Functional similarities and differences of an archaeal Hsp70(DnaK) stress protein compared with its homologue from the bacterium Escherichia coli

Archaea are prokaryotes but some of their chaperoning systems resemble those of eukaryotes. Also, not all archaea possess the stress protein Hsp70(DnaK), in contrast with bacteria and eukaryotes, which possess it without any known exception. Further, the primary structure of the archaeal DnaK resembles more the bacterial than the eukaryotic homologues. The work reported here addresses two questions: Is the archaeal Hsp70 protein a chaperone, like its homologues in the other two phylogenetic domains? And, if so, is the chaperoning mechanism of bacterial or eukaryotic type? The data have shown that the DnaK protein of the archaeon Methanosarcina mazei functions efficiently as a chaperone in luciferase renaturation in vitro, and that it requires DnaJ, and the other bacterial-type chaperone, GrpE, to perform its function. The M. mazei DnaK chaperone activity was enhanced by interaction with the bacterial co-chaperone DnaJ, but not by the eukaryotic homologue HDJ-2. Both the bacterial GrpE and DnaJ stimulated the ATPase activity of the M. mazei DnaK. The M. mazei DnaK-dependent chaperoning pathway in vitro is similar to that of the bacterium Escherichia coli used for comparison. However, in vivo analyses indicate that there are also significant differences. The M. mazei dnaJ and grpE genes rescued E.coli mutants lacking these genes, but E.coli dnaK mutants were not complemented by the M. mazei dnaK gene. Thus, while the data from in vitro tests demonstrate functional similarities between the M. mazei and E.coli DnaK proteins, in vivo results indicate that, intracellularly, the chaperones from the two species differ.     

A novel isoform of pantothenate synthetase in the Archaea

The linear biosynthetic pathway leading from alpha-ketoisovalerate to pantothenate (vitamin B5) and on to CoA comprises eight steps in the Bacteria and Eukaryota. Genes for up to six steps of this pathway can be identified by sequence homology in individual archaeal genomes. However, there are no archaeal homologs to known isoforms of pantothenate synthetase (PS) or pantothenate kinase. Using comparative genomics, we previously identified two conserved archaeal protein families as the best candidates for the missing steps. Here we report the characterization of the predicted PS gene from Methanosarcina mazei, which encodes a hypothetical protein (MM2281) with no obvious homologs outside its own family. When expressed in Escherichia coli, MM2281 partially complemented an auxotrophic mutant without PS activity. Purified recombinant MM2281 showed no PS activity on its own, but the enzyme enabled substantial synthesis of [14C]4'-phosphopantothenate from [14C]beta-alanine, pantoate and ATP when coupled with E. coli pantothenate kinase. ADP, but not AMP, was detected as a coproduct of the coupled reaction. MM2281 also transferred the 14C-label from [14C]beta-alanine to pantothenate in the presence of pantoate and ADP, presumably through isotope exchange. No exchange took place when pantoate was removed or ADP replaced with AMP. Our results indicate that MM2281 represents a novel type of PS that forms ADP and is strongly inhibited by its product pantothenate. These properties differ substantially from those of bacterial PS, and may explain why PS genes, in contrast to other pantothenate biosynthetic genes, were not exchanged horizontally between the Bacteria and Archaea.     

Structural basis of the interspecies interaction between the chaperone DnaK(Hsp70) and the co-chaperone GrpE of archaea and bacteria

Hsp70s are chaperone proteins that are conserved in evolution and present in all prokaryotic and eukaryotic organisms. In the archaea, which form a distinct kingdom, the Hsp70 chaperones have been found in some species only, including Methanosarcina mazei. Both the bacterial and archaeal Hsp70(DnaK) chaperones cooperate with a GrpE co-chaperone which stimulates the ATPase activity of the DnaK protein. It is currently believed that the archaeal Hsp70 system was obtained by the lateral transfer of chaperone genes from bacteria. Our previous finding that the DnaK and GrpE proteins of M. mazei can functionally cooperate with the Escherichia coli GrpE and DnaK supported this hypothesis. However, the cooperation was surprising, considering the very low identity of the GrpE proteins (26%) and the relatively low identity of the DnaK proteins (56%). The aim of this work was to investigate the molecular basis of the observed interspecies chaperone interaction. Infrared resolution-enhanced spectra of the M. mazei and E. coli DnaK proteins were almost identical, indicating high similarity of their secondary structures, however, some small differences in band position and in the intensity of amide I' band components were observed and discussed. Profiles of thermal denaturation of both proteins were similar, although they indicated a higher thermostability of the M. mazei DnaK compared to the E. coli DnaK. Electrophoresis under non-denaturing conditions demonstrated that purified DnaK and GrpE of E. coli and M. mazei formed mixed complexes. Protein modeling revealed high similarity of the 3-dimensional structures of the archaeal and bacterial DnaK and GrpE proteins.     

Characterization of a feedback-resistant mevalonate kinase from the archaeon Methanosarcina mazei

The mevalonate pathway is utilized for the biosynthesis of isoprenoids in many bacterial, eukaryotic, and archaeal organisms. Based on previous reports of its feedback inhibition, mevalonate kinase (MVK) may play an important regulatory role in the biosynthesis of mevalonate pathway-derived compounds. Here we report the purification, kinetic characterization, and inhibition analysis of the MVK from the archaeon Methanosarcina mazei. The inhibition of the M. mazei MVK by the following metabolites derived from the mevalonate pathway was explored: dimethylallyl diphosphate (DMAPP), geranyl pyrophosphate (GPP), farnesyl pyrophosphate (FPP), isopentenyl monophosphate (IP), and diphosphomevalonate. M. mazei MVK was not inhibited by DMAPP, GPP, FPP, diphosphomevalonate, or IP, a proposed intermediate in an alternative isoprenoid pathway present in archaea. Our findings suggest that the M. mazei MVK represents a distinct class of mevalonate kinases that can be differentiated from previously characterized MVKs based on its inhibition profile.     

A novel limb in the osmoregulatory network of Methanosarcina mazei Gö1: Nε-acetyl-β-lysine can be substituted by glutamate and alanine

N^ε-acetyl-β-lysine is a unique compatible solute found in methanogenic archaea grown at high salinities. Deletion of the genes that encode the lysine-2,3-aminomutase ( ablA ) and the β-lysine acetyltransferase ( ablB ) abolished the production of N^ε-acetyl-β-lysine in Methanosarcina mazei Gö1. The mutant grew well at low and intermediate salinities. Interestingly, growth at high salt (800 mM NaCl) was only slowed down but not impaired demonstrating that in M. mazei Gö1 N^ε-acetyl-β-lysine is not essential for growth at high salinities. Nuclear magnetic resonance (NMR) analysis revealed an increased glutamate pool in the mutant. In addition to α-glutamate, a novel solute, alanine, was produced. The intracellular alanine concentration was as high as 0.36 ± 0.05 μmol (mg protein)⁻¹ representing up to 18% of the total solute pool at 800 mM NaCl. The cellular alanine concentration increased with the salinity of the medium and decreased in the presence of glycine betaine in the medium, indicating that alanine is used as compatible solute by M. mazei Gö1.     

Re-evaluation of the function of the F420 dehydrogenase in electron transport of Methanosarcina mazei

Methanosarcina mazei is a methanogenic archaeon that is able to thrive on various substrates and therefore contains a variety of redox-active proteins involved in both cytoplasmic and membrane-bound electron transport. The organism possesses a complex branched respiratory chain that has the ability to utilize different electron donors. In this study, two knockout mutants of the membrane-bound F(420) dehydrogenase (ΔfpoF and ΔfpoA-O) were constructed and analyzed. They exhibited severe growth deficiencies with trimethylamine, but not with acetate, as substrates. In cell lysates of the fpo mutants, the F(420):heterodisulfide oxidoreductase activity was strongly reduced, although soluble F(420) hydrogenase was still present. This led to the conclusion that the predominant part of cellular oxidation of the reduced form of F(420) (F(420)H(2)) in Ms. mazei is performed by F(420) dehydrogenase. Enzyme assays of cytoplasmic fractions revealed that ferredoxin (Fd):F(420) oxidoreductase activity was essentially absent in the ΔfpoF mutant. Subsequently, FpoF was produced in Escherichia coli and purified for further characterization. The purified FpoF protein catalyzed the Fd:F(420) oxidoreductase reaction with high specificity (the K(M) for reduced Fd was 0.5 μM) but with low velocity (V(max) = 225 mU·mg(-1)) and was present in the Ms. mazei cytoplasm in considerable amounts. Consequently, soluble FpoF might participate in electron carrier equilibrium and facilitate survival of the Ms. mazei Δech mutant that lacks the membrane-bound Fd-oxidizing Ech hydrogenase.     

Coexistence of group I and group II chaperonins in the archaeon Methanosarcina mazei

Two distantly related classes of cylindrical chaperonin complexes assist in the folding of newly synthesized and stress-denatured proteins in an ATP-dependent manner. Group I chaperonins are thought to be restricted to the cytosol of bacteria and to mitochondria and chloroplasts, whereas the group II chaperonins are found in the archaeal and eukaryotic cytosol. Here we show that members of the archaeal genus Methanosarcina co-express both the complete group I (GroEL/GroES) and group II (thermosome/prefoldin) chaperonin systems in their cytosol. These mesophilic archaea have acquired between 20 and 35% of their genes by lateral gene transfer from bacteria. In Methanosarcina mazei G?1, both chaperonins are similarly abundant and are moderately induced under heat stress. The M. mazei GroEL/GroES proteins have the structural features of their bacterial counterparts. The thermosome contains three paralogous subunits, alpha, beta, and gamma, which assemble preferentially at a molar ratio of 2:1:1. As shown in vitro, the assembly reaction is dependent on ATP/Mg2+ or ADP/Mg2+ and the regulatory role of the beta subunit. The co-existence of both chaperonin systems in the same cellular compartment suggests the Methanosarcina species as useful model systems in studying the differential substrate specificity of the group I and II chaperonins and in elucidating how newly synthesized proteins are sorted from the ribosome to the proper chaperonin for folding.     

Histone stoichiometry and DNA circularization in archaeal nucleosomes.

Recombinant (r)HMfB (archaealhistone B fromMethanothermusfervidus) formed complexes with increasing stability with DNA molecules increasing in length from 52 to 100 bp, but not with a 39 bp molecule. By using125I-labeled rHMfB-YY (an rHMfB variant with I31Y and M35Y replacements) and32P-labeled 100 bp DNA, these complexes, designated archaeal nucleosomes, have been shown to contain an archaeal histone tetramer. Consistent with DNA bending and wrapping, addition of DNA ligase to archaeal nucleosomes assembled with 88 and 128 bp DNAs resulted in covalently-closed monomeric circular DNAs which, following histone removal, were positively supercoiled based on their electrophoretic mobilities in the presence of ethidium bromide before and after relaxation by calf thymus topoisomerase I. Ligase addition to mixtures of rHMfB with 53 or 30 bp DNA molecules also resulted in circular DNAs but these were circular dimers and trimers. These short DNA molecules apparently had to be ligated into longer linear multimers for assembly into archaeal nucleosomes and ligation into circles. rHMfB assembled into archaeal nucleosomes at lower histone to DNA ratios with the supercoiled, circular ligation product than with the original 88 bp linear version of this molecule. Archaeal histones are most similar to the globular histone fold region of eukaryal histone H4, and the results reported are consistent with archaeal nucleosomes resembling the structure formed by eukaryal histone (H3+H4)2tetramers.     

Redundant synthesis of cysteinyl-tRNACys in Methanosarcina mazei

A subset of methanogenic archaea synthesize the cysteinyl-tRNA(Cys) (Cys-tRNA(Cys)) needed for protein synthesis using both a canonical cysteinyl-tRNA synthetase (CysRS) as well as a set of two enzymes that operate via a separate indirect pathway. In the indirect route, phosphoseryl-tRNA(Cys) (Sep-tRNA(Cys)) is first synthesized by phosphoseryl-tRNA synthetase (SepRS), and this misacylated intermediate is then converted to Cys-tRNA(Cys) by Sep-tRNA:Cys-tRNA synthase (SepCysS) via a pyridoxal phosphate-dependent mechanism. Here, we explore the function of all three enzymes in the mesophilic methanogen Methanosarcina mazei. The genome of M. mazei also features three distinct tRNA(Cys) isoacceptors, further indicating the unusual and complex nature of Cys-tRNA(Cys) synthesis in this organism. Comparative aminoacylation kinetics by M. mazei CysRS and SepRS reveals that each enzyme prefers a distinct tRNA(Cys) isoacceptor or pair of isoacceptors. Recognition determinants distinguishing the tRNAs are shown to reside in the globular core of the molecule. Both enzymes also require the S-adenosylmethione-dependent formation of (m1)G37 in the anticodon loop for efficient aminoacylation. We further report a new, highly sensitive assay to measure the activity of SepCysS under anaerobic conditions. With this approach, we demonstrate that SepCysS functions as a multiple-turnover catalyst with kinetic behavior similar to bacterial selenocysteine synthase and the archaeal/eukaryotic SepSecS enzyme. Together, these data suggest that both metabolic routes and all three tRNA(Cys) species in M. mazei play important roles in the cellular physiology of the organism.     

Both DNA and histone fold sequences contribute to archaeal nucleosome stability.

The roles and interdependence of DNA sequence and archaeal histone fold structure in determining archaeal nucleosome stability and positioning have been determined and quantitated. The presence of four tandem copies of TTTAAAGCCG in the polylinker region of pLITMUS28 resulted in a DNA molecule with increased affinity (DeltaDeltaG of approximately 700 cal mol(-1)) for the archaeal histone HMfB relative to the polylinker sequence, and the dominant, quantitative contribution of the helical repeats of the dinucleotide TA to this increased affinity has been established. The rotational and translational positioning of archaeal nucleosomes assembled on the (TTTAAAGCCG)(4) sequence and on DNA molecules selectively incorporated into archaeal nucleosomes by HMfB have been determined. Alternating A/T- and G/C-rich regions were located where the minor and major grooves, respectively, sequentially faced the archaeal nucleosome core, and identical positioning results were obtained using HMfA, a closely related archaeal histone also from Methanothermus fervidus. However, HMfA did not have similarly high affinities for the HMfB-selected DNA molecules, and domain-swap experiments have shown that this difference in affinity is determined by residue differences in the C-terminal region of alpha-helix 3 of the histone fold, a region that is not expected to directly interact with DNA. Rather this region is thought to participate in forming the histone dimer:dimer interface at the center of an archaeal nucleosome histone tetramer core. If differences in this interface do result in archaeal histone cores with different sequence preferences, then the assembly of alternative archaeal nucleosome tetramer cores could provide an unanticipated and novel structural mechanism to regulate gene expression.     

Single replication origin of the archaeon Methanosarcina mazei revealed by the Z curve method

The genomic sequence of the archaeon Methanosarcina mazei has been analyzed by the Z curve method. The Z curve is a three-dimensional curve that uniquely represents the given DNA sequence. The three-dimensional Z curve and its x and y components for the genome of M. mazei show a sharp peak and relatively broad peak, respectively. The cdc6 gene is located exactly at the position of the sharp peak. Based on the known behavior of the Z curves for the archaea whose replication origins have been identified, we hypothesize that the replication origin and termination sites correspond to the positions of the sharp peak and broad peak, respectively. We have located an intergenic region that is between the cdc6 gene (MM1314) and the gene for an adjacent protein (MM1315), which shows strong characteristics of the known replication origins. This region is highly rich in AT and contains multiple copies of consecutive repeats. Our results strongly suggest that the single replication origin of M. mazei is situated at the intergenic region between the cdc6 gene and the gene for the adjacent protein, from 1,564,657 to 1,566,241 bp of the genome.     

Isolation and characterization of new strains of methanogens from cold terrestrial habitats

Five strains of methanogenic archaea (MT, MS, MM, MSP, ZB) were isolated from permanently and periodically cold terrestrial habitats. Physiological and morphological studies, as well as phylogenetic analyses of the new isolates were performed. Based on sequences of the 16S rRNA and methyl-coenzyme M reductase a-subunit (mcrA) genes all new isolates are closely related to known mesophilic and psychrotolerant methanogens. Both, phylogenetic analyses and phenotypic properties allow to classify strains MT, MS, and MM as members of the genus Methanosarcina. Strain MT is a new ecotype of Methanosarcina mazei, whereas strains MM and MS are very similar to each other and can be assigned to the recently described psychrotolerant species Methanosarcina lacustris. The hydrogenotrophic strain MSP is a new ecotype of the genus Methanocorpusculum. The obligately methylotrophic strain ZB is closely related to Methanomethylovorans hollandica and can be classified as new ecotype of this species. All new isolates, including the strains from permanently cold environments, are not true psychrophiles according to their growth temperature characteristics. In spite of the ability of all isolates to grow at temperatures as low as 1-5 degrees C, all of them have their growth optima in the range of moderate temperatures (25-35 degrees C). Thus, they can be regarded as psychrotolerant organisms. Psychrotolerant methanogens are thought to play an important role in methane production in both, habitats under seasonal temperature variations or from permanently cold areas.     

Systematic deletion analyses of the fla genes in the flagella operon identify several genes essential for proper assembly and function of flagella in the archaeon, Methanococcus maripaludis

The archaeal flagellum is a unique motility apparatus in the prokaryotic domain, distinct from the bacterial flagellum. Most of the currently recognized archaeal flagella-associated genes fall into a single fla operon that contains the genes for the flagellin proteins (two or more genes designated as flaA or flaB ), some variation of a set of conserved proteins of unknown function ( flaC , flaD , flaE , flaF , flaG and flaH ), an ATPase ( flaI ) and a membrane protein ( flaJ ). In addition, the flaD gene has been demonstrated to encode two proteins: a full-length gene product and a truncated product derived from an alternate, internal start site. A systematic deletion approach was taken using the methanogen Methanococcus maripaludis to investigate the requirement and a possible role for these proposed flagella-associated genes. Markerless in-frame deletion strains were created for most of the genes in the M. maripaludis fla operon. In addition, a strain lacking the truncated FlaD protein [FlaD M(191)I] was also created. DNA sequencing and Southern blot analysis confirmed each mutant strain, and the integrity of the remaining operon was confirmed by immunoblot. With the exception of the ΔFlaB3 and FlaD M(191)I strains, all mutants were non-motile by light microscopy and non-flagellated by electron microscopy. A detailed examination of the ΔFlaB3 mutant flagella revealed that these structures had no hook region, while the FlaD M(191)I strain appeared identical to wild type. Each deletion strain was complemented, and motility and flagellation was restored. Collectively, these results demonstrate for first time that these fla operon genes are directly involved and critically required for proper archaeal flagella assembly and function.