A global perspective on bacterial diversity in the terrestrial deep subsurface.

While recent efforts to catalogue Earth's microbial diversity have focused upon surface and marine habitats, 12-20 % of Earth's biomass is suggested to exist in the terrestrial deep subsurface, compared to ~1.8 % in the deep subseafloor. Metagenomic studies of the terrestrial deep subsurface have yielded a trove of divergent and functionally important microbiomes from a range of localities. However, a wider perspective of microbial diversity and its relationship to environmental conditions within the terrestrial deep subsurface is still required. Our meta-analysis reveals that terrestrial deep subsurface microbiota are dominated by Betaproteobacteria, Gammaproteobacteria and Firmicutes, probably as a function of the diverse metabolic strategies of these taxa. Evidence was also found for a common small consortium of prevalent Betaproteobacteria and Gammaproteobacteria operational taxonomic units across the localities. This implies a core terrestrial deep subsurface community, irrespective of aquifer lithology, depth and other variables, that may play an important role in colonizing and sustaining microbial habitats in the deep terrestrial subsurface. An in silico contamination-aware approach to analysing this dataset underscores the importance of downstream methods for assuring that robust conclusions can be reached from deep subsurface-derived sequencing data. Understanding the global panorama of microbial diversity and ecological dynamics in the deep terrestrial subsurface provides a first step towards understanding the role of microbes in global subsurface element and nutrient cycling.

Membrane-bound oxygen reductases of the anaerobic sulfate-reducing Desulfovibrio vulgaris Hildenborough: roles in oxygen defence and electron link with periplasmic hydrogen oxidation.

Cytoplasmic membranes of the strictly anaerobic sulfate-reducing bacterium Desulfovibrio vulgaris Hildenborough contain two terminal oxygen reductases, a bd quinol oxidase and a cc(b/o)o3 cytochrome oxidase (Cox). Viability assays pointed out that single Δbd, Δcox and double ΔbdΔcox deletion mutant strains were more sensitive to oxygen exposure than the WT strain, showing the involvement of these oxygen reductases in the detoxification of oxygen. The Δcox strain was slightly more sensitive than the Δbd strain, pointing to the importance of the cc(b/o)o3 cytochrome oxidase in oxygen protection. Decreased O2 reduction rates were measured in mutant cells and membranes using lactate, NADH, ubiquinol and menadiol as substrates. The affinity for oxygen measured with the bd quinol oxidase (Km, 300 nM) was higher than that of the cc(b/o)o3 cytochrome oxidase (Km, 620 nM). The total membrane activity of the bd quinol oxidase was higher than that of the cytochrome oxidase activity in line with the higher expression of the bd oxidase genes. In addition, analysis of the ΔbdΔcox mutant strain indicated the presence of at least one O2-scavenging membrane-bound system able to reduce O2 with menaquinol as electron donor with an O2 affinity that was two orders of magnitude lower than that of the bd quinol oxidase. The lower O2 reductase activity in mutant cells with hydrogen as electron donor and the use of specific inhibitors indicated an electron transfer link between periplasmic H2 oxidation and membrane-bound oxygen reduction via the menaquinol pool. This linkage is crucial in defence of the strictly anaerobic bacterium Desulfovibrio against oxygen stress.

Control of microbial sulfide production by limiting sulfate dispersal in a water-injected oil field.

Oil production by water injection often involves the use of makeup water to replace produced oil. Sulfate in makeup water is reduced by sulfate-reducing bacteria to sulfide, a process referred to as souring. In the MHGC field souring was caused by using makeup water with 4mM (384ppm) sulfate. Mixing with sulfate-free produced water gave injection water with 0.8mM sulfate. This was amended with nitrate to limit souring and was then distributed fieldwide. The start-up of an enhanced-oil-recovery pilot caused all sulfate-containing makeup water to be used for dissolution of polymer, which was then injected into a limited region of the field. Produced water from this pilot contained 10% of the injected sulfate concentration as sulfide, but was free of sulfate. Its use as makeup water in the main water plant of the field caused injection water sulfate to drop to zero. This in turn strongly decreased produced sulfide concentrations throughout the field and allowed a decreased injection of nitrate. The decreased injection of sulfate and nitrate caused major changes in the microbial community of produced waters. Limiting sulfate dispersal into a reservoir, which acts as a sulfate-removing biofilter, is thus a powerful method to decrease souring.

Oil sands tailings ponds harbour a small core prokaryotic microbiome and diverse accessory communities.

Oil sands tailings ponds store the waste slurry generated by extracting bitumen from surface-mined oil (tar) sands ores. The ponds support diverse microbial communities involved in element cycling, greenhouse gas production, and hydrocarbon biodegradation that influence pond management and their environmental footprint. Since previous reports indicate that there are similar microbial metabolic functions amongst ponds, analogous microbiomes may be expected but ponds actually harbour distinct communities. Partial 16S rRNA gene pyrotag sequences from 95 samples were obtained from six ponds managed by three operators. From these we discerned a core prokaryotic microbiome, a subset of microbes shared amongst different samples, defined as operational taxonomic units (OTUs) at the lowest taxonomic level identifiable in individual ponds and pooled pond datatsets. Of the ∼1500-2700 OTUs detected per pond, 4-10 OTUs were shared among ≥75% of the samples per pond, but these few OTUs represented 39-54% of the ponds' sequence reads. Only 2-5 OTUs were shared by the majority of samples from all ponds. Thus the prokaryotic communities within these ponds consist of a few core taxa and numerous accessory members that likely afford resiliency and functional redundancy including roles in iron-, nitrogen- and sulfur-cycling, syntrophy, fermentation, and methanogenesis.

Cloning of genes encoding redox proteins of known amino acid sequence from a library of the Desulfovibrio vulgaris (Hildenborough) genome.

A library of 900 recombinant phages has been constructed for the genome of Desulfovibrio vulgaris Hildenborough (1.7 x 10(6) bp) by cloning size-fractionated Sau3A fragments (15-20 kb) into the replacement vector lambda-2001. When a hydrogenase gene probe, a 4.7-kb SalI-EcoRI fragment of known nucleotide sequence, was used to screen the plaque lifted library, 23 positive clones were found, which together span 31 kb of D. vulgaris DNA. To facilitate the cloning of genes with oligodeoxynucleotides as probes, DNA was purified for all clones in the library and spotted on a 16 x 16-cm grid of nitrocellulose. This grid was incubated sequentially to identify lambda clones containing the gene for redox proteins of known amino acid sequence: cytochrome c3 (one 18-mer----four clones), flavodoxin (one 17-mer and one 26-mer----one clone) and rubredoxin (one 44-mer----21 clones). The four cyc-positive clones are also recognized by the rubredoxin oligodeoxynucleotide probe. Restriction mapping defines a 35-kb region of the D. vulgaris chromosome in which the rub and cyc loci are separated by 17.5 kb. The nucleotide sequence of the rubredoxin gene was determined and the deduced amino acid sequence found to agree with that determined in Bruschi [Biochim. Biophys. Acta 434 (1976) 4-17] with the exception of Thr-21 which is found to be encoded by GAC, an Asp codon. A plausible ribosome-binding site precedes the N-terminal initiator methionine residue. Rubredoxin does not have an N-terminal signal sequence which is in agreement with the cytoplasmic location of this redox protein.

Molecular biology of c-type cytochromes from Desulfovibrio vulgaris Hildenborough.

Sulfate reducing bacteria of the genus Desulfovibrio harbor a wide variety of redox proteins. Three different c-type cytochromes, cytochrome c-553, cytochrome c3 and the high molecular mass cytochrome have been isolated from these bacteria. The high molecular mass cytochrome is part of an operon that encodes a transmembrane protein complex that mediates electron transfer across the cytoplasmic membrane. The physiological function of the other two cytochromes is less clear. They are encoded by monocistronic genes and their redox partners can thus not be identified by gene sequencing. Expression of genes for c-type cytochromes in a foreign host are complicated due to the requirement for covalent heme insertion. Cytochrome c-553 is readily expressed in Escherichia coli in functional form, but cytochrome c3 and the high molecular mass cytochrome are for reasons that are presently not clear.

A universal system for the transport of redox proteins: early roots and latest developments.

The transport of proteins binding redox cofactors across a biological membrane is complicated by the fact that insertion of the redox cofactor is often a cytoplasmic process. These cytoplasmically assembled redox proteins must thus be transported in partially or completely folded form. The need for a special transport system for redox proteins was first recognized for periplasmic hydrogenases in gram-negative bacteria. These enzymes, which catalyze the reaction H2 <--> 2H+ + 2e, are composed of a large and a small subunit. Only the small subunit has an unusually long signal sequence of 30-50 amino acid residues, characterized by a conserved motif (S/T)-R-R-x-F-L-K at the N-terminus. This sequence directs export of the large and small subunit complex to the periplasm. Sequencing of microbial genes and genomes has shown that signal sequences with this conserved motif, now referred to as twin-arginine leaders, occur ubiquitously and export different classes of redox proteins, containing iron sulfur clusters, molybdopterin cofactors, polynuclear copper sites or flavin adenine dinucleotide. Mutations in an Escherichia coli operon referred to as mtt (membrane targeting and translocation) or tat (twin arginine translocation) are pleiotropic, i.e. these prevent the expression of a variety of periplasmic oxido-reductases in functional form. The Mtt or Tat pathway is distinct from the well-known Sec pathway and occurs ubiquitously in prokaryotes. The fact that its component proteins share sequence homology with proteins of the delta pH pathway for protein transport associated with chloroplast thylakoid assembly, illustrates the universal nature of this novel protein translocation system.

Isolation and physical studies of the intact supercoiled, the open circular and the linear forms of ColE1-plasmid DNA.

For the study of DNA conformations, conformational transitions, and DNA-protein interactions, covalently closed supercoiled ColE1-plasmid DNA has been purified from cultures of Escherichia coli harboring this plasmid and grown in the presence of chloramphenicol according to the method of D.B. Clewell [J. Bact. 110 (1972)667]. The open circular and linear forms of the plasmid were prepared by digestion of the covalently closed, supercoiled form with pancreatic deoxyribonuclease and EcoRI-restriction endonuclease, respectively. The linear form was found to be very homogeneous by electron microscopy and sedimenting boundary analysis. Its physical properties (s0 20,w=16.3 S,D0 20,W=1.98 X 10(-8) cm2 s-1 and [eta]=2605 ml g-1) have been carefully determined in 0.2 M NaCl, 0.002 M NaPO4 pH 7.0,0.002 M EDTA, at 23 degrees C. Combination of s0 20, w (obtained by quasielastic laser light scattering) gave Ms,D=4.39 x 10(6). This value is in reasonable agreement with the molecular weight from total intensity laser light scattering M=4.30 x 10(6). The covalently closed and open circular forms of the ColE1-plasmid are less homogeneous due to slight cross-contamination and the presence of small amounts of dimers in these preparations. The weight fractions of the various components as determined by boundary analysis or electron microscopy are given together with the average quantities obtained in the same solvent for the supercoiled form ((s0 20,w)w=25.4 S, (D0 20,w)z=2.89 x 10(-8) cm2 s-1, [eta]= 788 ML G-1,Ms,D=4.69 x 10(6) and Mw=4.59 x 10(6)) and the open circular form (s0 20, w)w=20.1 S, (D0 20,w)z=2.45 x 10(-8) cm2 s-1, [eta]=1421 ml g-1,Ms,D=4.37 x 10(6) and Mw=4.15 x 10(6)). Midpoint analysis of the sedimenting boundaries allows unambiguous determination of the sedimentation coefficients of these two forms: s0 20,w=24.5 S and s0 20,w=18.8 S, respectively. Also deduced from total intensity light scattering were radii of gyration Rg (103.5, 134.2 and 186 nm) and second virial coefficients A2 (0.7, 4.8 AND 5.4 x 10(-4) mole ml/g2) for the supercoiled, the open circular and linear forms, respectively. The data presented are discussed in relation to the conformational parameters for the three forms in solution.

Impact of nitrate-mediated microbial control of souring in oil reservoirs on the extent of corrosion.

The effect of microbial control of souring on the extent of corrosion was studied in a model system consisting of pure cultures of the nitrate-reducing, sulfide-oxidizing bacterium (NR-SOB) Thiomicrospira sp. strain CVO and the sulfate-reducing bacterium (SRB) Desulfovibrio sp. strain Lac6, as well as in an SRB consortium enriched from produced water from a Canadian oil reservoir. The average corrosion rate induced by the SRB consortium (1.4 g x m(-2) x day(-1)) was faster than that observed in the presence of strain Lac6 (0.2 g x m(-2) x day(-1)). Examination of the metallic coupons at the end of the tests indicated a uniform corrosion in both cases. Addition of CVO and 10 mM nitrate to a fully grown culture of Lac6 or the SRB consortium led to complete removal of sulfide from the system and a significant increase in the population of CVO, as determined by reverse sample genome probing. In the case of the SRB consortium addition of just nitrate (10 mM) had a similar effect. When grown in the absence of nitrate, the consortium was dominated by Desulfovibrio sp. strains Lac15 and Lac29, while growth in the presence of nitrate led to dominance of Desulfovibrio sp. strain Lac3. The addition of CVO and nitrate to the Lac6 culture or nitrate to the SRB consortium accelerated the average corrosion rate to 1.5 and 2.9 g x m(-2) x day(-1), respectively. Localized corrosion and the occurrence of pitting were apparent in both cases. Although the sulfide concentration (0.5-7 mM) had little effect on corrosion rates, a clear increase of the corrosion rate with increasing nitrate concentration was observed in experiments conducted with consortia enriched from produced water.

Biodegradation of C5+ hydrocarbons by a mixed bacterial consortium from a C(5+)-contaminated site.

C5+, a mixture of benzene, toluene, xylene, styrene, dicyclopentadiene (DCPD), naphthalene and other compounds, is a byproduct of polyethylene production and has been introduced into the environment via accidental release. The degradation of C5+ was studied using a defined consortium of 11 distinct bacterial strains isolated from C(5+)-contaminated soil. Vigorous growth of individual strains on C5+ was no prediction of dominance in the consortium, when the latter was grown under the same conditions. The defined consortium was able to degrade benzene, toluene, styrene and naphthalene, and to codegrade m-xylene in the presence of toluene or naphthalene. It was unable to degrade DCPD, which was inhibitory when degradation of pairs of C5+ components was examined. The complete C5+ mixture appeared to be the best substrate for the consortium.

Construction of a [NiFe]-hydrogenase deletion mutant of Desulfovibrio vulgaris Hildenborough.

A mutant of Desulfovibrio vulgaris Hildenborough lacking a gene for [NiFe] hydrogenase was generated. Growth studies, performed for the mutant in comparison with the wild-type, showed no strong differences during the exponential growth phase. However, the mutant cells died more rapidly in the stationary growth phase.

Binding of additional histones to chromatin core particles.

Isolated nucleosome core particles from chick erythrocytes and calf thymus have been used in experiments to show that chromatin subunits can absorb more than an additional equivalent of the histones making up the nucleosome octamer with no significant alteration in external shape and structure.

ISD1, an insertion element from the sulfate-reducing bacterium Desulfovibrio vulgaris Hildenborough: structure, transposition, and distribution.

Insertion element ISD1, discovered when its transposition caused the insertional inactivation of an introduced sacB gene, is present in two copies in the genome of Desulfovibrio vulgaris Hildenborough. Southern blot analysis indicated at least two insertion sites in the sacB gene. Cloning and sequencing of a transposed copy of ISD1 indicated a length of 1,200 bp with a pair of 44-bp imperfect inverted repeats at the ends, flanked by a direct repeat of the 4-bp target sequence. AAGG and AATT were found to function as target sequences. ISD1 encodes a transposase from two overlapping open reading frames by programmed translational frameshifting at an A6G shifty codon motif. Sequence comparison showed that ISD1 belongs to the IS3 family. Isolation and analysis of the chromosomal copies, ISD1-A and ISD1-B, by PCR and sequencing indicated that these are not flanked by direct repeats. ISD1-A is inserted in a region of the chromosome containing the gapdh-pgk genes (encoding glyceraldehyde-3-phosphate dehydrogenase and phosphoglycerate kinase). Active transposition to other loci in the genome was demonstrated, offering the potential of a new tool for gene cloning and mutagenesis. ISD1 is the first transposable element described for the sulfate reducers, a large and environmentally important group of bacteria. The distribution of ISD1 in genomes of sulfate-reducing bacteria is limited. A single copy is present in the genome of D. desulfuricans Norway.

Nucleotide sequence of the gene encoding the hydrogenase from Desulfovibrio vulgaris (Hildenborough).

The nucleotide sequence of the 4.7-kb SalI/EcoRI insert of plasmid pHV 15 containing the hydrogenase gene from Desulfovibrio vulgaris (Hildenborough) has been determined with the dideoxy chain-termination method. The structural gene for hydrogenase encodes a protein product of molecular mass 45820 Da. The NH2-terminal sequence of the enzyme deduced from the nucleic acid sequence corresponds exactly to the amino acid sequence determined by Edman degradation. The nucleic acid sequence indicates that a N-formylmethionine residue precedes the NH2-terminal amino acid Ser-1. There is no evidence for a leader sequence. The NH2-terminal part of the hydrogenase shows homology to the bacterial [8Fe-8S] ferredoxins. The sequence Cys-Ile-Xaa-Cys-Xaa-Xaa-Cys-Xaa-Xaa-Xaa-Cys-Pro-Xaa-Xaa-Ala-(Ile) occurs twice both in the hydrogenase and in [8Fe-8S] ferredoxins, where the Cys residues have been shown to coordinate two [4Fe-4S] clusters [Adman, E. T., Sieker, L. C. and Jensen, L. H. (1973) J. Biol. Chem. 248, 3987-3996]. These results, therefore, suggest that two electron-transferring ferredoxin-like [4Fe-4S] clusters are located in the NH2-terminal segment of the hydrogenase molecule. There are ten more Cys residues but it is not clear which four of these could participate in the formation of the third cluster, which is thought to be the hydrogen binding centre. Another gene, encoding a protein of molecular mass 13493 Da, was found immediately downstream from the gene for the 46-kDa hydrogenase. The nucleic acid sequence suggests that the hydrogenase and the 13.5-kDa protein belong to a single operon and are coordinately expressed. Since dodecylsulfate gel electrophoresis of purified hydrogenase indicates the presence of a 13.5-kDa polypeptide in addition to the 46-kDa component, it is proposed that the hydrogenase from D. vulgaris (Hildenborough) is a two-subunit enzyme.

Cloning and sequencing of the gene encoding cytochrome c3 from Desulfovibrio vulgaris (Hildenborough).

The gene encoding the redox protein cytochrome c3 from Desulfovibrio vulgaris (Hildenborough) has been cloned using two synthetic oligonucleotides (one 17-mer and one 18-mer), designed to recognize the structural gene. Plasmid pCYC3 was derived from the clone and contains a 7.5 X 10(3)-base EcoRI-HindIII insert of D. vulgaris DNA in pUC9. A 674-base-pair fragment of this insert was sequenced with the dideoxy-chain-termination procedure and found to contain the entire structural gene encoding cytochrome c3 bracketed by apparent Escherichia coli consensus sequences for initiation and termination of transcription. The amino acid sequence of 107 residues, derived from protein sequencing [Trousil, E. B. and Campbell, L. L. (1974) J. Biol. Chem. 249, 386-393], is confirmed by the nucleic acid sequence, which shows in addition that it is preceded by a hydrophobic, positively charged signal sequence of 21 residues. This amino-terminal extension functions in the export of cytochrome c3, which is thought to reside in the periplasm of D. vulgaris.

Overexpression, purification and immunodetection of DsrD from Desulfovibrio vulgaris Hildenborough.

Dissimilatory sulfite reductase (DsrAB) of the sulfate-reducing bacterium Desulfovibrio vulgaris Hildenborough is an alpha2beta2 tetramer of 180 kDa, encoded by the dsr operon. In addition to the dsrA and dsrB genes, this operon contains a gene (dsrD) encoding a protein of only 78 amino acids. Although, the function of DsrD is currently unknown, the presence of a dsrD gene has been demonstrated in a variety of sulfate-reducing bacteria and archaea. DsrD was expressed in Escherichia coli at a very high level and purified to homogeneity. Protein blotting experiments, using antisera raised against purified DsrD, demonstrated that it is expressed constitutively in D. vulgaris and does not copurify with DsrAB. Spectroscopic analysis of DsrD indicated that it does not bind either sulfite or sulfide, the substrate and product, respectively of the reaction catalyzed by DsrAB. Thus, although the conservation of this protein and its demonstrated presence in D. vulgaris, suggest an essential function in dissimilatory sulfite reduction, this function remains to be elucidated.