dnaJ in Archaea

Integration of two ancestral chaperone systems into one: the evolution of eukaryotic molecular chaperones in light of eukaryogenesis

Eukaryotic genomes are mosaics of genes acquired from their prokaryotic ancestors, the eubacterial endosymbiont that gave rise to the mitochondrion and its archaebacterial host. Genomic footprints of the prokaryotic merger at the origin of eukaryotes are still discernable in eukaryotic genomes, where gene expression and function correlate with their prokaryotic ancestry. Molecular chaperones are essential in all domains of life as they assist the functional folding of their substrate proteins and protect the cell against the cytotoxic effects of protein misfolding. Eubacteria and archaebacteria code for slightly different chaperones, comprising distinct protein folding pathways. Here we study the evolution of the eukaryotic protein folding pathways following the endosymbiosis event. A phylogenetic analysis of all 64 chaperones encoded in the Saccharomyces cerevisiae genome revealed 25 chaperones of eubacterial ancestry, 11 of archaebacterial ancestry, 10 of ambiguous prokaryotic ancestry, and 18 that may represent eukaryotic innovations. Several chaperone families (e.g., Hsp90 and Prefoldin) trace their ancestry to only one prokaryote group, while others, such as Hsp40 and Hsp70, are of mixed ancestry, with members contributed from both prokaryotic ancestors. Analysis of the yeast chaperone–substrate interaction network revealed no preference for interaction between chaperones and substrates of the same origin. Our results suggest that the archaebacterial and eubacterial protein folding pathways have been reorganized and integrated into the present eukaryotic pathway. The highly integrated chaperone system of yeast is a manifestation of the central role of chaperone-mediated folding in maintaining cellular fitness. Most likely, both archaebacterial and eubacterial chaperone systems were essential at the very early stages of eukaryogenesis, and the retention of both may have offered new opportunities for expanding the scope of chaperone-mediated folding.

Cumulative impact of chaperone-mediated folding on genome evolution

Molecular chaperones support protein folding and unfolding along with assembly and translocation of protein complexes. Chaperones have been recognized as important mediators between an organismal genotype and phenotype as well as important maintainers of cellular fitness under environmental conditions that induce high mutational loads. Here we review recent studies revealing that the folding assistance supplied by chaperones is evident in genomic sequences implicating chaperone-mediated folding as an influential factor during protein evolution. Interaction of protein with chaperones ensures a proper folding and function, yet an adaptation to obligatory dependence on such assistance may be irreversible, representing an evolutionary trap. A correlation between the requirement for a chaperone and protein expression level indicates that the evolution of substrate-chaperone interaction is bounded by the required substrate abundance within the cell. Accumulating evidence suggests that the utility of chaperones is governed by a delicate balance between their help in mitigating the risks of protein misfolding and aggregate formation on one hand and the slower rate of protein maturation and the energetic cost of chaperone synthesis on the other.

dnaJ gene sequence-based assay for species identification and phylogenetic grouping in the genus Staphylococcus

In the last few years, many attempts have been made to use conserved gene sequences for identification and for phylogenetic studies of Staphylococcus species. In an effort to identify a more reliable approach, a dnaJ gene sequence-based database was created. In this study, an approximately 883 bp portion of the dnaJ gene sequence from 45 staphylococcal type strains was compared with 16S rRNA and other conserved gene (hsp60, sodA and rpoB) sequences available in public databases. Nucleotide sequence comparisons revealed that the staphylococcal dnaJ gene showed higher discrimination (mean similarity 77.6 %) than the 16S rRNA (mean similarity 97.4 %), rpoB (mean similarity 86 %), hsp60 (mean similarity 82 %) and sodA (mean similarity 81.5 %) genes. Analysis of the dnaJ gene sequence from 20 Staphylococcus isolates representing two clinically important species showed <1 % sequence divergence. Phylogenetic data obtained from the dnaJ gene sequence were in general agreement with those of 16S rRNA gene sequence analysis and DNA-DNA reassociation studies. In conclusion, the dnaJ gene sequence-based assay is an effective alternative to currently used methods, including 16S rRNA gene sequencing, for identification and taxonomical analysis of Staphylococcus species.

Use of the dnaJ gene for the detection and identification of all Legionella pneumophila serogroups and description of the primers used to detect 16S rDNA gene sequences of major members of the genus Legionella

We sequenced about 930 bp of the dnaJ gene from 15 Legionella pneumophila serogroups and some other members of the genus Legionella. As L. pneumophila 16S rDNA sequences could not discriminate between all subspecies and serogroups, we assessed the use of dnaJ gene sequences to differentiate between Legionella subspecies as well as between L. pneumophila serogroups. A phylogenetic analysis revealed that dnaJ gene sequences were more variable between the L. pneumophila serogroups than mip gene and 16S rDNA sequences. By studying 61 strains from 41 species of the genus Legionella, as well as other genera, we established a PCR method that could amplify 285 bp of dnaJ gene from all L. pneumophila serogroups. This primer set was more sensitive than mip gene primers and was able to detect 0.25 ng of purified DNA. We also describe the 16S rDNA primers that were used to detect most Legionella genus members.

Stress genes and proteins in the archaea

The field covered in this review is new; the first sequence of a gene encoding the molecular chaperone Hsp70 and the first description of a chaperonin in the archaea were reported in 1991. These findings boosted research in other areas beyond the archaea that were directly relevant to bacteria and eukaryotes, for example, stress gene regulation, the structure-function relationship of the chaperonin complex, protein-based molecular phylogeny of organisms and eukaryotic-cell organelles, molecular biology and biochemistry of life in extreme environments, and stress tolerance at the cellular and molecular levels. In the last 8 years, archaeal stress genes and proteins belonging to the families Hsp70, Hsp60 (chaperonins), Hsp40(DnaJ), and small heat-shock proteins (sHsp) have been studied. The hsp70(dnaK), hsp40(dnaJ), and grpE genes (the chaperone machine) have been sequenced in seven, four, and two species, respectively, but their expression has been examined in detail only in the mesophilic methanogen Methanosarcina mazei S-6. The proteins possess markers typical of bacterial homologs but none of the signatures distinctive of eukaryotes. In contrast, gene expression and transcription initiation signals and factors are of the eucaryal type, which suggests a hybrid archaeal-bacterial complexion for the Hsp70 system. Another remarkable feature is that several archaeal species in different phylogenetic branches do not have the gene hsp70(dnaK), an evolutionary puzzle that raises the important question of what replaces the product of this gene, Hsp70(DnaK), in protein biogenesis and refolding and for stress resistance. Although archaea are prokaryotes like bacteria, their Hsp60 (chaperonin) family is of type (group) II, similar to that of the eukaryotic cytosol; however, unlike the latter, which has several different members, the archaeal chaperonin system usually includes only two (in some species one and in others possibly three) related subunits of approximately 60 kDa. These form, in various combinations depending on the species, a large structure or chaperonin complex sometimes called the thermosome. This multimolecular assembly is similar to the bacterial chaperonin complex GroEL/S, but it is made of only the large, double-ring oligomers each with eight (or nine) subunits instead of seven as in the bacterial complex. Like Hsp70(DnaK), the archaeal chaperonin subunits are remarkable for their evolution, but for a different reason. Ubiquitous among archaea, the chaperonins show a pattern of recurrent gene duplication-hetero-oligomeric chaperonin complexes appear to have evolved several times independently. The stress response and stress tolerance in the archaea involve chaperones, chaperonins, other heat shock (stress) proteins including sHsp, thermoprotectants, the proteasome, as yet incompletely understood thermoresistant features of many molecules, and formation of multicellular structures. The latter structures include single- and mixed-species (bacterial-archaeal) types. Many questions remain unanswered, and the field offers extraordinary opportunities owing to the diversity, genetic makeup, and phylogenetic position of archaea and the variety of ecosystems they inhabit. Specific aspects that deserve investigation are elucidation of the mechanism of action of the chaperonin complex at different temperatures, identification of the partners and substitutes for the Hsp70 chaperone machine, analysis of protein folding and refolding in hyperthermophiles, and determination of the molecular mechanisms involved in stress gene regulation in archaeal species that thrive under widely different conditions (temperature, pH, osmolarity, and barometric pressure). These studies are now possible with uni- and multicellular archaeal models and are relevant to various areas of basic and applied research, including exploration and conquest of ecosystems inhospitable to humans and many mammals and plants.

The archaeal molecular chaperone machine: peculiarities and paradoxes

A major finding within the field of archaea and molecular chaperones has been the demonstration that, while some species have the stress (heat-shock) gene hsp70(dnaK), others do not. This gene encodes Hsp70(DnaK), an essential molecular chaperone in bacteria and eukaryotes. Due to the physiological importance and the high degree of conservation of this protein, its absence in archaeal organisms has raised intriguing questions pertaining to the evolution of the chaperone machine as a whole and that of its components in particular, namely, Hsp70(DnaK), Hsp40(DnaJ), and GrpE. Another archaeal paradox is that the proteins coded by these genes are very similar to bacterial homologs, as if the genes had been received via lateral transfer from bacteria, whereas the upstream flanking regions have no bacterial markers, but instead have typical archaeal promoters, which are like those of eukaryotes. Furthermore, the chaperonin system in all archaea studied to the present, including those that possess a bacterial-like chaperone machine, is similar to that of the eukaryotic-cell cytosol. Thus, two chaperoning systems that are designed to interact with a compatible partner, e.g., the bacterial chaperone machine physiologically interacts with the bacterial but not with the eucaryal chaperonins, coexist in archaeal cells in spite of their apparent functional incompatibility. It is difficult to understand how these hybrid characteristics of the archaeal chaperoning system became established and work, if one bears in mind the classical ideas learned from studying bacteria and eukaryotes. No doubt, archaea are intriguing organisms that offer an opportunity to find novel molecules and mechanisms that will, most likely, enhance our understanding of the stress response and the protein folding and refolding processes in the three phylogenetic domains.

Putative heat shock protein 70 gene from Actinobacillus actinomycetemcomitans: molecular cloning and sequence analysis of its gene

We have cloned and sequenced two overlapping fragments of chromosomal DNA from Actinobacillus actinomycetemcomitans. The nucleotide sequence contained two open reading frames. The deduced amino acid sequences of the two open reading frames showed significant homology with the heat shock proteins hsp70 and hsp40 of other organisms respectively. The upstream open reading frame consisted of 1902 bp, corresponding to 634-amino-acid residues. The CAA codon for glutamines was frequently seen in hsp70, i.e., in 30 of 32 glutamines (93.8%). The spacing region between the two open reading frames was unusually long compared with other prokaryotic organisms. A number of unique and distinguishing features of the sequences in the hsp70 family were verified, and it was found that a particular spacing sequence between the hsp70 and hsp40 gene loci can be used to identify A. actinomycetemcomitans from the periodontal pocket.

Osmotically induced response in representatives of halophilic prokaryotes: the bacterium Halomonas elongata and the archaeon Haloferax volcanii

Haloferax volcanii and Halomonas elongata have been selected as representatives of halophilic Archaea and Bacteria, respectively, to analyze the responses to various osmolarities at the protein synthesis level. We have identified a set of high-salt-related proteins (39, 24, 20, and 15.5 kDa in H. elongata; 70, 68, 48, and 16 kDa in H. volcanii) whose synthesis rates increased with increasing salinities. A different set of proteins (60, 42, 15, and 6 kDa for H. elongata; 63, 44, 34, 18, 17, and 6 kDa for H. volcanii), some unique for low salinities, was induced under low-salt conditions. For both organisms, and especially for the haloarchaeon, adaptation to low-salt conditions involved a stronger and more specific response than adaptation to high-salt conditions, indicating that unique mechanisms may have evolved for low-salinity adaptation. In the case of H. volcanii, proteins with a typical transient response to osmotic shock, induced by both hypo- and hyperosmotic conditions, probably corresponding to described heat shock proteins and showing the characteristics of general stress proteins, have also been identified. Cell recovery after a shift to low salinities was immediate in both organisms. In contrast, adaptation to higher salinities in both cases involved a lag period during which growth and general protein synthesis were halted, although the high-salt-related proteins were induced rapidly. In H. volcanii, this lag period corresponded exactly to the time needed for cells to accumulate adequate intracellular potassium concentrations, while extrusion of potassium after the down-shift was immediate. Thus, reaching osmotic balance must be the main limiting factor for recovery of cell functions after the variation in salinity.

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.

Mini-Review; Stress Genes: An Introductory Overview

Molecular sequence data, made available in the last 15 years or so, have led to the classification of living cells into three phylogenetic domains: Bacteria, Archaea, and Eucarya. All the organisms that have been tested belonging to either domain were capable of mounting a stress response with essentially the same characteristics, regardless of the stressor. The protagonists in the cell's stress response are the stress genes and their protein products. Some of the latter are molecular chaperones. Under physiological conditions, these chaperones aid other cellular proteins to fold properly and achieve a native -functional- configuration, and to translocate from the place of synthesis to the cell's locale in which they will operate. In a stressed cell, the stress proteins that are chaperones protect other molecules from denaturation and help those partially damaged to regain a functional configuration. Thus, cell death is avoided and recovery is enhanced. The study of stress genes and proteins has progressed considerably in organisms belonging to the domains Bacteria and Eucarya. Less is known about the archaeal stress genes. Here, research with an organism from the Archaea is discussed, focusing on the stress genes of the hsp70 (dnaK) locus. Future perspectives for basic and applied research within the health sciences and biotechnology industries are presented.

Heat-shock proteins and molecular chaperones: implications for pathogenesis, diagnostics, and therapeutics

Cells react to physical (e.g., heat) or chemical (e.g., anoxia, low pH) stressors, mounting a stress (heat-shock) response. Most genes are turned down or off, while a few are activated. The latter encode the stress or heat-shock proteins (Hsps), whose levels increase in stressed cells. Various Hsps are molecular chaperones. These, and other molecular chaperones that are not Hsps, help the other cellular proteins to achieve their native state (correct folding or functional conformation), reach their final destination (e.g., the endoplasmic reticulum or the mitochondria), resist denaturing by stressors, and regain the native state after partial denaturation. Thus the Hsps and molecular chaperones occupy the stage's center whenever and wherever there is cellular and tissue injury caused by local or systemic stressors via protein damage. This feature, their participation in protein folding and transport, and their evolutionary conservation within the three phylogenetic domains, strongly suggest a vital role for Hsps and molecular chaperones. Their importance in pathogenesis, and as diagnostic markers and prognostic indicators, is beginning to be appreciated. The role of Hsps and molecular chaperones in cell recovery from injury by a variety of noxae of clinical and surgical relevance is also being assessed. Consequently, the potential of these molecules (and corresponding genes) as targets for treatment or as therapeutic tools is emerging and is being explored. Stroke, myocardial infarction, inflammatory syndromes, infectious and parasitic diseases, autoimmune disorders, cancer, and aging are but some examples of conditions in which Hsps and molecular chaperones are being scrutinized. The era of Hsp and molecular chaperone pathology has dawned. It is likely that genetic and acquired defects of Hsp and molecular chaperone structure and function will be identified, and will play a primary, or auxiliary but determinant, role in disease.

Archaeal grpE: transcription in two different morphologic stages of Methanosarcina mazei and comparison with dnaK and dnaJ

Transcription of the heat shock gene grpE was studied in two different morphologic stages of the archaeon Methanosarcina mazei S-6 that differ in resistance to physical and chemical traumas: single cells and packets. While single cells are directly exposed to environmental changes, such as temperature elevations, cells in packets are surrounded by intercellular and peripheral material that keeps them together in a globular structure which can reach several millimeters in diameter. grpE transcript levels determined by Northern (RNA) blotting peaked after a 15-min heat shock in single cells. In contrast, the highest transcript levels in packets were observed after the longest heat shock tested, 60 min. The same response profiles were demonstrated by primer extension experiments and S1 nuclease analysis. A comparison of the grpE response to heat shock with those of dnaK and dnaJ showed that the grpE transcript level was the most increased, closely followed by that of the dnaK transcript, with that of the dnaJ gene being the least augmented. Transcription of grpE started at the same site under normal and heat shock temperatures, and the transcript was consistently approximately 700 bases long. Codon usage patterns revealed that the three archaeal genes use most codons and have the same codon preference for 61% of the amino acids.

Heat-shock response in Archaea

The Archaea are one of the three phylogenetic domains into which all organisms have been classified, and include extreme halophiles, extreme thermophiles and methanogens. Some of these organisms inhabit inhospitable environments on Earth, and thus have evolved stress responses to cope with the extremes of heat, pH and salinity that they encounter. Although the archaeal stress or heat-shock response bears some similarity to the heat-shock responses of other organisms, it possesses some unique features. A better understanding of this response would facilitate its exploitation in the biotechnological industries; for example, in engineering cells that exhibit an improved ability to withstand, or recover from, stress.

Regulated gene expression in methanogens

Methanogens form a very large and diverse group of microorganisms within the domain of the Archaea. Energy for their growth is obtained by the reduction of a variety of substrates into methane. Several genes, coding for enzymes involved in methanogenesis or in the central metabolism have been cloned and studied. The molecular features of their expression signals have been compared with bacterial and eukaryal expression signals. This indicated that the transcription process is an intermediate form between the specific processes known in Bacteria and Eukarya. The translation system that is used in Archaea is very similar with the process in Bacteria. Although the molecular features of genes and expression signals in Archaea are well-studied, investigations on the regulation of gene expression in these organisms are very scarce. In order to give insight into molecular regulatory mechanisms in methanogens, the current knowledge of regulated systems in methanogens will be reviewed in this manuscript.

An archaeal trkA homolog near dnaK and dnaJ

The first trkA gene homolog in the phylogenetic domain Archaea is reported. The gene is located near the dnaK-dnaJ gene cluster in the genome of Methanosarcina mazei S-6, and encodes a protein homologous to the only other TrkA known, i.e., that of the bacterium Escherichia coli, involved in K+ transport. This finding supports an essential, evolutionarily early, and conserved role for this gene in cell survival and adaptation.