Biological sulphate reduction using food industry wastes as carbon sources

Biological treatment with dissimilatory sulphate-reducing bacteria has been considered the most promising alternative for decontamination of sulphate rich effluents. These wastewaters are usually deficient in electron donors and require their external addition to achieve complete sulphate reduction. The aim of the present study was to investigate the possibility of using food industry wastes (a waste from the wine industry and cheese whey) as carbon sources for dissimilatory sulphate-reducing bacteria. The results show that these wastes can be efficiently used by these bacteria provided that calcite tailing is present as a neutralizing and buffer material. A 95 and 50 % sulphate reduction was achieved within 20 days of experiment by a consortium of dissimilatory sulphate-reducing bacteria grown on media containing waste from the wine industry or cheese whey respectively. Identification of the dissimilatory sulphate-reducing bacteria community using the dsr gene revealed the presence of the species Desulfovibrio fructosovorans, Desulfovibrio aminophilus and Desulfovibrio desulfuricans. The findings of the present study emphasise the potential of using wastes from the wine industry as carbon source for dissimilatory sulphate-reducing bacteria, combined with calcite tailing, in the development of cost effective and environmentally friendly bioremediation processes.     

The bacteria of the sulphur cycle

This paper concentrates on the bacteria involved in the reductions and oxidations of inorganic sulphur compounds under anaerobic conditions. The genera of the dissimilatory sulphate-reducing bacteria known today are discussed with respect to their different capacities to decompose and oxidize various products of fermentative degradations of organic matter. The utilization of molecular hydrogen and formate by sulphate reducers shifts fermentations towards the energetically more favourable formation of acetate. Since acetate amounts to about two-thirds of the degradation products of organic matter, the complete anaerobic oxidation of acetate by several genera of the sulphate-reducing bacteria is an important function for terminal oxidation in sulphate-sufficient environments. The results of pure culture studies agree well with ecological investigations of several authors who showed the significance of sulphate reduction for the complete oxidation of organic matter in anaerobic marine habitats. In the dissimilatory sulphur-reducing bacteria of the genus Desulfuromonas the oxidation of acetate is linked to the reduction of elemental sulphur. Major characteristics of the anaerobic, sulphide-oxidizing phototrophic green and purple sulphur bacteria as well as of some facultative anoxygenic cyanobacteria, are given. By the formation of elemental sulphur and sulphate, these bacteria establish sulphur cycles with the sulphide-forming bacteria. In view of the morphological diversity of the sulphate-reducing bacteria and question of possible evolutionary relations to phototrophic sulphur bacteria is raised.     

Characterization of sulphate-reducing bacterial populations within marine and estuarine sediments with different rates of sulphate reduction

Viable counts of sulphate-reducing bacteria, able to use a range of different growth substrates were determined in sediments from two Sea Lochs (Etive and Eil) and an estuarine site (Tay), in Scotland. The composition of the sulphate-reducing bacterial population, in terms of substrate utilization, broadly corresponded to the in situ substrates for sulphate reduction and concentration of substrates at each site. Addition of acetate, lactate, propionate, butyrate, hydrogen and glutamate/serine (20 mM) to replicate slurries from each site resulted in stimulation of the corresponding population of sulphate-reducing bacteria and the in situ rates of sulphate reduction. The metabolism of the added substrates and changes in bacterial phospholipid fatty acids (PLFA) were quantified. With the exception of acetate and hydrogen, added substrates were incompletely oxidised, producing a mixture of further substrates, which predominantly were sequentially oxidised, and resulted in the stimulation of a mixed population of sulphate-reducing bacteria. There were significant changes in the PLFA of slurries with added substrate compared to controls. Acetate was completely removed at all sites and the small increase in even chain PLFA together with the absence of stimulation of any other biomarker, indicated that acetate was oxidised by sulphate-reducing bacteria distinctly different from those using other substrates. A biomarker for Desulfobacter, 10 Methyl 16:0, was not stimulated in any of the acetate slurries or in slurries where acetate was produced. Biomarkers for the propionate utilizing Desulfobulbus sp (17:1w6, 15:1w6) were always stimulated in propionate slurries and also in lactate slurries, where partial lactate fermentation produced propionate and acetate. In lactate and glutamate / serine slurries from the Tay estuary and lactate and hydrogen slurries from Loch Etive the biomarker for Desulfovibrio sp (i17:1w7) as well as those for Desulfobulbus were stimulated. This provides direct evidence for the significance of Desulfovibrio sp. within sediment slurries and demonstrates the competitive interaction between members of this genus and Desulfobulbus sp. for lactate, hydrogen and amino acid metabolism. At the estuarine site, sulphate reduction was limited at higher sulphate concentrations (about 3.5 mM) than the Sea Loch sites (<2 mM) and this had a significant effect on propionate and butyrate metabolism, as well as on methane production. These results demonstrate that although the sulphate-reducing bacterial population at each site could metabolise identical substrates, the types of sulphate-reducing bacteria involved and their sulphate thresholds were characteristically different.     

Reduction and precipitation of chromate by mixed culture sulphate-reducing bacterial biofilms

The ability of sulphate-reducing bacterial biofilms to reduce hexavalent chromium (Cr(VI)) to insoluble Cr(III), a process of environmental and biotechnological significance, was investigated. The reduction of chromate to insoluble form has been quantified and the effects of chromate on the carbon source utilization and sulphate-reducing activity of the bacterial biofilms evaluated. Using lactate as the carbon/energy source and in the presence of sulphate, reduction of 500 micromol l-1 Cr(VI) was monitored over a 48-h period where 88% of the total chromium was removed from solution. Mass balance calculations showed that ca 80% of the total chromium was precipitated out of solution with the bacterial biofilm retaining less than 10% of the chromium. Only ca 12% of the chromate added was not reduced to insoluble form. Although Cr(VI) did not have a significant effect on C source utilization, sulphate reduction was severely inhibited by 500 micromol-1 Cr(VI) and only ca 10% of the sulphate reducing activity detected in control biofilms occurred in the presence of Cr(VI). Low levels of sulphide were also produced in the presence of chromate, with control biofilms producing over 10-times more sulphide than Cr(VI)-exposed biofilms. Sulphide- or other chemically-mediated Cr(VI) reduction was not detected. The biological mechanism of Cr(VI) reduction is likely to be similar to that found in other sulphate-reducing bacteria.     

Acetogenesis and acetotrophy in a hexanoate-catabolizing microbial association isolated from anoxic landfill

Metabolism of the key intermediates, acetate and hydrogen, in anaerobic hexanoate catabolism by an interacting microbial association isolated from a landfill was examined in the presence of sulphate. Hydrogen (the β-oxidation product of hexanoate and butyrate), was competitively utilized by the component sulphate-reducing bacteria whereas in the absence of sulphate an interaction between H₂-utilizing acetogenic and methanogenic bacteria facilitated H₂ removal, with acetate catabolism restricted to methanogenic bacteria. A possible mechanism for energy conservation was suggested in which excess electrons were stored as acetate for subsequent usage as an energy source.     

Community analysis of a full-scale anaerobic bioreactor treating paper mill wastewater

To get insight into the microbial community of an Upflow Anaerobic Sludge Blanket reactor treating paper mill wastewater, conventional microbiological methods were combined with 16S rRNA gene analyses. Particular attention was paid to microorganisms able to degrade propionate or butyrate in the presence or absence of sulphate. Serial enrichment dilutions allowed estimating the number of microorganisms per ml sludge that could use butyrate with or without sulphate (10(5)), propionate without sulphate (10(6)), or propionate and sulphate (10(8)). Quantitative RNA dot-blot hybridisation indicated that Archaea were two-times more abundant in the microbial community of anaerobic sludge than Bacteria. The microbial community composition was further characterised by 16S rRNA-gene-targeted Denaturing Gradient Gel Electrophoresis (DGGE) fingerprinting, and via cloning and sequencing of dominant amplicons from the bacterial and archaeal patterns. Most of the nearly full length (approximately 1.45 kb) bacterial 16S rRNA gene sequences showed less than 97% similarity to sequences present in public databases, in contrast to the archaeal clones (approximately. 1.3 kb) that were highly similar to known sequences. While Methanosaeta was found as the most abundant genus, also Crenarchaeote-relatives were identified. The microbial community was relatively stable over a period of 3 years (samples taken in July 1999, May 2001, March 2002 and June 2002) as indicated by the high similarity index calculated from DGGE profiles (81.9+/-2.7% for Bacteria and 75.1+/-3.1% for Archaea). 16S rRNA gene sequence analysis indicated the presence of unknown and yet uncultured microorganisms, but also showed that known sulphate-reducing bacteria and syntrophic fatty acid-oxidising microorganisms dominated the enrichments.     

Delineation of the molecular mechanism for disulfide stress-induced aluminium toxicity

Following our previous finding that the sulfhydryl-oxidising chemical diamide induced a marked elevation of cellular Al(3+) (Wu et al., Int J Mol Sci, 12:8119-8132, 2011), a further investigation into the underlying molecular mechanism was carried out, using the eukaryotic model organism Saccharomyces cerevisiae. The effects of non-toxic dose of diamide (0.8?mM) and a mild dose of aluminium sulphate (Al(3+)) (0.4?mM) were determined prior to the screening of gene deletion mutants. A total of 81 deletion mutants were selected for this study according to the available screening data against Al(3+) only (Kakimoto et al., BioMetals, 18: 467-474, 2005) and diamide only (Thorpe et al., Proc Natl Acad Sci USA, 101: 6564-6569, 2004). On the basis of our screening data and the cluster analysis, a cluster containing the gene deletions (rpe1?, sec72?, pdr5? and ric1?) was found to be specifically sensitive to the mixture of diamide and Al(3+). However gnp1?, mch5? and ccc1? mutants were resistant. Dithiothreitol (DTT) and ascorbate markedly reversed the diamide-induced Al(3+) toxicity. Inductively-coupled plasma optical emission spectrometry demonstrated that DTT reduced the intracellular Al(3+) content in diamide/Al(3+)-treated yeast cells six-fold compared to the non-DTT controls. These data together revealed that the pleiotropic drug resistance transporter (Pdr5p) and vacuolar/vesicular transport-related proteins (Ric1p and Sec72p) are the targets of diamide. A dysfunctional membrane-bound Pdr5p terminates the detoxification pathway for Al(3+) at the final step, leading to intracellular Al(3+) accumulation and hence toxicity. As Al(3+) toxicity has been a problem in agriculture and human health, this study has provided a significant step forward in understanding Al(3+) toxicity.     

A comparison of carbon/energy and complex nitrogen sources for bacterial sulphate-reduction: potential applications to bioprecipitation of toxic metals as sulphides

Detailed nutrient requirements were determined to maximise efficacy of a sulphate-reducing bacterial mixed culture for biotechnological removal of sulphate, acidity and toxic metals from waste waters. In batch culture, lactate produced the greatest biomass, while ethanol was more effective in stimulating sulphide production and acetate was less effective. The presence of additional bicarbonate and H₂ only marginally stimulated sulphide production. The sulphide output per unit of biomass was greatest using ethanol as substrate. In continuous culture, ethanol and lactate were used directly as efficient substrates for sulphate reduction while acetate yielded only slow growth. Glucose was utilised following fermentation to organic acids and therefore had a deleterious effect on pH. Ethanol was selected as the most efficient substrate due to cost and efficient yield of sulphide. On ethanol, the presence of additional carbon sources had no effect on growth or sulphate reduction in batch culture but the presence of complex nitrogen sources (yeast extract or cornsteep) stimulated both. Cornsteep showed the strongest effect and was also preferred on cost grounds. In continuous culture, cornsteep significantly improved the yield of sulphate reduced per unit of ethanol consumed. These results suggest that the most efficient nutrient regime for bioremediation using sulphate-reducing bacteria required both ethanol as carbon source and cornsteep as a complex nitrogen source.     

Distribution of sulphur-cycle bacteria in the Ems-Dollard estuary

Summary A quantitative study of the sulphur cycle in the tidal flat-sediments of the Eems-Dollard estuary was started by determining the distribution of two physiologically different groups of bacteria: sulphate-reducing and sulphide-oxidizing bacteria. Viable counts of these bacterial groups were determined by most probable number techniques.The highest numbers of aerobic sulphide-oxidizing bacteria were found in the upper 2 cm of the sediment. A rapid decrease was observed with increasing depth.The anaerobic sulphate-reducing bacteria showed different distribution-patterns with depth. Frequently high numbers of these bacteria were found above the redox-discontinuity-layer. This may be attributed to the presence of anaerobic micro-pockets in this largely aerobic top-layer of the sediment.The horizontal distribution of the sulphide-oxidizing bacteria appeared to be highly correlated with sediment parameters such as organic carbon and clay content of the sediment. The sulphate-reducing bacteria showed only a small linear correlation with these parameters.By means of polyfactor-analysis mathematical models were made with bacterial numbers as the dependent variables and with some environmental parameters as independent variables. The parameters used in this models could explain the variance of the viable counts for approximately 70%. The clay content of the sediment and the number of sulphate reducing bacteria appeared to determine to a large extent the variance in numbers of sulphide-oxidizing bacteria. There are indications that a great deal of the sulphide-oxidizing bacteria might be mixotrophic.For the explanation of the variance in numbers of sulphate-reducing bacteria the most important parameters were the clay content of the sediment, the number of aerobic heterotrophic bacteria and temperature (or season). Therefore the numbers of these organisms were varying throughout the year. It is assumed that the heterotrophic bacteria supply the sulphate-reducing bacteria with organic substrates.     

Isolation and characterization of sulphate-reducing bacteria <Emphasis Type="Italic">Desulfovibrio vulgaris</Emphasis> from Vajreshwari thermal springs in Maharashtra,India

Sulphate-reducing bacteria (SRB) in the thermal springs of Vajreshwari were investigated with combined microbiological and molecular approaches. A sulphate-reducing bacteria medium containing lactate was used for enrichment and isolation, which yielded Gram negative, rod shaped, anaerobic, non-spore forming and motile bacteria capable of reducing sulphate to sulphide. These grew at temperatures ranging from 25 to 55 °C and could use pyruvate, lactate and ethanol as electron donors. Desulfoviridin was detected in all the isolates. The partial 16S rRNA and dissimilatory sulphite reductase (DSR) gene sequences of five representative isolates revealed that the strains belonged to the sulphur reducing bacterial species Desulfovibrio vulgaris.     

Thermophilic (55 degrees C) conversion of methanol in methanogenic-UASB reactors: influence of sulphate on methanol degradation and competition

Two upflow sludge bed reactors (UASB) were operated for 80 days at 55 degrees C with methanol as the substrate with an organic loading rate (OLR) of about 20 g CODl(-1) per day and a hydraulic retention time (HRT) of 10 h. One UASB was operated without sulphate addition (control reactor-R1) whereas the second was fed with sulphate at a COD:SO4(2-) ratio of 10 (sulphate-fed reactor-R2), providing an influent sulphate concentration of 0.6 g l(-1). For both reactors, methanogenesis was the dominant process with no considerable accumulation of acetate. The methanol removal averaged 93% and 83% for R1 and R2, respectively, and total sulphate removal was achieved in the latter. The pathway of methanol conversion for both sludges was investigated by measuring the fate of carbon in the presence and absence of bicarbonate or specific inhibitors for a sludge sample collected at day 72. In both sludges, about 70% of the methanol was syntrophically converted to methane and/or sulphide, via the intermediate H2/CO2. A strong competition between methanogens and sulphidogens took place in the R2 sludge with half of the methanol-COD being used by methane-producing bacteria and the other half by sulphate-reducing bacteria. Acetate was not an important intermediate for both sludges, and played a slightly more important role for the sulphate-adapted sludge (R2), sustained by the higher amount of bicarbonate produced during sulphate-reduction. The pathway study indicates that, although acetate does not represent an important intermediate, the system is susceptible to its accumulation.     

Sulphur and sulphate reduction with acetate and propionate in an aerobic process for sulphide removal

Summary Sulphide production rates of sulphur-and sulphate-reducing bacteria up to 50 mg per biomass support particle per day were observed in an aerated sulphide-removal reactor with polyurethane (PUR) foam as carrier material. The optimal pH and temperature for the sulphide-producing bacteria were 8.0 and 30°C respectively. Raschig rings and four types of cube-shaped PUR particles were tested as carrier materials. When using PUR particles, the sulphide production rate was always between 3% and 4% of the sulphide removal rate, dependent on the dimensions and pore size of the polyurethane support particles. With the Raschig rings this ratio was only 2% and for reactors in which no carrier materials were present it was even lower (0.6%). Media containing different mixtures of acetate, propionate, sulphur and sulphate inoculated under anoxic conditions with sludge from the aerated reactor showed the presence of acetate-degrading sulphur-reducing, but not of acetate-degrading sulphate-reducing, bacteria. With propionate as sole electron donor no degradation occurred in the presence of sulphur within 2 weeks, whereas sulphate-dependent propionate oxidation started after 5–6 days incubation. Bacteria were isolated and resembled Desulfuromonas acetoxidans and Desulfobulbus propionicus morphologically and physiologically.     

Bioaccumulation of silver by a multispecies community of bacteria

A stable community of bacteria that had unusually high tolerance of soluble silver was isolated from soil by chemostat enrichment. The community consisted of three bacteria: Pseudomonas maltophilia, Staphylococcus aureus and a coryneform organism. The pseudomonas was primarly responsible for the silver resistance. The tolerance of high silver concentrations, up to 100 mM Ag⁺, was greatly reduced when the community was grown in the absence of silver. Pseudomonas maltophilia comprised approximately 50% by numbers of the community when grown in chemostats in the presence or absence of Ag⁺ but large fluctuations occurred in population sizes of the other two bacteria; the S. aureus population was small (less than 1%) in the presence of Ag⁺ but comparised a third of the total numbers when Ag⁺ was omitted from the medium. Silver-resistant respiration of the silveradapted community was significant even when it was confronted with high concentrations of Ag⁺. In contrast the respiration of the coryneform organism and particularly S. aureus was highly sensitive to silver. The inhibition constants for silver-sensitive respiration were 0.78 mM and 0.04 mM for silver acclimatized and nonacclimatized communities respectively.The community had great capacity for silver bioaccumulation. Maximum concentrations of over 300 mg silver per g dry weight of biomass were recorded at an accumulation rate of 21 mg Ag⁺ h^-1 (g biomass)^-1. The extent of silver removal from solution was a function of initial concentration of silver; at low external concentrations (ca. 1 mM) all the silver was rapidly removed from solution, at high concentrations (ca. 12 mM) 84% removal occurred in 15 h.     

Biological availability and turnover rate of acetate in marine and estuarine sediments in relation to dissimilatory sulphate reduction

Abstract Acetate turnover rates were determined using ¹⁴C acetate in sediment slurries from two Scottish sea lochs and an estuary which had different rates of oxygen uptake and sulphate reduction. Turnover rates in Loch Etive and Loch Eil were 0.504 and 0.651 μMh⁻¹ respectively, but in the River Tay Estuary there was substantially higher acetate turnover (12.22 μMh⁻¹). The addition of 20 mM sodium molybdate, a specific metabolic inhibitor of sulphate-reducing bacteria (SRB), resulted in a complete inhibition of acetate turnover. These data suggest that SRB were solely responsible for acetate oxidation in these sediments. A comparison of acetate turnover rates in the absence of molybdate and accumulation rate in the presence of the inhibitor demonstrated that at least two pools of acetate with different biological availabilities existed. In Loch Etive only 19% of chemically measured acetate was available with corresponding values of 48% and 65% for Loch Eil and the Tay Estuary respectively.     

Competitive Formation of Hydroxycarbonate Green Rust 1 versus Hydroxysulphate Green Rust 2 in Shewanella putrefaciens Cultures

The formation of hydroxysulphate green rust 2, a Fe(II-III) compound commonly found during corrosion processes of iron-based materials in seawater, has not yet been reported in bacterial cultures. Here we used Shewanella putrefaciens, a dissimilatory iron-reducing bacterium to anaerobically catalyze the transformation of a ferric oxyhydroxide, lepidocrocite (γ-FeOOH), into Fe(II) in the presence of various sulphate concentrations. Biotransformation assays of γ-FeOOH were performed with formate as the electron donor under a variety of concentrations. The results showed that the competitive formation of hydroxycarbonate green rust 1 (GR1(CO₃ ^2?)) and hydroxysulphate green rust 2 (GR2(SO₄ ^{2 ?})) depended upon the relative ratio (R) of bicarbonate and sulphate concentrations. When R ≥ 0.17, GR1(CO₃ ^{2 ?}) only was formed whereas when R < 0.17, a mixture of GR2(SO₄ ^{2 ?}) and GR1(CO₃ ^{2 ?}) was obtained. These results demonstrated that the hydroxysulphate GR2 can originate from the microbial reduction of γ-FeOOH and confirmed the preference for carbonate over sulphate during green rust precipitation. The solid phases were characterized by X-ray diffraction, transmission Mössbauer spectroscopy and scanning electron microscopy. Diffuse reflectance infrared Fourier transform spectroscopy confirmed the presence of intercalated carbonate and sulphate in green rust's structure. This study sheds light on the influence of dissimilatory iron-reducing bacteria on microbiologically influenced corrosion.     

High rates of microbial sulphate reduction in a mesophilic ethanol-fed expanded-granular-sludge-blanket reactor

In a mesophilic (30–35 °C), sulphidogenic, ethanol-fed expanded-granular-sludge-blanket reactor, sulphate, at loading rates of up to 10.0–12.0 g Sl⁻¹␣day⁻¹, was removed with an average efficiency of more than 80%. The pH was between 7.7 and 8.3 and the maximal total dissolved sulphide concentration was up to 20 mM S (650 mg S/l). The alkaline pH was maintained by either a pH-control unit with sodium hydroxide or by stripping part of the sulphide and CO₂ from the recycle with nitrogen gas. The superficial upstream liquid velocity (v _up) was 3.0–4.5 m/h. The ratio of ethanol to sulphur was near stoichiometry. At alkaline pH, the activity of the acetotrophic sulphate-reducing bacteria, growing on acetate, was strongly enhanced, whereas at pH below 7.7 the acetotrophic sulphate-reducing bacteria were inhibited by aqueous H₂S. With regard to the removal efficiency and operational stability, external stripping with N₂ and pH control were equally successful. Received: 2 December 1996 / Received revision: 13 March 1997 / Accepted: 15 March 1997     

Coexistence of a sulphate-reducing Desulfovibrio species and the dehalorespiring Desulfitobacterium frappieri TCE1 in defined chemostat cultures grown with various combinations of sulfate and tetrachloroethene

A two-member co-culture consisting of the dehalorespiring Desulfitobacterium frappieri TCE1 and the sulphate-reducing Desulfovibrio sp. strain SULF1 was obtained via anaerobic enrichment from soil contaminated with tetrachloroethene (PCE). In this co-culture, PCE dechlorination to cis -dichloroethene was due to the activity of the dehalorespiring bacterium only. Chemostat experiments with lactate as the primary electron donor for both strains along with varying sulphate and PCE concentrations showed that the sulphate-reducing strain outnumbered the dehalogenating strain at relatively high ratios of sulphate/PCE. Stable co-cultures with both organisms present at similar cell densities were observed when both electron acceptors were supplied in the reservoir medium in nearly equimolar amounts. In the presence of low sulphate/PCE ratios, the Desulfitobacterium sp. became the numerically dominant strain within the chemostat co-culture. Surprisingly, in the absence of sulphate, strain SULF1 did not disappear completely from the co-culture despite the fact that there was no electron acceptor provided with the medium to be used by this sulphate reducer. Therefore, we propose a syntrophic association between the sulphate-reducing and the dehalorespiring bacteria via interspecies hydrogen transfer. The sulphate reducer was able to sustain growth in the chemostat co-culture by fermenting lactate and using the dehalogenating bacterium as a 'biological electron acceptor'. This is the first report describing growth of a sulphate-reducing bacterium in a defined two-member continuous culture by syntrophically coupling the electron and hydrogen transfer to a dehalorespiring bacterium.     

Genetic Diversity among Thermophilic Bacteria Isolated from Geothermal Sites by Using Two PCR Typing Methods

Microbial communities thriving at two hot springs, Hammam Pharaon (Pharaoh's Bath) and Oyoun Mossa (Moses springs), in Egypt was studied by cultural and molecular methods. Thirteen morphologically distinct strains of facultative anaerobic thermophilic bacterial isolates have been characterized and identified using phenotypic and genotypic characters including RAPD-PCR, ERIC-PCR typing, plasmid analysis and 16S rRNA sequencing. All isolates produced plasmid DNA with various sizes ranging from 0.7 kb to a larger plasmid 7.2 kb. The bacterial strains could tolerate a temperature range between 45 to 85°C and a pH between 4–11. Also, sulphate-reducing bacteria (SRB) in the thermal springs were investigated with combined biochemical and molecular approaches. A sulphate-reducing bacteria medium containing lactate was used for enrichment and isolation, which yielded Gram negative, rod shaped, anaerobic, non-spore-forming and motile bacteria capable of reducing sulphate to sulphide. These grew at temperatures ranging from 30 to 50°C and could use pyruvate, lactate and ethanol as electron donors. The dissimilatory sulphite reductase (DSR) gene sequences of eleven representative isolates revealed that the strains belonged to the sulphur reducing bacterial species Desulfovibrio vulgaris. 16S rRNA gene partial sequence results indicated the presence of novel or existing species of Bacillus (one species), Anoxybacillus (four species) and Geobacillus (eight species). In this study phenotypic and genotypic diversity were applied for the first time to differentiate thermophilic bacteria of such geothermal sites in Sinai, Egypt.     

Anaerobic degradation of naphthalene by a pure culture of a novel type of marine sulphate-reducing bacterium

Incubation of marine sediment in anoxic, sulphate-rich medium in the presence of naphthalene resulted in the enrichment of sulphate-reducing bacteria. Pure cultures with short, oval cells (1.3 by 1.3–1.9 μm) were isolated that grew with naphthalene as the only organic carbon source and electron donor for sulphate reduction to sulphide. One strain, NaphS2, was characterized. It affiliated with completely oxidizing sulphate-reducing bacteria of the δ-subclass of the Proteobacteria, as revealed by 16S rRNA sequence analysis. 2-Naphthoate, benzoate, pyruvate and acetate were used in addition to naphthalene. Quantification of substrate consumption, sulphide formation and formed cell mass revealed that naphthalene was completely oxidized with sulphate as the electron acceptor.