Reverse dissimilatory sulfite reductase as phylogenetic marker for a subgroup of sulfur-oxidizing prokaryotes

Sulfur-oxidizing prokaryotes (SOP) catalyse a central step in the global S-cycle and are of major functional importance for a variety of natural and engineered systems, but our knowledge on their actual diversity and environmental distribution patterns is still rather limited. In this study we developed a specific PCR assay for the detection of dsrAB that encode the reversely operating sirohaem dissimilatory sulfite reductase (rDSR) and are present in many but not all published genomes of SOP. The PCR assay was used to screen 42 strains of SOP (most without published genome sequence) representing the recognized diversity of this guild. For 13 of these strains dsrAB was detected and the respective PCR product was sequenced. Interestingly, most dsrAB -encoding SOP are capable of forming sulfur storage compounds. Phylogenetic analysis demonstrated largely congruent rDSR and 16S rRNA consensus tree topologies, indicating that lateral transfer events did not play an important role in the evolutionary history of known rDSR. Thus, this enzyme represents a suitable phylogenetic marker for diversity analyses of sulfur storage compound-exploiting SOP in the environment. The potential of this new functional gene approach was demonstrated by comparative sequence analyses of all dsrAB present in published metagenomes and by applying it for a SOP census in selected marine worms and an alkaline lake sediment.     

Phylogeography of sulfate-reducing bacteria among disturbed sediments, disclosed by analysis of the dissimilatory sulfite reductase genes (dsrAB)

Sediment samples were collected worldwide from 16 locations on four continents (in New York, California, New Jersey, Virginia, Puerto Rico, Venezuela, Italy, Latvia, and South Korea) to assess the extent of the diversity and the distribution patterns of sulfate-reducing bacteria (SRB) in contaminated sediments. The SRB communities were examined by terminal restriction fragment (TRF) length polymorphism (TRFLP) analysis of the dissimilatory sulfite reductase genes (dsrAB) with NdeII digests. The fingerprints of dsrAB genes contained a total of 369 fluorescent TRFs, of which <20% were present in the GenBank database. The global sulfidogenic communities appeared to be significantly different among the anthropogenically impacted (petroleum-contaminated) sites, but nearly all were less diverse than pristine habitats, such as mangroves. A global SRB indicator species of petroleum pollution was not identified. However, several dsrAB gene sequences corresponding to hydrocarbon-degrading isolates or consortium members were detected in geographically widely separated polluted sites. Finally, a cluster analysis of the TRFLP fingerprints indicated that many SRB microbial communities were most similar on the basis of close geographic proximity (tens of kilometers). Yet, on larger scales (hundreds to thousands of kilometers) SRB communities could cluster with geographically widely separated sites and not necessarily with the site with the closest proximity. These data demonstrate that SRB populations do not adhere to a biogeographic distribution pattern similar to that of larger eukaryotic organisms, with the greatest species diversity radiating from the Indo-Pacific region. Rather, a patchy SRB distribution is encountered, implying an initially uniform SRB community that has differentiated over time.     

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

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

Diversity of sulfate-reducing bacteria in oxic and anoxic regions of a microbial mat characterized by comparative analysis of dissimilatory sulfite reductase genes.

Sequence analysis of genes encoding dissimilatory sulfite reductase (DSR) was used to identify sulfate-reducing bacteria in a hypersaline microbial mat and to evaluate their distribution in relation to levels of oxygen. The most highly diverse DSR sequences, most related to those of the Desulfonema-like organisms within the delta-proteobacteria, were recovered from oxic regions of the mat. This observation extends those of previous studies by us and others associating Desulfonema-like organisms with oxic habitats.     

Evidence of the activity of dissimilatory sulfate-reducing prokaryotes in nonsulfidogenic tropical mobile muds

In spite of the nonsulfidic conditions and abundant reactive iron(III) commonly found in mobile tropical deltaic muds, genes encoding dissimilatory sulfite reductase (dsr) were successfully amplified from the upper approximately 1 m of coastal deposits sampled along French Guiana and in the Gulf of Papua. The dsr sequences retrieved were highly diverse, were generally represented in both study regions and fell into six large phylogenetic groupings: Deltaproteobacteria, Thermodesulfovibrio groups, Firmicutes and three groups without known cultured representatives. The spatial and temporal distribution of dsr sequences strongly supports the contention that the sulfate-reducing prokaryote communities in mobile mud environments are cosmopolitan and stable over a period of years. The decrease in the (35)SO(4) (2-) tracer demonstrates that, despite abundant reactive sedimentary iron(III) ( approximately 350-400 mumol g(-1)), the sulfate-reducing prokaryotes present are active, with the highest levels of sulfide being generated in the upper zones of the cores (0-30 cm). Both the time course of the (35)S-sulfide tracer activity and the lack of reduced sulfur in sediments demonstrate virtually complete anaerobic loss of solid phase sulfides. We propose a pathway of organic matter oxidation involving at least 5-25% of the remineralized carbon, wherein sulfide produced by sulfate-reducing prokaryotes is cyclically oxidized biotically or abiotically by metal oxides.     

Homology modeling of dissimilatory APS reductases (AprBA) of sulfur-oxidizing and sulfate-reducing prokaryotes

Background

The dissimilatory adenosine-5′-phosphosulfate (APS) reductase (cofactors flavin adenine dinucleotide, FAD, and two [4Fe-4S] centers) catalyzes the transformation of APS to sulfite and AMP in sulfate-reducing prokaryotes (SRP); in sulfur-oxidizing bacteria (SOB) it has been suggested to operate in the reverse direction. Recently, the three-dimensional structure of the Archaeoglobus fulgidus enzyme has been determined in different catalytically relevant states providing insights into its reaction cycle.

Methodology/Principal Findings

Full-length AprBA sequences from 20 phylogenetically distinct SRP and SOB species were used for homology modeling. In general, the average accuracy of the calculated models was sufficiently good to allow a structural and functional comparison between the beta- and alpha-subunit structures (78.8–99.3% and 89.5–96.8% of the AprB and AprA main chain atoms, respectively, had root mean square deviations below 1 Å with respect to the template structures). Besides their overall conformity, the SRP- and SOB-derived models revealed the existence of individual adaptations at the electron-transferring AprB protein surface presumably resulting from docking to different electron donor/acceptor proteins. These structural alterations correlated with the protein phylogeny (three major phylogenetic lineages: (1) SRP including LGT-affected Archaeoglobi and SOB of Apr lineage II, (2) crenarchaeal SRP Caldivirga and Pyrobaculum, and (3) SOB of the distinct Apr lineage I) and the presence of potential APS reductase-interacting redox complexes. The almost identical protein matrices surrounding both [4Fe-4S] clusters, the FAD cofactor, the active site channel and center within the AprB/A models of SRP and SOB point to a highly similar catalytic process of APS reduction/sulfite oxidation independent of the metabolism type the APS reductase is involved in and the species it has been originated from.

Conclusions

Based on the comparative models, there are no significant structural differences between dissimilatory APS reductases from SRP and SOB; this might be indicative for a similar catalytic process of APS reduction/sulfite oxidation.     

Structure of the dissimilatory sulfite reductase from the hyperthermophilic archaeon Archaeoglobus fulgidus

Conservation of energy based on the reduction of sulfate is of fundamental importance for the biogeochemical sulfur cycle. A key enzyme of this ancient anaerobic process is the dissimilatory sulfite reductase (dSir), which catalyzes the six-electron reduction of sulfite to hydrogen sulfide under participation of a unique magnetically coupled siroheme-[4Fe-4S] center. We determined the crystal structure of the enzyme from the sulfate-reducing archaeon Archaeoglobus fulgidus at 2-Å resolution and compared it with that of the phylogenetically related assimilatory Sir (aSir). dSir is organized as a heterotetrameric (αβ)₂ complex composed of two catalytically independent αβ heterodimers. In contrast, aSir is a monomeric protein built of two fused modules that are structurally related to subunits α and β except for a ferredoxin domain inserted only into the subunits of dSir. The [4Fe-4S] cluster of this ferredoxin domain is considered as the terminal redox site of the electron transfer pathway to the siroheme-[4Fe-4S] center in dSir. While aSir binds one siroheme-[4Fe-4S] center, dSir harbors two of them within each αβ heterodimer. Surprisingly, only one siroheme-[4Fe-4S] center in each αβ heterodimer is catalytically active, whereas access to the second one is blocked by a tryptophan residue. The spatial proximity of the functional and structural siroheme-[4Fe-4S] centers suggests that the catalytic activity at one active site was optimized during evolution at the expense of the enzymatic competence of the other. The sulfite binding mode and presumably the mechanism of sulfite reduction appear to be largely conserved between dSir and aSir. In addition, a scenario for the evolution of Sirs is proposed.     

Metabolism of sulfate-reducing prokaryotes

Dissimilatory sulfate reduction is carried out by a heterogeneous group of bacteria and archaea that occur in environments with temperatures up to 105 °C. As a group together they have the capacity to metabolize a wide variety of compounds ranging from hydrogen via typical organic fermentation products to hexadecane, toluene, and several types of substituted aromatics. Without exception all sulfate reducers activate sulfate to APS; the natural electron donor(s) for the ensuing APS reductase reaction is not known. The same is true for the reduction of the product bisulfite; in addition there is still some uncertainty as to whether the pathway to sulfide is a direct six-electron reduction of bisulfite or whether it involves trithionate and thiosulfate as intermediates. The study of the degradation pathways of organic substrates by sulfate-reducing prokaryotes has led to the discovery of novel non-cyclic pathways for the oxidation of the acetyl moiety of acetyl-CoA to CO₂. The most detailed knowledge is available on the metabolism ofDesulfovibrio strains, both on the pathways and enzymes involved in substrate degradation and on electron transfer components and terminal reductases. Problems encountered in elucidating the flow of reducing equivalents and energy transduction are the cytoplasmic localization of the terminal reductases and uncertainties about the electron donors for the reactions catalyzed by these enzymes. New developments in the study of the metabolism of sulfate-reducing bacteria and archaea are reviewed.     

Characterization of a new type of dissimilatory sulfite reductase present in Thermodesulfobacterium commune

A new type of dissimilatory bisulfite reductase, desulfofuscidin, was isolated from the nonsporeforming thermophilic sulfate-reducing microorganism Thermodesulfobacterium commune. The molecular weight of the enzyme was estimated at 167,000 by sedimentation equilibrium, and the protein was pure by both disc electrophoresis and ultracentrifugation. The bisulfite reductase was a tetramer and had two types of subunits with an α₂β₂ structure and an individual molecular weight of 47,000. The enzyme exhibited absorption maxima at 576, 389, and 279 nm, with a weak band at 693 nm. Upon the addition of dithionite, the absorption maxima at 576 and 693 nm were weakened, and a new band appeared at 605 nm. The protein reacted with CO in the presence of dithionite to give a complex with absorption peaks at 593, 548, and 395 nm. The extinction coefficients of the purified enzyme at 576, 389, and 279 nm were 89,000, 310,000, and 663,000 M⁻¹ cm⁻¹, respectively. Siroheme was detected as the prosthetic group. The protein contains 20 to 21 nonheme iron atoms and 16 to 17 acid-labile sulfur groups per molecule. The data suggest the presence of four sirohemes and probably four (4Fe-4S) centers per molecule by comparison with desulfoviridin, the dissimilatory sulfite reductase from Desulfovibrio species. The protein contains 36 cysteine residues and is high in acidic and aromatic amino acids. The N-terminal amino acids of the α and β subunits were threonine and serine, respectively. With reduced methyl viologen as electron donor, the major product of sulfite reduction was trithionate, and the pH optimum for activity was 6.0. The enzyme was stable to 70°C and denatured rapidly above this temperature. The dependence of T. commune bisulfite reductase activity on temperature was linear between 35 and 65°C, and the Q₁₀ values observed were above 3. The presence of this new type of dissimilatory bisulfite reductase in T. commune is discussed in terms of taxonomic significance.     

Purification and characterization of an inducible dissimilatory type sulfite reductase from Clostridium pasteurianum

An inducible sulfite reductase was purified from Clostridium pasteurianum. The pH optimum of the enzyme is 7.5 in phosphate buffer. The molecular weight of the reductase was determined to be 83,600 from sodium dodecyl sulfate gel electrophoresis with a proposed molecular structure: ₂₂. Its absorption spectrum showed a maximum at 275 nm, a broad shoulder at 370 nm and a very small absorption maximum at 585 nm. No siroheme chromophore was isolated from this reductase. The enzyme could reduced the following substrates in preferential order: NH₂OH> SeO ₃ ^2- >NO ₂ ^2- at rates 50% or less of its preferred substrate SO ₃ ^2- . The proposed dissimilatory intermediates, S₃O ₆ ^2- or S₂O ₃ ^2- , were not utilized by this reductase while KCN inhibited its activity. Varying the substrate concentration [SO ₃ ^2- ] from 1 to 2.5 mol affected the stoichiometry of the enzyme reaction by alteration of the ratio of H₂ uptake to S^2- formed from 2.5:1 to 3.1:1. The inducible sulfite reductase was found to be linked to ferredoxin which could be completely replaced by methyl viologen or partially by benzyl viologen. Some of the above-mentioned enzyme properties and physiological considerations indicated that it was a dissimilatory type sulfite reductase.Abbreviations SDS sodium dodecyl sulfate - BSA bovine serum albumin - LDH Lactate dehydrogenase     

Isolation of saccharolytic dissimilatory sulfate-reducing bacteria

Abstract Four unidentified saccharolytic dissimilatory sulfate-reducing strains were isolated from an anaerobic digester. Cells were Gram-negative, motile, nonsporulating rods which differ markedly from known sulfate reducers especially with respect to carbon source utilisation and sulfur sources which can be reduced. The strains were capable of metabolising at least 26 out of 50 carbohydrates tested. Carbohydrates were, in the absence of exogenous sulfate, fermented to acetate, ethanol, lactate, carbon dioxide and hydrogen. In the presence of excess sulfate carbohydrates were fermented to acetate, ethanol, carbon dioxide, hydrogen and hydrogen sulfide, but lactate was not detected. An oxidized organic or inorganic sulfur source, including elemental sulfur, was not required as a prerequisite for growth on carbohydrates, Lactate was, in the presence of sulfate, converted to acetate, ethanol, carbon dioxide, hydrogen and hydrogen sulfide. In the absence of sulfate no lactate was utilised and no growth was observed.     

Microorganisms with novel dissimilatory (bi)sulfite reductase genes are widespread and part of the core microbiota in low-sulfate peatlands

Peatlands of the Lehstenbach catchment (Germany) house as-yet-unidentified microorganisms with phylogenetically novel variants of the dissimilatory (bi)sulfite reductase genes dsrAB. These genes are characteristic of microorganisms that reduce sulfate, sulfite, or some organosulfonates for energy conservation but can also be present in anaerobic syntrophs. However, nothing is currently known regarding the abundance, community dynamics, and biogeography of these dsrAB-carrying microorganisms in peatlands. To tackle these issues, soils from a Lehstenbach catchment site (Schlöppnerbrunnen II fen) from different depths were sampled at three time points over a 6-year period to analyze the diversity and distribution of dsrAB-containing microorganisms by a newly developed functional gene microarray and quantitative PCR assays. Members of novel, uncultivated dsrAB lineages (approximately representing species-level groups) (i) dominated a temporally stable but spatially structured dsrAB community and (ii) represented “core” members (up to 1% to 1.7% relative abundance) of the autochthonous microbial community in this fen. In addition, denaturing gradient gel electrophoresis (DGGE)- and clone library-based comparisons of the dsrAB diversity in soils from a wet meadow, three bogs, and five fens of various geographic locations (distance of ∼1 to 400 km) identified that one Syntrophobacter-related and nine novel dsrAB lineages are widespread in low-sulfate peatlands. Signatures of biogeography in dsrB-based DGGE data were not correlated with geographic distance but could be explained largely by soil pH and wetland type, implying that the distribution of dsrAB-carrying microorganisms in wetlands on the scale of a few hundred kilometers is not limited by dispersal but determined by local environmental conditions.Peatlands contain 15% to 30% of the global soil carbon (13, 79) and represent a net carbon sink that has contributed to global cooling in the past 8,000 to 11,000 years (21). While peatlands are generally resilient to external perturbation, it is predicted that long-term global changes such as warming, decreased precipitation, and increased atmospheric deposition of reactive nitrogen and sulfur compounds will transform peatlands into new ecosystem types, accompanied by unforeseeable changes in the carbon balance (17). The carbon loss from peatlands is mediated largely by the anaerobic microbial decomposition of organic matter to the greenhouse gases carbon dioxide and methane (36), and it is estimated that 10 to 20% of the globally emitted methane is derived from peatlands (30, 87). Primary and secondary fermentation and subsequent methanogenesis are considered to be the main carbon degradation processes because of the absence or limited availability of alternative electron acceptors. However, other microbial processes, such as denitrification and dissimilatory iron and sulfate reduction, can occur together with methanogenesis in the same peat soil fraction and contribute considerably to anaerobic carbon mineralization (4, 5, 43, 44). Fluctuations in environmental conditions on short- and long-term scales govern trophic interdependencies among microorganisms. Transitions between synergistic (e.g., the syntrophic interspecies transfer of hydrogen/formate) and antagonistic (e.g., competition for the same substrates) microbial interactions determine the extent of carbon flow diversion away from methanogenesis. A prime example is the suppression of microorganisms catalyzing methanogenic carbon degradation by sulfate-reducing microorganisms (SRM) that are energetically favored in the competition for substrates such as acetate, alcohols, and hydrogen (22, 81, 82). While sulfate concentrations are generally low in peatlands (10 to 300 μM), ongoing sulfate reduction proceeds at rates (2.5 to 340 nmol cm⁻³ day⁻¹) that are comparable to rates in sulfate-rich environments such as marine sediments (5, 40, 41). It was previously proposed that such high sulfate reduction rates are fueled by an anoxic recycling of reduced sulfur compounds via the so-called “thiosulfate shunt” (5). The alternative replenishment of the sulfate pool by the reoxidation of reduced sulfur species in the presence of oxygen is dependent on the vegetation type and alternating periods of precipitation and drought (14, 18, 64, 68, 86). In addition, increasing global atmospheric sulfur pollution and acid precipitation contribute to terrestrial sulfate pools and are predicted to repress methane emissions from peatlands by up to 15% within the first third of this century (22).Given the significance of dissimilatory sulfate reduction in peatlands, it is surprising that most information about the identity of microorganisms catalyzing this process in peatlands is derived from studies of a single model fen system (Schlöppnerbrunnen) located in the forested Lehstenbach catchment (Bavaria, Germany). Different redox processes such as fermentation (25), methanogenesis (29), denitrification (63), Fe(III) reduction (69), and sulfate reduction (2, 51) are present and have been studied at this site (4). The atmospheric deposition of sulfur originating from the combustion of soft coal in Eastern Europe until the 1990s led to the accumulation of sulfur species in the soils of this catchment. Although air pollution affecting this site has decreased in recent years (39), historically deposited sulfate stored in upland soils can desorb and is then transported via groundwater flow into the fen, where it drives dissimilatory sulfate reduction (1). DNA stable isotope probing using in situ concentrations of typical ¹³C-labeled degradation intermediates (mixture of lactate, acetate, formate, and propionate) has shown that a low-abundance Desulfosporosinus species, representing on average only 0.006% of the total bacterial and archaeal 16S rRNA genes, has the potential to be responsible for a substantial part of the sulfate reduction in the studied fen. However, a large fraction of the sulfate reduction observed in situ still remains unexplained (67). Other microorganisms that are potentially involved in sulfate reduction were previously detected in this fen by using 16S rRNA gene- and dsrAB-based diversity analyses. Few of these dsrAB sequences were affiliated with the previously described SRM genera Desulfomonile and Syntrophobacter, but most of the retrieved dsrAB sequences may derive from new taxa, as they represent novel lineages without cultivated representatives (51, 67, 73). Microorganisms that respire sulfite or sulfate anaerobically depend on the dsrAB-encoded key enzyme dissimilatory (bi)sulfite reductase for energy conservation, and thus, these genes have been widely used as markers for PCR-based molecular diversity studies of this guild (16, 38, 46, 84). However, some organisms that are phylogenetically related to SRM but that have seemingly lost the ability for sulfite/sulfate reduction can also harbor dsrAB. The dsrAB sequences of these organosulfonate reducers (45) or syntrophs (32) can be amplified by the commonly used DSR1F-DSR4R PCR primer mix (50). DNA stable isotope probing experiments targeting dsrAB in incubations with a mixture of ¹³C-labeled lactate, acetate, formate, and propionate could therefore not unambiguously link members of the novel dsrAB lineages to sulfate reduction in the Schlöppnerbrunnen peatland (67). Besides their unknown identity and ecophysiological function, additional important questions regarding the ecology of these enigmatic dsrAB-containing microorganisms remain unanswered: what is their actual abundance in peatlands, are they a stable part of the microbial peatland community or do they occur only sporadically, and are they endemic to the Schlöppnerbrunnen fen site or more widely distributed in different types of wetlands? Using a set of molecular ecology tools, we address these questions in this study and demonstrate that some dsrAB-containing microorganisms are widespread in peatlands and can thrive in these systems in considerable numbers.     

X-ray structure of the gamma-subunit of a dissimilatory sulfite reductase: fixed and flexible C-terminal arms

The X-ray structure of the gamma-subunit of the dissimilatory sulfite reductase (DsrC) from Archaeoglobus fulgidus was determined at 1.12 and 2.1A resolution, in the two crystal forms named DsrC(nat) and DsrC(ox) the latter being cocrystallized with the oxidizing agent tert-butyl hydroperoxide. The fold corresponds to that of the homologous protein from Pyrobaculum aerophilum but is significantly more compact. The most interesting, highly conserved C-terminal arm adopts a well-defined conformation in A. fulgidus DsrC in contrast to the completely disordered conformation in P. aerophilum DsrC. The functional relevance of both conformations and of a potentially redox-active disulfide bond between the strictly invariant Cys103 and Cys114 are discussed.     

Oligonucleotide microarray for 16S rRNA gene-based detection of all recognized lineages of sulfate-reducing prokaryotes in the environment

For cultivation-independent detection of sulfate-reducing prokaryotes (SRPs) an oligonucleotide microarray consisting of 132 16S rRNA gene-targeted oligonucleotide probes (18-mers) having hierarchical and parallel (identical) specificity for the detection of all known lineages of sulfate-reducing prokaryotes (SRP-PhyloChip) was designed and subsequently evaluated with 41 suitable pure cultures of SRPs. The applicability of SRP-PhyloChip for diversity screening of SRPs in environmental and clinical samples was tested by using samples from periodontal tooth pockets and from the chemocline of a hypersaline cyanobacterial mat from Solar Lake (Sinai, Egypt). Consistent with previous studies, SRP-PhyloChip indicated the occurrence of Desulfomicrobium spp. in the tooth pockets and the presence of Desulfonema- and Desulfomonile-like SRPs (together with other SRPs) in the chemocline of the mat. The SRP-PhyloChip results were confirmed by several DNA microarray-independent techniques, including specific PCR amplification, cloning, and sequencing of SRP 16S rRNA genes and the genes encoding the dissimilatory (bi)sulfite reductase (dsrAB).     

Biogeography of sulfate-reducing prokaryotes in river floodplains

In this study, a large-scale field survey was conducted to describe the biogeography of sulfate-reducing prokaryotes (SRPs) in river floodplains. Fingerprints obtained with three methods, i.e. 16S rRNA gene-based oligonucleotide microarray, dsrB-based denaturing gradient gel electrophoresis (DGGE) and polar lipid-derived fatty acid (PLFA) analyses, were used as a proxy to describe the SRPs community diversity. Each set of profiles was subjected to a combined multivariate/correlation analysis in order to compare SRP community profiles and to highlight the environmental variables influencing the SRPs distribution along environmental gradients. Floodplain soils harbored distinct SRP communities displaying biogeographic patterns. Nearly all profiles from the tidal sites consistently separated from the nontidal sites, independently from the screening method and the multivariate statistics used. The distribution of the microarray/DGGE/PLFA-based fingerprints in the principal component plots could be correlated to eight soil variables, i.e. soil organic matter, total nitrogen, total phosphorous and total potassium, and extractable ammonium, nitrate, phosphate and sulfate, as well as seven pore water variables, i.e. phosphate, sulfate, sulfide, chloride, sodium, potassium and magnesium ions. Indication of a salinity- and plant nutrient-dependent distribution of SRPs related to Desulfosarcina, Desulfomonile and Desulfobacter was suggested by microarray, DGGE and PLFA analyses.     

Mechanism of dissimilatory sulfite reduction by Desulfovibrio desulfuricans: purification of a membrane-bound sulfite reductase and coupling iwth cytochrome c 3 and hydrogenase

The localization of the dissimilatory sulfite reductase in Desulfovibrio desulfuricans strain Essex 6 was investigated. After treatment of the cells with lysozyme, 90% of the sulfite reductase activity was found in the membrane fraction, compared to 30% after cell rupture with the French press. Sulfite reductase was purified from the membrane (mSiR) and the soluble (sSiR) fractiion. On SDS-PAGE, both mSiR and sSiR exhibited three bands at 50, 45 and 11 kDa, respectively. From their UV/VIS properties (distinct absorption maxima at 391, 410, 583, 630 nm, enzymes as isolated) and the characteristic red fluorescence in alkaline solution, mSiR and sSiR were identified as desulfoviridin. Sulfite reductase (HSO₃ ^-H₂S) activity was reconstituted by coupling of mSiR to hydrogenase and cytochrome c ₃ from D. desulfuricans. The specific activity of mSiR was 103 nmol H₂ min^-1 mg^-1, and sulfide was the major product (72% of theoretical yield). No coupling was found with sSiR under these conditions. Furthermore, carbon monoxide was used to diferentiate between the membrane-bound and the soluble sulfite reductase. In a colorimetric assay, with photochemically reduced methyl viologen as redox mediator, CO stimulated the activity of sSiR significantly. CO had no effect in the case of mSiR. These studies documented that, as isolated, both forms of sulfite reductase behaved differently in vitro. Clearly, in D. desulfuricans, the six electron conversion HSO₃ ^-H₂S was achieved by a membranebound desulfoviridin without the assistance of artificial redox mediators, such as methyl viologen.Abbreviations SiR sulfite reductase - mSiR sulfite reductase purified from membranes - sSiR sulfite reductase purified from the soluble fraction Enzymes Sulfite reductase, EC 1.8.99.1 Cytochrome c ₃ hydrogenase, EC 1.12.2.1     

Purification, crystallization and preliminary crystallographic analysis of a dissimilatory DsrAB sulfite reductase in complex with DsrC

Dissimilatory sulfite reductase (dSiR, DsrAB) is a key protein in dissimilatory sulfur metabolism, one of the earliest types of energy metabolism to be traced on earth. dSirs are large oligomeric proteins around 200kDa forming an alpha(2)beta(2) arrangement and including a unique siroheme-[4Fe-4S] coupled cofactor. Here, we report the purification, crystallization and preliminary X-ray diffraction analysis of dSir isolated from Desulfovibrio vulgaris Hildenborough, also known as desulfoviridin. In this enzyme the DsrAB protein is associated with DsrC, a protein of unknown function that is believed to play an important role in the sulfite reduction. Crystals belong to the monoclinic space group P2(1) with unit-cell parameters a=122.7, b=119.4 and c=146.7A and beta =110.0 degrees , and diffract X-rays to 2.8A on a synchrotron source.     

Recent events dominate interdomain lateral gene transfers between prokaryotes and eukaryotes and,with the exception of endosymbiotic gene transfers,few ancient transfer events persist

While there is compelling evidence for the impact of endosymbiotic gene transfer (EGT; transfer from either mitochondrion or chloroplast to the nucleus) on genome evolution in eukaryotes, the role of interdomain transfer from bacteria and/or archaea (i.e. prokaryotes) is less clear. Lateral gene transfers (LGTs) have been argued to be potential sources of phylogenetic information, particularly for reconstructing deep nodes that are difficult to recover with traditional phylogenetic methods. We sought to identify interdomain LGTs by using a phylogenomic pipeline that generated 13 465 single gene trees and included up to 487 eukaryotes, 303 bacteria and 118 archaea. Our goals include searching for LGTs that unite major eukaryotic clades, and describing the relative contributions of LGT and EGT across the eukaryotic tree of life. Given the difficulties in interpreting single gene trees that aim to capture the approximately 1.8 billion years of eukaryotic evolution, we focus on presence–absence data to identify interdomain transfer events. Specifically, we identify 1138 genes found only in prokaryotes and representatives of three or fewer major clades of eukaryotes (e.g. Amoebozoa, Archaeplastida, Excavata, Opisthokonta, SAR and orphan lineages). The majority of these genes have phylogenetic patterns that are consistent with recent interdomain LGTs and, with the notable exception of EGTs involving photosynthetic eukaryotes, we detect few ancient interdomain LGTs. These analyses suggest that LGTs have probably occurred throughout the history of eukaryotes, but that ancient events are not maintained unless they are associated with endosymbiotic gene transfer among photosynthetic lineages.     

Diversity of sulfur isotope fractionations by sulfate-reducing prokaryotes

Batch culture experiments were performed with 32 different sulfate-reducing prokaryotes to explore the diversity in sulfur isotope fractionation during dissimilatory sulfate reduction by pure cultures. The selected strains reflect the phylogenetic and physiologic diversity of presently known sulfate reducers and cover a broad range of natural marine and freshwater habitats. Experimental conditions were designed to achieve optimum growth conditions with respect to electron donors, salinity, temperature, and pH. Under these optimized conditions, experimental fractionation factors ranged from 2.0 to 42.0 per thousand. Salinity, incubation temperature, pH, and phylogeny had no systematic effect on the sulfur isotope fractionation. There was no correlation between isotope fractionation and sulfate reduction rate. The type of dissimilatory bisulfite reductase also had no effect on fractionation. Sulfate reducers that oxidized the carbon source completely to CO2 showed greater fractionations than sulfate reducers that released acetate as the final product of carbon oxidation. Different metabolic pathways and variable regulation of sulfate transport across the cell membrane all potentially affect isotope fractionation. Previous models that explained fractionation only in terms of sulfate reduction rates appear to be oversimplified. The species-specific physiology of each sulfate reducer thus needs to be taken into account to understand the regulation of sulfur isotope fractionation during dissimilatory sulfate reduction.     

The third subunit of desulfoviridin-type dissimilatory sulfite reductases.

In addition to the 50-kDa (alpha) and 40-kDa (beta) subunits, an 11-kDa polypeptide has been discovered in highly purified Desulfovibrio vulgaris (Hildenborough) dissimilatory sulfite reductase. This is in contrast with the hitherto generally accepted alpha 2 beta 2 tetrameric subunit composition. Purification, high-ionic-strength gel-filtration, native electrophoresis and isoelectric focussing do not result in dissociation of the 11-kDa polypeptide from the complex. Densitometric scanning of SDS gels and denaturing gel-filtration indicate a stoichiometric occurrence. A similar 11-kDa polypeptide is present in the desulfoviridin of D. vulgaris oxamicus (Monticello), D. gigas and D. desulfuricans ATCC 27774. We attribute an alpha 2 beta 2 gamma 2 subunit structure to desulfoviridin-type sulfite reductases. N-terminal sequences of the alpha, beta and gamma subunits are reported.