to methane uptake is much lower in the stationary phase than in the growth phase of the culture.     

Thermophilic degradation of cellulose by a triculture of Clostridium thermocellum, Methanobacterium sp. and Methanosarcina MP

Abstract The fermentation of cellulose at 55°C by different associations of the 3 bacteria Clostridium thermocellum, Methanobacterium sp. and Methanosarcina MP, was studied. C. thermocellum alone produced acetate, lactate, ethanol, H₂ and CO₂. The co-culture C. thermocellum-Methanobacterium sp. produced more acetate and less ethanol than the monoculture of Clostridium .
Methanosarcina MP used acetate only in the triculture including Methanobacterium sp. When methanol was added (5 mM) to the triculture, Methanosarcina MP had a shorter lag phase on acetate and degraded much more acetate. maximum methane production was 8.5 mmol CH₄/g cellulose degraded.     

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.     

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     

Sulfide-induced dissimilatory nitrate reduction to ammonia in anaerobic freshwater sediments

Abstract: Different reduced sulfur compounds (H₂S, FeS, S₂O₃²⁻) were tested as electron donors for dissimilatory nitrate reduction in nitrate-amended sediment slurries. Only in the free sulfide-enriched slurries was nitrate appreciably reduced to ammonia (     ), with concomitant oxidation of sulfide to S⁰ (     ). The initial concentration of free sulfide appears as a factor determining the type of nitrate reduction. At extremely low concentrations of free S²⁻ (metal sulfides) nitrate was reduced via denitrification whereas at higher S²⁻ concentrations, dissimilatory nitrate reduction to ammonia (DNRA) and incomplete denitrification to gaseous nitrogen oxides took place. Sulfide inhibition of NO- and N₂O- reductases is proposed as being responsible for the driving part of the electron flow from S²⁻ to NH₄⁺.     

Snow depth, soil freezing, and fluxes of carbon dioxide, nitrous oxide and methane in a northern hardwood forest

Soil–atmosphere fluxes of trace gases (especially nitrous oxide (N₂O)) can be significant during winter and at snowmelt. We investigated the effects of decreases in snow cover on soil freezing and trace gas fluxes at the Hubbard Brook Experimental Forest, a northern hardwood forest in New Hampshire, USA. We manipulated snow depth by shoveling to induce soil freezing, and measured fluxes of N₂O, methane (CH₄) and carbon dioxide (CO₂) in field chambers monthly (bi-weekly at snowmelt) in stands dominated by sugar maple or yellow birch. The snow manipulation and measurements were carried out in two winters (1997/1998 and 1998/1999) and measurements continued through 2000. Fluxes of CO₂ and CH₄ showed a strong seasonal pattern, with low rates in winter, but N₂O fluxes did not show strong seasonal variation. The snow manipulation induced soil freezing, increased N₂O flux and decreased CH₄ uptake in both treatment years, especially during winter. Annual N₂O fluxes in sugar maple treatment plots were 207 and 99 mg N m⁻² yr⁻¹ in 1998 and 1999 vs. 105 and 42 in reference plots. Tree species had no effect on N₂O or CO₂ fluxes, but CH₄ uptake was higher in plots dominated by yellow birch than in plots dominated by sugar maple. Our results suggest that winter fluxes of N₂O are important and that winter climate change that decreases snow cover will increase soil:atmosphere N₂O fluxes from northern hardwood forests.     

Spirochaeta smaragdinae sp. nov., a new mesophilic strictly anaerobic spirochete from an oil field

An obligately anaerobic spirochete designated strain SEBR 4228^T (T = type strain) was isolated from an oil field of Congo, Central Africa. The strain grew optimally with a sodium chloride concentration of 5% (sodium chloride concentration growth range 1.0–10%) at 37°C (growth temperature range 20–40°C) and pH of 7.0–7.2 (pH growth range pH 5.5–8.0). Strain SEBR 4228^T grew on carbohydrates (glucose, fructose, ribose, d -xylose, galactose, mannitol and mannose), glycerol, fumarate, peptides and yeast extract. Yeast extract was required for growth and could not be replaced by vitamins. It reduced thiosulfate and sulfur, to H₂S. Glucose was oxidised to lactate, acetate, CO₂ and H₂S in the presence of thiosulfate but in its absence lactate, ethanol, CO₂ and H₂ were produced. Fumarate was fermented to acetate and succinate. The G+C content of strain SEBR 4228^T was 50%. Strain SEBR 4228^T was spiral shaped measuring 5–30 by 0.3–0.5 μm and was motile with a corkscrew-like motion. Electron microscopy revealed the presence of periplasmic flagella in a 1-2-1 arrangement. Strain SEBR 4228^T possessed features typical of the members of the genus Spirochaeta . 16S rRNA sequence analysis revealed that it was closely related to Spirochaeta bajacaliforniensis (similarity 98.6%). The lack of DNA homology with S. bajacaliforniensis (38%), together with other phenotypic differences, indicated that strain SEBR 4228^T is a new species, which we have designated Spirochaeta smaragdinae . The type strain is SEBR 4228^T (= DSM 11293).     

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).     

Influence of freshwater sediment on the survival of Escherichia coli and Salmonella sp. as measured by three methods of enumeration

The thermophilic hydrogen-oxidizing eubacterium, Hydrogenobacter thermophilus was grown with a semi-continuous gas feed in a 150 1 fermentor, on different ratios of H₂, O₂ (air) and CO₂ and on media of variable mineral salts composition. The best gas ratio during the exponential phase was approximately 0.5:1.0:0.03 atm of H₂: air: CO₂. Cell densities were increased by increasing the concentration of ammonium and phosphate in the medium. The maximum cell density obtained under the most favourable conditions was 2.62 g wet wt 1^-1, corresponding to an absorption of 1.6 at 600 nm. The maximum specific growth rate ( u ) was 0.44 h^-1.     

Adaptation to high CO2 concentration in an optimal environment: radiation capture, canopy quantum yield and carbon use efficiency

The effect of elevated [CO₂] on wheat (Triticum aestivum L. Veery 10) productivity was examined by analysing radiation capture, canopy quantum yield, canopy carbon use efficiency, harvest index and daily C gain. Canopies were grown at either 330 or 1200 μ mol mol^–1[CO₂] in controlled environments, where root and shoot C fluxes were monitored continuously from emergence to harvest. A rapidly circulating hydroponic solution supplied nutrients, water and root zone oxygen. At harvest, dry mass predicted from gas exchange data was 102·8 ± 4·7% of the observed dry mass in six trials. Neither radiation capture efficiency nor carbon use efficiency were affected by elevated [CO₂], but yield increased by 13% due to a sustained increase in canopy quantum yield. CO₂ enrichment increased root mass, tiller number and seed mass. Harvest index and chlorophyll concentration were unchanged, but CO₂ enrichment increased average life cycle net photosynthesis (13%, P < 0·05) and root respiration (24%, P < 0·05). These data indicate that plant communities adapt to CO₂ enrichment through changes in C allocation. Elevated [CO₂] increases sink strength in optimal environments, resulting in sustained increases in photosynthetic capacity, canopy quantum yield and daily C gain throughout the life cycle.     

The effect of short-term H2S fumigation on water-soluble sulphydryl and glutathione levels in spinach

Abstract. Short-term fumigation of Spinacia oleracea with 380 μg m⁻³ H₂S (250 ppb) resulted in a rapid accumulation of water-soluble SH-compounds in the shoots. After 1 h exposure a substantial increase in the SH-content was already detectable and maximal accumulation, three- to four-fold that in control plants, was observed after 24 h of exposure. Irradiation during H₂S exposure only slightly affected the rate and level of SH-accumulation. H₂S fumigation did not affect the water-soluble SH-content of the roots. Glutathione was the sole water-soluble SH-compound accumulating upon exposure to H₂S. It was calculated that during the first hour of exposure to 380 μg m⁻³ H₂S 39% of the possible absorbed H₂S was converted into glutathione. The SH-content of the water-soluble proteins of the shoots was not affected by H₂S exposure. When fumigation was stopped, a rapid decrease in glutathione content was observed and after 48 h the content was comparable to that of the control plants. Contrary to H₂S, SO₂ fumigation did not result in a rapid accumulation of glutathione in spinach shoots. The possible role of glutathione accumulation during H₂S fumigation is discussed.     

Direct mass spectrometric measurement of gases in peat cores

Abstract Dissolved gas concentrations (O₂, CH₄, CO₂) in peat cores were monitored simultaneously using a fine (1.56 mm diameter) membrane inlet probe connected to a quadrupole mass spectrometer. This technique allows direct measurements at specific locations within the sample with minimal disturbance. Detailed gas profiles in completely waterlogged peat samples (hollows) and samples in which the water table was several cm below the vegetation surface (hummocks) were compared. The depth of the water table played a central role in the distribution of gases. In a hollow, oxygen was present (90 μM) at the surface but was not detectable (<0.5 μM) at depths greater than 2 cm. Concentrations of CH₄ and CO₂ increased from 6 and 300 μM respectively at the surface to maxima of 450 and 3900 μM at 13 cm depth. At a hummock, O₂ and CO₂ were present above the water table but CH₄ was not detectable. CH₄ was measurable 2 cm below the water table. Both CH₄ and CO₂ concentrations increased with depth but maxima were not attained in the sampled cores.     

Latitudinal differentiated water table control of carbon dioxide, methane and nitrous oxide fluxes from hydromorphic soils: feedbacks to climate change

The possibility of carbon (C) being locked away from the atmosphere for millennia is given in hydromorphic soils. However, the water-table-dependent feedback from soil organic matter (SOM) decomposition to the climate system is less clear. At least three greenhouse gases are produced: carbon dioxide (CO₂), methane (CH₄) and nitrous oxide (N₂O). These gases show emission peaks at different water table positions and have different global warming potentials (GWP), for example a factor of 23 for CH₄ and 296 for N₂O as compared with the equivalent mass of CO₂ on a 100-year time horizon. This review of available annual data on all three gases revealed that the radiative forcing effect of SOM decomposition is principally dictated by CO₂ despite its low GWP. Anaerobic SOM decomposition generally has a lower potential feedback to the climatic system than aerobic SOM decomposition. Concrete values are constrained by a lack of data from tropical and subarctic regions. Furthermore, data on N₂O and on plant effects are generally rare. However, there is a clear latitudinal differentiation for the GWP of soils under anaerobic conditions compared with aerobic conditions when looking at CO₂ and CH₄: in the tropical and temperate regions, the anaerobic GWP showed a range of 25–60% of the aerobic value, but values varied between 80% and 110% in the boreal zone. Hence, particularly in the vulnerable boreal zone, the feedback from ecosystems to climate change will highly depend on plant responses to changing water tables at elevated temperatures.