Distribution, diversity, and activity of sulfate-reducing bacteria in the water column in Gek-Gel lake, Azerbaijan

The distribution and activity of sulfate-reducing bacteria (SRB) in the water column of the alpine meromictic Gek-Gel lake were studied. Apart from traditional microbiological methods based on cultivation and on measuring the process rates with radioactive labels, in situ fluorescent hybridization (FISH) was used, which enables identification and quantification without cultivating organisms. The peak rate of sulfate reduction, 0.486 μg S 1⁻¹ day⁻¹, was found in the chemocline at 33 m. The peak SRB number of 2.5×10⁶ cells/ml, as determined by the most probable number method on selective media, was found at the same depth. The phylogenetic affiliation of the SRB, as determined by FISH, revealed the predominance of the Desulfovibrio spp., Desulfobulbus spp., and Desulfoarculus spp./Desulfomonile spp. groups. The numbers of spore-forming Desulfotomaculum spp. increased with depth. The low measured rates of sulfate reduction accompanied by high SRB numbers and the predominance of the groups capable of reducing a wide range of substrates permit us to assume utilization of electron acceptors other than sulfate as the main activity of the SRB in the water column. Original Russian Text ? O.V. Karnachuk, N.V. Pimenov, S.K. Yusupov, Yu.A. Frank, Ya.A. Puhakka, M.V. Ivanov, 2006, published in Mikrobiologiya, 2006, Vol. 75, No. 1, pp. 101–109.     

Anoxygenic phototrophic bacteria of the high-altitude meromictic Lake Gek-Gel,Azerbaijan

The anoxygenic phototrophic bacterial community of the high-altitude meromictic Lake Gek-Gel (Azerbaijan) was investigated in September 2003. The highest concentration of bacteriochlorophyll e (48 μg/l) was detected at a depth of 30 m; the peak of bacteriochlorophyll a (4.5 μg/l) occurred at 29 m. Phylogenetic analysis revealed that brown-colored green sulfur bacteria Chlorobium phaeobacteroides predominated in the lake. Nonsulfur purple bacteria phylogenetically close to Blastochloris sulfoviridis were found in insignificant amounts; these organisms have not been previously reported in Lake Gek-Gel.     

Methane formation and oxidation in the meromictic oligotrophic Lake Gek-Gel (Azerbaijan)

The production and oxidation of methane and diversity of culturable aerobic methanotrophic bacteria in the water column and upper sediments of the meromictic oligotrophic Lake Gek-Gel (Azerbaijan) were studied by radioisotope, molecular, and microbiological techniques. The rate of methane oxidation was low in the aerobic mixolimnion, increased in the chemocline, and peaked at the depth where oxygen was detected in the water column. Aerobic methanotrophic bacteria of type II belonging to the genus Methylocystis were identified in enrichment cultures obtained from the chemocline. Methane oxidation in the anaerobic water of the monimolimnion was much more intense than in the aerobic zone. However, below 29–30 m methane concentration increased and reached 68 μM at the bottom. The highest rate of methane oxidation under anaerobic conditions was revealed in the upper layer of bottom sediments. The rate of methane oxidation significantly exceeding that of methane production suggests a deep source of methane in this lake.     

Inorganic carbon fixation by sulfate-reducing bacteria in the Black Sea water column

The Black Sea is the largest anoxic water basin on Earth and its stratified water column comprises an upper oxic, middle suboxic and a lower permanently anoxic, sulfidic zone. The abundance of sulfate-reducing bacteria (SRB) in water samples was determined by quantifying the copy number of the dsrA gene coding for the alpha subunit of the dissimilatory (bi)sulfite reductase using real-time polymerase chain reaction. The dsrA gene was detected throughout the whole suboxic and anoxic zones. The maximum dsrA copy numbers were 5 x 10(2) and 6.3 x 10(2) copies ml(-1) at 95 m in the suboxic and at 150 m in the upper anoxic zone, respectively. The proportion of SRB to total Bacteria was 0.1% in the oxic, 0.8-1.9% in the suboxic and 1.2-4.7% in the anoxic zone. A phylogenetic analysis of 16S rDNA clones showed that most clones from the anoxic zone formed a coherent cluster within the Desulfonema-Desulfosarcina group. A similar depth profile as for dsrA copy numbers was obtained for the concentration of non-isoprenoidal dialkyl glycerol diethers (DGDs), which are most likely SRB-specific lipid biomarkers. Three different DGDs were found to be major components of the total lipid fractions from the anoxic zone. The DGDs were depleted in (13)C relative to the delta(13)C values of dissolved CO(2) (delta(13)C(CO2)) by 14-19 per thousand. Their delta(13)C values [delta(13)C(DGD(II-III))] co-varied with depth showing the least (13)C-depleted values in the top of the sulfidic, anoxic zone and the most (13)C-depleted values in the deep anoxic waters at 1500 m. This co-variation provides evidence for CO(2) incorporation by the DGD(II-III)-producing SRB, while the 1:2 relationship between delta(13)C(CO2) and delta(13)C(DGD(II-III)) indicates the use of an additional organic carbon source.     

Antigenic diversity of cytochromes c3 from the anaerobic,sulfate-reducing bacteria,Desulfovibrio

An indirect enzyme-linked immunoadsorption assay (ELISA) was developed for cytochrome c₃ using antisera to the cytochromes fromDesulfovibrio africanus Benghazi, Desulfovibrio vulgaris Hildenborough andDesulfovibrio salexigens British Guiana. The ELISA system was used to test for cross-reactions between these antisera and the heterologous antigens. In contrast to previous experiments using the Ouchterlony technique, all of the cytochromes c₃ tested exhibited some degree of cross-reaction. Considerable variation was seen in cross-reactions for cytochromes c₃ from differing strains ofD. desulfuricans. This observation raises questions about the taxonomic relatedness of these strains. No cross-reaction was seen with eukaryotic cytochrome c or withD. vulgaris cytochrome c₅₅₃. The data demonstrate that cytochrome c₃ is capable of undergoing nonprecipitating cross-reactions, and thus may not be as immunologically unique as was once thought.Abbreviations ELISA Enzyme-linked immunoadsorption assay     

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 SO(4)(2-) 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.     

Comparison of the diversity of sulfate-reducing bacterial communities in the water column and the surface sediments of a Japanese meromictic lake

The diversity and abundance of sulfate-reducing bacteria (SRB) were investigated in Lake Suigetsu, a meromictic lake in Japan characterized by a permanent oxycline at a depth between 3 and 8 m separating the aerobic freshwater epilimnion from the anaerobic, saline, sulfidogenic hypolimnion. A quantitative competitive PCR targeting the gene coding for a portion of the α-subunit of dissimilatory sulfite reductase (dsrA) was used to assess the distribution of the SRB in the stratified water column and the surface sediments. The diversity of the SRB communities was assessed using a sequence analysis of the differing dsrA isomers. The dsrA gene copy numbers of SRB in the hypolimnic waters were from 9.6 × 10³ to 7.5 × 10⁵ copies ml⁻¹, whereas higher dsrA copy numbers of SRB were observed in surface sediments, ranging from 1.8–8.1 × 10⁷ copies ml⁻¹ as estimated by competitive PCR. Phylogenetic analysis of the dsrA sequences retrieved from the surface sediments shows most belong to a deeply branching lineage of diverse dsrA sequences not related to any cultured SRB group. In contrast, dsrA sequences found in the oxycline waters were related to sequences of members of the genera Desulfonema, Desulfosarcina, and Dusulfococcus and to sequences of the incomplete oxidizers from the Desulfobulbaceae family. Diversity and abundance of dsrA genes significantly differed between the samples from the oxycline waters and the surface sediments of Lake Suigetsu, indicating habitat-specific SRB communities may contribute to the biogeochemical cycling of carbon and sulfur.     

海水养殖生境中硫酸盐还原菌活性的抑制机制

【目的】海水养殖生境中的硫化物(H₂S)严重损害养殖生物健康,控制该条件下硫酸盐还原菌(sulfate-reducing bacteria,SRB)的代谢活性是有效抑制H₂S产生的重要途径。【方法】本研究利用稀释涂布-叠皿夹法对海水养殖生境底泥中SRB进行富集筛选,获得SRB菌株,通过投加硝酸盐对菌株产H₂S的活性进行抑制。【结果】获得的2株SRB Desulfovibrio sp.NY-1和Clostridium sp.NH-1,能够在35℃、pH为7.0及盐度为20–30 mg/L条件下,分别积累高达435和150 mg/L H₂S。硝酸盐不能有效抑制NY-1产H₂S的活性,基因调控作用以及缺乏将硝酸盐作为电子受体的酶体系是其不能被抑制的主要原因。硝酸盐对NH-1 H₂S产生活性有可逆性抑制,其具有硝酸盐异化还原成铵(dissimilatory nitrate reduction to ammonium,DNRA)的能力,优先利用硝酸盐作为电子受体。DNRA作用下的中间代谢产物亚硝酸盐是有效抑制菌株NH-1产H₂S活性的主要原因,其抑制机理主要为抑制菌株的生长繁殖。【结论】硝酸盐对不同SRB菌株具有不同的抑制机制和效果,在进行硫化物污染控制前需要对产生硫化物的SRB菌群进行分析判别。     

DsrB gene-based DGGE for community and diversity surveys of sulfate-reducing bacteria

A denaturing gradient gel electrophoresis (DGGE) method was developed to assess the diversity of dsrB (dissimilatory sulfite reductase beta-subunit)-genes in sulfate-reducing communities. For this purpose a PCR primer pair was optimized for the amplification of a approximately 350 bp dsrB gene fragment that after DGGE gel electrophoresis enabled us to discriminate between dsrB genes of different SRB-subgroups,-genera and -species. The dsrB-DGGE method revealed considerable genetic diversity when applied to DNA extracts obtained from aquifer samples that were derived from monitoring wells of an in situ metal precipitation (ISMP) pilot project conducted at the site of a non-ferrous industry or from environmental heavy metal contaminated samples. The sequences of the excised and sequenced DGGE bands represented dsrB genes of different SRB-subgroups,-genera and -species, thus confirming the broad applicability of the PCR primer pair. Linking the results of the physico-chemical follow-up of the field and lab experiments to the dsrB-DGGE data will provide a better understanding of the contribution of the SRB populations to the ongoing ISMP processes.     

Diversity, activity, and abundance of sulfate-reducing bacteria in saline and hypersaline soda lakes

Soda lakes are naturally occurring highly alkaline and saline environments. Although the sulfur cycle is one of the most active element cycles in these lakes, little is known about the sulfate-reducing bacteria (SRB). In this study we investigated the diversity, activity, and abundance of SRB in sediment samples and enrichment cultures from a range of (hyper)saline soda lakes of the Kulunda Steppe in southeastern Siberia in Russia. For this purpose, a polyphasic approach was used, including denaturing gradient gel electrophoresis of dsr gene fragments, sulfate reduction rate measurements, serial dilutions, and quantitative real-time PCR (qPCR). Comparative sequence analysis revealed the presence of several novel clusters of SRB, mostly affiliated with members of the order Desulfovibrionales and family Desulfobacteraceae. We detected sulfate reducers and observed substantial sulfate reducing rates (between 12 and 423 micromol/dm(3) day(-1)) for most lakes, even at a salinity of 475 g/liter. Enrichments were obtained at salt saturating conditions (4 M Na(+)), using H(2) or volatile fatty acids as electron donors, and an extremely halophilic SRB, strain ASO3-1, was isolated. Furthermore, a high dsr gene copy number of 10(8) cells per ml was detected in a hypersaline lake by qPCR. Our results indicate the presence of diverse and active SRB communities in these extreme ecosystems.     

Diversity and distribution of sulfate-reducing bacteria in permanently frozen Lake Fryxell, McMurdo Dry Valleys, Antarctica

The permanently frozen freshwater Lake Fryxell, located in the Dry Valleys of Antarctica, exhibits an ideal geochemistry for microbial sulfate reduction. To investigate the population of sulfate-reducing bacteria in Lake Fryxell, both 16S rRNA gene and metabolic primer sets targeting the dsrA gene for the dissimilatory sulfite reductase alpha subunit were employed to analyze environmental DNA obtained from the water column and sediments of Lake Fryxell. In addition, enrichment cultures of sulfate-reducing bacteria established at 4 degrees C from Lake Fryxell water were also screened using the dsrA primer set. The sequence information obtained showed that a diverse group of sulfate-reducing prokaryotes of the domain Bacteria inhabit Lake Fryxell. With one exception, the enrichment culture sequences were not represented within the environmental sequences. Sequence data were compared with the geochemical profile of Lake Fryxell to identify possible connections between the diversity of sulfate-reducing bacteria and limnological conditions. Several clone groups were highly localized with respect to lake depth and, therefore, experienced specific physiochemical conditions. However, all sulfate-reducing bacteria inhabiting Lake Fryxell must function under the constantly cold conditions characteristic of this extreme environment.     

Distribution, diversity and ecology of aerobic CO-oxidizing bacteria

Numerous studies indicate that carbon monoxide (CO) participates in a broader range of processes than any other single molecule, ranging from subcellular to planetary scales. Despite its toxicity to many organisms, a diverse group of bacteria that span multiple phylogenetic lineages metabolize CO. These bacteria are globally distributed and include pathogens, plant symbionts and biogeochemically important lineages in soils and the oceans. New molecular and isolation techniques, as well as genome sequencing, have greatly expanded our knowledge of the diversity of CO oxidizers. Here, we present a newly emerging picture of the distribution, diversity and ecology of aerobic CO-oxidizing bacteria.     

Molecular diversity of sulfate-reducing bacteria from two different continental margin habitats

This study examined the natural diversity and distributions of sulfate-reducing bacteria along a natural carbon gradient extending down the shelf-slope transition zone of the eastern Pacific continental margin. Dissimilatory (bi)sulfite reductase gene sequences (dsrAB) were PCR amplified and cloned from five different sampling sites, each at a discrete depth, from two different margin systems, one off the Pacific coast of Mexico and another off the coast of Washington State. A total of 1,762 clones were recovered and evaluated by restriction fragment length polymorphism (RFLP) analysis. The majority of the gene sequences recovered showed site and depth restricted distributions; however, a limited number of gene sequences were widely distributed within and between the margin systems. Cluster analysis identified 175 unique RFLP patterns, and nucleotide sequences were determined for corresponding clones. Several different continental margin DsrA sequences clustered with those from formally characterized taxa belonging to the delta subdivision of the class Proteobacteria (Desulfobulbus propionicus, Desulfosarcina variabilis) and the Bacillus-Clostridium (Desulfotomaculum putei) divisions, although the majority of the recovered sequences were phylogenetically divergent relative to all of the other DsrA sequences available for comparison. This study revealed extensive new genetic diversity among sulfate-reducing bacteria in continental margin sedimentary habitats, which appears to be tightly coupled to slope depth, specifically carbon bioavailability.     

Sulfur cycling in the water column of Little Rock Lake, Wisconsin

The S cycle in the water column of a small, soft-water lake was studied for 9 years as part of an experimental study of the effects of acid rain on lakes. The two basins of the lake were artificially separated, and one basin was experimentally acidified with sulfuric acid while the other served as a reference or control. Spatial and seasonal patterns of sulfate uptake by plankton (53–70 mmol m^–2 yr^–1), deposition of sulfur to sediments in settling seston (53 mmol m^–2 yr^–1), and sulfate diffusion (0–39 mmol m^–2 yr^–1) into sediments were examined. Measurements of inputs (12–108 mmol m^–2 yr^–1) and outputs (5.5–25 mmol m^–2 yr^–1) allowed construction of a mass balance that was then compared with rates of S accumulation in sediments cores (10–28 mmol m^–2 yr^–1) and measured fluxes of S into the sediments. Because of the low SO₄ ^2– concentrations (µmole L^–1) in the lake, annual uptake by plankton (53–70 mmol m^–2 yr^–1) represented a large fraction (>50%) of the SO₄ ^2– inventory in the lake. Despite this large flux through the plankton, only small seasonal fluctuations in SO₄ ^2– concentrations (µmole L^–1) were observed; rapid mineralization of organic matter (half-life <3 months) prevented sulfate depletion in the water column. The turnover time for sulfate in the water column is only 1.4 yr; much less than the 11-yr turnover time of a conservative ion in this seepage lake. Sulfate diffusion into and reduction in the sediments (0–160 µmole m^–2 d^–1) caused SO₄ ^2– depletion in the hypolimnion. Modeling of seasonal changes in lake-water SO₄ ^2– concentrations indicated that only 30–50% of the diffusive flux of sulfate to the sediments was permanently incorporated in solid phases, and about 15% of sulfur in settling seston was buried in the sediments. The utility of sulfur mass balances for seepage lakes would be enhanced if uncertainty about the deposition velocity for both sulfate aerosols and SO₂, uncertainty in calculation of a lake-wide rate of S accumulation in sediments, and uncertainty in the measured diffusive fluxes could be further constrained.