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Stress-Induced Production of Biofilm in the Hyperthermophile Archaeoglobus fulgidus.

Archaeoglobus fulgidus, an anaerobic marine hyperthermophile, forms a biofilm in response to environmental stresses. The biofilm is a heterogeneous, morphologically variable structure containing protein, polysaccharide, and metals. Production of the biofilm can be induced by nonphysiological extremes of pH and temperature, by high concentrations of metals, and by addition of antibiotics, xenobiotics, or oxygen. Cells within the biofilm show an increased tolerance to otherwise toxic environmental conditions. Metals sequestered within the biofilm stimulate growth of A. fulgidus cells in metal-depleted medium. These data suggest that cells may produce biofilm as a mechanism for concentrating cells and attaching to surfaces, as a protective barrier, and as a reserve nutrient. Because similar biofilms are formed by Archaeoglobus profundus, Methanococcus jannaschii, and Methanobacterium thermoautotrophicum, biofilm formation might be a common stress response mechanism among the archaea.

Journal Article↗

Characterization of a tetrameric inositol monophosphatase from the hyperthermophilic bacterium Thermotoga maritima.

Inositol monophosphatase (I-1-Pase) catalyzes the dephosphorylation step in the de novo biosynthetic pathway of inositol and is crucial for all inositol-dependent processes. An extremely heat-stable tetrameric form of I-1-Pase from the hyperthermophilic bacterium Thermotoga maritima was overexpressed in Escherichia coli. In addition to its different quaternary structure (all other known I-1-Pases are dimers), this enzyme displayed a 20-fold higher rate of hydrolysis of D-inositol 1-phosphate than of the L isomer. The homogeneous recombinant T. maritima I-1-Pase (containing 256 amino acids with a subunit molecular mass of 28 kDa) possessed an unusually high V(max) (442 micromol min(-1) mg(-1)) that was much higher than the V(max) of the same enzyme from another hyperthermophile, Methanococcus jannaschii. Although T. maritima is a eubacterium, its I-1-Pase is more similar to archaeal I-1-Pases than to the other known bacterial or mammalian I-1-Pases with respect to substrate specificity, Li(+) inhibition, inhibition by high Mg(2+) concentrations, metal ion activation, heat stability, and activation energy. Possible reasons for the observed kinetic differences are discussed based on an active site sequence alignment of the human and T. maritima I-1-Pases.

Enzyme Stability↗

Culture-dependent and culture-independent characterization of microbial assemblages associated with high-temperature petroleum reservoirs.

Recent investigations of oil reservoirs in a variety of locales have indicated that these habitats may harbor active thermophilic prokaryotic assemblages. In this study, we used both molecular and culture-based methods to characterize prokaryotic consortia associated with high-temperature, sulfur-rich oil reservoirs in California. Enrichment cultures designed for anaerobic thermophiles, both autotrophic and heterotrophic, were successful at temperatures ranging from 60 to 90 degrees C. Heterotrophic enrichments from all sites yielded sheathed rods (Thermotogales), pleomorphic rods resembling Thermoanaerobacter, and Thermococcus-like isolates. The predominant autotrophic microorganisms recovered from inorganic enrichments using H(2), acetate, and CO(2) as energy and carbon sources were methanogens, including isolates closely related to Methanobacterium, Methanococcus, and Methanoculleus species. Two 16S rRNA gene (rDNA) libraries were generated from total community DNA collected from production wellheads, using either archaeal or universal oligonucleotide primer sets. Sequence analysis of the universal library indicated that a large percentage of clones were highly similar to known bacterial and archaeal isolates recovered from similar habitats. Represented genera in rDNA clone libraries included Thermoanaerobacter, Thermococcus, Desulfothiovibrio, Aminobacterium, Acidaminococcus, Pseudomonas, Halomonas, Acinetobacter, Sphingomonas, Methylobacterium, and Desulfomicrobium. The archaeal library was dominated by methanogen-like rDNAs, with a lower percentage of clones belonging to the Thermococcales. Our results strongly support the hypothesis that sulfur-utilizing and methane-producing thermophilic microorganisms have a widespread distribution in oil reservoirs and the potential to actively participate in the biogeochemical transformation of carbon, hydrogen, and sulfur in situ.

Archaea↗

Distribution and diversity of archaea corresponding to the limnological cycle of a hypersaline stratified lake (Solar lake, Sinai, Egypt).

The vertical and seasonal distribution and diversity of archaeal sequences was investigated in a hypersaline, stratified, monomictic lake, Solar Lake, Sinai, Egypt, during the limnological development of stratification and mixing. Archaeal sequences were studied via phylogenetic analysis of 16S rDNA sequences as well as denaturing gradient gel electrophoresis analysis. The 165 clones studied were grouped into four phylogenetically different clusters. Most of the clones isolated from both the aerobic epilimnion and the sulfide-rich hypolimnion were defined as cluster I, belonging to the Halobacteriaceae family. The three additional clusters were all isolated from the anaerobic hypolimnion. Cluster II is phylogenetically located between the genera Methanobacterium and Methanococcus. Clusters III and IV relate to two previously documented groups of uncultured euryarchaeota, remotely related to the genus Thermoplasma. No crenarchaeota were found in the water column of the Solar Lake. The archaeal community in the Solar Lake under both stratified and mixed conditions was dominated by halobacteria in salinities higher than 10%. During stratification, additional clusters, some of which may possibly relate to uncultured halophilic methanogens, were found in the sulfide- and methane-rich hypolimnion.

Archaea↗

beta-Glutamate as a substrate for glutamine synthetase.

The conversion of beta-glutamate to beta-glutamine by archaeal and bacterial glutamine synthetase (GS) enzymes has been examined. The GS from Methanohalophilus portucalensis (which was partially purified) is capable of catalyzing the amidation of this substrate with a rate sevenfold less than the rate obtained with alpha-glutamate. Recombinant GS from the archaea Methanococcus jannaschii and Archaeoglobus fulgidus were considerably more selective for alpha-glutamate than beta-glutamate as a substrate. All the archaeal enzymes were much less selective than the two bacterial GS (from Escherichia coli and Bacillus subtilis), whose specific activities towards beta-glutamate were much smaller than rates with the alpha-isomer. These results are discussed in light of the observation that beta-glutamate is accumulated as an osmolyte in many archaea while beta-glutamine (produced by glutamine synthetase) is used as an osmolyte only in M. portucalensis.

Animals↗

Phylogenetic diversity of nitrogenase (nifH) genes in deep-sea and hydrothermal vent environments of the Juan de Fuca Ridge.

The subseafloor microbial habitat associated with typical unsedimented mid-ocean-ridge hydrothermal vent ecosystems may be limited by the availability of fixed nitrogen, inferred by the low ammonium and nitrate concentrations measured in diffuse hydrothermal fluid. Dissolved N2 gas, the largest reservoir of nitrogen in the ocean, is abundant in deep-sea and hydrothermal vent fluid. In order to test the hypothesis that biological nitrogen fixation plays an important role in nitrogen cycling in the subseafloor associated with unsedimented hydrothermal vents, degenerate PCR primers were designed to amplify the nitrogenase iron protein gene nifH from hydrothermal vent fluid. A total of 120 nifH sequences were obtained from four samples: a nitrogen-poor diffuse vent named marker 33 on Axial Volcano, sampled twice over a period of 1 year as its temperature decreased; a nitrogen-rich diffuse vent near Puffer on Endeavour Segment; and deep seawater with no detectable hydrothermal plume signal. Subseafloor nifH genes from marker 33 and Puffer are related to anaerobic clostridia and sulfate reducers. Other nifH genes unique to the vent samples include proteobacteria and divergent Archaea. All of the nifH genes from the deep-seawater sample are most closely related to the thermophilic, anaerobic archaeon Methanococcus thermolithotrophicus (77 to 83% amino acid similarity). These results provide the first genetic evidence of potential nitrogen fixers in hydrothermal vent environments and indicate that at least two sources contribute to the diverse assemblage of nifH genes detected in hydrothermal vent fluid: nifH genes from an anaerobic, hot subseafloor and nifH genes from cold, oxygenated deep seawater.

Archaea↗

Biosynthesis of phosphoserine in the Methanococcales.

Methanococcus maripaludis and Methanocaldococcus jannaschii produce cysteine for protein synthesis using a tRNA-dependent pathway. These methanogens charge tRNA(Cys) with l-phosphoserine, which is also an intermediate in the predicted pathways for serine and cystathionine biosynthesis. To establish the mode of phosphoserine production in Methanococcales, cell extracts of M. maripaludis were shown to have phosphoglycerate dehydrogenase and phosphoserine aminotransferase activities. The heterologously expressed and purified phosphoglycerate dehydrogenase from M. maripaludis had enzymological properties similar to those of its bacterial homologs but was poorly inhibited by serine. While bacterial enzymes are inhibited by micromolar concentrations of serine bound to an allosteric site, the low sensitivity of the archaeal protein to serine is consistent with phosphoserine's position as a branch point in several pathways. A broad-specificity class V aspartate aminotransferase from M. jannaschii converted the phosphohydroxypyruvate product to phosphoserine. This enzyme catalyzed the transamination of aspartate, glutamate, phosphoserine, alanine, and cysteate. The M. maripaludis homolog complemented a serC mutation in the Escherichia coli phosphoserine aminotransferase. All methanogenic archaea apparently share this pathway, providing sufficient phosphoserine for the tRNA-dependent cysteine biosynthetic pathway.

Archaeal Proteins↗

Identification of diverse archaeal proteins with class III signal peptides cleaved by distinct archaeal prepilin peptidases.

Most secreted archaeal proteins are targeted to the membrane via a tripartite signal composed of a charged N terminus and a hydrophobic domain, followed by a signal peptidase-processing site. Signal peptides of archaeal flagellins, similar to class III signal peptides of bacterial type IV pilins, are distinct in that their processing sites precede the hydrophobic domain, which is crucial for assembly of these extracytoplasmic structures. To identify the complement of archaeal proteins with class III signal sequences, a PERL program (FlaFind) was written. A diverse set of proteins was identified, and many of these FlaFind positives were encoded by genes that were cotranscribed with homologs of pilus assembly genes. Moreover, structural conservation of primary sequences between many FlaFind positives and subunits of bacterial pilus-like structures, which have been shown to be critical for pilin assembly, have been observed. A subset of pilin-like FlaFind positives contained a conserved domain of unknown function (DUF361) within the signal peptide. Many of the genes encoding these proteins were in operons that contained a gene encoding a novel euryarchaeal prepilin-peptidase, EppA, homolog. Heterologous analysis revealed that Methanococcus maripaludis DUF361-containing proteins were specifically processed by the EppA homolog of this archaeon. Conversely, M. maripaludis preflagellins were cleaved only by the archaeal preflagellin peptidase FlaK. Together, the results reveal a diverse set of archaeal proteins with class III signal peptides that might be subunits of as-yet-undescribed cell surface structures, such as archaeal pili.

Archaea↗

Polyadenylated RNA isolated from the archaebacterium Halobacterium halobium.

Polyadenylated [poly(A)+] RNA has been isolated from the halophilic archaebacterium Halobacterium halobium by binding, at 4 degrees C, to oligo(dT)-cellulose. H. halobium contains approximately 12 times more poly(A) per unit of RNA than does the methanogenic archaebacterium Methanococcus vannielii. The 3' poly(A) tracts in poly(A)+ RNA molecules are approximately twice as long (average length of 20 nucleotides) in H. halobium as in M. vannielii. In both archaebacterial species, poly(A)+ RNAs are unstable.

Electrophoresis, Agar Gel↗

Structure and comparative analysis of the genes encoding component C of methyl coenzyme M reductase in the extremely thermophilic archaebacterium Methanothermus fervidus.

A 6-kilobase-pair (kbp) region of the genome of the extremely thermophilic arachaebacterium Methanothermus fervidus which encodes the alpha, beta, and gamma subunit polypeptides of component C of methyl coenzyme M reductase was cloned and sequenced. Genes encoding the beta (mcrB) and gamma (mcrG) subunits were separated by two open reading frames (designated mcrC and mcrD) which encode unknown gene products. The M. fervidus genes were preceded by ribosome-binding sites, separated by short A + T-rich intergenic regions, contained unexpectedly few NNC codons, and exhibited inflexible codon usage at some locations. Sites of transcription initiation and termination flanking the mcrBDCGA cluster of genes in M. fervidus were identified. The sequences of the genes, the encoded polypeptides, and transcription regulatory signals in M. fervidus were compared with the functionally equivalent sequences from two mesophilic methanogens (Methanococcus vannielii and Methanosarcina barkeri) and from a moderate thermophile (Methanobacterium thermoautotrophicum Marburg). The amino acid sequences of the polypeptides encoded by the mcrBCGA genes in the two thermophiles were approximately 80% identical, whereas all other pairs of these gene products contained between 50 and 60% identical amino acid residues. The mcrD gene products have diverged more than the products of the other mcr genes. Identification of highly conserved regions within mcrA and mcrB suggested oligonucleotide sequences which might be developed as hybridization probes which could be used for identifying and quantifying all methanogens.

Amino Acid Sequence↗

Cloning and physical mapping of RNA polymerase genes from Methanobacterium thermoautotrophicum and comparison of homologies and gene orders with those of RNA polymerase genes from other methanogenic archaebacteria.

The structural genes encoding the four largest subunits of RNA polymerase, A, B', B", and C, were physically mapped in Methanobacterium thermoautotrophicum Winter. The genes formed a cluster in the order B", B', A, C and had a common orientation. DNA hybridization experiments yielded different degrees of homology between RNA polymerase gene sequences of different species of Methanobacterium and Methanococcus voltae. No homology was detectable between Methanobacterium thermoautotrophicum and Methanosarcina barkeri. From Southern hybridization experiments in which probes of the four genes from Methanobacterium thermoautotrophicum Winter and restriction digests of the genomic DNAs of the different methanogens were used, a common gene order of the RNA polymerase genes could be deduced.

Archaea↗

Transcription in vivo and in vitro of the histone-encoding gene hmfB from the hyperthermophilic archaeon Methanothermus fervidus.

Immediately upstream of the hmfB gene, in a DNA fragment cloned from Methanothermus fervidus, are two identical tandemly repeated copies of a 73-bp sequence that contain the sequence 5'TTTATATA, which conforms precisely to the consensus TATA box element proposed for methanogen promoters. By using this duplicated region as the template DNA and a cell-free transcription system derived from Methanococcus thermolithotrophicus, transcription in vitro was found to initiate at two identical sites 73 bp apart, each 25 bp downstream from a TATA box, thus providing strong evidence for the functional conservation of this transcriptional signal in two phylogenetically very diverse methanogens. Transcription of the hmfB gene in vivo in M. fervidus was found to occur at only one of these sites, and consistent with this observation, recloning and sequencing of this intergenic region after its amplification by the polymerase chain reaction demonstrated that the genome of M. fervidus contains only one copy of the 73-bp sequence upstream of the hmfB gene. Since the second copy of the 73-bp sequence, presumably generated artifactually during the original hmfB cloning, functioned equally well as a promoter in the M. thermolithotrophicus transcription system, all information needed by the heterologous RNA polymerase to initiate transcription accurately in vitro must be present within this sequence. The hmfB gene encodes HMf-2, one of the two subunits of HMf, an abundant DNA binding protein in M. fervidus which binds to DNA molecules in vitro, forming nucleosomelike structures. Cell-free transcription was inhibited by adding HMf or eucaryotic core histones at protein-to-DNA mass ratios of 0.3:1 and 1:1, respectively, whereas the archael histonelike protein HTa from Thermoplasma acidophilum inhibited transcription in vitro only at much higher protein-to-DNA mass ratios and the bacterial histonelike protein HU from Escherichia coli had no detectable effect on transcription.

Archaeal Proteins↗

Tryptophan biosynthesis genes trpEGC in the thermoacidophilic archaebacterium Sulfolobus solfataricus.

A DNA fragment containing the trpEGC gene cluster was isolated from the thermoacidophilic archaebacterium Sulfolobus solfataricus. The products of trpE, trpG, and trpC from S. solfataricus were compared to the homologous products from a eukaryote, a eubacterium, and two archaebacteria, namely, a methanogen and an extreme halophile. They appeared to be equally related to the proteins from Escherichia coli and Saccharomyces cerevisiae, the percentages of conserved amino acids being roughly the same as those measured when comparing the eubacterial and eukaryotic sequences directly. These percentages did not rise significantly when a comparison with the proteins from Haloferax volcanii was drawn, while a slightly closer relationship with the proteins from Methanococcus thermoautotrophicum was found.

Amino Acid Sequence↗

Cloning and sequencing of the gene encoding glutamine synthetase I from the archaeum Pyrococcus woesei: anomalous phylogenies inferred from analysis of archaeal and bacterial glutamine synthetase I sequences.

The gene glnA encoding glutamine synthetase I (GSI) from the archaeum Pyrococcus woesei was cloned and sequenced with the Sulfolobus solfataricus glnA gene as the probe. An operon reading frame of 448 amino acids was identified within a DNA segment of 1,528 bp. The encoded protein was 49% identical with the GSI of Methanococcus voltae and exhibited conserved regions characteristic of the GSI family. The P. woesei GSI was aligned with available homologs from other archaea (S. solfataricus, M. voltae) and with representative sequences from cyanobacteria, proteobacteria, and gram-positive bacteria. Phylogenetic trees were constructed from both the amino acid and the nucleotide sequence alignments. In accordance with the sequence similarities, archaeal and bacterial sequences did not segregate on a phylogeny. On the basis of sequence signatures, the GSI trees could be subdivided into two ensembles. One encompassed the GSI of cyanobacteria and proteobacteria, but also that of the high-G + C gram-positive bacterium Streptomyces coelicolor (all of which are regulated by the reversible adenylylation of the enzyme subunits); the other embraced the GSI of the three archaea as well as that of the low-G + C gram-positive bacteria (Clostridium acetobutilycum, Bacillus subtilis) and Thermotoga maritima (none of which are regulated by subunit adenylylation). The GSIs of the Thermotoga and the Bacillus-Clostridium lineages shared a direct common ancestor with that of P. woesei and the methanogens and were unrelated to their homologs from cyanobacteria, proteobacteria, and S. coelicolor. The possibility is presented that the GSI gene arose among the archaea and was then laterally transferred from some early methanogen to a Thermotoga-like organism. However, the relationship of the cyanobacterial-proteobacterial GSIs to the Thermotoga GSI and the GSI of low-G+C gram-positive bacteria remains unexplained.

Amino Acid Sequence↗

Isolation and characterization of flagella and flagellin proteins from the Thermoacidophilic archaea Thermoplasma volcanium and Sulfolobus shibatae.

Isolated flagellar filaments of Sulfolobus shibatae were 15 nm in diameter, and they were composed of two major flagellins which have M(r)s of 31,000 and 33,000 and which stained positively for glycoprotein. The flagellar filaments of Thermoplasma volcanium were 12 nm in diameter and were composed of one major flagellin which has an M(r) of 41,000 and which also stained positively for glycoprotein. N-terminal amino acid sequencing indicated that 18 of the N-terminal 20 amino acid positions of the 41-kDa flagellin of T. volcanium were identical to those of the Methanococcus voltae 31-kDa flagellin. Both flagellins of S. shibatae had identical amino acid sequences for at least 23 of the N-terminal positions. This sequence was least similar to any of the available archaeal flagellin sequences, consistent with the phylogenetic distance of S. shibatae from the other archaea studied.

Amino Acid Sequence↗

The Helicobacter pylori ureC gene codes for a phosphoglucosamine mutase.

The function of UreC, the product of a 1,335-bp-long open reading frame upstream from the urease structural genes (ureAB) of Helicobacter pylori, was investigated. We present data showing that the ureC gene product is a phosphoglucosamine mutase. D. Mengin-Lecreulx and J. van Heijenoort (J. Biol. Chem. 271:32-39, 1996) observed that UreC is similar (43% identity) to the GlmM protein of Escherichia coli. Those authors showed that GlmM is a phosphoglucosamine mutase catalyzing interconversion of glucosamine-6-phosphate into glucosamine-1-phosphate, which is subsequently transformed into UDP-N-acetylglucosamine. The latter product is one of the main cytoplasmic precursors of cell wall peptidoglycan and outer membrane lipopolysaccharides. The present paper reports that, like its E. coli homolog glmM, the H. pylori ureC gene is essential for cell growth. It was known that growth of a lethal conditional glmM mutant of E. coli at a nonpermissive temperature can be restored in the presence of the ureC gene. We showed that complete complementation of the glmM mutant can be obtained with a plasmid overproducing UreC. The peptidoglycan content and the specific phosphoglucosamine mutase activity of such a complemented strain were measured; these results demonstrated that the ureC gene product functions as a phosphoglucosamine mutase. Homologs of the UreC and GlmM proteins were identified in Haemophilus influenzae, Mycobacterium leprae, Clostridium perfringens, Synechocystis sp. strain PCC6803, and Methanococcus jannaschii. Significant conservation of the amino acid sequence of these proteins in such diverse organisms suggests a very ancient common ancestor for the genes and defines a consensus motif for the phosphoglucosamine mutase active site. We propose renaming the H. pylori ureC gene the glmM gene.

Amino Acid Sequence↗

Compositional biases of bacterial genomes and evolutionary implications.

We compare and contrast genome-wide compositional biases and distributions of short oligonucleotides across 15 diverse prokaryotes that have substantial genomic sequence collections. These include seven complete genomes (Escherichia coli, Haemophilus influenzae, Mycoplasma genitalium, Mycoplasma pneumoniae, Synechocystis sp. strain PCC6803, Methanococcus jannaschii, and Pyrobaculum aerophilum). A key observation concerns the constancy of the dinucleotide relative abundance profiles over multiple 50-kb disjoint contigs within the same genome. (The profile is rhoXY* = fXY*/fX*fY* for all XY, where fX* denotes the frequency of the nucleotide X and fY* denotes the frequency of the dinucleotide XY, both computed from the sequence concatenated with its inverted complementary sequence.) On the basis of this constancy, we refer to the collection [rhoXY*] as the genome signature. We establish that the differences between [rhoXY*] vectors of 50-kb sample contigs of different genomes virtually always exceed the differences between those of the same genomes. Various di- and tetranucleotide biases are identified. In particular, we find that the dinucleotide CpG=CG is underrepresented in many thermophiles (e.g., M. jannaschii, Sulfolobus sp., and M. thermoautotrophicum) but overrepresented in halobacteria. TA is broadly underrepresented in prokaryotes and eukaryotes, but normal counts appear in Sulfolobus and P. aerophilum sequences. More than for any other bacterial genome, palindromic tetranucleotides are underrepresented in H. influenzae. The M. jannaschii sequence is unprecedented in its extreme underrepresentation of CTAG tetranucleotides and in the anomalous distribution of CTAG sites around the genome. Comparative analysis of numbers of long tetranucleotide microsatellites distinguishes H. influenzae. Dinucleotide relative abundance differences between bacterial sequences are compared. For example, in these assessments of differences, the cyanobacteria Synechocystis, Synechococcus, and Anabaena do not form a coherent group and are as far from each other as general gram-negative sequences are from general gram-positive sequences. The difference of M. jannaschii from low-G+C gram-positive proteobacteria is one-half of the difference from gram-negative proteobacteria. Interpretations and hypotheses center on the role of the genome signature in highlighting similarities and dissimilarities across different classes of prokaryotic species, possible mechanisms underlying the genome signature, the form and level of genome compositional flux, the use of the genome signature as a chronometer of molecular phylogeny, and implications with respect to the three putative eubacterial, archaeal, and eukaryote domains of life and to the origin and early evolution of eukaryotes.

Bacteria↗

The Helicobacter pylori gene encoding phosphatidylserine synthase: sequence, expression, and insertional mutagenesis.

The Helicobacter pylori pss gene, coding for phosphatidylserine synthase (PSS), was cloned and sequenced in this study. A polypeptide of 237 amino acids was deduced from the PSS sequence. H. pylori PSS exhibits significant amino acid sequence identity with the PSS proteins found in the archaebacterium Methanococcus jannaschii, the gram-positive bacterium Bacillus subtilis, and the yeast Saccharomyces cerevisiae but none with its Escherichia coli counterpart. Expression of the putative pss gene in maxicells gave rise to a product of approximately 26 kDa, which is in agreement with the predicted molecular mass of 26,617 Da. A manganese-dependent PSS activity was found in the membrane fractions of the E. coli cells overexpressing the H. pylori pss gene product. This result indicates that this enzyme is a membrane-bound protein, a conclusion which is supported by the fact that the PSS protein contains several local hydrophobic segments which could form transmembrane helices. The pss gene was inactivated with a chloramphenicol acetyltransferase cassette on the plasmid. However, an isogenic pss gene-disrupted mutant of H. pylori UA802 could not be obtained, suggesting that this enzyme plays an essential role in the growth of this organism.

Amino Acid Sequence↗