Have archaeal genes contributed to bacterial virulence?
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Phylogenetic analyses of two "archaeal" genes in thermotoga maritima reveal multiple transfers between archaea and bacteria.
The genome sequence of Thermotoga maritima revealed that 24% of its open reading frames (ORFs) showed the highest similarity scores to archaeal genes in BLAST analyses. Here we screened 16 strains from the genus Thermotoga and other related Thermotogales for the occurrence of two of these "archaeal" genes: the gene encoding the large subunit of glutamate synthase (gltB) and the myo-inositol 1P synthase gene (ino1). Both genes were restricted to the Thermotoga species within the Thermotogales. The distribution of the two genes, along with results from phylogenetic analyses, showed that they were acquired from Archaea during the divergence of the Thermotogales. Database searches revealed that three other bacteria-Dehalococcoides ethenogenes, Sinorhizobium meliloti, and Clostridium difficile-possess archaeal-type gltBs, and the phylogenetic analyses confirmed at least two lateral gene transfer (LGT) events between Bacteria and Archaea. These LGT events were also strongly supported by gene structure data, as the three domains in bacterial-type gltB are homologous to three independent ORFs in Archaea and Bacteria with archaeal-type gltBs. The ino1 gene has a scattered distribution among Bacteria, and apart from the Thermotoga strains it is found only in Aquifex aeolicus, D. ethenogenes, and some high-G+C Gram-positive bacteria. Phylogenetic analysis of the ino1 sequences revealed three highly supported prokaryotic clades, all containing a mixture of archaeal and bacterial sequences, and suggested that all bacterial ino1 genes had been recruited from archaeal donors. The Thermotoga strains and A. aeolicus acquired this gene independently from different archaeal species. Although transfer of genes from hyperthermophilic Archaea may have facilitated the evolution of bacterial hyperthermophily, between-domain transfers also affect mesophilic species. For hyperthermophiles, we hypothesize that LGT may be as much a consequence as the cause of adaptation to hyperthermophily.
Bacteria↗
Rare codon clusters at 5'-end influence heterologous expression of archaeal gene in Escherichia coli.
Proteins from hyperthermophilic microorganisms are attractive candidates for novel biocatalysts because of their high resistance to temperature extremes. However, archaeal genes are usually poorly expressed in Escherichia coli because of differences in codon usage. Genes from the thermoacidophilic archaea Sulfolobus solfataricus and Thermoplasma acidophilum contain high proportions of rare codons for arginine, isoleucine, and leucine, which are recognized by the tRNAs encoded by the argU, ileY, and leuW genes, respectively, and which are rarely used in E. coli. To examine the effects of these rare codons on heterologous expression, we expressed the Sso_gnaD and Tac_gnaD genes from S. solfataricus and T. acidophilum, respectively, in E. coli. The Sso_gnaD product was expressed at very low levels when the open reading frame (ORF) was cloned in pRSET and expressed in E. coli BL21(DE3), and was expressed at much higher levels in the E. coli BL21(DE3)-CodonPlus RIL strain, which contains extra copies of the argU, ileY, and leuW tRNA genes. In contrast, Tac_gnaD was expressed at similar levels in both E. coli strains. Comparison of the Sso_gnaD and Tac_gnaD gene sequences revealed that the 5'-end of the Sso_gnaD sequence was rich in AGA(arg) and ATA(Ile) codons. These codons were replaced with the codons commonly used in E. coli by polymerase chain reaction-mediated site-directed mutagenesis. The results of expression studies showed that a non-tandem repeat of rare codons is critical in the observed interference in heterologous expression of this gene. We concluded that the level of heterologous expression of Sso_gnaD in E. coli was limited by the clustering of the rare codons in the ORF, rather than on the rare codon frequency.
Codon↗
Adenylosuccinate synthetase genes: molecular cloning and phylogenetic analysis of a highly conserved archaeal gene.
Adenylosuccinate synthetase (PurA) catalyzes the first step in the de novo AMP synthesis and has been extensively studied in both Bacteria and Eukarya. We cloned the purA gene from the hyperthermophilic archaeon, Pyrococcus furiosus. The gene appears to be individually transcribed and encodes a protein of 339 amino acids. The amino acid sequence comparison with other archael PurAs found from recent genome analyses indicated that two deletions, one central and the other C-terminal, are a common feature of archaeal PurAs. None of the 21 PurA homologues analyzed from Eukarya and Bacteria exhibited this feature. Amino acid sequences of PurAs in Archaea showed 64% average identities which were significantly higher than the 50% and 55% calculated for Bacteria and Eukarya, respectively. Several residues conserved in PurAs of both Eukarya and Bacteria and shown to be of catalytic importance are missing in the archaeal PurAs. Phylogenetic analysis using PurA as the marker grouped life into 3 domains, hence it was consistent with results derived from 16-18S ribosomal RNA sequences. The topology within the three domains, in general, portrayed the hitherto accepted evolutionary relationship among the organisms utilized. PurA can, thus, serve as an additional marker to evaluate phylogenetic inferences drawn from sequence data from rRNA and other conserved genes. The presence of two unique deletions in both euryarchaeal and crenarchaeal PurAs, but not in those of Bacteria and Eukarya, is a strong evidence confirming the common lineage of these two subdomains of Archaea.
Adenylosuccinate Synthase↗
Horizontal transfer of archaeal genes into the deinococcaceae: detection by molecular and computer-based approaches.
Members of the Deinococcaceae (e.g., Thermus, Meiothermus, Deinococcus) contain A/V-ATPases typically found in Archaea or Eukaryotes which were probably acquired by horizontal gene transfer. Two methods were used to quantify the extent to which archaeal or eukaryotic genes have been acquired by this lineage. Screening of a Meiothermus ruber library with probes made against Thermoplasma acidophilum DNA yielded a number of clones which hybridized more strongly than background. One of these contained the prolyl tRNA synthetase (RS) gene. Phylogenetic analysis shows the M. ruber and D. radiodurans prolyl RS to be more closely related to archaeal and eukaryal forms of this gene than to the typical bacterial type. Using a bioinformatics approach, putative open reading frames (ORFs) from the prerelease version of the D. radiodurans genome were screened for genes more closely related to archaeal or eukaryotic genes. Putative ORFs were searched against representative genomes from each of the three domains using automated BLAST. ORFs showing the highest matches against archaeal and eukaryotic genes were collected and ranked. Among the top-ranked hits were the A/V-ATPase catalytic and noncatalytic subunits and the prolyl RS genes. Using phylogenetic methods, ORFs were analyzed and trees assessed for evidence of horizontal gene transfer. Of the 45 genes examined, 20 showed topologies in which D. radiodurans homologues clearly group with eukaryotic or archaeal homologues, and 17 additional trees were found to show probable evidence of horizontal gene transfer. Compared to the total number of ORFs in the genome, those that can be identified as having been acquired from Archaea or Eukaryotes are relatively few (approximately 1%), suggesting that interdomain transfer is rare.
Archaea↗
Identification of archaeal genes encoding a novel stationary phase-response protein.
A novel stationary phase-response protein has been identified in the acid-soluble protein extract of the thermophilic archaeon, Thermococcus zilligii. N-Terminal sequencing data were used to identify likely genes for homologues of the protein in the complete genome sequences of various archaeal species. The corresponding genes were identified and analysed. The genes encode a protein ranging from 83 to 92 amino acids in length, with a calculated pI ranging from 4.6 to 9.7. The amino acid sequences of the genes were highly conserved, even between members belonging to the different archaeal kingdoms. The computed secondary structure of the protein indicates it consists of four large helical regions separated by short coiled regions. We propose this protein as a candidate regulator of gene expression in stationary phase.
Amino Acid Sequence↗
Control regions of an archaeal gene. A TATA box and an initiator element promote cell-free transcription of the tRNA(Val) gene of Methanococcus vannielii.
To identify the DNA sequences required for initiation of transcription in archaea, the 5'-flanking region of the tRNA(Val) gene of Methanococcus vannielii was modified by deletions, restructuring and site-directed mutagenesis, and the tRNA encoding sequence was replaced by a fortuitous Escherichia coli sequence. The effects of these mutations on promoter function were tested in an homologous cell-free transcription system. The DNA region from position -35 to +9 relative to the transcription start site was sufficient for maximal initiation of cell-free transcription. Removal of the DNA region between -35 and -30 reduced initiation by a factor of 2. Deletions extending to position -24 almost completely abolished specific transcription. Analysis of 16 site-specific mutations in the region from -33 to +2 provided evidence that a conserved A + T-rich sequence (TATA box), centered at -25, is essential for initiation of transcription. Single point mutations in six positions of the TATA box reduced initiation of transcription from 0.2 to 0.01 of wild-type levels. A second conserved motif at the transcription start site (consensus ATGC) could be replaced by some sequences containing a pyrimidine-purine dinucleotide but appeared necessary for a maximal rate of gene transcription. Mutations altering the spacing between the two conserved elements demonstrated that initiation occurs at a strictly defined distance of 22 to 27 base-pairs downstream from the TATA box. Our results support the conclusion that the TATA box is the major DNA region mediating promoter recognition, influencing the efficiency of transcription and specifying the site of transcription initiation. This Methanococcus promoter element closely resembles in structure and function the TATA box of promoters of eukaryotic protein-encoding genes transcribed by RNA polymerase II.
Base Sequence↗
An archaeal gene upstream of grpE different from eubacterial counterparts.
In some eubacteria with a dnaK locus in which grpE is close upstream of dnaK, grpE is preceded by an open reading frame (orf) believed to be a heat-shock gene. We also found an orf, orf16, upstream of grpE in the archaeon Methanosarcina mazei S-6, but this gene differs from the eubacterial counterpart: it is shorter, does not respond to a temperature upshift as heat-shock genes do, and the deduced protein Orf16, does not resemble the proteins coded by the eubacterial equivalents. orf16 is expressed monocistronically, with a transcription initiation site 24 bases upstream of the translation start codon, 22 bases downstream of a putative promoter identical to the consensus promoter for genes in methanogens. This initiation site is used by heat-shocked and non-heat-shocked cells in the two morphologic stages of M. mazei S-6 tested, i.e., packets and single cells. Three transcription termination sites were identified, one of which is detectable only in non-heat-shocked cells. Data from comparative analyses of the Orf16 deduced amino acid sequence and those of other known proteins, as well as the apparent biochemical characteristics of Orf16, suggest that the latter is a membrane molecule.
Amino Acid Sequence↗
A Methanocaldococcus jannaschii archaeal signature gene encodes for a 5-formaminoimidazole-4-carboxamide-1-beta-D-ribofuranosyl 5'-monophosphate synthetase. A new enzyme in purine biosynthesis.
We have identified and characterized a new member of the ATP-grasp enzyme family that catalyzes the ATP- and formate-dependent formylation of 5-aminoimidazole-4-carboxamide-1-beta-D-ribofuranosyl 5'-monophosphate (AICAR) to 5-formaminoimidazole-4-carboxamide-1-beta-D-ribofuranosyl 5'-monophosphate (FAICAR) in the absence of folates. The enzyme, which we designate as PurP, is the product of the Methanocaldococcus jannaschii purP gene (MJ0136), which is a signature gene for Archaea. As is characteristic of reactions catalyzed by this family of enzymes, the other products of the reaction, ADP and P(i), were produced stoichiometrically with the amount of ATP, formate, and AICAR used. Formyl phosphate was found to substitute for ATP and formate in the reaction, yet the methylene analog, phosphonoacetaldehyde, was not an inhibitor or substrate for the reaction. The enzyme, along with PurO, which catalyzes the cyclization of FAICAR to inosine 5'-monophosphate, catalyzes the same overall transformation in purine biosynthesis as is accomplished by PurH in bacteria and eukaryotes. No homology exists between PurH and either PurO or PurP. 1H NMR and gas chromatography-mass spectrometry analysis of an M. jannaschii cell extract showed the presence of free formate that can be used by the enzyme for purine biosynthesis. This formate arises by the reduction of CO2 with hydrogen; this was demonstrated by incorporating 13C into the formate when M. jannaschii cell extracts were incubated with H13CO3- and hydrogen gas. The presence of this signature gene in all of the Archaea indicates the presence of a purine biosynthetic pathway proceeding in the absence of folate coenzymes.
Adenosine Triphosphate↗
The adenylosuccinate synthetase from the hyperthermophilic archaeon Pyrococcus species displays unusual structural features.
The first example of a hyperthermophilic adenylosuccinate synthetase is reported, which is an enzyme that must maintain its folded structure at temperatures as high as 102 degrees C. The amino acid sequence of this key enzyme has been determined after cloning and sequencing the purA-like gene from the archaeal Pyrococcus sp. strain ST700. The corresponding protein displays two unexpected features: (1) it is 21% shorter than the homologous mesophilic enzymes and this shortening corresponds to the loss of two alpha-helices and three beta-strands present in the Escherichia coli enzyme; (2) surprisingly, the archaeal adenylosuccinate synthetase has a significant number of substitutions in residues that are conserved in all other homologous enzymes from bacteria to man. In E. coli, the conserved residues have been described as essential for catalytic activity and/or for maintaining the folded structure of the homodimer. Despite these drastic differences, the purA-like archaeal gene seems to be normally expressed and its product functions in vivo in bacteria, since it complemented an E. coli purA auxotroph. The archaeal adenylosuccinate synthetase appears to be a good example of a bona fide orthologous protein. Reconstruction of phylogenetic trees showed that the archaeal gene is equally distantly related to both eukaryotes and bacteria, independently of the numerous substitutions observed at critical positions.
Adenylosuccinate Synthase↗
Cell-free transcription of the nifH1 gene of Methanococcus thermolithotrophicus indicates that promoters of archaeal nif genes share basic features with the methanogen consensus promoter.
The nifH1 gene of Methanococcus thermolithotrophicus, which encodes the putative dinitrogenase reductase of an archaeon, was accurately transcribed in a homologous cell-free transcription system. Extracts of cells grown with N2 or ammonia as nitrogen source initiated transcription at the nifH1 promoter with similar efficiencies. We confirmed that cells grown under non-N2-fixing conditions do not contain significant amounts of nifH1-specific mRNA. The levels of cell-free transcription initiation at the nifH1 promoter were similar to those observed at a tRNA promoter. The DNA sequence from -40 to +5 relative to the initiator nucleotide of nifH1 mRNA contained all the information required for promoter activity. A mutational analysis of this section of DNA demonstrated that a TATA box at -25 and the TTGT motif (initiator element) at the transcription start site are essential for cell-free transcription. These elements are similar to the structural determinants of a known tRNA promoter of Methanococcus. Mutation of a sequence, showing homology to the bacterial NifA site, which overlaps the transcription start site, did not affect promoter activity. Hence, cell-free transcription of the Methanococcus nifH1 gene is independent of upstream activator elements and does not require alternate cis-acting sequences that differ from the methanogen consensus promoter. These findings suggest that the activation of nif promoters is brought about by fundamentally different mechanisms in Archaea and bacteria.
Ammonia↗
Genomes in flux: the evolution of archaeal and proteobacterial gene content.
In the course of evolution, genomes are shaped by processes like gene loss, gene duplication, horizontal gene transfer, and gene genesis (the de novo origin of genes). Here we reconstruct the gene content of ancestral Archaea and Proteobacteria and quantify the processes connecting them to their present day representatives based on the distribution of genes in completely sequenced genomes. We estimate that the ancestor of the Proteobacteria contained around 2500 genes, and the ancestor of the Archaea around 2050 genes. Although it is necessary to invoke horizontal gene transfer to explain the content of present day genomes, gene loss, gene genesis, and simple vertical inheritance are quantitatively the most dominant processes in shaping the genome. Together they result in a turnover of gene content such that even the lineage leading from the ancestor of the Proteobacteria to the relatively large genome of Escherichia coli has lost at least 950 genes. Gene loss, unlike the other processes, correlates fairly well with time. This clock-like behavior suggests that gene loss is under negative selection, while the processes that add genes are under positive selection.
Amino Acid Substitution↗
Phylogenetic analysis of bacterial and archaeal arsC gene sequences suggests an ancient, common origin for arsenate reductase.
BACKGROUND: The ars gene system provides arsenic resistance for a variety of microorganisms and can be chromosomal or plasmid-borne. The arsC gene, which codes for an arsenate reductase is essential for arsenate resistance and transforms arsenate into arsenite, which is extruded from the cell. A survey of GenBank shows that arsC appears to be phylogenetically widespread both in organisms with known arsenic resistance and those organisms that have been sequenced as part of whole genome projects. RESULTS: Phylogenetic analysis of aligned arsC sequences shows broad similarities to the established 16S rRNA phylogeny, with separation of bacterial, archaeal, and subsequently eukaryotic arsC genes. However, inconsistencies between arsC and 16S rRNA are apparent for some taxa. Cyanobacteria and some of the gamma-Proteobacteria appear to possess arsC genes that are similar to those of Low GC Gram-positive Bacteria, and other isolated taxa possess arsC genes that would not be expected based on known evolutionary relationships. There is no clear separation of plasmid-borne and chromosomal arsC genes, although a number of the Enterobacteriales (gamma-Proteobacteria) possess similar plasmid-encoded arsC sequences. CONCLUSION: The overall phylogeny of the arsenate reductases suggests a single, early origin of the arsC gene and subsequent sequence divergence to give the distinct arsC classes that exist today. Discrepancies between 16S rRNA and arsC phylogenies support the role of horizontal gene transfer (HGT) in the evolution of arsenate reductases, with a number of instances of HGT early in bacterial arsC evolution. Plasmid-borne arsC genes are not monophyletic suggesting multiple cases of chromosomal-plasmid exchange and subsequent HGT. Overall, arsC phylogeny is complex and is likely the result of a number of evolutionary mechanisms.
Adenosine Triphosphatases↗
Incidence of novel and potentially archaeal nitrogenase genes in the deep Northeast Pacific Ocean.
Archaea have been detected throughout the oceanic water column and are quantitatively important members of picoplankton in the deep ocean. Two common groups, group I Crenarchaeota and group II Euryarchaeota, are consistently detected in warm hydrothermal fluid and are assumed to have been drawn into the subseafloor, mixed with hydrothermal fluid and then expelled. However, because they remain resistant to cultivation, very little is known about their physiology. Here we show that cold deep-seawater from the axial valley of Endeavour Segment on the Juan de Fuca Ridge contains not only groups I and II archaea as expected, but also unique potentially archaeal nitrogenase (nifH) genes, which are required for nitrogen fixation. These nifH genes are phylogenetically distinct and have dissimilar G+C content compared with those of hydrothermal vent archaea, suggesting that they belong to non-thermophilic deep-sea archaea. Furthermore, this sample did not contain mcrA genes, which are present in methanogens, the only known archaeal nitrogen fixers. These nifH genes were not detected in upper water column samples, or in a deep-seawater sample 100 km away from the spreading axis of the Juan de Fuca Ridge. We propose that these unique nifH genes may be localized to archaea that circulate through the nitrogen-poor subseafloor at the mid-ocean ridge as part of their life cycle.
Archaea↗
Gene capture in archaeal chromosomes.
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Chromosomes, Archaeal↗
Comprehensive comparison between locations of orthologous genes on archaeal and bacterial genomes.
MOTIVATION: Following an extensive search for orthologous genes between the complete genomes from archaea and bacteria, the spatial association of the orthologs has been investigated in terms of synteny, the conservation of the order of neighboring genes. However, the relationships between the relative locations of remote orthologs over entire genomes have not been shown. RESULTS: Comprehensive comparisons between the locations of orthologs on nineteen archaeal and bacterial genomes are presented by the location to location correspondence based on the gene-location distance. When the two genomes are rotated such that a pair of orthologs with the shortest distance is set in the same angle, a statistically significant number of orthologs maintain their relative locations between the genomes. Even by the short distances at the 5% significance level, the rotations are restricted within a narrow range, suggesting an intrinsic angle for realizing similar locations between the orthologs in each genome pair. Furthermore, the rotations in the restricted range agree with the replication origin and terminus sites for the analyzed genomes where such sites are known. The relationship between location-maintained orthologs and gene function is also discussed.
Chromosome Mapping↗
Updating carbamoylphosphate synthase (CPS) phylogenies: occurrence and phylogenetic identity of archaeal CPS genes.
Among Bacteria the carA and carB genes encoding the small (CarA) and large (CarB) subunits of carbamoylphosphate synthase (CPS) have been lost in certain symbionts (Haemophylus influenzae) and in most obligate intracellular parasites (Chlamydiae, Spirochaetes, Mycoplasmatales, Rickettsiae) having genome sizes in the 0.7- to 1.1-Mb range. Compared to Bacteria, Archaea exhibit a more varied pattern of CPS gene losses and an unusual propensity to incorporate CPS genes derived from both Bacteria and other Archaea. Schematically they fall into three groups. Group 1 taxa (the crenarchaeon Aeropyrum pernix and the euryarchaea Pyrococcus horikoshi and Pyrococcus abyssii) lack CPS genes altogether. Group 2 taxa (comprising Halobacteriales, Thermoplasmales, Methanococcales, Methanomicrobiales, Archaeoglobales) harbor CPS genes whose encoded CarB and CarA subunit proteins are ostensibly bacterial in origin; that is, they are intermixed with bacterial homologues on a phylogeny of concatenated CarA and CarB sequences and are not distinguishable from bacterial sequences after searching for domain-specific amino acid residue positions. Group 3 taxa (the crenarchaea Pyrobaculum aerophilum, Sulfolobus solfataricus, and Sulfolobus tokodaii and the euryarchaeon Pyrococcus furiosus) harbor CPS genes whose encoded proteins appear to be archaeal: consistent with an archaeal origin, the CarA and CarB sequences in this group possess both unique signatures and signatures affiliating them to Eukarya. Based on the topology of the clade comprising the four Group 3 taxa, we argue that CPS genes of P. furiosus (a euryarchaeon) and those of the crenarchaea P. aerophilum, S. solfataricus, and S. tokodaii are of a single type, resulting from the two genes being laterally transferred from a crenarchaeon to P. furiosus.
Amino Acid Motifs↗
Evidence for lateral gene transfer between Archaea and bacteria from genome sequence of Thermotoga maritima.
The 1,860,725-base-pair genome of Thermotoga maritima MSB8 contains 1,877 predicted coding regions, 1,014 (54%) of which have functional assignments and 863 (46%) of which are of unknown function. Genome analysis reveals numerous pathways involved in degradation of sugars and plant polysaccharides, and 108 genes that have orthologues only in the genomes of other thermophilic Eubacteria and Archaea. Of the Eubacteria sequenced to date, T. maritima has the highest percentage (24%) of genes that are most similar to archaeal genes. Eighty-one archaeal-like genes are clustered in 15 regions of the T. maritima genome that range in size from 4 to 20 kilobases. Conservation of gene order between T. maritima and Archaea in many of the clustered regions suggests that lateral gene transfer may have occurred between thermophilic Eubacteria and Archaea.
Archaea↗