A Study of the Relative Dominance of Selected Anaerobic Sulfate-Reducing Bacteria in a Continuous Bioreactor by Fluorescence <Emphasis Type="Italic">in Situ</Emphasis> Hybridization

The diversity and the community structure of sulfate-reducing bacteria (SRB) in an anaerobic continuous bioreactor used for treatment of a sulfate-containing wastewater were investigated by fluorescence in situ hybridization. Hybridization to the 16S rRNA probe EUB338 for the domain Bacteria was performed, followed by a nonsense probe NON338 as a control for nonspecific staining. Sulfate-reducing consortia were identified by using five nominally genus-specific probes (SRB129 for Desulfobacter, SRB221 for Desulfobacterium, SRB228 for Desulfotomaculum, SRB660 for Desulfobulbus, and SRB657 for Desulfonema) and four group-specific probes (SRB385 as a general SRB probe, SRB687 for Desulfovibrioaceae, SRB814 for Desulfococcus group, and SRB804 for Desulfobacteriaceae). The total prokaryotic population was determined by 4′,6-diamidino-2-phenylindole staining. Hybridization analysis using these 16S rRNA-targeted oligonucleotide probes showed that, of those microbial groupings investigated, Desulfonema, Desulfobulbus, spp., and Desulfobacteriaceae group were the main sulfate-reducing bacteria in the bioreactor when operated at steady state at 35°C, pH 7.8, and a 2.5-day residence time with feed stream containing 2.5 kg m⁻³ sulfate as terminal electron acceptor and 2.3 kg m⁻³ acetate as carbon source and electron donor.     

Detection of anaerobic sulfate-reducing bacteria in oxygen-containing upper water layers of the Black and Baltic Seas

Fluorescent in situ hybridization (FISH) and PCR were used for analysis of phylogenetic structure of anaerobic sulfate-reducing bacterial communities in oxygen-containing upper water layers of meromictic basins: the Black Sea and the Gdansk Deep of the Baltic Sea. In the Black Sea (continental slope at depths 30–70 m), cells of sulfate-reducing bacteria (SRB) hybridizing with 16S rRNA-specific FISH-probes for Desulfotomaculum, Desulfobacter, and Desulfovibrio genera were revealed, whereas Desulfomicrobium-related bacteria were prevalent in the chemocline zone at a 150-m depth. Besides Desulfotomaculum (SRB subgroup 1), Desulfobacter (SRB subgroup 4), and Desulfovibrio-Desulfomicrobium (SRB subgroup 6), nested PCR with the use of 16S rRNA gene-specific primers detected the presence of Desulfococcus–Desulfonema–Desulfosarcina (SRB subgroup 5) in the oxygen-containing water column of the Black and Baltic seas. Active enrichment SRB culture that contained bacterium Desulfosporosinus sp. as a major component was obtained from the Black Sea water sample collected at a 70-m depth.     

Co-existence of physiologically similar sulfate-reducing bacteria in a full-scale sulfidogenic bioreactor fed with a single organic electron donor

A combination of culture-dependent and independent methods was used to study the co-existence of different sulfate-reducing bacteria (SRB) in an upflow anaerobic sludge bed reactor treating sulfate-rich wastewater. The wastewater was fed with ethanol as an external electron donor. Twenty six strains of SRB were randomly picked and isolated from the highest serial dilution that showed growth (i.e. 10⁸). Repetitive enterobacterial palindromic polymerase chain reaction and whole cell protein profiling revealed a low genetic diversity, with only two genotypes among the 26 strains obtained in the pure culture. The low genetic diversity suggests the absence of micro-niches within the reactor, which might be due to a low spatial and temporal micro-heterogeneity. The total 16S rDNA sequencing of two representative strains L3 and L7 indicated a close relatedness to the genus Desulfovibrio. The two strains differed in as many as five physiological traits, which might allow them to occupy distinct niches and thus co-exist within the same habitat. Whole cell hybridisation with fluorescently labeled oligonucleotide probes was performed to characterise the SRB community in the reactor. The isolated strains Desulfovibrio L3 and Desulfovibrio L7 were the most dominant SRB, representing 30–35% and 25–35%, respectively, of the total SRB community. Desulfobulbus-like bacteria contributed for 20–25%, and the Desulfobacca acetoxidans-specific probe targeted approximately 15–20% of the total SRB. The whole cell hybridisation results thus revealed a consortium of four different species of SRB that can be enriched and maintained on a single energy source in a full-scale sulfidogenic reactor.     

Abundance and Diversity of Sulfate-Reducing Bacteria in High Arsenic Shallow Aquifers

The abundance, diversity, and relative distribution of sulfate-reducing bacteria (SRB) in high arsenic (As) groundwater aquifers of Hangjinhouqi County in the Hetao Basin, Inner Mongolia was investigated using denaturing gradient gel electrophoresis (DGGE) and quantitative polymerase chain reaction (qPCR) analysis of dsrB genes (encoding dissimilatory sulfite reductase beta-subunit). DGGE results revealed that SRB populations were diverse, but were mainly composed of Desulfotomaculum, Desulfobulbus, Desulfosarcina, and Desulfobacca. The abundance of Desulfobulbus was positively correlated with the ratio of Fe(II)/Fe(III). Although qPCR results showed that the dsrB gene abundance in groundwater samples ranged from below detection to 4.9 × 10⁶ copies/L, and the highest percentage of dsrB gene copies to bacterial 16S rRNA gene copies was 2.1%. Geochemical analyses showed that As(III) content and the ratio of Fe(II) to Fe(III) increased with total As, while sulfate concentrations decreased. Interestingly, the dsrB gene abundance was positively correlated with As concentrations. These results indicate that sulfate reduction occurs simultaneously with As and Fe reduction, and might result in increased As release and mobilization when As is not incorporated into iron sulfides. This study improves our understanding of SRB and As cycling in high As groundwater systems.     

Investigation of the sulfate-reducing bacterial community in the aerobic water and chemocline zone of the Black Sea by the fish technique

Fluorescent in situ hybridization (FISH) was used to analyze the abundance and phylogenetic composition of sulfate-reducing bacteria in the aerobic waters and in the oxic/anoxic transitional zone (chemocline) of the Black Sea, where biogenic formation of reduced sulfur compounds was detected by radioisotope techniques. Numerous sulfate-reducing bacteria of the genera Desulfotomaculum (30.5% of detected bacterial cells), Desulfovibrio (29.6%), and Desulfobacter (6.7%) were revealed in the aerobic zone at a depth of 30 m, while Desulfomicrobium-related bacteria (33.5%) were prevalent in the upper chemocline waters at 150-m depth. Active cells of sulfate-reducing bacteria were much more abundant in the samples collected in summer than in the winter samples from the deep-sea zone. The presence of physiologically active sulfate reducers in oxic and chemocline waters of the Black Sea correlates with the hydrochemical data on the presence of reduced sulfur compounds in the aerobic water column.     

Characterization of a new thermophilic sulfate-reducing bacterium

A thermophilic sulfate-reducing vibrio isolated from thermal vent water in Yellowstone Lake, Wyoming, USA is described. The gram-negative, curved rod-shaped cells averaged 0.3 m wide and 1.5 m long. They were motile by means of a single polar flagellum. Growth was observed between 40° and 70 °C with optimal growth at 65 °C. Cultures remained viable for one year at 27 °C although spore-formation was not observed. Sulfate, thiosulfate and sulfite were used as electron acceptors. Sulfur, fumarate and nitrate were not reduced. In the presence of sulfate, growth was observed only with lactate, pyruvate, hydrogen plus acetate, or formate plus acetate. Pyruvate was the only compound observed to support fermentative growth. Pyruvate and lactate were oxidized to acetate. Desulfofuscidin and c-type cytochromes were present. The G+C content was 29.5 mol%. The divergence in the 16S ribosomal RNA sequences between the new isolate and Thermodesulfobacterium commune suggests that these two thermophilic sulfate-reducing bacteria represent different genera. These two bacteria depict a lineage that branches deeply within the Bacteria domain and which is clearly distinct from previously defined phylogenetic lines of sulfate-reducing bacteria. Strain YP87 is described as the type strain of the new genus and species Thermodesulfovibrio yellowstonii. Yellowstone Lake (Wyoming, USA) is located within one of the most tectonically active regions in the world (Klump et al. 1988; Remsen et al. 1990). Hydrothermal springs, hot gas fumaroles and elevated substrata temperatures have been observed within the lake itself (e.g., Remsen et al. 1990). Hydrothermal vent waters were reported to be anoxic, high in dissolved nutrients relative to the lake water and to have temperatures in excess of 80 °C (Klump et al. 1988; Remsen et al. 1990). Sulfate concentrations averaged 380 M in vent waters and 80 M in bulk lake water (Klump et al. 1988; Remsen et al. 1990). On the basis of on these physical and chemical characteristics, and the observation (e.g., Zeikus et al. 1983) that microbial sulfate reduction is prevalent in the thermal aquatic environments of Yellowstone National Park, we hypothesized that hydrothermal vent waters in Yellowstone Lake could support the growth of thermophilic sulfate reducers.Here we describe the general characteristics of a new thermophilic sulfate reducing bacterium, Thermodesulfovibrio yellowstonii, which was isolated from hydrothermal vent water in Sedge Bay of Yellowstone Lake, Wyoming, USA. In addition, we report on the phylogenetic relationship of this new isolate with other thermophilic and mesophilic sulfate-reducing bacteria.Dedicated to the memory of Friedhelm Bak     

Nested PCR-Denaturing Gradient Gel Electrophoresis Approach To Determine the Diversity of Sulfate-Reducing Bacteria in Complex Microbial Communities

Here, we describe a three-step nested-PCR-denaturing gradient gel electrophoresis (DGGE) strategy to detect sulfate-reducing bacteria (SRB) in complex microbial communities from industrial bioreactors. In the first step, the nearly complete 16S rRNA gene was amplified using bacterial primers. Subsequently, this product was used as a template in a second PCR with group-specific SRB primers. A third round of amplification was conducted to obtain fragments suitable for DGGE. The largest number of bands was observed in DGGE patterns of products obtained with primers specific for the Desulfovibrio-Desulfomicrobium group, indicating a large diversity of these SRBs. In addition, members of other phylogenetic SRB groups, i.e., Desulfotomaculum, Desulfobulbus, and Desulfococcus-Desulfonema-Desulfosarcina, were detected. Bands corresponding to Desulfobacterium and Desulfobacter were not detected in the bioreactor samples. Comparative sequence analysis of excised DGGE bands revealed the identity of the community members. The developed three-step PCR-DGGE strategy is a welcome tool for studying the diversity of sulfate-reducing bacteria.     

Molecular phylogenetic and biogeochemical studies of sulfate-reducing bacteria in the rhizosphere of spartina alterniflora

The population composition and biogeochemistry of sulfate-reducing bacteria (SRB) in the rhizosphere of the marsh grass Spartina alterniflora was investigated over two growing seasons by molecular probing, enumerations of culturable SRB, and measurements of SO42- reduction rates and geochemical parameters. SO42- reduction was rapid in marsh sediments with rates up to 3.5 &mgr;mol ml-1 day-1. Rates increased greatly when plant growth began in April and decreased again when plants flowered in late July. Results with nucleic acid probes revealed that SRB rRNA accounted for up to 43% of the rRNA from members of the domain Bacteria in marsh sediments, with the highest percentages occurring in bacteria physically associated with root surfaces. The relative abundance (RA) of SRB rRNA in whole-sediment samples compared to that of Bacteria rRNA did not vary greatly throughout the year, despite large temporal changes in SO42- reduction activity. However, the RA of root-associated SRB did increase from <10 to >30% when plants were actively growing. rRNA from members of the family Desulfobacteriaceae comprised the majority of the SRB rRNA at 3 to 34% of Bacteria rRNA, with Desulfobulbus spp. accounting for 1 to 16%. The RA of Desulfovibrio rRNA generally comprised from <1 to 3% of the Bacteria rRNA. The highest Desulfobacteriaceae RA in whole sediments was 26% and was found in the deepest sediment samples (6 to 8 cm). Culturable SRB abundance, determined by most-probable-number analyses, was high at >10(7) ml-1. Ethanol utilizers were most abundant, followed by acetate utilizers. The high numbers of culturable SRB and the high RA of SRB rRNA compared to that of Bacteria rRNA may be due to the release of SRB substrates in plant root exudates, creating a microbial food web that circumvents fermentation.     

Characterization of microbial communities in anaerobic bioreactors using molecular probes

The microbial community structure of twenty-one single-phase and one two-phase full-scale anaerobic sewage sludge digesters was evaluated using oligonucleotide probes complementary to conserved tracts of the 16S rRNAs of phylogenetically defined groups of methanogens and sulfate-reducing bacteria. These probe results were interpreted in combination with results from traditional chemical analyses and metabolic activity assays. It was determined that methanogens in healthy mesophilic, single-phase sewage sludge digesters accounted for approximately 8–12% of the total community and thatMethanosarcinales andMethanomicrobiales constituted the majority of the total methanogen population.Methanobacteriales andMethanococcales played a relatively minor role in the digesters. Phylogenetic groups of mesophilic, Gram-negative sulfate-reducing bacteria were consistently present at significant levels:Desulfovibrio andDesulfobulbus spp. were the dominant sulfate-reducing populations,Desulfobacter andDesulfobacterium spp. were present at lower levels, andDesulfosarcina, Desulfococcus, andDesulfobotulus spp. were absent. Sulfate reduction by one or more of these populations played a significant role in all digesters evaluated in this study. In addition, sulfate-reducing bacteria played a role in favoring methanogenesis by providing their substrates. The analysis of the two-phase digester indicated that true phase separation was not accomplished: significant levels of active methanogens were present in the first phase. It was determined that the dominant populations in the second phase were different from those in the single-phase digesters.     

Population Dynamics of a Single-Stage Sulfidogenic Bioreactor Treating Synthetic Zinc-Containing Waste Streams

Waste streams from industrial processes such as metal smelting or mining contain high concentrations of sulfate and metals with low pH. Dissimilatory sulfate reduction carried out by sulfate-reducing bacteria (SRB) at low pH can combine sulfate reduction with metal-sulfide precipitation and thus open possibilities for selective metal recovery. This study investigates the microbial diversity and population changes of a single-stage sulfidogenic gas-lift bioreactor treating synthetic zinc-rich waste water at pH 5.5 by denaturing gradient gel electrophoresis of 16S rRNA gene fragments and quantitative polymerase chain reaction. The results indicate the presence of a diverse range of phylogenetic groups with the predominant microbial populations belonging to the Desulfovibrionaceae from δ-Proteobacteria. Desulfovibrio desulfuricans-like populations were the most abundant among the SRB during the three stable phases of varying sulfide and zinc concentrations and increased from 13% to 54% of the total bacterial populations over time. The second largest group was Desulfovibrio marrakechensis-like SRB that increased from 1% to about 10% with decreasing sulfide concentrations. Desulfovibrio aminophilus-like populations were the only SRB to decrease in numbers with decreasing sulfide concentrations. However, their population was <1% of the total bacterial population in the reactor at all analyzed time points. The number of dissimilatory sulfate reductase (DsrA) gene copies per number of SRB cells decreased from 3.5 to 2 DsrA copies when the sulfide concentration was reduced, suggesting that the cells' sulfate-reducing capacity was also lowered. This study has identified the species present in a single-stage sulfidogenic bioreactor treating zinc-rich wastewater at low pH and provides insights into the microbial ecology of this biotechnological process.     

Extracellular Metabolites of Hydrocarbon-Oxidizing Bacteria as Substrates for Sulfate Reduction

The relationship between bacterial oxidation of hydrocarbons and sulfate reduction was studied in an experimental system with liquid paraffin used as a source of organic compounds inoculated with silt taken from a reservoir. Pseudomonads dominated in the hydrocarbon-oxidizing silt bacteriocenosis. However, Rodococcusand Arthrobacteria amounted to no more than 3%. Arthrobacteria dominated the microbial association formed in the paraffin film of the model system. Sulfate-reducing bacteria were represented by genera Desulfomonas, Desulfotomaculum, and Desulfovibrio. The growth of sulfate-reducing bacteria in media containing paraffin, successive products of its oxidation (cetyl alcohol, stearate, and acetate), and extracellular metabolites of hydrocarbon-reducing bacteria was studied. The data showed that sulfate-reducing bacteria did not use paraffin or cetyl alcohol as growth substrates. However, active growth of sulfate-reducing bacteria was observed in the presence of stearate and extracellular water-soluble or lipid metabolites of Arthrobacteria.     

Diversity and Characterization of Sulfate-Reducing Bacteria in Groundwater at a Uranium Mill Tailings Site

Microbially mediated reduction and immobilization of U(VI) to U(IV) plays a role in both natural attenuation and accelerated bioremediation of uranium-contaminated sites. To realize bioremediation potential and accurately predict natural attenuation, it is important to first understand the microbial diversity of such sites. In this paper, the distribution of sulfate-reducing bacteria (SRB) in contaminated groundwater associated with a uranium mill tailings disposal site at Shiprock, N.Mex., was investigated. Two culture-independent analyses were employed: sequencing of clone libraries of PCR-amplified dissimilatory sulfite reductase (DSR) gene fragments and phospholipid fatty acid (PLFA) biomarker analysis. A remarkable diversity among the DSR sequences was revealed, including sequences from δ-Proteobacteria, gram-positive organisms, and the Nitrospira division. PLFA analysis detected at least 52 different mid-chain-branched saturate PLFA and included a high proportion of 10me16:0. Desulfotomaculum and Desulfotomaculum-like sequences were the most dominant DSR genes detected. Those belonging to SRB within δ-Proteobacteria were mainly recovered from low-uranium (≤302 ppb) samples. One Desulfotomaculum-like sequence cluster overwhelmingly dominated high-U (>1,500 ppb) sites. Logistic regression showed a significant influence of uranium concentration over the dominance of this cluster of sequences (P = 0.0001). This strong association indicates that Desulfotomaculum has remarkable tolerance and adaptation to high levels of uranium and suggests the organism's possible involvement in natural attenuation of uranium. The in situ activity level of Desulfotomaculum in uranium-contaminated environments and its comparison to the activities of other SRB and other functional groups should be an important area for future research.     

Microbial community of sulfate-reducing up-flow sludge bed in the SANI<Superscript>®</Superscript> process for saline sewage treatment

This study investigated the microbial community of the sulfate-reducing up-flow sludge bed (SRUSB) of a novel sulfate reduction, autotrophic denitrification, and nitrification integrated (SANI®) process for saline sewage treatment. The investigation involved a lab-scale SANI® system treating synthetic saline sewage and a pilot-scale SANI® plant treating 10 m³/day of screened saline sewage. Sulfate-reducing bacteria (SRB) were the dominant population, responsible for more than 80% of the chemical oxygen demand removal, and no methane-producing archaea were detected in both SRUSBs. Thermotogales-like bacteria were the dominant SRB in the pilot-scale SRUSB while Desulforhopalus-like bacteria were the major species in the lab-scale SRUSB.     

Activity and Diversity of Sulfate-Reducing Bacteria in a Petroleum Hydrocarbon-Contaminated Aquifer

Microbial sulfate reduction is an important metabolic activity in petroleum hydrocarbon (PHC)-contaminated aquifers. We quantified carbon source-enhanced microbial SO₄²⁻ reduction in a PHC-contaminated aquifer by using single-well push-pull tests and related the consumption of sulfate and added carbon sources to the presence of certain genera of sulfate-reducing bacteria (SRB). We also used molecular methods to assess suspended SRB diversity. In four consecutive tests, we injected anoxic test solutions (1,000 liters) containing bromide as a conservative tracer, sulfate, and either propionate, butyrate, lactate, or acetate as reactants into an existing monitoring well. After an initial incubation period, 1,000 liters of test solution-groundwater mixture was extracted from the same well. Average total test duration was 71 h. We measured concentrations of bromide, sulfate, and carbon sources in native groundwater as well as in injection and extraction phase samples and characterized the SRB population by using fluorescence in situ hybridization (FISH) and denaturing gradient gel electrophoresis (DGGE). Enhanced sulfate reduction concomitant with carbon source degradation was observed in all tests. Computed first-order rate coefficients ranged from 0.19 to 0.32 day⁻¹ for sulfate reduction and from 0.13 to 0.60 day⁻¹ for carbon source degradation. Sulfur isotope fractionation in unconsumed sulfate indicated that sulfate reduction was microbially mediated. Enhancement of sulfate reduction due to carbon source additions in all tests and variability of rate coefficients suggested the presence of specific SRB genera and a high diversity of SRB. We confirmed this by using FISH and DGGE. A large fraction of suspended bacteria hybridized with SRB-targeting probes SRB385 plus SRB385-Db (11 to 24% of total cells). FISH results showed that the activity of these bacteria was enhanced by addition of sulfate and carbon sources during push-pull tests. However, DGGE profiles indicated that the bacterial community structure of the dominant species did not change during the tests. Thus, the combination of push-pull tests with molecular methods provided valuable insights into microbial processes, activities, and diversity in the sulfate-reducing zone of a PHC-contaminated aquifer.     

Sulfate-reducing bacterial community structure and their contribution to carbon mineralization in a wastewater biofilm growing under microaerophilic conditions

The community structure of sulfate-reducing bacteria (SRB) and the contribution of SRB to carbon mineralization in a wastewater biofilm growing under microaerophilic conditions were investigated by combining molecular techniques, molybdate inhibition batch experiments, and microelectrode measurements. A 16S rDNA clone library of bacteria populations was constructed from the biofilm sample. The 102 clones analyzed were grouped into 53 operational taxonomic units (OTUs), where the clone distribution was as follows: Cytophaga-Flexibacter-Bacteroides (41%), Proteobacteria (41%), low-G+C Gram-positive bacteria (18%), and other phyla (3%). Three additional bacterial clone libraries were also constructed from SRB enrichment cultures with propionate, acetate, and H₂ as electron donors to further investigate the differences in SRB community structure due to amendments of different carbon sources. These libraries revealed that SRB clones were phylogenetically diverse and affiliated with six major SRB genera in the delta-subclass of the Proteobacteria. Fluorescent in situ hybridization (FISH) analysis revealed that Desulfobulbus and Desulfonema were the most abundant SRB species in this biofilm, and this higher abundance (ca. 2–4×10⁹ cells cm^–3 and 5×10⁷ filaments cm^–3, respectively) was detected in the surface of the biofilm. Microelectrode measurements showed that a high sulfate-reducing activity was localized in a narrow zone located just below the oxic/anoxic interface when the biofilm was cultured in a synthetic medium with acetate as the sole carbon source. In contrast, a broad sulfate-reducing zone was found in the entire anoxic strata when the biofilm was cultured in the supernatant of the primary settling tank effluent. This is probably because organic carbon sources diffused into the biofilm from the bulk water and an unknown amount of volatile fatty acids was produced in the biofilm. A combined approach of molecular techniques and batch experiments with a specific inhibitor (molybdate) clearly demonstrated that Desulfobulbus is a numerically important member of SRB populations and the main contributor to the oxidation of propionate to acetate in this biofilm. However, acetate was preferentially utilized by nitrate-reducing bacteria but not by acetate-utilizing SRB.     

Comparative Genomic Analysis of the <Emphasis Type="Italic">sigB</Emphasis> Operon in <Emphasis Type="Italic">Listeria monocytogenes</Emphasis> and in Other Gram-Positive Bacteria

The stress-responsive, alternative sigma factor ^B has been described in members of three Gram-positive genera, Bacillus, Listeria, and Staphylococcus. In these bacteria, ^B appears to play an important role in facilitating rapid adaptation to and survival in stressful environments. ^B activity is regulated through a complex system of phosphatases and kinases encoded by rsb (regulator of sigma B) genes. We describe the sigB operon structure for the facultative intracellular pathogen Listeria monocytogenes and apply this sequence as well as other previously described sigB operon sequences to probe the evolution and functional conservation of the ^B stress response system among different Gram-positive bacteria. While ^B as well as two Rsbs (RsbS and RsbT) are highly conserved (73%, 84%, and 79% average amino acid [aa] identities, respectively), the predicted aa sequences of the other Rsb proteins showed less conservation (62–71% aa identities). Furthermore, the sigB operon structure varies among bacterial species. Bacterial species differ in the numbers and identities of rsb genes encoded in their genomes. We thus conclude that the ^B stress-response system as represented by the sigB operon has diverged in both its overall components as well as in the sequences of its individual proteins, even among closely related bacterial species. Differential evolution of this stress response system among various genera may represent a strategy that enables bacteria to adapt cellular response and survival systems to a variety of stress conditions.     

Diversity of culturable sulfidogenic bacteria in two oil–water separation tanks in the north-eastern oil fields of India

Sulfidogenic communities in the production waters of onshore oil fields in north-eastern India were examined using a culturing approach. Production water samples were inoculated into medium selective for Sulfate reducing bacteria (SRB) and Thiosulfate Reducing Bacteria (TRB). The total number of viable sulfidogenic microorganisms in the samples obtained from the two production water tanks was approximately 10⁵ MPN ml^?1 (most probable number per ml). Most of the isolates were thermo-tolerant and could be grown between 40 and 45 °C. Hydrogen sulfide production by TRB was significantly higher than by SRB. Based on 16S rRNA gene sequencing, the isolates were grouped in nine different phylotypes. Phylogenetic analysis indicated that most of the SRB were affiliated with the phylum Proteobacteria, encompassing Gram-negative bacteria, belonging to the genera Desulfovibrio, Desulfomicrobium, and Desulfobulbus. However, five isolates grouped with the genus Desulfotomaculum were found to be gram-positive SRB. Most of the thiosulfate reducing isolates was affiliated with the phylum Firmicutes, including Clostridium and Fusibacter and also with the phylum Proteobacteria, including the genera Enterobacter and Citrobacter. Phylotypes related to Clostridium (69%) and Desulfovibrio (53%) dominated the community in the production water samples. This study demonstrates the diversity of the TRB and SRB that play a critical role in the souring mediated corrosion of the oil–water separation tanks in the north-eastern India oil fields.     

荧光原位杂交在喀斯特山地土壤硫酸盐还原菌检测中的应用

采用荧光原位杂交(Florescence in situ Hybridization,FISH)技术分析了喀斯特山地土壤硫酸盐还原菌(SRB)的数量和空间分布状况.运用16S rRNA特异性探针,结合DAPI全细胞染色和样品稀释,FISH技术准确、高效地原位检测出土壤剖面中SRB的数量和分布状况.结果显示,在所研究的土壤剖面各层均有SRB检出,最低为(0.8±0.4)×107个/g,最高为(6.2±1.3)×107个/g,平均为(2.7±1.2)×107个/g.FISH能同时对土壤中的SRB进行定性和定量分析,是研究环境中SRB时空分布的快速有效的检测技术.     

Bacterial communities involved in sulfur transformations in wastewater treatment plants

The main sulfate-reducing (SRB) and sulfur-oxidizing bacteria (SOB) in six wastewater treatment plants (WWTPs) located at southern Brazil were described based on high-throughput sequencing of the 16S rDNA. Specific taxa of SRB and SOB were correlated with some abiotic factors, such as the source of the wastewater, oxygen content, sample type, and physical chemical attributes of these WWTPs. When the 22 families of SRB and SOB were clustered together, the samples presented a striking distribution, demonstrating grouping patterns according to the sample type. For SOB, the most abundant families were Spirochaetaceae, Chromatiaceae, Helicobacteriaceae, Rhodospirillaceae, and Neisseriaceae, whereas, for SRB, were Syntrophaceae, Desulfobacteraceae, Nitrospiraceae, and Desulfovibriaceae. The structure and composition of the major families related to the sulfur cycle were also influenced by six chemical attributes (sulfur, potassium, zinc, manganese, phosphorus, and nitrogen). Sulfur was the chemical attribute that most influenced the variation of bacterial communities in the WWTPs (λ = 0.14, p = 0.008). The OTUs affiliated to Syntrophus showed the highest response to the increase of total sulfur. All these findings can contribute to improve the understanding in relation to the sulfur-oxidizing and sulfate-reducing communities in WWTPs aiming to reduce H₂S emissions.     

Geological gas-storage shapes deep life

Around the world, several dozen deep sedimentary aquifers are being used for storage of natural gas. Ad hoc studies of the microbial ecology of some of them have suggested that sulfate reducing and methanogenic microorganisms play a key role in how these aquifers' communities function. Here, we investigate the influence of gas storage on these two metabolic groups by using high-throughput sequencing and show the importance of sulfate-reducing Desulfotomaculum and a new monophyletic methanogenic group. Aquifer microbial diversity was significantly related to the geological level. The distance to the stored natural gas affects the ratio of sulfate-reducing Firmicutes to deltaproteobacteria. In only one aquifer, the methanogenic archaea dominate the sulfate-reducers. This aquifer was used to store town gas (containing at least 50% H₂) around 50 years ago. The observed decrease of sulfates in this aquifer could be related to stimulation of subsurface sulfate-reducers. These results suggest that the composition of the microbial communities is impacted by decades old transient gas storage activity. The tremendous stability of these gas-impacted deep subsurface microbial ecosystems suggests that in situ biotic methanation projects in geological reservoirs may be sustainable over time.