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The gene that codes for the putative dihydroorotase in the hyperthermophilic archaeon Methanococcus jannaschii was subcloned in pET-21a and expressed in Escherichia coli. A purification protocol was devised. The purity of the protein was evaluated by SDS-PAGE and the protein was confirmed by sequencing using LC-MS. The calculated molecular mass is 48104 Da. SEC-LS suggested that the protein is a monomer in solution. ICP-MS showed that there are two Zn ions per monomer. Kinetic analysis of the recombinant protein gave hyperbolic kinetics with V = 12.2 µmol/min/mg and K = 0.14 mM at 25 °C. Furthermore the activity of the protein increased with temperature consistent with the hyperthermophilic nature of the organism. A homology model was constructed using the mesophilic Bacillus anthracis protein as the template. Residues known to be critical for Zn and substrate binding were conserved. The activity of the enzyme at 85 and 90 °C was found to be relatively constant over 160 min and this correlates with the temperature of optimal growth of the organism of 85 °C. The amino acid sequences and structures of the two proteins were compared and this gave insight into some of the factors that may confer thermostability-more Lys and Ile, fewer Ala, Thr, Gln and Gly residues, and shorter N- and C-termini. Additional and better insight into the thermostabilization strategies adopted by this enzyme will be provided when its crystal structure is determined. [ABSTRACT FROM AUTHOR]

Two-pore domain potassium (K) channels are membrane proteins widely identified in mammals, plants, and other organisms. A functional channel is a dimer with each subunit comprising two pore-forming loops and four transmembrane domains. The genome of the model plant Arabidopsis thaliana harbors five genes coding for K channels. Homologs of Arabidopsis K channels have been found in all higher plants sequenced so far. As with the K channels in mammals, plant K channels are targets of external and internal stimuli, which fine-tune the electrical properties of the membrane for specialized transport and/or signaling tasks. Plant K channels are modulated by signaling molecules such as intracellular H and calcium and physical factors like temperature and pressure. In this review, we ask the following: What are the similarities and differences between K channels in plants and animals in terms of their physiology? What is the nature of the last common ancestor (LCA) of these two groups of proteins? To answer these questions, we present physiological, structural, and phylogenetic evidence that discards the hypothesis proposing that the duplication and fusion that gave rise to the K channels occurred in a prokaryote LCA. Conversely, we argue that the K LCA was most likely a eukaryote organism. Consideration of plant and animal K channels in the same study is novel and likely to stimulate further exchange of ideas between students of these fields. [ABSTRACT FROM AUTHOR]

Bacterial Hfq proteins are structural homologs of archaeal and eukaryotic Sm/Lsm proteins, which are characterized by a 5-stranded β-sheet and an N-terminal α-helix. Previously, it was shown that archaeal Lsm proteins (SmAP) could produce long fibrils spontaneously, in contrast to the Hfq from Escherichia coli that could form similar fibrils only after special treatment. The organization of these fibrils is significantly different, but the reason for the dissimilarity has not been found. In the present work, we studied the process of fibril formation by bacterial protein Hfq from Pseudomonas aeruginosa and archaeal protein SmAP from Methanococcus jannaschii. Both proteins have high homology with E. coli Hfq. We found that Hfq from P. aeruginosa could form fibrils after substitutions in the conserved Sm2 motif only. SmAP from M. jannaschii, like other archaeal Lsm proteins, form fibrils spontaneously. Despite differences in the fibril formation conditions, the architecture of both was similar to that described for E. coli Hfq. Therefore, universal nature of fibril architecture formed by Hfq proteins is suggested. [ABSTRACT FROM AUTHOR]

The crystal structure of a mutant of archaeal ribosomal protein L1 from Methanococcus jannaschii with the deletion of a nonconserved positively charged cluster consisting of eight C-terminal amino acid residues is determined by the molecular replacement method at 1.75 Å resolution. This mutant is shown to form more stable and ordered crystals belonging to a space group other than that of the wild-type protein crystals. The positively charged C-terminal region has only a slight effect on the interaction between protein L1 and RNA molecules. Hence, this mutant can be used to prepare protein-RNA complexes and obtain their crystals. [ABSTRACT FROM AUTHOR]

Thermosipho globiformans (rod-shaped thermophilic fermenter) and Methanocaldococcus jannaschii (coccal hyperthermophilic hydrogenotrophic methanogen) established H-mediated syntrophy at 68 °C, forming exopolysaccharide-based aggregates. Electron microscopy showed that the syntrophic partners connected to each other directly or via intercellular bridges made from flagella, which facilitated transfer of H. Elemental sulfur (S) interrupted syntrophy; polysulfides abiotically formed from S intercepted electrons that were otherwise transferred to H to produce H, resulting in the generation of sulfide (sulfur respiration). However, Fe(III) oxides significantly reduced the interruption by S, accompanied by stiffening of Fe(II) sulfides produced by the reduction of Fe(III) oxides with the sulfur respiration-generated sulfide. Sea sand replacing Fe(III) oxides failed to generate stiffening or protect the syntrophy. Several experimental results indicated that the stiffening of Fe(II) sulfides shielded the liquid from S, resulting in methane production in the liquid. Field-emission scanning electron microscopy showed that the stiffened Fe(II) sulfides formed a network of spiny structures in which the microorganisms were buried. The individual fermenter rods likely produced Fe(II) sulfides on their surface and became local centers of a core of spiny structures, and the connection of these cores formed the network, which was macroscopically recognized as stiffening. [ABSTRACT FROM AUTHOR]

Ribosomal protein L4 is a regulator of protein synthesis in the Escherichia coli S10 operon, which contains genes of 11 ribosomal proteins. In this work, we have investigated regulatory functions of ribosomal protein L4 of the thermophilic archaea Methanococcus jannaschii. The S10-like operon from M. jannaschii encodes not 11, but only five ribosomal proteins (L3, L4, L23, L2, S19), and the first protein is L3 instead of S10. We have shown that MjaL4 and its mutant form lacking an elongated loop specifically inhibit expression of the first gene of the S10-like operon from the same organism in a coupled transcription?translation system in vitro. By deletion analysis, an L4-binding regulatory site has been found on MjaL3 mRNA, and a fragment of mRNA with length of 40 nucleotides has been prepared that is necessary and sufficient for the specific interaction with the MjaL4 protein. [ABSTRACT FROM AUTHOR]

Identification of the earliest traces of life is made difficult by the scarcity of the preserved microbial remains and by the alteration and potential contamination of the organic matter (OM) content of rocks. These factors can confuse interpretations of the biogenicity and syngenicity of fossilised structures and organic molecules found in ancient rocks. In order to improve our knowledge of the fossilisation processes and their effects at the molecular level, we made a preliminary study of the fate of OM during experimental fossilisation. Changes in the composition and quantity of amino acids, monosaccharides and fatty acids were followed with HPLC, GC and GC-MS analyses during 1 year of silicification of the hyperthermophilic Archaea Methanocaldococcus jannaschii. Although the cells themselves did not fossilise and the accompanying extracellular polymeric substances (EPS) did, our analyses showed that the OM initially present in both cells and EPS was uniformly preserved in the precipitated silica, with amino acids and fatty acids being the best preserved compounds. This study thus completes previous data obtained by electron microscopy investigations of simulated microbial fossilisation and can help better identification and interpretation of microbial biosignatures in both ancient rocks and in recent hydrothermal formations and sediments. [ABSTRACT FROM AUTHOR]

Sequence specific resonance assignments have been obtained for H, C and N nuclei of the 21 kDa (188 residues long) glutamine amido transferase subunit of guanosine monophosphate synthetase from Methanocaldococcus jannaschii. From an analysis of H and C, C secondary chemical shifts, JHH scalar coupling constants and sequential, short and medium range H-H NOEs, it was deduced that the glutamine amido transferase subunit has eleven strands and five helices as the major secondary structural elements in its tertiary structure. [ABSTRACT FROM AUTHOR]

Recently, unusual non-regulated ATP-dependent 6-phosphofructokinases (PFK) that belong to the PFK-B family have been described for the hyperthermophilic archaea Desulfurococcus amylolyticus and Aeropyrum pernix. Putative homologues were found in genomes of several archaea including the hyperthermophilic archaeon Methanocaldococcus jannaschii. In this organism, open reading frame MJ0406 had been annotated as a PFK-B sugar kinase. The gene encoding MJ0406 was cloned and functionally expressed in Escherichia coli. The purified recombinant enzyme is a homodimer with an apparent molecular mass of 68 kDa composed of 34 kDa subunits. With a temperature optimum of 85°C and a melting temperature of 90°C, the M. jannaschii nucleotide kinase represents one of the most thermoactive and thermostable members of the PFK-B family described so far. The recombinant enzyme was characterized as a functional nucleoside kinase rather than a 6-PFK. Inosine, guanosine, and cytidine were the most effective phosphoryl acceptors. Besides, adenosine, thymidine, uridin and xanthosine were less efficient. Extremely low activity was found with fructose-6-phosphate. Further, the substrate specificity of closely related PFK-Bs from D. amylolyticus and A. pernix were reanalysed. [ABSTRACT FROM AUTHOR]

Methanocaldococcus jannaschii has been notorious as an archaeon in which the replication origins are difficult to identify. Although extensive efforts have been exerted on this issue, the locations of replication origins still remain elusive 7 years after the publication of its complete genome sequence in 1996. Ambiguous results were obtained in identifying the replication origins of M. jannaschii based on all theoretical and experimental approaches. In the genome of M. jannaschii, we found that an ORF (MJ0774), annotated as a hypothetical protein, is a homologue of the Cdc6 protein. The position of the gene is at a global minimum of the x component of the Z curve, i.e., RY disparity curve, which has been used to identify replication origins in other Archaea. In addition, an intergenic region (694,540–695,226 bp) that is between the cdc6 gene and an adjacent ORF shows almost all the characteristics of known replication origins, i.e., it is highly rich in AT composition (80%) and contains multiple copies of repeat elements and AT stretches. Therefore, these lines of evidence strongly suggest that the identified region is a replication origin, which is designated as oriC1. The analysis of the y component of the Z curve, i.e., MK disparity curve, suggests the presence of another replication origin corresponding to one of the peaks in the MK disparity curve at around 1,388 kb of the genome. [ABSTRACT FROM AUTHOR]

The hydride carrier coenzyme F420 contains the unusual chromophore 7,8-didemethyl-8-hydroxy-5-deazariboflavin (FO). Microbes that generate F420 produce this FO moiety using a pyrimidine intermediate from riboflavin biosynthesis and the 4-hydroxyphenylpyruvate precursor of tyrosine. The fbiC gene, cloned from Mycobacterium smegmatis, encodes the bifunctional FO synthase. Expression of this protein in Escherichia coli caused the host cells to produce FO during growth, and activated cell-free extracts catalyze FO biosynthesis in vitro. FO synthase in the methanogenic euryarchaeon Methanocaldococcus jannaschii comprises two proteins encoded by cofG (MJ0446) and cofH (MJ1431). Both subunits were required for FO biosynthesis in vivo and in vitro. Cyanobacterial genomes encode homologs of both genes, which are used to produce the coenzyme for FO-dependent DNA photolyases. A molecular phylogeny of the paralogous cofG and cofH genes is consistent with the genes being vertically inherited within the euryarchaeal, cyanobacterial, and actinomycetal lineages. Ancestors of the cyanobacteria and actinomycetes must have acquired the two genes, which subsequently fused in actinomycetes. Both CofG and CofH have putative radical S-adenosylmethionine binding motifs, and pre-incubation with S-adenosylmethionine, Fe2+, sulfide, and dithionite stimulates FO production. Therefore a radical reaction mechanism is proposed for the biosynthesis of FO. [ABSTRACT FROM AUTHOR]

We utilized several computational approaches to evaluate the binding energies of tyrosine (Tyr) and several unnatural Tyr analogs, to several orthogonal aaRSes derived from Methanocaldococcus jannaschii and Escherichia coli tyrosyl-tRNA synthetases. The present study reveals the following: (1) AutoDock Vina and ROSETTA were able to distinguish binding energy differences for individual pairs of favorable and unfavorable aaRS-amino acid complexes, but were unable to cluster together all experimentally verified favorable complexes from unfavorable aaRS-Tyr complexes; (2) MD-MM/PBSA provided the best prediction accuracy in terms of clustering favorable and unfavorable enzyme-substrate complexes, but also required the highest computational cost; and (3) MM/PBSA based on single energy-minimized structures has a significantly lower computational cost compared to MD-MM/PBSA, but still produced sufficiently accurate predictions to cluster aaRS-amino acid interactions. Although amino acid-aaRS binding is just the first step in a complex series of processes to acylate a tRNA with its corresponding amino acid, the difference in binding energy, as shown by MD-MM/PBSA, is important for a mutant orthogonal aaRS to distinguish between a favorable unnatural amino acid (unAA) substrate from unfavorable natural amino acid substrates. Our computational study should assist further designing and engineering of orthogonal aaRSes for the genetic encoding of novel unAAs. [ABSTRACT FROM AUTHOR]