Microbial Populations Stimulated for Hexavalent Uranium Reduction in Uranium Mine Sediment

Uranium-contaminated sediment and water collected from an inactive uranium mine were incubated anaerobically with organic substrates. Stimulated microbial populations removed U almost entirely from solution within 1 month. X-ray absorption near-edge structure analysis showed that U(VI) was reduced to U(IV) during the incubation. Observations by transmission electron microscopy, selected area diffraction pattern analysis, and energy-dispersive X-ray spectroscopic analysis showed two distinct types of prokaryotic cells that precipitated only a U(IV) mineral uraninite (UO₂) or both uraninite and metal sulfides. Prokaryotic cells associated with uraninite and metal sulfides were inferred to be sulfate-reducing bacteria. Phylogenetic analysis of 16S ribosomal DNA obtained from the original and incubated sediments revealed that microbial populations were changed from microaerophilic Proteobacteria to anaerobic low-G+C gram-positive sporeforming bacteria by the incubation. Forty-two out of 94 clones from the incubated sediment were related to sulfate-reducing Desulfosporosinus spp., and 23 were related to fermentative Clostridium spp. The results suggest that, if in situ bioremediation were attempted in the uranium mine ponds, Desulfosporosinus spp. would be a major contributor to U(VI) and sulfate reduction and Clostridium spp. to U(VI) reduction.     

Effect of Phosphate on the Corrosion of Carbon Steel and on the Composition of Corrosion Products in Two-Stage Continuous Cultures of Desulfovibrio desulfuricans

A field isolate of Desulfovibrio desulfuricans was grown in defined medium in a two-stage continuous culture apparatus with different concentrations of phosphate in the feed medium. The first state (V1) was operated as a conventional chemostat (D = 0.045 h⁻¹) that was limited in energy source (lactate) or phosphate. The second stage (V2) received effluent from V1 but no additional nutrients, and contained a healthy population of transiently starved or resting cells. An increase in the concentration of phosphate in the medium fed to V1 resulted in increased corrosion rates of carbon steel in both V1 and V2. Despite the more rapid corrosion observed in growing cultures relative to that in resting cultures, corrosion products that were isolated under strictly anaerobic conditions from the two culture modes had similar bulk compositions which varied with the phosphate content of the medium. Crystalline mackinawite (Fe₉S₈), vivianite [Fe₃(PO₄)₂ · 8H₂O], and goethite [FeO(OH)] were detected in amounts which varied with the culture conditions. Chemical analyses indicated that the S in the corrosion product was almost exclusively in the form of sulfides, while the P was present both as phosphate and as unidentified components, possibly reduced P species. Some differential localization of S and P was observed in intact corrosion products. Cells from lactate-limited, but not from phosphate-limited, cultures contained intracellular granules that were enriched in P and Fe. The results are discussed in terms of several proposed mechanisms of microbiologically influenced corrosion.     

Bacterial Disproportionation of Elemental Sulfur Coupled to Chemical Reduction of Iron or Manganese

A new chemolithotrophic bacterial metabolism was discovered in anaerobic marine enrichment cultures. Cultures in defined medium with elemental sulfur (S⁰) and amorphous ferric hydroxide (FeOOH) as sole substrates showed intense formation of sulfate. Furthermore, precipitation of ferrous sulfide and pyrite was observed. The transformations were accompanied by growth of slightly curved, rod-shaped bacteria. The quantification of the products revealed that S⁰ was microbially disproportionated to sulfate and sulfide, as follows: 4S⁰ + 4H₂O → SO₄^2- + 3H₂S + 2H⁺. Subsequent chemical reactions between the formed sulfide and the added FeOOH led to the observed precipitation of iron sulfides. Sulfate and iron sulfides were also produced when FeOOH was replaced by FeCO₃. Further enrichment with manganese oxide, MnO₂, instead of FeOOH yielded stable cultures which formed sulfate during concomitant reduction of MnO₂ to Mn²⁺. Growth of small rod-shaped bacteria was observed. When incubated without MnO₂, the culture did not grow but produced small amounts of SO₄^2- and H₂S at a ratio of 1:3, indicating again a disproportionation of S⁰. The observed microbial disproportionation of S⁰ only proceeds significantly in the presence of sulfide-scavenging agents such as iron and manganese compounds. The population density of bacteria capable of S⁰ disproportionation in the presence of FeOOH or MnO₂ was high, > 10⁴ cm^-3 in coastal sediments. The metabolism offers an explanation for recent observations of anaerobic sulfide oxidation to sulfate in anoxic sediments.     

Aqueous iron-sulfur systems in rice field soils of Louisiana

Summary A phase diagram of an aqueous iron-sulfur system constructed from thermodynamic data for initial concentrations of 100 ppm H₂S and 100 ppm Fe permitted us to predict that the principal precipitate found in the Eh - pH range of flooded Louisiana rice paddys would be FeS₂. Analysis of precipitates formed in the laboratory at Eh and pH levels simulating paddy conditions showed that both FeS₂ and FeS were present; however more FeS than predicted was actually precipitated in the FeS₂ field of dominance. A multiparameter diagram for an aqueous system was constructed relating equilibrium iron concentration, Eh, pH and the equilibrium H₂S concentration (that H₂S which is in equilibrium with precipitated sulfides). It was demonstrated from the diagram and associated thermodynamic equations that the H₂S⇌FeS₂ equilibrium predicts theoritical values of H₂S in agreement with experimental values of H₂S from rice paddy soil samples⁸.     

Efficient separation of subfossil Chironomidae from lake sediments

Electron transport system (ETS) activity, CO₂ evolution, O₂ consumption, N₂-fixation (C₂H₂ reduction) and methanogenesis were appropriately measured in aerobic and anaerobically incubated sediment at 4, 10 and 20 ° C to better characterize these activities under different incubation conditions. ETS activity was always higher in the aerobically incubated sediment at all three incubation temperatures, whereas (C₂H₂ reduction was always greater in the anaerobic sediment. Carbon dioxide evolution was detected only in the aerobic sediment at 10 and 20 ° C but not at 4 ° C. Methane evolution in anaerobic sediment increased gradually with an increase in the incubation temperature.     

Sedimentary Sulphur:Iron Ratio Indicates Vivianite Occurrence: A Study from Two Contrasting Freshwater Systems

An increasing number of studies constrain the importance of iron for the long-term retention of phosphorus (P) under anoxic conditions, i.e. the formation of reduced iron phosphate minerals such as vivianite (Fe₃(PO₄)₂⋅8H₂O). Much remains unknown about vivianite formation, the factors controlling its occurrence, and its relevance for P burial during early sediment diagenesis. To study the occurrence of vivianite and to assess its relevance for P binding, surface sediments of two hydrologically contrasting waters were analysed by heavy-liquid separation and subsequent powder X-ray diffraction. In Lake Arendsee, vivianite was present in deeper sediment horizons and not in the uppermost layers with a sharp transition between vivianite and non-vivianite bearing layers. In contrast, in lowland river Lower Havel vivianite was present in the upper sediment layers and not in deeper horizons with a gradual transition between non-vivianite and vivianite bearing layers. In both waters, vivianite occurrence was accompanied by the presence of pyrite (FeS₂). Vivianite formation was favoured by an elevated iron availability through a lower degree of sulphidisation and was present at a molar ratio of total sulphur to reactive iron smaller than 1.1, only. A longer lasting burden of sediments by organic matter, i.e. due to eutrophication, favours the release of sulphides, and the formation of insoluble iron sulphides leading to a lack of available iron and to less or no vivianite formation. This weakening in sedimentary P retention, representing a negative feedback mechanism (P release) in terms of water quality, could be partly compensated by harmless Fe amendments.     

Growth and Plating Efficiency of Methanococci on Agar Media

Plating techniques for cultivation of methanogenic bacteria have been optimized for two members of the genus Methanococcus. Methanococcus maripaludis and Methanococcus voltae were cultivated on aerobically and anaerobically prepared agar media. Maintenance of O₂ levels below 5 μl/liter within an anaerobic glove box was necessary during plating and incubation for 90% recovery of plated cells. Under an atmosphere of H₂, CO₂, and H₂S (79:20:1), 2 to 3 days of incubation at 37°C were sufficient for the formation of visible colonies. The viability of plated cells was significantly affected by the growth phase of the culture, H₂S concentration, and the volume of medium per plate. In addition, colony size of methanococci was affected by agar type, as well as by the concentrations of agar, H₂S, and bicarbonate.     

H2 Production by Selenomonas ruminantium in the Absence and Presence of Methanogenic Bacteria

Selenomonas ruminantium is a nonsporeforming anaerobe that ferments carbohydrates primarily to lactate, propionate, acetate and CO₂. H₂ production by this species has not been previously reported. We found, however, that some strains produce trace amounts of H₂ which can be detected by sensitive gas chromatographic procedures. H₂ production is increased markedly, in some cases almost 100-fold, when the selenomonads are co-cultured with methane-producing bacteria. Growth of the methane-producing bacteria depends on H₂ production by the selenomonads and the subsequent use of H₂ for the reduction of CO₂ to CH₄. Although no free H₂ accumulates in the mixed cultures, the amount of H₂ formed by the selenomonads can be calculated from the amount of methane produced. These studies indicate that the conventional methods for measuring H₂ production by pure cultures do not provide an adequate estimate of an organism's potential for forming H₂ in an anaerobic ecosystem where H₂ is rapidly used, e.g., for formation of CH₄.     

Formation of Ni- and Zn-Sulfides in Cultures of Sulfate-Reducing Bacteria

The purpose of this study was to characterize Ni- and Zn-sulfides precipitated in sulfate-reducing bacterial cultures. Fe-free media containing 58 mM SO ₄ ^2? were amended with Ni and Zn chloride followed by inoculation. Precipitates were sampled from cultures after two weeks of incubation at 22, 45, and 60 ^° C. Abiotic controls were prepared by reacting bacteria-free liquid media with Na ₂ S solutions under otherwise identical conditions. Precipitates were collected anaerobically, freeze-dried and analyzed by x-ray diffraction (XRD), scanning electron microscopy, and for total Ni, Zn, and S. In Ni-containing media, biogenic sulfide precipitates were mostly heazelwoodite (Ni ₃ S ₂ ), whereas abiotic precipitates were mixed heazelwoodite and vaesite (NiS ₂ ). The biogenic Ni-precipitates were better crystalline than the corresponding abiotic samples. Sphalerite (ZnS) was identified by XRD in precipitates sampled from Zn-containing media. Scanning electron microscopy revealed disordered morphological features for the sulfides, which occurred mostly as aggregates of fine particles in biogenic samples, whereas abiotic precipitates contained more plate- and needle-like structures.     

Formation of Covellite (CuS) Under Biological Sulfate-Reducing Conditions

Sulfate-reducing bacteria (SRB) play a major role in the precipitation of metal sulfides in the environment. In this work, biogenic copper sulfide formation was examined in cultures of SRB and compared to chemically initiated Cu sulfide precipitation as a reference system. Mixed cultures of SRB were incubated at 22, 45, and 60°C in nutrient solutions that contained copper sulfate. Abiotic reference samples were produced by reacting uninoculated liquid media with Na₂S solutions under otherwise identical conditions. Precipitates were collected anaerobically by centrifugation, frozen in liquid N₂, and freeze-dried, followed by analysis using X-ray diffraction (XRD), X-ray fluorescence, and scanning electron microscopy. Covellite (CuS) was the only mineral found in the precipitates. Covellite was less crystalline in the biogenic precipitates than in the abiotic samples based on XRD peak widths and peak to background ratios. Poor crystallinity may be the result of slower precipitation rates in bacterial cultures as compared to the abiotic reference systems. Furthermore, bacterial cells may inhibit the nucleation steps that lead to crystal formation. Incubation at elevated temperatures improved the crystallinity of the biotic specimens.     

Biogas production using anaerobic groundwater containing a subterranean microbial community associated with the accretionary prism

In a deep aquifer associated with an accretionary prism, significant methane (CH₄) is produced by a subterranean microbial community. Here, we developed bioreactors for producing CH₄ and hydrogen (H₂) using anaerobic groundwater collected from the deep aquifer. To generate CH₄, the anaerobic groundwater amended with organic substrates was incubated in the bioreactor. At first, H₂ was detected and accumulated in the gas phase of the bioreactor. After the H₂ decreased, rapid CH₄ production was observed. Phylogenetic analysis targeting 16S rRNA genes revealed that the H₂-producing fermentative bacterium and hydrogenotrophic methanogen were predominant in the reactor. The results suggested that syntrophic biodegradation of organic substrates by the H₂-producing fermentative bacterium and the hydrogenotrophic methanogen contributed to the CH₄ production. For H₂ production, the anaerobic groundwater, amended with organic substrates and an inhibitor of methanogens (2-bromoethanesulfonate), was incubated in a bioreactor. After incubation for 24 h, H₂ was detected from the gas phase of the bioreactor and accumulated. Bacterial 16S rRNA gene analysis suggested the dominance of the H₂-producing fermentative bacterium in the reactor. Our study demonstrated a simple and rapid CH₄ and H₂ production utilizing anaerobic groundwater containing an active subterranean microbial community.     

Role of Polysulfides in Reduction of Elemental Sulfur by the Hyperthermophilic Archaebacterium Pyrococcus furiosus

Polysulfides formed through the breakdown of elemental sulfur or other sulfur compounds were found to be reduced to H₂S by the hyperthermophilic archaebacterium Pyrococcus furiosus during growth. Metabolism of polysulfides by the organism was dissimilatory, as no incorporation of ³⁵S-labeled elemental sulfur was detected. However, [³⁵S]cysteine and [³⁵S]methionine were incorporated into cellular protein. Contact between the organism and elemental sulfur is not necessary for metabolism. The sulfide generated from metabolic reduction of polysulfides dissociates to a strong nucleophile, HS⁻, which in turn opens up the S₈ elemental sulfur ring. In addition to H₂S, P. furiosus cultures produced methyl mercaptan in a growth-associated fashion.     

Factors affecting iron sulfide-enhanced bacteriophage plaque assays in Salmonella

Reaction of ferric ions with hydrogen sulfide (H₂S) enhances contrast of phage plaques in H₂S+ Salmonella, but contrast diminishes in weak H₂S+ strains. H₂S was affected by concentrations of peptones, glucose, ferric ammonium citrate (FAC) and sodium thiosulfate (ST), and by FAC:ST ratio, temperature, pH, air, and host strain. Increasing peptone levels was most important for improving contrast in weak H₂S+ strains.     

The effect of inorganic phosphate and hydrogenase on the corrosion of mild steel

The data reported in this investigation revealed that phosphate and hydrogenase can affect the corrosion of mild steel. Phosphate reacted on mild-steel with concomitant evolution of hydrogen gas (H₂) and the formation of vivianite. The enzyme hydrogenase was shown to accelerate this reaction by oxidizing the H₂ produced, its known substrate. The components of biological growth media, one of which has been identified as phosphate, can interact with mild steel and cause corrosion. The implications of these findings to the corrosion industry are discussed. Correspondence to: E. Laishley     

Control of Oxidative Sulfur Metabolism of Chlorobium limicola forma thiosulfatophilum

A metered blend of anaerobic-grade N₂, CO₂, and H₂S gases was introduced into an illuminated, 800-ml liquid volume, continuously stirred tank reactor. The system, described as an anaerobic gas-to-liquid phase fed-batch reactor, was used to investigate the effects of H₂S flow rate and light energy on the accumulation of oxidized sulfur compounds formed by the photoautotroph Chlorobium limicola forma thiosulfatophilum during growth. Elemental sulfur was formed and accumulated in stoichiometric quantities when light energy and H₂S molar flow rate levels were optimally adjusted in the presence of nonlimiting CO₂. Deviation from the optimal H₂S and light energy levels resulted in either oxidation of sulfur or complete inhibition of sulfide oxidation. Based on these observations, a model of sulfide and sulfur oxidases electrochemically coupled to the photosynthetic reaction center of Chlorobium spp. is presented. The dynamic deregulation of oxidative pathways may be a mechanism for supplying the photosynthetic reaction center with a continuous source of electrons during periods of varying light and substrate availability, as in pond ecosystems where Chlorobium spp. are found. Possible applications for a sulfide gas removal process are discussed.     

Characterisation of an anaerobic symbiont and the associated aerobic bacterial flora of Pyrrhocoris apterus (Heteroptera: Pyrrhocoridae)

A Gram-positive anaerobic bacterium was regularly found in great numbers in histological sections and anaerobic cultures of the third bulbous mid-gut portion of Pyrrhocoris apterus (Linné 1758). It formed long chains of irregular pear-shaped cells with large spherical involutions. The fermentation products were L-lactic acid, ethanol and acetic acid, CO₂ and H₂. The peptidoglycan belongs to the Lys-Asp type. The G + C content was determined to be around 61 mol%. The organism is supposed to be a symbiont of P. apterus and to be a species of a new genus.In the aerobic cultures Streptococcus lactis, an as yet not classified Streptococcus of the serological group D and Hafnia alvei were isolated from the third part of the mid-gut.     

Oxidation of organic compounds to CO2 with sulfur or thiosulfate as electron acceptor in the anaerobic hyperthermophilic archaea Thermoproteus tenax and Pyrobaculum islandicum proceeds via the citric acid cycle

The oxidation of organic compounds with elemental sulfur or thiosulfate as electron acceptor was studied in the anaerobic hyperthermophilic archaea Thermoproteus tenax and Pyrobaculum islandicum. T. tenax was grown on either glucose or casamino acids and sulfur; P. islandicum on peptone and either elemental sulfur or thiosulfate as electron acceptor. During exponential growth only CO₂ and H₂S rather than acetate, alanine, lactate, and succinate were detected as fermentation products of both organisms; the ratio of CO₂/H₂S formed was 1:2 with elemental sulfur and 1:1 with thiosulfate as electron acceptor. Cell extracts of T. tenax and P. islandicum contained all enzymes of the citric acid cycle in catabolic activities: citrate synthase, aconitase, isocitrate dehydrogenase (NADP⁺-reducing), oxoglutarate: benzylviologen oxidoreductase, succinyl-CoA synthetase, succinate dehydrogenase, fumarase and malate dehydrogenase (NAD⁺-reducing). Carbon monoxide dehydrogenase activity was not detected. We conclude that in T. tenax and P. islandicum organic compounds are completely oxidized to CO₂ with sulfur or thiosulfate as electron acceptor and that acetyl-CoA oxidation to CO₂ proceeds via the citric acid cycle.     

Hydrogenase-3 Contributes to Anaerobic Acid Resistance of Escherichia coli

Background

Hydrogen production by fermenting bacteria such as Escherichia coli offers a potential source of hydrogen biofuel. Because H₂ production involves consumption of 2H⁺, hydrogenase expression is likely to involve pH response and regulation. Hydrogenase consumption of protons in E. coli has been implicated in acid resistance, the ability to survive exposure to acid levels (pH 2–2.5) that are three pH units lower than the pH limit of growth (pH 5–6). Enhanced survival in acid enables a larger infective inoculum to pass through the stomach and colonize the intestine. Most acid resistance mechanisms have been defined using aerobic cultures, but the use of anaerobic cultures will reveal novel acid resistance mechanisms.

Methods and Principal Findings

We analyzed the pH regulation of bacterial hydrogenases in live cultures of E. coli K-12 W3110. During anaerobic growth in the range of pH 5 to 6.5, E. coli expresses three hydrogenase isoenzymes that reversibly oxidize H₂ to 2H⁺. Anoxic conditions were used to determine which of the hydrogenase complexes contribute to acid resistance, measured as the survival of cultures grown at pH 5.5 without aeration and exposed for 2 hours at pH 2 or at pH 2.5. Survival of all strains in extreme acid was significantly lower in low oxygen than for aerated cultures. Deletion of hyc (Hyd-3) decreased anoxic acid survival 3-fold at pH 2.5, and 20-fold at pH 2, but had no effect on acid survival with aeration. Deletion of hyb (Hyd-2) did not significantly affect acid survival. The pH-dependence of H₂ production and consumption was tested using a H₂-specific Clark-type electrode. Hyd-3-dependent H₂ production was increased 70-fold from pH 6.5 to 5.5, whereas Hyd-2-dependent H₂ consumption was maximal at alkaline pH. H₂ production, was unaffected by a shift in external or internal pH. H₂ production was associated with hycE expression levels as a function of external pH.

Conclusions

Anaerobic growing cultures of E. coli generate H₂ via Hyd-3 at low external pH, and consume H₂ via Hyd-2 at high external pH. Hyd-3 proton conversion to H₂ is required for acid resistance in anaerobic cultures of E. coli.     

Growth and adaptive hydrogen production of Rhodospirillum rubrum (F1) in anaerobic dark cultures

Rhodospirillum rubrum (F₁) maintained electron balance mainly by producing propionate, formate and H₂ during fermentation metabolism. H₂ formation was inversely correlated with the production of propionate.In diluted, growing cultures high amounts of H₂ and only traces or no propionate were produced from pyruvate. In dense cultures or in resting cultures without (NH₄)₂SO₄, however, propionate was formed from pyruvate in relatively high amounts Cultures always produced much more propionate than H₂ from fructose in contrast to cells with pyruvate. Kinetic studies of growth and excretion of fermentation products indicated that the enzyme system for H₂ formation is adaptive. Chloramphenicol (3 μg/ml) completely inhibited the formation of H₂ if the cells were not adapted to fermentation metabolism. The production of propionate, on the other hand, was not prevented by chloramphenicol after shifting the cells from aerobic dark culture with malate to fermentation conditions with pyruvate.H₂ formation was not influenced by sodium ascorbate but it was significantly decreased by K₃[Fe(CN)₆].Poly(β-hydroxybutyric acid) was also synthesized by the cells during anaerobic dark metabolism especially in dense cultures, probably favoured by the rapid acidification of the medium. Formate can also accumulate in the fermentation metabolism, especially in young growing cultures.These results give an explanation for the differing reports in the literature on the fermentation metabolism of R. rubrum.     

Alkaliphilic sulfidogenesis on cellulose by combined cultures

Soda lakes are characterized by an intense sulfur cycle that begins with sulfidogenesis. Model laboratory experiments that involved combining of pure cultures showed that, during anaerobic decomposition of cellulose by Clostridium alkalicellulosi, the sulfate-reducing bacteria (SRB) of the species Desulfonatronovibrio hydrogenovorans, Desulfonatronum lacustre, and Desulfonatronum cooperativum, different in their nutritional requirements, may directly use the cellulose fermentation products for sulfidogenesis without mediatory microorganisms. In binary cocultures with SRB, the amount of the H₂S formed constituted from one-third to two-thirds of the cellulose [H] equivalents; acetate was among the products formed. When the syntrophic Contubernalis alkalaceticum, capable of acetate oxidation, was incorporated into the trophic chain along with hydrogenotrophic SRB, the amount of the H₂S formed exceeded by 33–42% the amount of the [H] equivalents in the utilized cellulose, water being the source of additional hydrogen. Thus, the trophic pathway from plant residues to sulfide, previously considered to be the longest in the alkaliphilic microbial community, may involve a minimal number of stages and do without intermediate participation of dissipotrophic fermenting organisms.