Soil organic sulfur dynamics in a coniferous forest

Sulfate microbial immobilization and the mineralization of organic S were measured in vitro in soil horizons (LFH, Ae, Bhf, Bf and C) of the Lake Laflamme watershed (47°17 N, 71°14 O) using ³⁵SO₄. LFH samples immobilized from 23 to 77% of the added ³⁵SO₄ within 2 to 11 days. The ³⁵SO₄ microbial immobilization increased with temperature and reached an asymptote after a few days. The mineral soil generally immobilized less than 20% of the added ³⁵SO₄, and an asymptote was reached after 2 days. An isotopic equilibrium was rapidly reached in mineral horizons. A two-compartment (SO₄ and organic S) model adequately described ³⁵SO₄ microbial immobilization kinetics. The active organic reservoir in the whole soil profile represented less than 1% of the total organic S. The average concentrations of dissolved organic S (DOS) in the soil solutions leaving the LFH, Bhf and Bf horizons were respectively 334, 282 and 143 µgL^–1. Assuming that the DOS decrease with soil depth corresponded to the quantities adsorbed in the B horizons, we estimated that 12 800 kgha^–1 of organic S could have been formed since the last glaciation, which is about 13 times the size of the actual B horizons reservoirs. Our results suggest that the organic S reservoirs present in mineral forest soils are mostly formed by the DOS adsorption resulting from incomplete litter decomposition in the humus layer. The capability of these horizons to immobilize SO₄ from the soil solution would be restricted to a 1% active fraction composed of microorganisms. Despite their refractory nature, these reservoirs can, however, be slowly decomposed by microorganisms and contribute to the S-SO₄ export from the watershed in the long term.     

Phylogenetic diversity and activity of anaerobic microorganisms of high-temperature horizons of the Dagang oil field (P. R. China)

The number of microorganisms of major metabolic groups and the rates of sulfate reduction and methanogenesis processes in the formation waters of the high-temperature horizons of Dagang oil field have been determined. Using cultural methods, it was shown that the microbial community contained aerobic bacteria oxidizing crude oil, anaerobic fermentative bacteria, sulfate-reducing bacteria, and methanogens. Using cultural methods, the possibility of methane production from a mixture of hydrogen and carbon dioxide (H₂ + CO₂) and from acetate was established, and this result was confirmed by radioisotope methods involving NaH¹⁴CO₃ and ¹⁴CH₃COONa. Analysis of enrichment cultures 16S rDNA of methanogens demonstrated that these microorganisms belong to Methanothermobacter sp. (M. thermautotrophicus), which consumes hydrogen and carbon dioxide as basic substrates. The genes of acetate-utilizing bacteria were not revealed. Phylotypes of the representatives of Thermococcus spp. were found among archaeal 16S rDNA. 16S rRNA genes of bacterial clones belong to the orders Thermoanaerobacteriales (Thermoanaerobacter, Thermovenabulum, Thermacetogenium, and Coprothermobacter spp.), Thermotogales, Nitrospirales (Thermodesulfovibrio sp.) and Planctomycetales. 16S rDNA of a bacterium capable of oxidizing acetate in the course of syntrophic growth with H₂-utilizing methanogens was found in high-temperature petroleum reservoirs for the first time. These results provide further insight into the composition of microbial communities of high-temperature petroleum reservoirs, indicating that syntrophic processes play an important part in acetate degradation accompanied by methane production.     

Effect of methanogenic substrates on coenzyme F420-dependent N5,N10-methylene-H4MPT dehydrogenase,N5,N10-methenyl-H4MPT cyclohydrolase and F420-reducing hydrogenase activities in Methanosarcina barkeri

We measured F₄₂₀-dependent N⁵,N¹⁰-methylenetetrahydro-methanopterin dehydrogenase, N⁵, N¹⁰-methenyltetrahydro-methanopterin cyclohydrolase, and F₄₂₀-reducing hydrogenase levels in Methanosarcina barkeri grown on various substrates. Variation in dehydrogenase levels during growth on a specific substrate was usually <3-fold, and much less for cyclohydrolase. H₂–CO₂-, methanol-, and H₂–CO₂+ methanol-grown cells had roughly equivalent levels of dehydrogenase and cyclohydrolase. In acetate-grown cells cyclohydrolase level was lowered 2 to 3-fold and dehydrogenase 10 to 80-fold; this was not due to repression by acetate, since, if cultures growing on acetate were supplemented with methanol or H₂–CO₂, dehydrogenase levels increased 14 to 19-fold, and cyclohydrolase levels by 3 to 4-fold. Compared to H₂–CO₂- or methanol-grown cells, acetate-or H₂–CO₂ + methanol-grown cells had lower levels of and less growth phase-dependent variation in hydrogenase activity. Our data are consistent with the following hypotheses: 1. M. barkeri oxidizes methanol via a portion of the CO₂-reduction pathway operated in the reverse direction. 2. When steps from CO₂ to CH₃-S-CoM in the CO₂-reduction pathway (in either direction) are not used for methanogenesis, hydrogenase activity is lowered.Abbreviations MF methanofuran - H₄MPT 5,6,7,8-tetrahydromethanopterin - HS-HTP 7-mercaptoheptanoylthreonine phosphate - CoM-S-S-HTP heterodisulfide of HS-CoM and HS-HTP - F₄₂₀ coenzyme F₄₂₀ (a 7,8-didemethyl-8-hydroxy-5-deaza-riboflavin derivative) - H₂F₄₂₀ reduced coenzyme F₄₂₀ - HC⁺=H₄MPT N⁵,N¹⁰-methenyl-H₄MPT - H₂C=H₄MPT N⁵,N¹⁰-methylene-H₄MPT - H₃C=H₄MPT N⁵-methyl-H₄MPT - BES 2-bromoethanesulfonic acid     

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.     

The Gibbs Free Energy Threshold for the Invasion of a Microbial Population Under Kinetic Constraints

Possible chemotrophic metabolism at a site of interest is controlled not only by the catabolic energy expressed as the Gibbs energy of reaction (Δ_rG) but also by the kinetic constraints due to the availability of electron acceptors and donors. We introduced graphical and stochastic approaches for determining the Δ_rG threshold required to support a microbial population with a specific catabolic strategy under kinetic constraints. Invasibility as an indicator of the present reproductive ability of a microbial population was evaluated by simultaneously calculating Δ_rG for the catabolic reaction and the microbial catalytic rate. For example, the neutrophilic iron-oxidizing bacteria's invasibility was calculated by randomly choosing the Fe²⁺ and O₂ concentrations between 10^?8 and 10^?2 mol L^?1, and pH between 4 and 8, to determine the Δ_rG threshold for invasion. Parameters were estimated from batch experiments of neutrophilic iron-oxidizing bacteria reported in previous studies. Under the given conditions, the stochastic approach predicted that the neutrophilic iron-oxidizing bacteria can always invade a system in which the Δ_rG for Fe oxidation is below ?90 kJ mol Fe^?1, can occasionally invade if Δ_rG is between ?45 and ?90 kJ mol Fe^?1, and can never invade if Δ_rG is above ?45 kJ mol Fe^?1. The Δ_rG threshold for invasion is sifted by the growth yield coefficient, the loss rate of cells, the maximum cell-specific Fe oxidation rate constant, and the temperature. The Δ_rG threshold for invasion may be unable to rigorously predict the stable dominance of microbial metabolism, but can provide a rough indication for the possible microbial metabolism under current conditions.     

Desulfotomaculum and Methanobacterium spp. Dominate a 4- to 5-Kilometer-Deep Fault

Alkaline, sulfidic, 54 to 60°C, 4 to 53 million-year-old meteoric water emanating from a borehole intersecting quartzite-hosted fractures >3.3 km beneath the surface supported a microbial community dominated by a bacterial species affiliated with Desulfotomaculum spp. and an archaeal species related to Methanobacterium spp. The geochemical homogeneity over the 650-m length of the borehole, the lack of dividing cells, and the absence of these microorganisms in mine service water support an indigenous origin for the microbial community. The coexistence of these two microorganisms is consistent with a limiting flux of inorganic carbon and SO₄²⁻ in the presence of high pH, high concentrations of H₂ and CH₄, and minimal free energy for autotrophic methanogenesis. Sulfide isotopic compositions were highly enriched, consistent with microbial SO₄²⁻ reduction under hydrologic isolation. An analogous microbial couple and similar abiogenic gas chemistry have been reported recently for hydrothermal carbonate vents of the Lost City near the Mid-Atlantic Ridge (D. S. Kelly et al., Science 307:1428-1434, 2005), suggesting that these features may be common to deep subsurface habitats (continental and marine) bearing this geochemical signature. The geochemical setting and microbial communities described here are notably different from microbial ecosystems reported for shallower continental subsurface environments.     

Pyruvate oxidation by Methanococcus spp.

In the absence of H₂, Methanococcus spp. utilized pyruvate as an electron donor for methanogenesis. For Methanococcus voltae A3, Methanococcus maripaludis JJ1, and Methanococcus vannielii, typical rates of pyruvate-dependent methanogenesis were 3.4, 2.8, and 3.9 nmol min^-1 mg^-1 cell dry wt, respectively. These rates were 1–4% of the rates of H₂-dependent methanogenesis. For M. voltae, the concentration of pyruvate required for one-half the maximum rate of methanogenesis was 7 mM, and pyruvate-dependent methanogenesis was linear for 3 days. Radiolabeled acetate was formed from [3-¹⁴C]pyruvate, and the stoichiometry of pyruvate consumed per acetate produced was 1.12±0.27. The stoichiometry of pyruvate consumed per CH₄ produced was 3.64±0.34. These values are close to the expected values of 1 acetate and 4 CH₄. Although 10–30% of total cell carbon could be obtained from exogenous pyruvate during growth with H₂, pyruvate did not replace the nutritional requirement for acetate in Methanococcus voltae A3 or two acetate auxotrophs of Methanococcus maripaludis, JJ6 and JJ7. These results suggest that pyruvate was not oxidized in the presence of H₂. The inability to oxidize pyruvate during H₂-dependent methanogenesis would prevent a futile cycle of pyruvate oxidation and biosynthesis during autotrophic growth.     

A 14-year study of habitat use and diet of brown trout (Salmo trutta) and Arctic charr (Salvelinus alpinus) in Lake Atnsjøen, a subalpine Norwegian lake

To reveal the mechanisms of sedimental H₂S accumulation, annual investigations on sedimental environments were conducted in two temperate estuarine lagoons. The lagoons, Gamo and Idoura (Japan), have similar shapes, locations, and topographical properties but different degrees of H₂S accumulation. Water stagnation causes a high phytoplankton biomass (Chl. a; 26–52 g l^–1) in the inner Gamo Lagoon. Gamo Lagoon sediment was characterized by high bounded sulfides (bounded Smainly FeS) and H₂S contents, and low C/N ratios (mean = 10.4) and iron (reactive Fe²⁺ and total Fe) contents. H₂S was not detected in Idoura Lagoon where phytoplankton biomass was much lower (Chl. a; 0.6–4 g l^–1). Idoura Lagoon sediment had high C/N ratios (mean=17.9) and high iron contents. The C/N ratio difference implies that organic matter in Gamo Lagoon originates mainly from more decomposable phytoplankton, while organic matter in Idoura Lagoon derives mainly from terrestrial vascular plants with lower decomposability. The excess loading of phytoplanktonic detritus in Gamo accelerates sedimentary microbial activity, including sulfate reduction (i.e., H₂S production). High Fe²⁺and low bounded S contents in Idoura sediment indicate a high chemical buffering capacity toward H₂S. In contrast, almost all Fe²⁺ in Gamo Lagoon had already reacted with H₂S as FeS. H₂S accumulation in Gamo Lagoon is caused by low sedimentary chemical buffering capacity toward H₂S, as well as higher microbial H₂S production, caused by the excess loading of phytoplanktonic detritus.     

The Impact of Indigenous Microorganisms on the Mineral Corrosion and Mineral Trapping in the SO2 Co-injected CO2-Saline-Sandstone Interaction

The impact of indigenous microorganisms on the mineral corrosion and mineral trapping in the SO₂ co-injected CO₂-saline-sandstone interaction was investigated in this study by lab experiments under 55?°C, 15?M pa. The results verified that co-injection of SO₂ resulted in a decrease in biomass and shifts in microbial communities within 90?days, but some microorganisms still could adapt to acidic, high-temperature, high-pressure, and high-salinity environments. Firmicutes and Proteobacteria remained dominant phylum, but phylum Proteobacteria showed better tolerance to the co-injection of SO₂ in the initial period. In the SO₂ co-injected CO₂-saline-sandstone interaction under microbial mediation, acid-producing bacteria further promoted the corrosion of K-feldspar, albite, and clay minerals, meanwhile mobilizing more K⁺, Na⁺, Ca²⁺, Mg²⁺ into solution. The acidogenic effect may be linked to the dominant genus of Bacillus, Paenibacillus, Acinetobacter, Pseudomonas and Exiguobacterium. Co-injection of SO₂ inhibited the carbonates capture, while microbial acid production further reduced the pH, further inhibiting carbonates capture. As a result, no secondary carbonate (e.g., calcite) was observed on a short time scale within 90?days. So, microbial acidogenic effect was not conducive to carbonates capture in short term.     

Sulfur Transformation in Microbially Mediated Pyrite Oxidation by Acidithiobacillus ferrooxidans: Insights From X-ray Photoelectron Spectroscopy-Based Quantitative Depth Profiling

The oxidation of pyrite and other sulfides is responsible for the generation of acid mine drainage and acid rock drainage, which leads to further contamination of soil and water. In these processes, microbial oxidation usually prevails over chemical oxidation. To determine the mechanism of microbial oxidation of pyrite, the interaction of Acidithiobacillus ferrooxidans with pyrite was comprehensively studied, and the sulfur transformation in the interaction was disclosed using X-ray photoelectron spectroscopy (XPS) depth profiling. Abundant bacterial cells attach to pyrite surface and form biofilms, which greatly enhances surface corrosion and results in two types of etching pits: bacteria-driven rod-shaped and chemically driven hexagonal etching pits. The details of XPS depth profiles on a reacted pyrite surface reveal that the surface sulfur was first oxidized into elemental sulfur. Thereafter, elemental sulfur was further oxidized to intermediate species S₂O₃^2?, SO₃^2?, and ultimately to SO₄^2?. The oxidation sequence of sulfur is S₂^2?/S^2?→S_n^2?, S⁰→SO₃^2?, and S₂O₃^2?→SO₄^2?. Meanwhile, the remnant ferrous iron in the surface layer was released into solution and subsequently oxidized into Fe³⁺ by A. ferrooxidans and dissolved oxygen, which in turn enhanced the oxidation of sulfur. Fe³⁺, sulfate, and other ions (e.g., K⁺, Na⁺, NH₄⁺) in the solution precipitated as jarosite, hydroniumjarosite, and ammoniojarosite. On the basis of results, a three-staged model is proposed to interpret the kinetics of microbial oxidation of pyrite.     

Bioinspired FeIIICdII and FeIIIHgII complexes: synthesis, characterization and promiscuous catalytic activity evaluation

In this work we report on the synthesis, crystal structure, and physicochemical characterization of the novel dinuclear [Fe^IIICd^II(L)(μ-OAc)₂]ClO₄·0.5H₂O (1) complex containing the unsymmetrical ligand H₂L = 2-bis[{(2-pyridyl-methyl)-aminomethyl}-6-{(2-hydroxy-benzyl)-(2-pyridyl-methyl)}-aminomethyl]-4-methylphenol. Also, with this ligand, the tetranuclear [Fe₂^IIIHg₂^II(L)₂(OH)₂](ClO₄)₂·2CH₃OH (2) and [Fe^IIIHg^II(L)(μ-CO₃)Fe^IIIHg^II(L)](ClO₄)₂·H₂O (3) complexes were synthesized and fully characterized. It is demonstrated that the precursor [Fe^III₂Hg^II₂(L)₂(OH)₂](ClO₄)₂·2CH₃OH (2) can be converted to (3) by the fixation of atmospheric CO₂ since the crystal structure of the tetranuclear organometallic complex [Fe^IIIHg^II(L)(μ-CO₃)Fe^IIIHg^II(L)](ClO₄)₂·H₂O (3) with an unprecedented {Fe^III(μ-O_phenoxo)₂(μ-CO₃)Fe^III} core was obtained through X-ray crystallography. In the reaction 2 → 3 a nucleophilic attack of a Fe^III-bound hydroxo group on the CO₂ molecule is proposed. In addition, it is also demonstrated that complex (3) can regenerate complex (2) in aqueous/MeOH/NaOH solution. Magnetochemical studies reveal that the Fe^III centers in 3 are antiferromagnetically coupled (J = − 7.2 cm^− 1) and that the Fe^III-OR-Fe^III angle has no noticeable influence in the exchange coupling. Phosphatase-like activity studies in the hydrolysis of the model substrate bis(2,4-dinitrophenyl) phosphate (2,4-bdnpp) by 1 and 2 show Michaelis-Menten behavior with 1 being ~ 2.5 times more active than 2. In combination with k_H/k_D isotope effects, the kinetic studies suggest a mechanism in which a terminal Fe^III-bound hydroxide is the hydrolysis-initiating nucleophilic catalyst for 1 and 2. Based on the crystal structures of 1 and 3, it is assumed that the relatively long Fe^III…Hg^II distance could be responsible for the lower catalytic effectiveness of 2.     

Thermophilic H2 production from a cellulose-containing wastewater

Cellulose in wastewater was converted into H₂ by a mixed culture in batch experiments at 55°C with various wastewaters pH (5.5–8.5) and cellulose concentrations (10–40 g l^–1). At the optimal pH of 6.5, the maximum H₂ yield was 102 ml g^–1 cellulose and the maximum production rate was 287 ml d^–1 for each gram of volatile suspended solids (VSS). Analysis of 16S rDNA sequences showed that the cellulose-degrading mixed culture was composed of microbes closely affiliated to genus Thermoanaerobacterium.     

模拟SO42-沉降对闽江口淡水感潮野慈姑湿地甲烷排放通量的影响

2015年12月—2016年10月,每月小潮日原位定期向闽江口塔礁洲淡水感潮野慈姑(Sagittaria trifolia L.)湿地施加剂量为60、120 kg S hm~(-2)a~(-1)的K_2SO_4溶液(分别记做S-60和S-120),探讨模拟硫酸根(SO_4~(2-))沉降对河口淡水感潮湿地甲烷(CH4)排放通量及间隙水SO_4~(2-)浓度的影响。对照、S-60和S-120处理组CH_4排放通量年均值分别为(7.88±1.00)mg h~(-1)m~(-2)、(6.55±0.97)mg h~(-1)m~(-2)和(6.66±1.49)mg h~(-1)m~(-2)。在年尺度上,两个高强度模拟SO_4~(2-)沉降处理组均未显著降低闽江口淡水感潮野慈姑湿地CH_4排放通量(P0.05),即高强度SO_4~(2-)沉降不会对河口淡水感潮湿地CH_4排放通量产生类似于其对泥炭湿地和水稻田的显著抑制效应。在年尺度以及秋、冬季,两个施加K_2SO_4溶液处理显著增加了野慈姑湿地10 cm深度土壤间隙水SO_4~(2-)浓度。对于各个处理组,温度较高的夏、秋季CH_4排放通量均显著高于温度相对较低的冬、春季(P0.05)。不同处理组CH_4排放通量均与土壤温度呈显著正相关关系,温度仍然是影响亚热带河口淡水感潮湿地CH_4排放通量的重要环境因子。     

Catalysis of an isotopic exchange between CO2 and the carboxyl group of acetate by Methanosarcina barkeri grown on acetate

Cell suspensions of Methanosarcina barkeri (strain Fusaro) grown on acetate were found to catalyze the formation of methane and CO₂ from acetate (30–40 nmol/min·mg protein) and an isotopic exchange between the carboxyl group of acetate and ¹⁴CO₂ (30–40 nmol/min·mg protein). An isotopic exchange between [¹⁴C]-formate and acetate was not observed. Cells grown on methanol mediated neither methane formation from acetate nor the exchange reactions. The data indicate that the isotopic exchange between CO₂ and the carboxyl group of acetate is a partial reaction of methanogenesis from acetate. Both reactions were completely inhibited by low concentrations of cyanide (20 M) or of hydrogen (0.5% in the gas phase). Methane formation from acetate was also completely inhibited by low concentrations of carbon monoxide (0.2% in the gas phase) whereas only significantly higher concentrations of CO had an effect on the exchange reaction. In the concentration range tested KCN, H₂ and CO had no effect on methane formation from methanol or from H₂ and CO₂; however, cyanide (20 M) also affected methane formation from CO. The results are discussed with respect to proposed mechanisms of methane and CO₂ formation from acetate.     

Microbial processes of the carbon and sulfur cycles in the Chukchi Sea

The research performed in August 2004 within the framework of the Russian-American Long-term Census of the Arctic (RUSALCA) resulted in the first data concerning the rates of the key microbial processes in the water column and bottom sediments of the Bering strait and the Chukchi Sea. The total bacterial counts in the water column varied from 30 × 10³ cells ml^?1 in the northern and eastern parts to 245 × 10³ cells ml^?1 in the southern part. The methane content in the water column of the Chukchi sea varied from 8 nmol CH₄l^?1 in the eastern part of the sea to 31 nmol CH₄l^?1 in the northern part of the Herald Canyon. Microbial activity occurred in the upper 0–3 cm of the bottom sediments; the methane formation rate varied from 0.25 to 16 nmol CH₄dm^?3 day^?1. The rates of methane oxidation varied from 1.61 to 14.7 nmol CH₄dm^?3 day^?1. The rates of sulfate reduction varied from 1.35 to 16.2 μmol SO ₄ ^2? dm^?1 day^?1. The rate of methane formation in the sediments increased with depth, while sulfate reduction rates decreased (less than 1 μmol SO ₄ ^2? dm^?3 day^?1). These high concentrations of biogenic elements and high rates of microbial processes in the upper sediment layers suggest a specific type of trophic chain in the Chukchi Sea. The approximate calculated balance of methane emission from the water column into the atmosphere is from 5.4 to 57.3 μmol CH₄m^?2 day^?1.     

The carbon and hydrogen stable isotope composition of bacteriogenic methane: A laboratory study using a landfill inoculum

Anaerobic bacterial degradation of landfill waste produces a globally significant source of the greenhouse gas methane. Stable isotopic measurements of methane [δ^I3C(CH₄) and δD(CH₄)] can often fingerprint different sources of methane (natural vs. anthro‐pogenic) and help identify the bacterial processes involved in methane production. Landfill microbial communities are complex and diverse, and hence so too is the biogeochem‐istry of methane formation. To investigate the influence of (l) the methane formation pathway (acetoclastic methanogenesis and CO₂ reduction), and (2) SD of water on the stable isotopic composition of landfill methane, two model butyrate‐degrading landfill systems were established. The systems were inoculated with domestic refuse from a landfill and incubated in the laboratory for 92 days. Both systems were identical except δD of water initially added to system 2 was 118% heavier than system 1. Between days 39 and 72 the systems were resupplemented with butyrate. Production of CH₄ and CO₂ and changes in volatile fatty acid concentration confirmed that active methanogenic populations had been established. CH₄ became ¹³C enriched in both incubations with time. Interpreting changes in acetate, butyrate, and propionate concentration during incubation is complicated, but these observations and other information suggest that the dominant methanogenic substrate changed front CO₂/H₂ to acetate as the experiment progressed. This is also consistent with the observed ¹³C enrichment of CH₄, as ¹³C discrimination during methane production from acetate is less than from CO₂. In contrast, δD(CH₄) remained relatively constant, suggesting that this measurement may not provide a reliable basis for distinguishing between CH₄ from CO₂ reduction and acetoclastic methanogenesis, as has previously been suggested.     

μ- and μ4-η coordination of A2H2 (A = C, Si, Ge, Sn and Pb) ligands with transition metals

The heavier analogs of C₂H₂ have been studied at the B3LYP level for their μ and μ₄-η² coordination properties with the transition metals. Based on known alkyne compounds, transition metal fragments [W₂(μ-NH)(Cp)₂(Cl)₂] and [Fe₄(CO)₁₂] have been chosen. The SBKJC relativistic effective core potentials and their associated basis sets were used on W, Fe, Sn and Pb, and the 6-31G(d) basis set was used on all other elements. All the complexes of Si₂H₂, Ge₂H₂, Sn₂H₂ and Pb₂H₂ are found to be local minima. The trans-twist nature of the ligand A₂H₂ (A = Si-Pb) is large in μ-coordinated complexes of W, and it is very small in μ₄-η² coordinated complexes of Fe. The electronic structure of these complexes was investigated using fragment molecular orbital method (FMO).     

Evidence for the involvement and role of a corrinoid enzyme in methane formation from acetate in Methanosarcina barkeri

Methane formation from acetate in cell suspensions of Methanosarcina barkeri was inhibited by low concentrations (5 M) of propyl iodide. Inhibition was abolished by short exposure of the suspension to light which strongly indicates that a corrinoid enzyme is involved in methanogenesis from acetate. Propyl iodide (5M) had no effect on the exchange reaction between the carboxyl group of acetate and ¹⁴CO₂, and on methane formation from methanol, from H₂ and methanol, or from H₂ and CO₂. These findings indicate that the proposed corrinoid enzyme has a role in methyl group transfer to coenzyme M after C-C cleavage of acetate.Dedicated to Professor N. Pfennig on the occasion of his 60th birthday     

Nitrogen nutrition of rice plants under salinity

Two rice (Oryza sativa L.) cultivars, Koshihikari and Pokkali, were grown in solution culture at three concentrations of NaCl or Na₂SO₄ [0 (S0), 50 (S1), and 100 (S2) mmol dm^–3] and three N contents [0.7 (N1), 7 (N2) and 14 (N3) mmol dm^–3]. Salinity significantly decreased dry matter of both cultivars. Pokkali had better growth than Koshihikari under both saline and non-saline conditions. Applications of N enhanced development of shoot dry mass under S0 and S1 treatments up to N2. Under S2, N application had no effect on shoot dry mass of both cultivars. Root dry mass of both cultivars decreased with increasing N application at S1 and S2. Shoot and root NO₃-N content in both rice cultivars increased with increasing N concentration in the nutrient solutions. The absorption of NO₃-N was less in Koshihikari than Pokkali plants, and also was much less in Cl^– than SO₄ ^2– salinity suggesting the antagonism between Cl^– and NO₃ ^–. In addition a significant negative correlation between concentrations of NO₃-N and Cl^– in the shoots or roots was observed in both cultivars     

Volatile Fatty Acids and Hydrogen as Substrates for Sulfate-Reducing Bacteria in Anaerobic Marine Sediment

The addition of 20 mM MoO₄²⁻ (molybdate) to a reduced marine sediment completely inhibited the SO₄²⁻ reduction activity by about 50 nmol g⁻¹ h⁻¹ (wet sediment). Acetate accumulated at a constant rate of about 25 nmol g⁻¹ h⁻¹ immediately after MoO₄²⁻ addition and gave a measure of the preceding utilization rate of acetate by the SO₄²⁻-reducing bacteria. Similarly, propionate and butyrate (including isobutyrate) accumulated at constant rates of 3 to 7 and 2 to 4 nmol g⁻¹ h⁻¹, respectively. The rate of H₂ accumulation was variable, and a range of 0 to 16 nmol g⁻¹ h⁻¹ was recorded. An immediate increase of the methanogenic activity by 2 to 3 nmol g⁻¹ h⁻¹ was apparently due to a release of the competition for H₂ by the absence of SO₄²⁻ reduction. If propionate and butyrate were completely oxidized by the SO₄²⁻-reducing bacteria, the stoichiometry of the reactions would indicate that H₂, acetate, propionate, and butyrate account for 5 to 10, 40 to 50, 10 to 20, and 10 to 20%, respectively, of the electron donors for the SO₄²⁻-reducing bacteria. If the oxidations were incomplete, however, the contributions by propionate and butyrate would only be 5 to 10% each, and the acetate could account for as much as two-thirds of the SO₄²⁻ reduction. The presence of MoO₄²⁻ seemed not to affect the fermentative and methanogenic activities; an MoO₄²⁻ inhibition technique seems promising in the search for the natural substrates of SO₄²⁻ reduction in sediments.