Heavy Metal Resistance and Accumulation Characteristics in Willows

The resistance of Salix to Cu, Cd, Ni, and Zn was investigated in hydroponic culture, with phytoextraction potential evaluated for Cu. Root elongation (indicative of resistance level) was significantly affected, with considerable variation between and within individual clones. Resistance appeared to be clone- or hybrid-specific, rather than species-specific. S. caprea clones (and hybrids) were among the most resistant, but a secondary S. caprea clone from a different provenance was much less tolerant. S. viminalis and S. triandra clones were the most sensitive. Highest resistance was found in response to Cd, while Cu and Ni were extremely toxic. A resistant S. caprea ecotype originating from a metalliferous mine spoil was identified using this technique. Copper concentration reached a maximum of 2000, 400, and 82 μg g^-1 (d.wt) in roots, wood, and foliage, respectively, after 1 month in hydroponic culture. The level of variation in the response of Salix to metals may cause difficulties in phytoremediation screening programs, but may be essential in providing genetic variation for selection of metal resistance traits, where the contaminant profile is heterogeneous, mixed, or subject to change. Clone selection for metal phytoextraction is feasible, but a longer field-scale study on metal-contaminated soils is needed before their role in phytoremediation can be confirmed.     

Bacteria Metabolically Engineered for Enhanced Phytochelatin Production and Cadmium Accumulation

Phytochelatins (PCs) with good binding affinities for a wide range of heavy metals were exploited to develop microbial sorbents for cadmium removal. PC synthase from Schizosaccharomyces pombe (SpPCS) was overexpressed in Escherichia coli, resulting in PC synthesis and 7.5-times-higher Cd accumulation. The coexpression of a variant γ-glutamylcysteine synthetase desensitized to feedback inhibition (GshI*) increased the supply of the PC precursor glutathione, resulting in further increases of 10- and 2-fold in PC production and Cd accumulation, respectively. A Cd transporter, MntA, was expressed with SpPCS and GshI* to improve Cd uptake, resulting in a further 1.5-fold increase in Cd accumulation. The level of Cd accumulation in this recombinant E. coli strain (31.6 μmol/g [dry weight] of cells) was more than 25-fold higher than that in the control strain.     

Extracellular Accumulation of DNA by Hydrocarbon-utilizing Bacteria

Some hydrocarbon-utilizing bacteria grown on n-paraffin as the sole source of carbon accumulated extracellularly a considerable amount of DNA (0.1 g to 0.6 g per liter) which was free from intact cells and slime materials. This was particularly noted when the strains belonging to Pseudomonad were employed. n-Paraffin was a preferable carbon source for the accumulation of DNA by Pseudomonad, while a strain of Arthrobacter accumulated DNA by growing it on glucose.

The DNA thus accumulated was easily isolated and purified free from other cellular components. The purified DNA was highly polymerized (above 4 × l0⁶ daltons), having the same base composition as the cellular DNA.     

Detection and Quantification of Functional Genes of Cellulose- Degrading,Fermentative, and Sulfate-Reducing Bacteria and Methanogenic Archaea

Cellulose degradation, fermentation, sulfate reduction, and methanogenesis are microbial processes that coexist in a variety of natural and engineered anaerobic environments. Compared to the study of 16S rRNA genes, the study of the genes encoding the enzymes responsible for these phylogenetically diverse functions is advantageous because it provides direct functional information. However, no methods are available for the broad quantification of these genes from uncultured microbes characteristic of complex environments. In this study, consensus degenerate hybrid oligonucleotide primers were designed and validated to amplify both sequenced and unsequenced glycoside hydrolase genes of cellulose-degrading bacteria, hydA genes of fermentative bacteria, dsrA genes of sulfate-reducing bacteria, and mcrA genes of methanogenic archaea. Specificity was verified in silico and by cloning and sequencing of PCR products obtained from an environmental sample characterized by the target functions. The primer pairs were further adapted to quantitative PCR (Q-PCR), and the method was demonstrated on samples obtained from two sulfate-reducing bioreactors treating mine drainage, one lignocellulose based and the other ethanol fed. As expected, the Q-PCR analysis revealed that the lignocellulose-based bioreactor contained higher numbers of cellulose degraders, fermenters, and methanogens, while the ethanol-fed bioreactor was enriched in sulfate reducers. The suite of primers developed represents a significant advance over prior work, which, for the most part, has targeted only pure cultures or has suffered from low specificity. Furthermore, ensuring the suitability of the primers for Q-PCR provided broad quantitative access to genes that drive critical anaerobic catalytic processes.The gene encoding the 16S small ribosomal subunit has served as a highly suitable target for studying bacterial species. When one obtains 16S rRNA gene sequence information, it is sometimes possible to infer function from an identical match to a well-characterized pure culture. More commonly, however, the similarity to pure cultures is low, and/or the highest similarities correspond to 16S rRNA gene sequences identified without isolation or phenotypic characterization. In either case, care must be taken, because distinct phenotypes [e.g., dissimilatory Fe(III) reduction, chlorate reduction] are found in microorganisms with highly similar (e.g., 99.5%) 16S rRNA gene sequences (1). In addition, 16S rRNA gene surveys of broad phylogenetic groups can be time-, labor-, and cost-intensive. For example, it is estimated that the 16S rRNA gene-based detection of all recognized lineages of sulfate-reducing bacteria (SRB) would require approximately 132 16S rRNA gene-targeted microarray probes (32).A more-direct approach for the study of microbes that span phylogenetic groups is to target them as a physiologically coherent guild by using specific genetic markers (functional genes) for the functions of interest. Functional genes have been successfully targeted in bioremediation studies to investigate microbial populations responsible for the degradation of various contaminants. Some examples include the use of the large alpha subunit of benzylsuccinate synthase to monitor anaerobic hydrocarbon-degrading bacteria (5), the monitoring of ars genes for the identification and quantification of arsenic-metabolizing bacteria (45), and the detection of catechol 1,2-dioxygenase in aromatic-hydrocarbon-degrading Rhodococcus spp. (48). In the field of mine drainage/metal remediation, functional genes have been used to target SRB (17, 26), but the methods have suffered both from a lack of broad specificity for SRB and from the inability to distinguish SRB from sulfur-oxidizing bacteria (SOB). A general challenge to the functional-gene approach has been the relative lack of characterization and unavailability of target sequences. As a consequence, the primer sets that are available tend to be more relevant to pure cultures than to complex environmental samples.Microbial communities in natural and engineered anaerobic environments that utilize cellulose as the primary carbon source, such as those in rumina (56), termite guts (54), decomposing wood (7), sulfate-reducing and methanogenic sediments (9, 22), wetlands (28), and sulfate-reducing bioreactors (26), are particularly challenging to characterize. 16S rRNA gene-based studies have revealed the complexity of these microbial communities and their high levels of phylogenetic and functional diversity. In such anaerobic environments, mineralization of complex organic matter occurs through the concerted action of a variety of microorganisms. Primary fermenters, such as cellulose degraders, break down the complex molecules and ferment the hydrolysis products. Secondary fermenters also ferment the hydrolysis products. When sulfate is available, SRB utilize the fermentation products as carbon and energy sources. In addition, methanogens can also utilize some of the fermentation products. In many cases, functionally important members, such as SRB, are present only as a small fraction of the community (36, 38), making them difficult to detect by use of 16S rRNA gene-targeted fingerprinting methods. Furthermore, the phylogenetic diversity of cellulose degraders, fermenters, and SRB prevents their quantification using a small number of 16S rRNA gene-targeted probes.In this study, degenerate PCR primers were developed, validated, and demonstrated for the amplification of key functional groups in anaerobic environments possessing genes encoding glycoside hydrolases of families 5 (collectively designated cel5 in this study) and 48 (collectively designated cel48 in this study) (cellulose degradation), the alpha subunit of iron hydrogenase (hydA) (fermentation), dissimilatory sulfite reductase (dsrA) (sulfate reduction), and methyl coenzyme M reductase (mcrA) (methanogenesis). This work is particularly novel considering that the vast majority of existing methods are suitable only for pure cultures, especially in the cases of cel5, cel48, and hydA (21, 44, 47). Thus, the approach provides access to uncultured and unsequenced markers, a critical feature for the study of key anaerobic processes in complex environments. Specificity was also enhanced where possible, notably in the case of dsrA, for which existing primers either do not distinguish SRB from SOB (14, 17) or have good alignment with only a narrow range of SRB (31, 52). Finally, all primers in this study were designed and validated for quantitative PCR (Q-PCR), in order to provide valuable quantitative functional information about complex anaerobic communities. The approach is demonstrated on mine drainage remediation systems and is expected to be of broad value to a variety of fields, including advancing the understanding of biohydrogen production, global carbon cycling, and other important biogeochemical processes.     

Trace Metal Imaging of Sulfate-Reducing Bacteria and Methanogenic Archaea at Single-Cell Resolution by Synchrotron X-Ray Fluorescence Imaging

Metal cofactors are required for many enzymes in anaerobic microbial respiration. This study examined iron, cobalt, nickel, copper, and zinc in cellular and abiotic phases at the single-cell scale for a sulfate-reducing bacterium (Desulfococcus multivorans) and a methanogenic archaeon (Methanosarcina acetivorans) using synchrotron X-ray fluorescence microscopy. Relative abundances of cellular metals were also measured by inductively coupled plasma mass spectrometry. For both species, zinc and iron were consistently the most abundant cellular metals. M. acetivorans contained higher nickel and cobalt content than D. multivorans, likely due to elevated metal requirements for methylotrophic methanogenesis. Cocultures contained spheroid zinc sulfides and cobalt/copper sulfides.     

Distribution of Methanogenic and Sulfate-Reducing Bacteria in Near-Shore Marine Sediments

The distribution of methanogenic and sulfate-reducing bacteria was examined in sediments from three sites off the coast of eastern Connecticut and five sites in Long Island Sound. Both bacterial groups were detected at all sites. Three distributional patterns were observed: (i) four sites exhibited methanogenic and sulfate-reducing populations which were restricted to the upper 10 to 20 cm, with a predominance of sulfate reducers; (ii) three sites in western Long Island Sound exhibited a methanogenic population most abundant in sediments deeper than those occupied by sulfate reducers; (iii) at one site that was influenced by fresh groundwater, methanogens and sulfate reducers were numerous within the same depths; however, the number of sulfate reducers varied vertically and temporally with sulfate concentrations. It was concluded that the distributions of abundant methanogenic and sulfate-reducing bacteria were mutually exclusive. Methanogenic enrichments yielded all genera of methanogens except Methanosarcina, with the methanobacteria predominating.     

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

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

硫酸盐还原菌鉴定和检测方法的研究进展

硫酸盐还原菌有着重要的生态、经济和环境意义。系统地论述了硫酸盐还原菌鉴定和检测常用手段,如硫酸盐还原菌分离纯化培养方法、检测遗传标记的分子生物学方法和生物特征化合物方法。这些技术的发展,不断扩展了硫酸盐还原菌的研究领域和深度并使对硫酸盐还原菌在分子水平的研究成为可能。     

Sulfate-Reducing Bacteria in Gypsum Karst Lakes of Northern Lithuania

Microbiological studies were performed in three small gypsum karst lakes in northern Lithuania, most typical of the region. Samples were taken in different seasons of 2001. The conditions for microbial growth in the lakes are determined by elevated content of salts (from 0.5 to 2.0 g/l), dominated by SO ₄ ^2? and Ca²⁺ ions (up to 1.4 and 0.6 g/l, respectively). The elevated sulfate concentration is favorable for sulfate-reducing bacteria (SRBs). Summer and winter stratification gives rise to anaerobic water layers enriched in products of anaerobic degradation: H₂S and CH₄. The lakes under study contain abundant SRBs not only in bottom sediments (from 10³ to 10⁷ cells/dm³) but also in the water column (from 10² to 10⁶ cells/ml). The characteristic spatial and temporal variations in the rate of sulfate reduction were noted. The highest rates of this process were recorded in summer: 0.95–2.60 mg S^2?/dm³ per day in bottom sediments and up to 0.49 mg S^2?/l per day in the water column. The maximum values (up to 11.36 mg S^2?/dm³) were noted in areas where bottom sediments were enriched in plankton debris. Molecular analysis of conservative sequences of the gene for 16S rRNA in sulfate-reducing microorganisms grown on lactate allowed them to be identified as Desulfovibrio desulfuricans.     

Molecular Characterization of Sulfate-Reducing Bacteria in the Guaymas Basin

The Guaymas Basin (Gulf of California) is a hydrothermal vent site where thermal alteration of deposited planktonic and terrestrial organic matter forms petroliferous material which supports diverse sulfate-reducing bacteria. We explored the phylogenetic and functional diversity of the sulfate-reducing bacteria by characterizing PCR-amplified dissimilatory sulfite reductase (dsrAB) and 16S rRNA genes from the upper 4 cm of the Guaymas sediment. The dsrAB sequences revealed that there was a major clade closely related to the acetate-oxidizing delta-proteobacterial genus Desulfobacter and a clade of novel, deeply branching dsr sequences related to environmental dsr sequences from marine sediments in Aarhus Bay and Kysing Fjord (Denmark). Other dsr clones were affiliated with gram-positive thermophilic sulfate reducers (genus Desulfotomaculum) and the delta-proteobacterial species Desulforhabdus amnigena and Thermodesulforhabdus norvegica. Phylogenetic analysis of 16S rRNAs from the same environmental samples resulted in identification of four clones affiliated with Desulfobacterium niacini, a member of the acetate-oxidizing, nutritionally versatile genus Desulfobacterium, and one clone related to Desulfobacula toluolica and Desulfotignum balticum. Other bacterial 16S rRNA bacterial phylotypes were represented by non-sulfate reducers and uncultured lineages with unknown physiology, like OP9, OP8, as well as a group with no clear affiliation. In summary, analyses of both 16S rRNA and dsrAB clone libraries resulted in identification of members of the Desulfobacteriales in the Guaymas sediments. In addition, the dsrAB sequencing approach revealed a novel group of sulfate-reducing prokaryotes that could not be identified by 16S rRNA sequencing.     

Biochemical and Immunological Study of Cell Envelope Proteins in Sulfate-Reducing Bacteria

The envelope proteins of 5 strains of the genus Desulfotomaculum and 12 strains of the genus Desulfovibrio were studied by sodium dodecyl sulfate-polyacrylamide gel electrophoresis and immunoblotting. The Desulfovibrio strains exhibited a typical gram-negative cell envelope, whereas the cell envelope of Desulfotomaculum strains appeared to be gram-positive. A close relationship between strains of Desulfotomaculum nigrificans was observed. A comparison between different species of Desulfotomaculum revealed some degree of similarity between Desulfotomaculum nigrificans and Desulfotomaculum ruminis, whereas Desulfotomaculum orientis seemed unique. The strains of Desulfovibrio salexigens were quite different from the strains of the other species of Desulfovibrio. In two of the strains of Desulfovibrio desulfuricans, a species-specific antigen was observed. The strains of Desulfovibrio vulgaris, Desulfovibrio africanus, and Desulfovibrio gigas and one strain of Desulfovibrio desulfuricans exhibited a similar outer membrane protein profile and also showed very similar antigenic reactions.     

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.     

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.     

砂岩型铀矿床硫酸盐还原菌与铀地球化学分布关系研究

利用生物学方法对十红滩砂岩型铀矿床各亚带硫酸盐还原菌分布特征和各亚带铀含量与硫酸盐还原菌之间关系进行了分析探讨.结果表明:硫酸盐还原菌在矿石带种类、数量较多,硫酸盐还原菌这种分布特征与铀的地球化学分布呈相关性,这为砂岩型铀矿中铀的地球化学分布研究提供生物学检测手段.     

Lack of DNA Homology between the Legume GLYCINE MAX and Its Symbiotic Rhizobium Bacteria

Any common genes of Glycine max and its symbiotic rhizobium bacteria 61A76 represent less than 0.6% of the bacterial genome. Thus, if any sizable exchange of DNA between host and symbiote occurs it must result in unstable DNA association which is lost with subsequent generations.     

Growth and Activities of Sulfate-Reducing and Methanogenic Bacteria in Human Oral Cavity

Viable counts and activities of sulfate-reducing bacteria (SRB) and methanogenic bacteria were determined in the oral cavities of eight volunteers. Of these, seven harbored viable SRB populations, and six harbored viable methanogenic bacterial populations. Two volunteers classified as type III periodontal patients had both SRB and methanogenic bacteria. Six separate sites were sampled: posterior tongue, anterior tongue, mid-buccal mucosa, vestibular mucosa, supragingival plaque, and subgingival plaque. The SRB was found in all areas in one volunteer, and it was mostly present in posterior tongue, anterior tongue, supragingival, and subgingival plaques in many volunteers. The methanogenic bacteria were mostly found in supragingival and subgingival plaques. The activities of sulfate reduction and methane production were determined in randomly selected isolates. Received: 27 July 2002 / Accepted: 27 August 2002     

Electron Donors Utilized by Sulfate-Reducing Bacteria in Eutrophic Lake Sediments

Mineralization rates of ¹⁴C-labeled substrates were determined in the presence and absence of Na₂MoO₄, an inhibitor of sulfate reduction, in the profundal sediments of a shallow eutrophic lake. Sulfate reduction was inhibited by Na₂MoO₄ at all concentrations tested (0.2 to 200 mM), whereas methane production was inhibited at Na₂MoO₄ concentrations greater than 20 mM. Initial mineralization rates of glucose were unaffected by Na₂MoO₄; however, Na₂MoO₄ decreased the mineralization rates of lactate (58%), propionate (52%), an amino acid mixture (85%), and acetate (14%). These decreases in the rates of mineralization were attributed to inhibition of sulfate reduction. Hydrogen stimulated the reduction of ³⁵SO₄²⁻ 2.5- to 2.8-fold, demonstrating potential hydrogen oxidation by sulfate-reducing bacteria. These results indicate that sulfate reducers utilize an array of substrates as electron donors and are of potential significance to the in situ mineralization of lactate, propionate, and free amino acids in these sediments.     

Improved Most-Probable-Number Method To Detect Sulfate-Reducing Bacteria with Natural Media and a Radiotracer

A greatly improved most-probable-number (MPN) method for selective enumeration of sulfate-reducing bacteria (SRB) is described. The method is based on the use of natural media and radiolabeled sulfate (³⁵SO₄²⁻). The natural media used consisted of anaerobically prepared sterilized sludge or sediment slurries obtained from sampling sites. The densities of SRB in sediment samples from Kysing Fjord (Denmark) and activated sludge were determined by using a normal MPN (N-MPN) method with synthetic cultivation media and a tracer MPN (T-MPN) method with natural media. The T-MPN method with natural media always yielded significantly higher (100- to 1,000-fold-higher) MPN values than the N-MPN method with synthetic media. The recovery of SRB from environmental samples was investigated by simultaneously measuring sulfate reduction rates (by a ³⁵S-radiotracer method) and bacterial counts by using the T-MPN and N-MPN methods, respectively. When bacterial numbers estimated by the T-MPN method with natural media were used, specific sulfate reduction rates (qSO₄²⁻) of 10⁻¹⁴ to 10⁻¹³ mol of SO₄²⁻ cell⁻¹ day⁻¹ were calculated, which is within the range of qSO₄²⁻ values previously reported for pure cultures of SRB (10⁻¹⁵ to 10⁻¹⁴ mol of SO₄²⁻ cell⁻¹ day⁻¹). qSO₄²⁻ values calculated from N-MPN values obtained with synthetic media were several orders of magnitude higher (2 × 10⁻¹⁰ to 7 × 10⁻¹⁰ mol of SO₄²⁻ cell⁻¹ day⁻¹), showing that viable counts of SRB were seriously underestimated when standard enumeration media were used. Our results demonstrate that the use of natural media results in significant improvements in estimates of the true numbers of SRB in environmental samples.