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

Heat-stable enzymes from extremely thermophilic and hyperthermophilic microorganisms

Only in the last decade have microorganisms been discovered which grow near or above 100°C. The enzymes that are formed by these extremely thermophilic (growth temperature 65 to 85°C) and hyperthermophilic (growth temperature 85 to 110°C) microorganisms are of great interest. This review covers the extracellular and intracellular enzymes of these exotic microorganisms that have recently been described. Polymer-hydrolysing enzymes, such as amylolytic, cellulolytic, hemicellulolytic and proteolytic enzymes, will be discussed. In addition, the properties of the intracellular enzymes involved in carbohydrate and amino-acid metabolism and DNA-binding and chaperones and chaperone-like proteins from hyperthermophiles are described. Due to the unusual properties of these heat-stable enzymes, they are expected to fill the gap between biological and chemical processes.

Cloning, expression and purification of Pwo polymerase from Pyrococcus woesei

BACKGROUND AND OBJECTIVES

Pyrococcus woesei is a hyperthermophilic archaea and produces a heat stable polymerase (Pwo polymerase) that has proofreading activity.

MATERIALS AND METHODS

In this study, this microorganism was cultured, its DNA was extracted and the pwo gene polymerase was cloned, expressed and purified. The DNA sequence of the cloned gene was verified by sequencing. The pwo polymerase gene consists of 2,328 bps (775 amino acids with about 90 kD molecular weight). Cloning was done by GATEWAY™ Cloning System and for purification of recombinant protein; His6x-Tag was added to the C-terminus of the recombinant protein.

RESULTS AND CONCLUSION

We could purify Pwo polymerase enzyme by Ni-NTA resin. PCR assay showed that Pwo polymerase activity is comparable to a commercial Pfu polymerase activity.

Metabolic and evolutionary relationships among Pyrococcus Species: genetic exchange within a hydrothermal vent environment

Pyrococcus furiosus and Pyrococcus woesei grow optimally at temperatures near 100 degrees C and were isolated from the same shallow marine volcanic vent system. Hybridization of genomic DNA from P. woesei to a DNA microarray containing all 2,065 open reading frames (ORFs) annotated in the P. furiosus genome, in combination with PCR analysis, indicated that homologs of 105 ORFs present in P. furiosus are absent from the uncharacterized genome of P. woesei. Pulsed-field electrophoresis indicated that the sizes of the two genomes are comparable, and the results were consistent with the hypothesis that P. woesei lacks the 105 ORFs found in P. furiosus. The missing ORFs are present in P. furiosus mainly in clusters. These clusters include one cluster (Mal I, PF1737 to PF1751) involved in maltose metabolism and another cluster (PF0691 to PF0695) whose products are thought to remove toxic reactive nitrogen species. Accordingly, it was found that P. woesei, in contrast to P. furiosus, is unable to utilize maltose as a carbon source for growth, and the growth of P. woesei on starch was inhibited by addition of a nitric oxide generator. In P. furiosus the ORF clusters not present in P. woesei are bracketed by or are in the vicinity of insertion sequences or long clusters of tandem repeats (LCTRs). While the role of LCTRs in lateral gene transfer is not known, the Mal I cluster in P. furiosus is a composite transposon that undergoes replicative transposition. The same locus in P. woesei lacks any evidence of insertion activity, indicating that P. woesei is a sister or even the parent of P. furiosus. P. woesei may have acquired by lateral gene transfer more than 100 ORFs from other organisms living in the same thermophilic environment to produce the type strain of P. furiosus.

Nitrate reduction and the nitrogen cycle in archaea

The nitrogen cycle (N-cycle) in the biosphere, mainly driven by prokaryotes, involves different reductive or oxidative reactions used either for assimilatory purposes or in respiratory processes for energy conservation. As the N-cycle has important agricultural and environmental implications, bacterial nitrogen metabolism has become a major research topic in recent years. Archaea are able to perform different reductive pathways of the N-cycle, including both assimilatory processes, such as nitrate assimilation and N(2) fixation, and dissimilatory reactions, such as nitrate respiration and denitrification. However, nitrogen metabolism is much less known in archaea than in bacteria. The availability of the complete genome sequences of several members of the eury- and crenarchaeota has enabled new approaches to the understanding of archaeal physiology and biochemistry, including metabolic reactions involving nitrogen compounds. Comparative studies reveal that significant differences exist in the structure and regulation of some enzymes involved in nitrogen metabolism in archaea, giving rise to important conclusions and new perspectives regarding the evolution, function and physiological relevance of the different N-cycle processes. This review discusses the advances that have been made in understanding nitrate reduction and other aspects of the inorganic nitrogen metabolism in archaea.

The consistent phylogenetic signal in genome trees revealed by reducing the impact of noise

Phylogenetic trees based on gene repertoires are remarkably similar to the current consensus of life history. Yet it has been argued that shared gene content is unreliable for phylogenetic reconstruction because of convergence in gene content due to horizontal gene transfer and parallel gene loss. Here we test this argument, by filtering out as noise those orthologous groups that have an inconsistent phylogenetic distribution, using two independent methods. The resulting phylogenies do indeed contain small but significant improvements. More importantly, we find that the majority of orthologous groups contain some phylogenetic signal and that the resulting phylogeny is the only detectable signal present in the gene distribution across genomes. Horizontal gene transfer or parallel gene loss does not cause systematic biases in the gene content tree.

A phylogenomic approach to bacterial phylogeny: evidence of a core of genes sharing a common history

It has been claimed that complete genome sequences would clarify phylogenetic relationships between organisms, but up to now, no satisfying approach has been proposed to use efficiently these data. For instance, if the coding of presence or absence of genes in complete genomes gives interesting results, it does not take into account the phylogenetic information contained in sequences and ignores hidden paralogies by using a BLAST reciprocal best hit definition of orthology. In addition, concatenation of sequences of different genes as well as building of consensus trees only consider the few genes that are shared among all organisms. Here we present an attempt to use a supertree method to build the phylogenetic tree of 45 organisms, with special focus on bacterial phylogeny. This led us to perform a phylogenetic study of congruence of tree topologies, which allows the identification of a core of genes supporting similar species phylogeny. We then used this core of genes to infer a tree. This phylogeny presents several differences with the rRNA phylogeny, notably for the position of hyperthermophilic bacteria.

Genetics of nitrogen regulation in Methanococcus maripaludis

We have used genetic methods in Methanococcus maripaludis to study nitrogen metabolism and its regulation. We present evidence for a "nitrogen regulon" in Methanococcus and Methanobacterium species containing genes of nitrogen metabolism that are regulated coordinately at the transcriptional level via a common repressor binding site sequence, or operator. The implied mechanism for regulation resembles the general bacterial paradigm for repression, but contrasts with well-known mechanisms of nitrogen regulation in bacteria, which occur by activation. Genes in the nitrogen regulons include those for nitrogen fixation, glutamine synthetase, (methyl)ammonia transport, the regulatory protein GlnB, and ammonia-dependent NAD synthetase, as well as a gene of unknown function. We also studied the function of two novel GlnB homologues that are encoded within the nif gene cluster of diazotrophic methanogens. The phenotype resulting from a glnB null mutation in M. maripaludis provides direct evidence that glnB-like genes are involved in "ammonia switch-off," the post-transcriptional inhibition of nitrogen fixation upon addition of ammonia. Finally, we show that the gene nifX is not required for nitrogen fixation, in agreement with findings in several bacteria. These studies illustrate the utility of genetic methods in M. maripaludis and show the enhanced perspective that studies in the Archaea can bring to known biological systems.

Discontinuous occurrence of the hsp70 (dnaK) gene among Archaea and sequence features of HSP70 suggest a novel outlook on phylogenies inferred from this protein

Occurrence of the hsp70 (dnaK) gene was investigated in various members of the domain Archaea comprising both euryarchaeotes and crenarchaeotes and in the hyperthermophilic bacteria Aquifex pyrophilus and Thermotoga maritima representing the deepest offshoots in phylogenetic trees of bacterial 16S rRNA sequences. The gene was not detected in 8 of 10 archaea examined but was found in A. pyrophilus and T. maritima, from which it was cloned and sequenced. Comparative analyses of the HSP70 amino acid sequences encoded in these genes, and others in the databases, showed that (i) in accordance with the vicinities seen in rRNA-based trees, the proteins from A. pyrophilus and T. maritima form a thermophilic cluster with that from the green nonsulfur bacterium Thermomicrobium roseum and are unrelated to their counterparts from gram-positive bacteria, proteobacteria/mitochondria, chlamydiae/spirochetes, deinococci, and cyanobacteria/chloroplasts; (ii) the T. maritima HSP70 clusters with the homologues from the archaea Methanobacterium thermoautotrophicum and Thermoplasma acidophilum, in contrast to the postulated unique kinship between archaea and gram-positive bacteria; and (iii) there are exceptions to the reported association between an insert in HSP70 and gram negativity, or vice versa, absence of insert and gram positivity. Notably, the HSP70 from T. maritima lacks the insert, although T. maritima is phylogenetically unrelated to the gram-positive bacteria. These results, along with the absence of hsp70 (dnaK) in various archaea and its presence in others, suggest that (i) different taxa retained either one or the other of two hsp70 (dnaK) versions (with or without insert), regardless of phylogenetic position; and (ii) archaea are aboriginally devoid of hsp70 (dnaK), and those that have it must have received it from phylogenetically diverse bacteria via lateral gene transfer events that did not involve replacement of an endogenous hsp70 (dnaK) gene.

Protein phylogenies and signature sequences: A reappraisal of evolutionary relationships among archaebacteria, eubacteria, and eukaryotes

The presence of shared conserved insertion or deletions (indels) in protein sequences is a special type of signature sequence that shows considerable promise for phylogenetic inference. An alternative model of microbial evolution based on the use of indels of conserved proteins and the morphological features of prokaryotic organisms is proposed. In this model, extant archaebacteria and gram-positive bacteria, which have a simple, single-layered cell wall structure, are termed monoderm prokaryotes. They are believed to be descended from the most primitive organisms. Evidence from indels supports the view that the archaebacteria probably evolved from gram-positive bacteria, and I suggest that this evolution occurred in response to antibiotic selection pressures. Evidence is presented that diderm prokaryotes (i.e., gram-negative bacteria), which have a bilayered cell wall, are derived from monoderm prokaryotes. Signature sequences in different proteins provide a means to define a number of different taxa within prokaryotes (namely, low G+C and high G+C gram-positive, Deinococcus-Thermus, cyanobacteria, chlamydia-cytophaga related, and two different groups of Proteobacteria) and to indicate how they evolved from a common ancestor. Based on phylogenetic information from indels in different protein sequences, it is hypothesized that all eukaryotes, including amitochondriate and aplastidic organisms, received major gene contributions from both an archaebacterium and a gram-negative eubacterium. In this model, the ancestral eukaryotic cell is a chimera that resulted from a unique fusion event between the two separate groups of prokaryotes followed by integration of their genomes.

The hyperthermophilic bacterium Thermotoga maritima has two different classes of family C DNA polymerases: evolutionary implications

Bacterial DNA polymerase III (family C DNA polymerase), the principal chromosomal replicative enzyme, is known to occur in at least three distinct forms which have provisionally been classified as class I ( Escherichia coli DNA pol C-type), class II ( Bacillus subtilis DNA pol C-type) and class III (cyanobacteria DNA pol C-type). We have identified two family C DNA polymerase sequences in the hyperthermophilic bacterium Thermotoga maritima. One DNA polymerase consisting of 842 amino acid residues and having a molecular weight of 97 213 belongs to class I. The other one, consisting of 1367 amino acid residues and having a molecular weight of 155 361, is a member of class II. Comparative sequence analyses suggest that the class II DNA polymerase is the principal DNA replicative enzyme of the microbe and that the class I DNA polymerase may be functionally inactive. A phylogenetic analysis using the class II enzyme indicates that T.maritima is closely related to the low G+C Gram-positive bacteria, in particular to Clostridium acetobutylicum, and mycoplasmas. These results are in conflict with 16S rRNA-based phylogenies, which placed T.maritima as one of the deepest branches of the bacterial tree.

Life's third domain (Archaea): an established fact or an endangered paradigm?

The three-domain proposal of Woese et al. (Proc. Natl. Acad. Sci. USA 87, 4576 (1990)) divides all living organisms into three primary groups or domains named Archaea (or archaebacteria), Bacteria (or eubacteria), and Eucarya (or eukaryotes), with Eucarya being relatives (or descendants) of Archaea. Although this proposal is currently widely accepted, sequence features and phylogenies derived from many highly conserved proteins are inconsistent with it and point to a close and specific relationship between archaebacteria and gram-positive bacteria, whereas gram-negative bacteria are indicated to be phylogenetically distinct. A closer relationship of archaebacteria to gram-positive bacteria in comparison to gram-negative bacteria is generally seen for the majority of the available gene/protein sequences. To account for these results, and the fact that both archaebacteria and gram-positive bacteria are prokaryotes surrounded by a single cell membrane, I propose that the primary division within prokaryotes is between Monoderm prokaryotes (surrounded by a single membrane) and Diderm prokaryotes (i.e., all true gram-negative bacteria containing both an inner cytoplasmic membrane and an outer membrane). This proposal is consistent with both cell morphology and signature sequences in different proteins. Protein phylogenies and signature sequences also show that all eukaryotic cells have received significant gene contributions from both an archaebacterium and a gram- negative eubacterium. Thus, the hypothesis that archaebacteria and eukaryotes shared a common ancestor exclusive of eubacteria, or that the ancestral eukaryotic cell directly descended from an archaea, is erroneous. These results call into question the validity of the currently popular three-domain proposal and the assignment of a domain status to archaebacteria. A new classifica- tion of organisms consistent with phenotype and macromolecular sequence data is proposed.

Thermozymes

Enzymes synthesized by thermophiles (organisms with optimal growth temperatures > 60 degrees C) and hyperthermophiles (optimal growth temperatures > 80 degrees C) are typically thermostable (resistant to irreversible inactivation at high temperatures) and thermophilic (optimally active at high temperatures, i.e., > 60 degrees C). These enzymes, called thermozymes, share catalytic mechanisms with their mesophilic counterparts. When cloned and expressed in mesophilic hosts, thermozymes usually retain their thermal properties, suggesting that these properties are genetically encoded. Sequence alignments, amino acid content comparisons, and crystal structure comparisons indicate that thermozymes are, indeed, very similar to mesophilic enzymes. No obvious sequence or structural features account for enzyme thermostability and thermophilicity. Thermostability and thermophilicity molecular mechanisms are varied, differing from enzyme to enzyme. Thermostability and thermophilicity are usually caused by the accumulation of numerous subtle sequence differences. This review concentrates on the mechanisms involved in enzyme thermostability and thermophilicity. Their relationships with protein rigidity and flexibility and with protein folding and unfolding are discussed. Intrinsic stabilizing forces (e.g., salt bridges, hydrogen bonds, hydrophobic interactions) and extrinsic stabilizing factors are examined. Finally, thermozymes' potential as catalysts for industrial processes and specialty uses are discussed, and lines of development (through new applications, and protein engineering) are also proposed.

What are archaebacteria: life's third domain or monoderm prokaryotes related to gram-positive bacteria? A new proposal for the classification of prokaryotic organisms

The evolutionary relationship within prokaryotes is examined based on signature sequences (defined as conserved inserts or deletions shared by specific taxa) and phylogenies derived from different proteins. Archaebacteria are indicated as being monophyletic by a number of proteins related to the information transfer processes. In contrast, for several other highly conserved proteins, common signature sequences are present in archaebacteria and Gram-positive bacteria, whereas Gram-negative bacteria are indicated as being distinct. For these proteins, archaebacteria do not form a phylogenetically distinct clade but show polyphyletic branching within Gram-positive bacteria. A closer relationship of archaebacteria to Gram-positive bacteria in comparison with Gram-negative bacteria is generally seen for the majority of the available gene/ protein sequences. To account for these results and the fact that both archaebacteria and Gram-positive bacteria are prokaryotes surrounded by a single cell membrane, I propose that the primary division within prokaryotes is between monoderm prokaryotes (surrounded by a single membrane) and diderm prokaryotes (i.e. all true Gram-negative bacteria containing both an inner cytoplasmic membrane and an outer membrane). This proposal is consistent with both cell morphology and signature sequences in different proteins. The monophyletic nature of archaebacteria for some genes, and their polyphyletic branching within Gram-positive bacteria as suggested by others, is critically examined, and several explanations, including derivation of archaebacteria from Gram-positive bacteria in response to antibiotic selection pressure, are proposed. Signature sequences in proteins also indicate that the low-G+C Gram-positive bacteria are phylogenetically distinct from the high-G+C Gram-positive group and that the diderm prokaryotes (i.e. Gram-negative bacteria) appear to have evolved from the latter group. Protein phylogenies and signature sequences also show that all eukaryotic cells have received significant gene contributions from both an archaebacterium and a Gram-negative eubacterium. Thus, the hypothesis that archaebacteria and eukaryotes shared a common ancestor exclusive of eubacteria is not supported. These observations provide evidence for an alternate view of the evolutionary relationship among living organisms that is different from the currently popular three-domain proposal.

A dissimilatory sirohaem-sulfite-reductase-type protein from the hyperthermophilic archaeon Pyrobaculum islandicum

A sulfite-reductase-type protein was purified from the hyperthermophilic crenarchaeote Pyrobaculum islandicum grown chemoorganoheterotrophically with thiosulfate as terminal electron acceptor. In common with dissimilatory sulfite reductases the protein has an alpha 2 beta 2 structure and contains high-spin sirohaem, non-haem iron and acid-labile sulfide. The oxidized protein exhibits absorption maxima at 280, 392, 578 and 710 nm with shoulders at 430 and 610 nm. The isoelectric point of pH 8.4 sets the protein apart from all dissimilatory sulfite reductases characterized thus far. The genes for the alpha- and beta-subunits (dsrA and dsrB) are contiguous in the order dsrAdsrB and most probably comprise an operon with the directly following dsrG and dsrC genes. dsrG and dsrC encode products which are homologous to eukaryotic glutathione S-transferases and the proposed gamma-subunit of Desulfovibrio vulgaris sulfite reductase, respectively. dsrA and dsrB encode 44.2 kDa and 41.2 kDa peptides which show significant similarity to the two homologous subunits DsrA and DsrB of dissimilatory sulfite reductases. Phylogenetic analyses indicate a common protogenotic origin of the P. islandicum protein and the dissimilatory sulfite reductases from sulfate-reducing and sulfide-oxidizing prokaryotes. However, the protein from P. islandicum and the sulfite reductases from sulfate-reducers and from sulfur-oxidizers most probably evolved into three independent lineages prior to divergence of archaea and bacteria.

Archaea and the prokaryote-to-eukaryote transition

Since the late 1970s, determining the phylogenetic relationships among the contemporary domains of life, the Archaea (archaebacteria), Bacteria (eubacteria), and Eucarya (eukaryotes), has been central to the study of early cellular evolution. The two salient issues surrounding the universal tree of life are whether all three domains are monophyletic (i.e., all equivalent in taxanomic rank) and where the root of the universal tree lies. Evaluation of the status of the Archaea has become key to answering these questions. This review considers our cumulative knowledge about the Archaea in relationship to the Bacteria and Eucarya. Particular attention is paid to the recent use of molecular phylogenetic approaches to reconstructing the tree of life. In this regard, the phylogenetic analyses of more than 60 proteins are reviewed and presented in the context of their participation in major biochemical pathways. Although many gene trees are incongruent, the majority do suggest a sisterhood between Archaea and Eucarya. Altering this general pattern of gene evolution are two kinds of potential interdomain gene transferrals. One horizontal gene exchange might have involved the gram-positive Bacteria and the Archaea, while the other might have occurred between proteobacteria and eukaryotes and might have been mediated by endosymbiosis.

The presence of a dnaK (HSP70) multigene family in members of the orders Planctomycetales and Verrucomicrobiales

Sequences of the dnaK gene, coding for the 70-kDa heat shock protein (HSP70), were determined for six members of the order Planctomycetales, including representatives of three genera, and for the only cultivated member of the order Verrucomicrobiales, Verrucomicrobium spinosum. A fragment of the dnaK gene was amplified from these strains by PCR with oligonucleotide primers targeting regions of the dnaK gene that are conserved at the amino acid level, and the resulting PCR products were cloned into a plasmid vector. Sequence analysis of the cloned dnaK fragments revealed the presence of two different types of dnaK sequence in one of the planctomycete strains, Planctomyces maris, and in V. spinosum. Only one type of dnaK sequence was found for each of the remaining strains. Phylogenetic analysis of the partial sequence data suggested that the majority of planctomycete strains, including one of the Planctomyces maris sequences, form a coherent phylogenetic group branching adjacent to other main lines of descent within the domain Bacteria, as has been shown previously by 16S rRNA sequence analysis. One of the two V. spinosum dnaK sequences also appears to constitute a separate lineage within the gram-negative bacteria. Each of the remaining sequences from P. maris and V. spinosum, together with the single sequence obtained from Planctomyces limnophilus, appeared to be unrelated to the other planctomycete sequences and to occupy a position distant from that of other gram-negative bacteria. The phylogenetic diversity of dnaK sequences exhibited by P. maris and V. spinosum was comparable to that found in Synechococcus sp. strain PCC7942 and Escherichia coli, the only other prokaryotes for which a dnaK multigene family has been demonstrated.

Cloning, sequencing, and expression of the gene encoding extracellular alpha-amylase from Pyrococcus furiosus and biochemical characterization of the recombinant enzyme

The gene encoding the hyperthermophilic extracellular alpha-amylase from Pyrococcus furiosus was cloned by activity screening in Escherichia coli. The gene encoded a single 460-residue polypeptide chain. The polypeptide contained a 26-residue signal peptide, indicating that this Pyrococcus alpha-amylase was an extracellular enzyme. Unlike the P. furiosus intracellular alpha-amylase, this extracellular enzyme showed 45 to 56% similarity and 20 to 35% identity to other amylolytic enzymes of the alpha-amylase family and contained the four consensus regions characteristic of that enzyme family. The recombinant protein was a homodimer with a molecular weight of 100,000, as estimated by gel filtration. Both the dimer and monomer retained starch-degrading activity after extensive denaturation and migration on sodium dodecyl sulfate-polyacrylamide gels. The P. furiosus alpha-amylase was a liquefying enzyme with a specific activity of 3,900 U mg-1 at 98 degrees C. It was optimally active at 100 degrees C and pH 5.5 to 6.0 and did not require Ca2+ for activity or thermostability. With a half-life of 13 h at 98 degrees C, the P. furiosus enzyme was significantly more thermostable than the commercially available Bacillus licheniformis alpha-amylase (Taka-therm).

Cloning, sequencing, and expression of the gene encoding amylopullulanase from Pyrococcus furiosus and biochemical characterization of the recombinant enzyme

The gene encoding the Pyrococcus furiosus hyperthermophilic amylopullulanase (APU) was cloned, sequenced, and expressed in Escherichia coli. The gene encoded a single 827-residue polypeptide with a 26-residue signal peptide. The protein sequence had very low homology (17 to 21% identity) with other APUs and enzymes of the alpha-amylase family. In particular, none of the consensus regions present in the alpha-amylase family could be identified. P. furiosus APU showed similarity to three proteins, including the P. furiosus intracellular alpha-amylase and Dictyoglomus thermophilum alpha-amylase A. The mature protein had a molecular weight of 89,000. The recombinant P. furiosus APU remained folded after denaturation at temperatures of < or = 70 degrees C and showed an apparent molecular weight of 50,000 in sodium dodecyl sulfate-polyacrylamide gel electrophoresis. Denaturating temperatures of above 100 degrees C were required for complete unfolding. The enzyme was extremely thermostable, with an optimal activity at 105 degrees C and pH 5.5. Ca2+ increased the enzyme activity, thermostability, and substrate affinity. The enzyme was highly resistant to chemical denaturing reagents, and its activity increased up to twofold in the presence of surfactants.

The sequences of heat shock protein 40 (DnaJ) homologs provide evidence for a close evolutionary relationship between the Deinococcus-thermus group and cyanobacteria

The genes encoding for heat shock protein 40 (Hsp40 or DnaJ) homologs were cloned and sequenced from the archaebacterium Halobacterium cutirubrum and the eubacterium Deinococcus proteolyticus to add to sequences from the gene banks. These genes were identified downstream of the Hsp70 (or DnaK) genes in genomic fragments spanning this region and, as in other prokaryotic species, Hsp70-Hsp40 genes are likely part of the same operon. The Hsp40 homolog from D. proteolyticus was found to be lacking a central 204 base pair region present in H. cutirubrum that encodes for the four cysteine-rich domains of the repeat consensus sequence CxxCxGxG (where x is any amino acid), present in most Hsp40 homologs. The available sequences from various archaebacteria, eubacteria, and eukaryotes show that the same deletion is also present in the homologs from Thermus aquaticus and two cyanobacteria, but in no other species tested. This unique deletion and the clustering of homologs from the Deinococcus-Thermus group and cyanobacterial species in the Hsp40 phylogenetic trees suggest a close evolutionary relationship between these groups as was also shown recently for Hsp70 sequences (R.S. Gupta et al., J Bacteriol 179:345-357, 1997). Sequence comparisons indicate that the Hsp40 homologs are not as conserved as the Hsp70 sequences. Phylogenetic analysis provides no reliable information concerning evolutionary relationship between prokaryotes and eukaryotes and their usefulness in this regard is limited. However, in phylogenetic trees based on Hsp40 sequences, the two archaebacterial homologs showed a polyphyletic branching within Gram-positive bacteria, similar to that seen with Hsp70 sequences.

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.

Characterization of recombinant glutamine synthetase from the hyperthermophilic archaeon Pyrococcus sp. strain KOD1

The glnA gene encoding glutamine synthetase was cloned from the hyperthermophilic archaeon Pyrococcus sp. strain KOD1, and its nucleotide sequence was determined. The glnA gene was expressed in Escherichia coli ME8459 (glnA mutant strain), and the protein was purified to homogeneity and shown to be functional in a dodecameric from (637,000 Da), exhibiting both transferase and synthetase activities. However, kinetic studies indicated that the enzyme possessed low biosynthetic activity, suggesting that the reaction was biased towards glutamate production. The optimum temperature for both activities was 60 degrees C, which was lower than the optimal growth temperature of KOD1. Recombinant KOD1 GlnA exhibited different optimum pHs depending on the reaction employed (pH 7.8 for the synthetase reaction and pH 7.2 for the transferase reaction). Of the various nucleoside triphosphates tested, GTP as well as ATP was involved in the synthetase reaction.

Distribution, diversity and evolution of the bacterial mercury resistance (mer) operon

Mercury and its compounds are distributed widely across the earth. Many of the chemical forms of mercury are toxic to all living organisms. However, bacteria have evolved mechanisms of resistance to several of these different chemical forms, and play a major role in the global cycling of mercury in the natural environment. Five mechanisms of resistance to mercury compounds have been identified, of which resistance to inorganic mercury (HgR) is the best understood, both in terms of the mechanisms of resistance to mercury and of resistance to heavy metals in general. Resistance to inorganic mercury is encoded by the genes of the mer operon, and can be located on transposons, plasmids and the bacterial chromosome. Such systems have a worldwide geographical distribution, and furthermore, are found across a wide range of both Gram-negative and Gram-positive bacteria from both natural and clinical environments. The presence of mer genes in bacteria from sediment cores suggest that mer is an ancient system. Analysis of DNA sequences from mer operons and genes has revealed genetic variation both in operon structure and between individual genes from different mer operons, whilst analysis of bacteria which are sensitive to inorganic mercury has identified a number of vestigial non-functional operons. It is hypothesised that mer, due to its ubiquity with respect to geographical location, environment and species range, is an ancient system, and that ancient bacteria carried genes conferring resistance to mercury in response to increased levels of mercury in natural environments, perhaps resulting from volcanic activity. Models for the evolution of both a basic mer operon and for the Tn21-related family of mer operons and transposons are suggested. The study of evolution in bacteria has recently become dominated by the generation of phylogenies based on 16S rRNA genes. However, it is important not to underestimate the roles of horizontal gene transfer and recombinational events in evolution. In this respect mer is a suitable system for evaluating phylogenetic methods which incorporate the effects of horizontal gene transfer. In addition, the mer operon provides a model system in the study of environmental microbiology which is useful both as an example of a genotype which is responsive to environmental pressures and as a generic tool for the development of new methodology for the analysis of bacterial communities in natural environments.

Sequencing of heat shock protein 70 (DnaK) homologs from Deinococcus proteolyticus and Thermomicrobium roseum and their integration in a protein-based phylogeny of prokaryotes

The 70-kDa heat shock protein (hsp70) sequences define one of the most conserved proteins known to date. The hsp70 genes from Deinococcus proteolyticus and Thermomicrobium roseum, which were chosen as representatives of two of the most deeply branching divisions in the 16S rRNA trees, were cloned and sequenced. hsp70 from both these species as well as Thermus aquaticus contained a large insert in the N-terminal quadrant, which has been observed before as a unique characteristic of gram-negative eubacteria and eukaryotes and is not found in any gram-positive bacteria or archaebacteria. Phylogenetic analysis of hsp70 sequences shows that all of the gram-negative eubacterial species examined to date (which includes members from the genera Deinococcus and Thermus, green nonsulfur bacteria, cyanobacteria, chlamydiae, spirochetes, and alpha-, beta-, and gamma-subdivisions of proteobacteria) form a monophyletic group (excluding eukaryotic homologs which are derived from this group via endosybitic means) strongly supported by the bootstrap scores. A closer affinity of the Deinococcus and Thermus species to the cyanobacteria than to the other available gram-negative sequences is also observed in the present work. In the hsp7O trees, D. proteolyticus and T. aquaticus were found to be the most deeply branching species within the gram-negative eubacteria. The hsp70 homologs from gram-positive bacteria branched separately from gram-negative bacteria and exhibited a closer relationship to and shared sequence signatures with the archaebacteria. A polyphyletic branching of archaebacteria within gram-positive bacteria is strongly favored by different phylogenetic methods. These observations differ from the rRNA-based phylogenies where both gram-negative and gram-positive species are indicated to be polyphyletic. While it remains unclear whether parts of the genome may have variant evolutionary histories, these results call into question the general validity of the currently favored three-domain dogma.

Bacterial diversity based on type II DNA topoisomerase genes

Type II DNA topoisomerases are essential and ubiquitous DNA metabolic enzymes that alter DNA topology. Eubacteria have two indispensable type II DNA topoisomerases, DNA gyrase encoded by gyrB and gyrA and topoisomerase IV encoded by parE and parC. These genes belong to a single family whose members span both eukaryotes and prokaryotes. The highly conserved motifs in these genes provide a rationale for the design of universal primers used in the polymerase chain reaction in order to systematically generate a data set suitable for bacterial diversity studies at the macro-diversity level, as well as at the micro-diversity level displaying individual species and isolates. This family of genes is the subject of intensive biochemical and genetic analyses, which provide an opportunity for comprehensive understanding of sequence conservation and variability and their relationship to function. These genes are ideally suited for microbial identification and biodiversity analyses.

Cloning, characterization and sequence comparison of the gene coding for IMP dehydrogenase from Pyrococcus furiosus

We have cloned and characterized the gene encoding inosine monophosphate dehydrogenase (IMPDH) from Pyrococcus furiosus (Pf), a hyperthermophillic archeon. Sequence analysis of the Pf gene indicated an open reading frame specifying a protein of 485 amino acids (aa) with a calculated M(r) of 52900. Canonical Archaea promoter elements, Box A and Box B, are located -49 and -17 nucleotides (nt), respectively, upstream of the putative start codon. The sequence of the putative active-site region conforms to the IMPDH signature motif and contains a putative active-site cysteine. Phylogenetic relationships derived by using all available IMPDH sequences are consistent with trees developed for other molecules; they do not precisely resolve the history of Pf IMPDH but indicate a close similarity to bacterial IMPDH proteins. The phylogenetic analysis indicates that a gene duplication occurred prior to the division between rodents and humans, accounting for the Type I and II isoforms identified in mice and humans.

Sequence, expression in Escherichia coli, and analysis of the gene encoding a novel intracellular protease (PfpI) from the hyperthermophilic archaeon Pyrococcus furiosus

A previously identified intracellular proteolytic activity in the hyperthermophilic archaeon Pyrococcus furiosus (I. I. Blumentals, A. S. Robinson, and R. M. Kelly, Appl. Environ. Microbiol. 56:1992-1998, 1990) was found to be a homomultimer consisting of 18.8-kDa subunits. Dissociation of this native P. furiosus protease I (PfpI) into a single subunit was seen by sodium dodecyl sulfate-polyacrylamide gel electrophoresis (SDS-PAGE) but only after trichloroacetic acid precipitation; heating to 95 degrees C in the presence of 2% SDS and 80 mM dithiothreitol did not dissociate the protein. The gene (pfpI) coding for this protease was located in genomic digests by Southern blotting with probes derived from the N-terminal amino acid sequence. pfpI was cloned, sequenced, and expressed in active form in Escherichia coli as a fusion protein with a histidine tag. The recombinant protease from E. coli showed maximum proteolytic activity at 95 degrees C, and its half-life was 19 min at this temperature. This level of stability was significantly below that previously reported for the enzyme purified by electroelution of a 66-kDa band from SDS-PAGE after extended incubation of cell extracts at 98 degrees C in 1% SDS (>30 h). The pfpI gene codes for a polypeptide of 166 amino acid residues lacking any conserved protease motifs; no protease activity was detected for the 18.8-kDa PfpI subunit (native or recombinant) by substrate gel assay. Although an immunological relationship of this protease to the eukaryotic proteasome has been seen previously, searches of the available databases identified only two similar amino acid sequences: an open reading frame of unknown function from Staphylococcus aureus NCTC 8325 (171 amino acid residues, 18.6 kDa, 41% identity) and an open reading frame also of unknown function in E. coli (172 amino acid residues, 18.8 kDa, 47% identity). Primer extension experiments with P. furiosus total RNA defined the 5' end of the transcript. There are only 10 nucleotides upstream of the start of translation; therefore, it is unlikely that there are any pre- or pro-regions associated with PfpI which could have been used for targeting or assembly of this protease. Although PfpI activity appears to be the dominant proteolytic activity in P. furiosus cell extracts, the physiological function of PfpI is unclear.

Sensitivity of ribosomes of the hyperthermophilic bacterium Aquifex pyrophilus to aminoglycoside antibiotics

A poly(U)-programmed cell-free system from the hyperthermophilic bacterium Aquifex pyrophilus has been developed, and the susceptibility of Aquifex ribosomes to the miscoding-inducing and inhibitory actions of all known classes of aminoglycoside antibiotics has been assayed at temperatures (75 to 80 degrees C) close to the physiological optimum for cell growth. Unlike Thermotoga maritima ribosomes, which are systematically refractory to all known classes of aminoglycoside compounds (P. Londei, S. Altamura, R. Huber, K. O. Stetter, and P. Cammarano, J. offteriol. 170-4353-4360, 1988), Aquifex ribosomes are susceptible to all of the aminoglycosides tested (disubstituted 2-deoxystreptamines, monosubstituted 2-deoxystreptamines, sand streptidine compounds). The significance of this result in light of the Aquifex and Thermotoga placements in phylogenetic trees of molecular sequences is discussed.

Molecular evolution of the histidine biosynthetic pathway

The available sequences of genes encoding the enzymes associated with histidine biosynthesis suggest that this is an ancient metabolic pathway that was assembled prior to the diversification of the Bacteria, Archaea, and Eucarya. Paralogous duplications, gene elongation, and fusion events involving different his genes have played a major role in shaping this biosynthetic route. Evidence that the hisA and the hisF genes and their homologous are the result of two successive duplication events that apparently took place before the separation of the three cellular lineages is extended. These two successive gene duplication events as well as the homology between the hisH genes and the sequences encoding the TrpG-type amidotransferases support the idea that during the early stages of metabolic evolution at least parts of the histidine biosynthetic pathway were mediated by enzymes of broader substrate specificities. Maximum likelihood trees calculated for the available sequences of genes encoding these enzymes have been obtained. Their topologies support the possibility of an evolutionary proximity of archaebacteria with low GC Gram-positive bacteria. This observation is consistent with those detected by other workers using the sequences of heat-shock proteins (HSP70), glutamine synthetases, glutamate dehydrogenases, and carbamoylphosphate synthetases.

Bacterial classifications derived from recA protein sequence comparisons

RecA protein sequences from 62 eubacterial sources were compared with one another and relative to one archaebacterial RecA-like and a number of eukaryotic RecA-like sequences. Pairwise similarity scores were determined by a novel method based on significant segment pair alignment. The sequences of different species were grouped on the basis of mutually high similarity scores within groups and consistency of score ranges in comparison to other groups. Following this protocol, the gamma-proteobacteria can be subclassified into two major groups, those of mostly vertebrate hosts and those of mostly soil habitat. The alpha-proteobacterial sequences also divide into two distinct groups, whereas classification of the beta-proteobacteria is more complex. The gram-positive bacterial sequences split into three groups of low and three groups of high G+C genome content. However, neither the combined low-G+C-content nor the combined high-G+C-content group nor the aggregate of all gram-positive bacteria form homogeneous groups. The mycoplasma sequences score best with the Bacillus subtilis sequence, consistent with their presumed origin from a gram-positive ancestor. The eukaryotic RAD proteins generally show a single high-scoring segment pair with the proteobacterial RecA sequences around the ATP-binding domain. The bacteriophage T4 UvsX protein aligns best with RecA sequences on two segments disjoint from the ATP-binding domain. The distribution of the most highly conserved regions shared between RecA and noneubacterial RecA-like sequences suggests a mosaic character and evolution of RecA. The discussion considers some questions on the validity and consistency of bacterial classifications derived from RecA sequence comparisons.

Arrangement and nucleotide sequence of the gene (fus) encoding elongation factor G (EF-G) from the hyperthermophilic bacterium Aquifex pyrophilus: phylogenetic depth of hyperthermophilic bacteria inferred from analysis of the EF-G/fus sequences

The gene fus (for EF-G) of the hyperthermophilic bacterium Aquifex pyrophilus was cloned and sequenced. Unlike the other bacteria, which display the streptomycin-operon arrangement of EF genes (5'-rps12-rps7-fus-tuf-3'), the Aquifex fus gene (700 codons) is not preceded by the two small ribosomal subunit genes although it is still followed by a tuf gene (for EF-Tu). The opposite strand upstream from the EF-G coding locus revealed an open reading frame (ORF) encoding a polypeptide having 52.5% identity with an E. coli protein (the pdxJ gene product) involved in pyridoxine condensation. The Aquifex EF-G was aligned with available homologs representative of Deinococci, high G+C Gram positives, Proteobacteria, cyanobacteria, and several Archaea. Outgroup-rooted phylogenies were constructed from both the amino acid and the DNA sequences using first and second codon positions in the alignments except sites containing synonymous changes. Both datasets and alternative tree-making methods gave a consistent topology, with Aquifex and Thermotoga maritima (a hyperthermophile) as the first and the second deepest offshoots, respectively. However, the robustness of the inferred phylogenies is not impressive. The branching of Aquifex more deeply than Thermotoga and the branching of Thermotoga more deeply than the other taxa examined are given at bootstrap values between 65 and 70% in the fus-based phylogenies, while the EF-G(2)-based phylogenies do not provide a statistically significant level of support (< or = 50% bootstrap confirmation) for the emergence of Thermotoga between Aquifex and the successive offshoot (Thermus genus). At present, therefore, the placement of Aquifex at the root of the bacterial tree, albeit reproducible, can be asserted only with reservation, while the emergence of Thermotoga between the Aquificales and the Deinococci remains (statistically) indeterminate.

Extremozymes: expanding the limits of biocatalysis

The study of enzymes isolated from organisms inhabiting unconventional ecosystems has led to the realization that biocatalysis need not be constrained to mild conditions and can be considered at pH's, temperatures, pressures, ionic and solvent environments long thought to be destructive to biomolecules. Parallel to this, it has been demonstrated that even conventional enzymes will catalyze reactions in solvents other than water. However, the intrinsic basis for biological function under extreme conditions is only starting to be addressed, as are associated applications. This was the focus of a recent NSF/NIST-sponsored workshop on extremozymes. Given the information acquired from the study of extremozymes, modification of enzymes to improve their ranges of stability and activity remains a possibility. Ultimately, by expanding the range of conditions suitable for enzyme function, new opportunities to use biocatalysis will be created.

The effects of heavy meteorite bombardment on the early evolution--the emergence of the three domains of life

A characteristic of many molecular phylogenies is that the three domains of life (Bacteria, Archaea, Eucarya) are clearly separated from each other. The analyses of ancient duplicated genes suggest that the last common ancestor of all presently known life forms already had been a sophisticated cellular prokaryote. These findings are in conflict with theories that have been proposed to explain the absence of deep branching lineages. In this paper we propose an alternative scenario, namely, a large meteorite impact that wiped out almost all life forms present on the early Earth. Following this nearly complete frustation of life on Earth, two surviving extreme thermophilic species gave rise to the now existing major groups of living organisms, the Bacteria and Archaea. [The latter also contributed the major portion to the nucleo-cytoplasmic component of the Eucarya]. An exact calibration of the molecular record with regard to time is not yet possible. The emergence of Eucarya in fossil and molecular records suggests that the proposed late impact should have occurred before 2100 million years before present (BP). If the 3500 million year old microfossils [Schopf, J. W. 1993: Science 260: 640-646] are interpreted as representatives of present day existing groups of bacteria (i.e., as cyanobacteria), then the impact is dated to around 3700 million years BP. The analysis of molecular sequences suggests that the separation between the Eucarya and the two prokaryotic domains is less deep then the separation between Bacteria and Archaea. The fundamental cell biological differences between Archaea and Eucarya were obtained over a comparatively short evolutionary distance (as measured in number of substitution events in biological macromolecules). Our interpretation of the molecular record suggests that life emerged early in Earth's history even before the time of the heavy bombardment was over. Early life forms already had colonized extreme habitats which allowed at least two prokaryotic species to survive a late nearly ocean boiling impact. The distribution of ecotypes on the rooted universal tree of life should not be interpreted as evidence that life originated in extremely hot environments.

Isolation and characterization of a heat-stable pullulanase from the hyperthermophilic archaeon Pyrococcus woesei after cloning and expression of its gene in Escherichia coli

The gene encoding an extremely heat-stable pullulanase from the hyperthermophilic archaeon Pyrococcus woesei was cloned and expressed in Escherichia coli. Purification of the enzyme to homogeneity was achieved after heat treatment of the recombinant E. coli cells, affinity chromatography on a maltotriose-coupled Sepharose 6B column, and anion-exchange chromatography on Mono Q. The pullulanase, which was purified 90-fold with a final yield of 15%, is composed of a single polypeptide chain with a molecular mass of 90 kDa. The enzyme is optimally active at 100 degrees C and pH 6.0 and shows 40% activity at 120 degrees C. Enzyme activation up to 370% is achieved in the presence of calcium ions and reducing agents such as beta-mercaptoethanol and dithiothreitol, whereas N-bromosuccinimide and alpha-cyclodextrin are inhibitory. The high rigidity of the heat-stable enzyme is demonstrated by fluorescence spectroscopic studies in the presence of denaturing agents such as sodium dodecyl sulfate. At temperatures above 80 degrees C, the enzyme seems to switch from the compact to the unfolded form, which is accompanied by an apparent shift in the molecular mass from 45 to 90 kDa.

Chromosomal organization and nucleotide sequence of the fus-gene encoding elongation factor 2 (EF-2) of the hyperthermophilic archaeum Pyrococcus woesei

A Pyrococcus woesei EcoRI DNA fragment (3400 bp) harbouring the gene fus for elongation factor 2 (EF-2) was cloned and almost completely sequenced. Unlike Methanococcus vannielii (which displays the 'str operon'-like fus and tuf gene context, 5'-rps12-rps7-fus-tuf-3'), and similar to Sulfolobus acidocaldarius and Desulfurococcus mobilis, the Pyrococcus fus gene (732 codons) is unlinked to the rps and tuf genes, and is immediately followed (57 bp intergenic spacing) by an ORF of 106 codons. Both ORFs are preceded by potential archaeal promoters located 52 bp (for fus) and 37 bp (for ORF106) upstream of the putative start codons. The Pyrococcus EF-2(G) equivalent factor is somewhat closer to the eukaryal than to the bacterial homolog, and also shares with the former the C-terminal sequence required for ADP ribosylation of EF-2 by Diphtheria toxin.

Evolution of the chaperonin families (Hsp60, Hsp10 and Tcp-1) of proteins and the origin of eukaryotic cells

The members of the 10 kDa and 60 kDa heat-shock chaperonin proteins (Hsp10 and Hsp60 or Cpn10 and Cpn60), which form an operon in bacteria, are present in all eubacteria and eukaryotic cell organelles such as mitochondria and chloroplasts. In archaebacteria and eukaryotic cell cytosol, no close homologues of Hsp10 or Hsp60 have been identified. However, these species (or cell compartments) contain the Tcp-1 family of proteins (distant homologues of Hsp60). Phylogenetic analysis based on global alignments of Hsp60 and Hsp10 sequences presented here provide some evidence regarding the evolution of mitochondria from a member of the alpha-subdivision of Gram-negative bacteria and chloroplasts from cyanobacterial species, respectively. This interference is strengthened by the presence of sequence signatures that are uniquely shared between Hsp60 homologues from alpha-purple bacteria and mitochondria on one hand, and the chloroplasts and cyanobacterial hsp60s on the other. Within the alpha-purple subdivision, species such as Rickettsia and Ehrlichia, which live intracellularly within eukaryotic cells, are indicated to be the closest relatives of mitochondrial homologues. In the Hsp60 evolutionary tree, rooted using the Tcp-1 homologue, the order of branching of the major groups was as follows: Gram-positive bacteria--cyanobacteria and chloroplasts--chlamydiae and spirochaetes--beta- and gamma-Gram-negative purple bacteria--alpha-purple bacteria--mitochondria. A similar branching order was observed independently in the Hsp10 tree. Multiple Hsp60 homologues, when present in a group of species, were found to be clustered together in the trees, indicating that they evolved by independent gene-duplication events. This review also considers in detail the evolutionary relationship between Hsp60 and Tcp-1 families of proteins based on two different models (viz. archaebacterial and chimeric) for the origin of eukaryotic cell nucleus. Some predictions of the chimeric model are also discussed.

Purification and characterization of a thermostable thiol protease from a newly isolated hyperthermophilic Pyrococcus sp

A hyperthermophilic archaeon strain, KOD1, was isolated from a solfatara at a wharf on Kodakara Island, Kagoshima, Japan. The growth temperature of the strain ranged from 65 to 100 degrees C, and the optimal temperature was 95 degrees C. The anaerobic strain was an S0-dependent heterotroph. Cells were irregular cocci and were highly motile with several polar flagella. The membrane lipid was of the ether type, and the GC content of the DNA was estimated to be 38 mol%. The 16S rRNA sequence was 95% homologous to that of Pyrococcus abyssi. The optimum growth pH and NaCl concentration of the strain KOD1 were 7.0 and 3%, respectively. Therefore, strain KOD1 was identified as a Pyrococcus sp. Strain KOD1 produced at least three extracellular proteases. One of the most thermostable proteases was purified 21-fold, and the molecular size was determined to be 44 kDa by sodium dodecyl sulfate-polyacrylamide gel electrophoresis and 45 kDa by gel filtration chromatography. The specific activity of the purified protease was 2,160 U/mg of protein. The enzyme exhibited its maximum activity at approximately pH 7.0 and at a temperature of 110 degrees with azocasein as a substrate. The enzyme activity was completely retained after heat treatment at 90 degrees C for 2 h, and the half-life of enzymatic activity at 100 degrees C was 60 min. The proteolytic activity was significantly inhibited by p-chloromercuribenzoic acid or E-64 but not by EDTA or phenylmethylsulfonyl fluoride. Proteolytic activity was enhanced threefold in the presence of 8 mM cysteine. These experimental results indicated that the enzyme was a thermostable thiol protease.

Phylogenetic analysis of 70 kD heat shock protein sequences suggests a chimeric origin for the eukaryotic cell nucleus

BACKGROUND

The evolutionary relationships between archaebacteria, eubacteria and eukaryotic cells are of central importance in biology. The current view is that each of these three groups of organisms constitutes a monophyletic domain, and that eukaryotic cells have evolved fom an archaebacterial ancestor. Recent studies on a number of highly conserved protein sequences do not, however, support this view and raise important questions concerning the evolutionary relationships between all extant organisms, particularly regarding the origin of eukaryotic cells.

RESULTS

RESULTS

We have used sequences of 70 kD heat shock protein (hsp70)--the most conserved protein found to date in all species--to examine the evolutionary relationship between various species. We have obtained two new archaebacterial hsp70 sequences from the species, Thermoplasma acidophilum and Halobacterium cutirubrum. A global comparison of hsp70 sequences, including our two new sequences, shows that all known archaebacterial homologs share a number of sequence signatures with the Gram-positive group of bacteria that are not found in any other prokaryotic or eukaryotic species. In contrast, the eukaryotic homologs are shown to share a number of unique sequence features with the Gram-negative bacteria that are not present in any archaebacteria. Detailed phylogenetic analyses of hsp70 sequences strongly support a specific evolutionary relationship between archaebacteria and Gram-positive bacteria on the one hand, and Gram-negative bacteria and eukaryotes on the other. The phylogenetic analyses also indicate a polyphyletic branching of archaebacteria within the Gram-positive species. The possibility that the observed relationships are due to horizontal gene transfers can be excluded on the basis of sequence characteristics of different groups of homologs.

CONCLUSIONS

Our results do not support the view that archaebacteria constitute a monophyletic domain, but instead suggest a close evolutionary linkage between archaebacteria and Gram-positive bacteria. Furthermore, in contrast to the presently accepted view, eukaryotic hsp70s show a close and specific relationship to those from Gram-negative species. To explain the phylogenies based on different gene sequences, a chimeric model for the origin of the eukaryotic cell nucleus involving fusion between an archaebacterium and a Gram-negative eubacterium is proposed. Several predictions from the chimeric model are discussed.