The preferred electron acceptor of Desulfovibrio desulfuricans CSN

Abstract: The sulfate-reducing bacterium Desulfovibrio desulfuricans strain CSN (DSM 104) oxidized H₂ with thiosulfate, sulfate, sulfite, nitrite, nitrate and oxygen with rates increasing (in the order listed) from 20 to 525 nmol H₂ min⁻¹ mg⁻¹ protein. Nitrate reduction was induced by nitrate or limiting concentrations of sulfate during growth, while all other activities were constitutive. Oxygen prevented reduction of all other electron acceptors, while nitrate and nitrite blocked the reduction of the sulfur compounds. In the presence of H₂ and reduced sulfur compounds, H₂ was the preferred electron donor. The cells oxidized thiosulfate or sulfite coupled to the reduction of nitrate to ammonia. This represents a novel type of metabolism connecting the sulfur and nitrogen cycles. It is concluded that oxygen is the preferred electron acceptor of D. desulfuricans . Sulfate reduction in oxic environments must be due to different organisms or mechanisms.     

Arsenic respiration and detoxification by purple non-sulphur bacteria under anaerobic conditions

Two arsenic-resistant purple non-sulphur bacteria (PNSB), Q3B and Q3C, were isolated (from industrial contaminated site and paddy fields) and identified by SSU rRNA gene sequencing as Rhodospirillum and Rhodospirillaceae species, respectively. Maximum arsenic reduction by these PNSB was observed in anaerobic conditions. Rhodospirillum sp. Q3B showed 74.92% (v/v) arsenic reduction while Rhodospirillaceae sp. Q3C reduced arsenic up to 76.67% (v/v) in anaerobic conditions. Rhodospirillaceae sp. Q3C was found to contain highest carotenoid content up to 5.6 mg·g⁻¹. Under anaerobic conditions, the isolates were able to respire arsenic in the presence of lactate, citrate, and oxalate. Rhodospirillum sp. Q3B and Rhodospirillaceae sp. Q3C were also found to produce hydrogen gas. Such diverse bacteria can be useful tools for bioremediation purposes. These bacteria can be further exploited and optimized to treat wastewater containing arsenic along with bio-hydrogen production.     

Dissimilatory reduction of extracellular electron acceptors in anaerobic respiration

An extension of the respiratory chain to the cell surface is necessary to reduce extracellular electron acceptors like ferric iron or manganese oxides. In the past few years, more and more compounds were revealed to be reduced at the surface of the outer membrane of Gram-negative bacteria, and the list does not seem to have an end so far. Shewanella as well as Geobacter strains are model organisms to discover the biochemistry that enables the dissimilatory reduction of extracellular electron acceptors. In both cases, c-type cytochromes are essential electron-transferring proteins. They make the journey of respiratory electrons from the cytoplasmic membrane through periplasm and over the outer membrane possible. Outer membrane cytochromes have the ability to catalyze the last step of the respiratory chains. Still, recent discoveries provided evidence that they are accompanied by further factors that allow or at least facilitate extracellular reduction. This review gives a condensed overview of our current knowledge of extracellular respiration, highlights recent discoveries, and discusses critically the influence of different strategies for terminal electron transfer reactions.     

Kinetics of sulfate respiration by free-living and particle-associated sulfate-reducing bacteria

Abstract Effects on sulfate respiration of association of sulfate-reducing bacteria (SRB) with solid particles (anion exchange resin and FeS-precipitate) were examined using Desulfovibrio desulfuricans . The rates of sulfide production by resin- and FeS-associated cells were 2–3% and 19–56% of that by free-living ones, respectively, under sulfate- and lactate-rich conditions. On the other hand, under sulfate-poor (less than 50 μM) and lactate-rich conditions the rate by FeS-associated cells was higher than that by free-living ones. The values of K _m (μM), half saturation constant of the Michaelis-Menten model, for sulfate were 244 for free-living cells, 8.96 for resin-associated ones and 8.42 for FeS-associated ones. Under lactate-poor and sulfate-rich conditions the rate by FeS-associated cells was similar to that by free-living ones. These results suggest that FeS-associated SRB are more advantageous than free-living ones under sulfate-poor environments such as freshwater sediments.     

Fermentation of cysteate by a sulfate-reducing bacterium

We isolated a strictly anaerobic bacterium, strain GRZCYSA, from a sludge digestor for its ability to ferment cysteate (2-amino-3-sulfopropionate). The organism also fermented the organosulfonates isethionate (2-hydroxyethanesulfonate) and aminomethanesulfonate, but taurine (2-aminoethanesulfonate) was not a substrate. Strain GRZCYSA, a gram-negative, oxidase-negative and catalase-positive vibrio that could reduce sulfate and contained desulfoviridin, was tentatively identified as Desulfovibrio sp. Utilization of cysteate as a substrate for fermentative growth led to the formation of four products identified as acetate, ammonia, and equimolar amounts of sulfide and sulfate. The fermentation was in balance. Some reactions involved in this novel process were detected in cell-free extracts in which ammonia and acetate were formed from cysteate. Received: 10 March 1997 / Accepted: 14 May 1997     

Sulphate respiration from hydrogen in Desulfovibrio bacteria: a structural biology overview

Sulphate-reducing organisms are widespread in anaerobic enviroments, including the gastrointestinal tract of man and other animals. The study of these bacteria has attracted much attention over the years, due also to the fact that they can have important implications in industry (in biocorrosion and souring of oil and gas deposits), health (in inflamatory bowel diseases) and the environment (bioremediation). The characterization of the various components of the electron transport chain associated with the hydrogen metabolism in Desulfovibrio has generated a large and comprehensive list of studies. This review summarizes the more relevant aspects of the current information available on the structural data of various molecules associated with hydrogen metabolism, namely hydrogenases and cytochromes. The transmembrane redox complexes known to date are also described and discussed. Redox-Bohr and cooperativity effects, observed in a few cytochromes, and believed to be important for their functional role, are discussed. Kinetic studies performed with these redox proteins, showing clues to their functional inter-relationship, are also addressed. These provide the groundwork for the application of a variety of molecular modelling approaches to understanding electron transfer and protein interactions among redox partners, leading to the characterization of several transient periplasmic complexes. In contrast to the detailed understanding of the periplasmic hydrogen oxidation process, very little is known about the cytoplasmic side of the respiratory electron transfer chain, in terms of molecular components (with exception of the terminal reductases), their structure and the protein–protein interactions involved in sulphate reduction. Therefore, a thorough understanding of the sulphate respiratory chain in Desulfovibrio remains a challenging task.     

Reduction of molybdate by sulfate-reducing bacteria

Molybdate is an essential trace element required by biological systems including the anaerobic sulfate-reducing bacteria (SRB); however, detrimental consequences may occur if molybdate is present in high concentrations in the environment. While molybdate is a structural analog of sulfate and inhibits sulfate respiration of SRB, little information is available concerning the effect of molybdate on pure cultures. We followed the growth of Desulfovibrio gigas ATCC 19364, Desulfovibrio vulgaris Hildenborough, Desulfovibrio desulfuricans DSM 642, and D. desulfuricans DSM 27774 in media containing sub-lethal levels of molybdate and observed a red-brown color in the culture fluid. Spectral analysis of the culture fluid revealed absorption peaks at 467, 395 and 314 nm and this color is proposed to be a molybdate–sulfide complex. Reduction of molybdate with the formation of molybdate disulfide occurs in the periplasm D. gigas and D. desulfuricans DSM 642. From these results we suggest that the occurrence of poorly crystalline Mo-sulfides in black shale may be a result from SRB reduction and selective enrichment of Mo in paleo-seawater.     

Reduction of diverse electron acceptors by Aeromonas hydrophila

Aeromonas hydrophila ATCC 7966 grew anaerobically on glycerol with nitrate, fumarate, Fe(III), Co(III), or Se(VI) as the sole terminal electron acceptor, but did not ferment glycerol. Final cell yields were directly proportional to the amount of terminal electron acceptor provided. Twenty-four estuarine mesophilic aeromonads were isolated; all reduced nitrate, Fe(III), or Co(III), and five strains reduced Se(VI). Dissimilatory Fe(III) reduction by A. hydrophila may involve cytochromes. Difference spectra obtained with whole cells showed absorption maxima at wavelengths characteristic of c-type cytochromes (419, 522, and 553 nm). Hydrogen-reduced cytochromes within intact cells were oxidized by the addition of Fe(III) or nitrate. Studies with respiratory inhibitors yielded results consistent with a respiratory chain involving succinate (flavin-containing) dehydrogenase, quinones and cytochromes, and a single Fe(III) reductase. Neither anaerobic respiration nor dissimilatory metal reduction by members of the genus Aeromonas have been reported previously. Received: 24 June 1997 / Accepted: 20 October 1997     

Molecular characterization of sulfate-reducing bacteria in anaerobic hydrocarbon-degrading consortia and pure cultures using the dissimilatory sulfite reductase (dsrAB) genes

The characterization of sulfate-reducing bacteria (SRBs) is presented using the dissimilatory sulfite reductase (dsrAB) gene from various samples capable of mineralizing petroleum components. These samples include several novel, sulfidogenic pure cultures which degrade alkanes, toluene, and tribromophenol. Additionally, we have sulfidogenic consortia which re-mineralize benzene, naphthalene, 2-methylnaphthalene, and phenanthrene as a sole carbon source. In this study, 22 new dsrAB genes were cloned and sequenced. The dsrAB genes from our pollutant-degrading cultures or consortia were distributed among known SRBs and previously described dsrAB environmental clones, suggesting that many biodegradative SRBs are phylogenetically distinct and geographically wide spread. Specifically, the same dsrAB gene was discovered in independently established consortia capable of benzene, phenanthrene, and methylnaphthalene degradation, indicating that this particular SRB may be a key player in anaerobic degradation of hydrocarbons in the environment.     

A study on electron transport-driven proton translocation in Desulfovibrio desulfuricans

Proton translocation by washed cells of the sulfate-reducing bacterium Desulfovibrio desulfuricans strain Essex 6 was studied by means of pH and sulfide electrodes. Reversible extrusion of protons could be induced either by addition of electron acceptors to cells incubated under hydrogen, or by addition of hydrogen to cells incubated in the presence of an appropriate electron acceptor. Proton translocation was increased in the presence of ionophores that dissipate the membrane potential (thiocyanate, methyl triphenylphosphonium cation, but not valinomycin) and was sensitive to the uncoupler carbonylcyanide m-chlorophenylhydrazone (CCCP). Upon micromolar additions of H₂, usually sulfide was formed in stoichiometric amounts, and extrapolated H⁺/H₂ ratios were 1.8±0.5 with sulfate, 2.3±0.3 with sulfite and 0.5±0.1 with thiosulfate. In several experiments hydrogen pulses caused increased proton extrusion not associated with sulfide production. This was a hint that sulfite might be reduced via intermediates. In the absence of H₂S formation, extrapolated H⁺/H₂ ratios were 3.1±0.8 with sulfate, 3.4±1.1 with sulfite, 4.4±0.8 with thiosulfate and 6.3±1.2 with oxygen. Micromolar pulses of electron acceptors to cells incubated under H₂ caused less proton translocation than H₂ pulses in presence of excess of electron acceptor; extrapolated H⁺/H₂ ratios were 1.3±0.4 with sulfite, 3.3±0.9 with nitrite and 4.2±0.5 with oxygen. No proton translocation was observed after micromolar pulses of sulfate, thiosulfate or nitrate to cells incubated under hydrogen in the presence of thiocyanate. Inhibition experiments with CO and CuCl₂ revealed that the hydrogenase activity was localized in the intracellular space, and that no periplasmic hydrogenase was present. The results indicate that D. desulfuricans can generate a proton gradient by pumping protons across the cytoplasmic membrane.Abbreviations APS adenosine 5-phosphosulfate - CCCP carbonyl cyanide m-chlorophenylhydrazone - MTTP⁺ methyl triphenylphosphonium cation     

Survival of sulfate-reducing bacteria in oxic surface sediment of a seawater lake

Abstract Microhabitats and survival of sulfate-reducing bacteria (SRB) in an oxic surface sediment of a seawater lake were examined. The size of fractionation of the sediment suspension showed that most of SRB were associated with sediment particles larger than 10 μm. The D values (time in h required to destroy 90% of the initial viable population) for SRB in the whole sediment suspension and for SRB i n the < μ m and the < 5 μ m fractions were, respectively, 23.7, 10 and 4 when the SRB were exposed to air. Survival of the FeS-associated Desulfovibrio desulfuricans ( D value, 9.3) was higher than that of the free-living ones ( D value, 1.8). These results show that particle-associated SRB are more protected against oxygen than free-living ones in oxic sediments.     

Demonstration of HOQNO and antimycin A sensitive coupling of NADH oxidation and APS and sulfite reduction in a marine Desulfovibrio strain

Abstract In cell suspensions of the marine sulfate-reducing bacterium Desulfovibrio 20020 (DSM 3099) permeabilized with formaldehyde or Triton X-100, sulfite-dependent NADH oxidation activities of 0.05 μmol · min⁻¹· mg⁻¹ protein were detected. NADH oxidation coupled to APS, thiosulfate and fumarate reduction was also demonstrated. All the activities were subject to inhibition by HOQNO and antimycin A. The rate of NADH oxidation coupled to the reduction of sulfite was extremely low in cell-free extracts. The physiological function and possible mechanism of the NADH oxidation coupled to the reduction of various electron acceptors are discussed.     

Occurrence of corrinoid-containing membrane proteins in anaerobic bacteria

In Methanobacterium thermoautotrophicum a corrinoid-carrying membrane protein complex has been found, to which a tentative role in methane formation has been ascribed. To test this hypothesis representatives from different orders of methanogenic bacteria were examined for membrane-bound cobamides. These species differed in cell carbon precursor, in methane precursor, in occurrence of cytochromes and of the enzyme CO dehydrogenase, and in the systematic position (Methanobacteriales, Methanomicrobiales). All methanogenic bacteria contained cobamides in the membranes in amounts of about 60 nmol/g cell dry weight, in addition to different amounts of cobamides in the soluble cell fraction. The only central metabolic reaction obviously common to all of these methanogens was methyl coenzyme M reduction to CH₄. It is concluded that the membrane corrinoid participates in this energy-conserving reaction.Sulfate-reducing and acetogenic bacteria were included in this survey. They contained different amounts of cobamides in the soluble cell fraction but not in the membrane, a possible exception being Acetobacterium woodii.     

Adenylylsulfate reductase in some new sulfate-reducing bacteria

Four recently described species of new genera of sulfate-reducing bacteria, Desulfobulbus propionicus, Desulfobacter postgatei, Desulfococcus multivorans and Desulfosarcina variabilis were examined with respect to adenylylsulfate reductase. All of the species examined contained the enzyme in sufficient concentrations to account for dissimilatory sulfate reduction.Adenylylsulfate reductase was enriched 17.1-fold from Desulfobulbus propionicus by ammonium sulfate fractionation, ion exchange chromatography and gel filtration. The molecular weight was 175,000 and the enzyme contained 1 mol of flavin, 8 mol of non heme iron and 8 mol of labile sulfide per mol enzyme. Either ferricyanide or cytochrome c could be used as electron acceptors; the pH optimum was 7.7 with ferricyanide and 8.8 with cytochrome c. K _m values for AMP and sulfite were 90 M and 1.3 M with ferricyanide and 91 M and 71 M with cytochrome c as electron acceptor. K _m values for ferricyanide and cytochrome c were 89 M and 21 M, respectively. The properties of the enzyme were compared with those of purified adenylylsulfate reductases from other microorganisms.Non-common abbreviation APS adenylylsulfate     

Initial reactions of anaerobic metabolism of alkylbenzenes in denitrifying and sulfate-reducing bacteria

The initial activation reactions of anaerobic oxidation of the aromatic hydrocarbons toluene and ethylbenzene were investigated in cell extracts of a toluene-degrading, sulfate-reducing bacterium, Desulfobacula toluolica, and in cell extracts of strain EbN1, a denitrifying bacterium capable of degrading toluene and ethylbenzene. Extracts of toluene-grown cells of both species catalysed the addition of fumarate to the methyl group of [phenyl-¹⁴C]-toluene and formed [¹⁴C]-labeled benzylsuccinate. Extracts of ethylbenzene-grown cells of strain EbN1 did not catalyse this reaction, but catalysed the formation of 1-phenylethanol and acetophenone from [methylene-¹⁴C]-ethylbenzene. Toluene-grown cells of D. toluolica and strain EbN1 synthesised highly induced polypeptides corresponding to the large subunits of benzylsuccinate synthase from Thauera aromatica. These polypeptides were absent in strain EbN1 after growth on ethylbenzene, although a number of different polypeptides were highly induced. Thus, formation of benzylsuccinate from toluene and fumarate appears to be the general initiating step in anaerobic toluene degradation by bacteria affiliated with the phylogenetically distinct β-subclass (strain EbN1 and T. aromatica) and δ-subclass (D. toluolica) of the Proteobacteria. Anaerobic ethylbenzene oxidation proceeds via a different pathway involving a two-step oxidation of the methylene group to an alcohol and an oxo group; these steps are most probably followed by a biotin-independent carboxylation reaction and thiolytic cleavage. Received: 16 March 1998 / Accepted: 27 June 1998     

Plasmid transfer by conjugation in Desulfovibrio desulfuricans

Conjugational transfer of several IncQ plasmids from Escherichia coli to the strictly anaerobic, sulfate-reducing bacterium Desulfovibrio desulfuricans strain G100A was demonstrated. Plasmid DNA from exconjugants was visualized on agarose gels and was used to transform E. coli to the appropriate antibiotic resistances. Neither transfer of IncW and IncP plasmids to strain G100A, nor transfer of any plasmid to D. desulfuricans strain ATCC 27774 was observed. Conjugation of suicide plasmids containing either Tn5 or Tn9 into D. desulfuricans did not result in detectable transposition. Optimal conditions for conjugational transfer and antibiotic resistance levels of strain G100A were examined.     

Desulfomonile tiedjei gen. nov. and sp. nov., a novel anaerobic,dehalogenating, sulfate-reducing bacterium

An anaerobic, dehalogenating, sulfate-reducing bacterium, strain DCB-1, is described and nutritionally characterized. The bacterium is a Gram-negative, nonmotile, non-sporeforming large rod with an unusual morphological feature which resembles a collar. The microorganism reductively dehalogenates meta substituted halobenzoates and also reduces sulfate, sulfite and thiosulfate as electron acceptors. The bacterium requires nicotinamide, 1,4-naphthoquinone and thiamine for optimal growth in a defined medium. The microorganism can grow autotrophically on H₂:CO₂ with sulfate or thiosulfate as terminal electron acceptors. It can also grow heterotrophically with pyruvate, several methoxybenzoates, formate plus sulfate or benzoate plus sulfate. It ferments pyruvate to acetate and lactate in the absence of other electron acceptors. The bacterium is inhibited by MoO _inf4 ^sup2- or SeO _inf4 ^sup2- as well as tetracycline, chloramphenicol, kanamycin or streptomycin. Cytochrome c₃ and desulfoviridin have been purified from cells grown in defined medium. 16S rRNA sequence analysis indicates the organism is a new genus of sulfate-reducing bacteria in the delta subdivision of the class Proteobacteria. We propose that the strain be named Desulfomonile tiedjei.Non-standard abbreviations PIPES piperazine-N,N-bis[2-ethanesulfonic acid] - MES 2-[N-morpholino]ethanesulfonic acid - TES N-tris[hydroxymethyl]methyl-2-aminoethanesulfonic acid - HQNO 2-N-heptyl-4-hydroxy-quinoline-N-oxide - CCCP carbonyl-cyanide-m-chlorophenylhydrazine - CM carboxymethyl     

Comparative evaluation of anaerobic bacterial communities associated with roots of submerged macrophytes growing in marine or brackish water sediments

Sediment microbial communities are important for seagrass growth and carbon cycling, however relatively few studies have addressed the composition of prokaryotic communities in seagrass bed sediments. Selective media were used enumerate culturable anaerobic bacteria associated with the roots of the seagrass, Halodule wrightii, the fresh to brackish water plant, Vallisneria americana, and the respective vegetated and unvegetated sediments. H. wrightii roots and sediments had high numbers of sulfate-reducing bacteria whereas iron-reducing bacteria appeared to have a more significant role in V. americana roots and sediments. Numbers of glucose-utilizing but not acetate-utilizing iron reducers were higher on the roots of both plants relative to the vegetated sediments indicating a difference within the iron reducing bacterial community. H. wrightii roots had lower glucose-utilizing iron reducers, and higher acetogenic bacteria than did V. americana roots suggesting different aquatic plants support different anaerobic microbial communities. Sulfur-disproportionating and sulfide-oxidizing bacteria were also cultured from the roots and sediments. These results provide evidence of the potential importance of sulfur cycle bacteria, in addition to sulfate-reducing bacteria, in seagrass bed sediments.     

Selective enrichment of Geobacter sulfurreducens from anaerobic granular sludge with quinones as terminal electron acceptors

A quinone-respiring, enrichment culture derived from methanogenic granular sludge was phylogenetically characterized by using a combined cloning-denaturing gradient gel electrophoresis (DGGE) method, which revealed that the consortium developed was dominated by a single microorganism: 97% related, in a sequence of 1520 base pairs, to Geobacter sulfurreducens. The enrichment culture could grow with acetate, formate or H₂ when humic acids, the humic model compound, anthraquinone-2,6-disulfonate (AQDS), or chelated Fe(III) was provided as a terminal electron acceptor. The occurrence of a humic acid- or quinone-respiring microorganism in the microbial community of a wastewater treatment system suggests that this type of microorganisms may play a potential role in anaerobic bioreactors treating humus-containing wastewaters.