Effect of proteasome inhibitor clasto-lactacystin-beta-lactone on the proteome of the haloarchaeon Haloferax volcanii. (41/150)

Proteasomes play key roles in a variety of eukaryotic cell functions, including translation, transcription, metabolism, DNA repair and cell-cycle control. The biological functions of these multicatalytic proteases in archaea, however, are poorly understood. In this study, Haloferax volcanii was used as a model to determine the influence the proteasome-specific inhibitor clasto-lactacystin-beta-lactone (cLbetaL) has on archaeal proteome composition. Addition of 20-30 microM cLbetaL had a widespread effect on the proteome, with a 38-42 % increase in the number of 2-D gel electrophoresis (2-DE) protein spots, from an average of 627 to 1036 spots. Protein identities for 17 of the spots that were easily separated by 2-DE and unique and/or increased 2- to 14-fold in the cLbetaL-treated cells were determined by tandem mass spectrometry (MS/MS). These included protein homologues of the DJ-1/ThiJ family, mobilization of sulfur system, translation elongation factor EF-1 A, ribosomal proteins, tubulin-like FtsZ, divalent metal ABC transporter, dihydroxyacetone kinase DhaL, aldehyde dehydrogenase and 2-oxoacid decarboxylase E1beta. Based on these results, inhibition of H. volcanii proteasomes had a global influence on proteome composition, including proteins involved in central functions of the cell.  (+info)

Structure in an extreme environment: NMR at high salt. (42/150)

Proteins from halophiles have adapted to challenging environmental conditions and require salt for their structure and function. How halophilic proteins adapted to a hypersaline environment is still an intriguing question. It is important to mimic the physiological conditions of the archae extreme halophiles when characterizing their enzymes, including structural characterization. The NMR derived structure of Haloferax volcanii dihydrofolate reductase in 3.5 M NaCl is presented, and represents the first high salt structure calculated using NMR data. Structure calculations show that this protein has a solution structure which is similar to the previously determined crystal structure with a difference at the N terminus of beta3 and the type of beta-turn connection beta7 and beta8.  (+info)

Transcriptional linkage of Haloferax volcanii proteasomal genes with non-proteasomal gene neighbours including RNase P, MOSC domain and SAM-methyltransferase homologues. (43/150)

Comparative genomics reveals a common theme of 20S proteasome and proteasome-activating nucleotidase genes dispersed throughout archaeal genomes yet arranged in conserved linkages with gene homologues of translation and/or transcription machineries. To provide biological evidence for these linkages as well as insight into proteasome operon organization, transcripts of the five proteasomal genes of the halophilic archaeon Haloferax volcanii were analysed by Northern (RNA) blotting, RT-PCR and primer extension. These included psmA, psmB and psmC, encoding the 20S proteasomal subunits alpha1, beta and alpha2, as well as panA and panB, encoding the PanA and PanB proteasome-activating nucleotidase proteins, respectively. All five of these genes are dispersed throughout the H. volcanii genome. For each proteasomal gene, a distinct transcript was detected by Northern blotting that was similar in size to the respective coding region. For both psmA and psmC, an additional transcript was detected that was 1.34 and 0.85 kb greater, respectively, than the coding region. Further analysis by Northern blotting and RT-PCR revealed that psmA was co-transcribed with genes encoding a Pop5 homologue of the RNase P endoRNase as well as an S-adenosylmethionine (SAM)-dependent methyltransferase. Likewise, psmC was co-transcribed with a downstream gene encoding a molybdenum cofactor sulfurase C-terminal (MOSC) domain protein. Additional proteasomal and neighbouring gene-specific transcriptional linkages were detected by RT-PCR. These results provide the first evidence that proteasome and tRNA modification genes are co-transcribed, reveal that a number of additional enzymes including those predicted to facilitate metal-sulfur cluster assembly are co-regulated with proteasomes at the transcriptional level, and provide further insight into proteasome gene transcription in archaea.  (+info)

Three 2-oxoacid dehydrogenase operons in Haloferax volcanii: expression, deletion mutants and evolution. (44/150)

Two unrelated protein families catalyse the oxidative decarboxylation of 2-oxoacids, i.e. the 2-oxoacid dehydrogenase complexes (OADHCs) and the 2-oxoacid ferredoxin oxidoreductases (OAFORs). In halophilic archaea, OAFORs were found to be responsible for decarboxylation of pyruvate and 2-oxoglutarate. Nevertheless, two gene clusters encoding OADHCs were found previously in Haloferax volcanii, but their biological function remained obscure. Here a third oadhc gene cluster of H. volcanii is presented. To characterize the function, the genes encoding the E1 subunit were inactivated in all three gene clusters by in-frame deletions. Under aerobic conditions none of the three mutants showed any phenotypic difference from the wild-type in various media. However, growth yields of two mutants were considerably lower than that of wild-type under nitrate-respirative conditions in complex medium. Northern blot analyses revealed (1) that polycistronic transcripts are formed and all three gene clusters are bona fide operons and (2) that transcription of all three operons is induced under anaerobic conditions compared to aerobic conditions. Taken together, the three H. volcanii enzymes do not fulfil one of the 'usual' aerobic functions of typical OADHCs, but decarboxylate an as-yet-unidentified novel substrate under anaerobic conditions. A survey of all 28 fully sequenced archaeal genomes revealed that nearly all archaea contain several OAFORs (three to four on average), suggesting that this protein family was already present in their last common ancestor. In contrast, only nine archaea encode one or two OADHCs, indicating that this protein family entered archaea by lateral transfer of the cognate genes from bacteria. This view is underscored by a phylogenetic tree of 33 archaeal and bacterial OADHCs.  (+info)

Genetic and proteomic analyses of a proteasome-activating nucleotidase A mutant of the haloarchaeon Haloferax volcanii. (45/150)

The halophilic archaeon Haloferax volcanii encodes two related proteasome-activating nucleotidase proteins, PanA and PanB, with PanA levels predominant during all phases of growth. In this study, an isogenic panA mutant strain of H. volcanii was generated. The growth rate and cell yield of this mutant strain were lower than those of its parent and plasmid-complemented derivatives. In addition, a consistent and discernible 2.1-fold increase in the number of phosphorylated proteins was detected when the panA gene was disrupted, based on phosphospecific fluorescent staining of proteins separated by 2-dimensional gel electrophoresis. Subsequent enrichment of phosphoproteins by immobilized metal ion and metal oxide affinity chromatography (in parallel and sequentially) followed by tandem mass spectrometry was employed to identify key differences in the proteomes of these strains as well as to add to the restricted numbers of known phosphoproteins within the Archaea. In total, 625 proteins (approximately 15% of the deduced proteome) and 9 phosphosites were identified by these approaches, and 31% (195) of the proteins were identified by multiple phosphoanalytical methods. In agreement with the phosphostaining results, the number of identified proteins that were reproducibly exclusive or notably more abundant in one strain was nearly twofold greater for the panA mutant than for the parental strain. Enriched proteins exclusive to or more abundant in the panA mutant (versus the wild type) included cell division (FtsZ, Cdc48), dihydroxyacetone kinase-linked phosphoenolpyruvate phosphotransferase system (EI, DhaK), and oxidoreductase homologs. Differences in transcriptional regulation and signal transduction proteins were also observed, including those differences (e.g., OsmC and BolA) which suggest that proteasome deficiency caused an up-regulation of stress responses (e.g., OsmC versus BolA). Consistent with this, components of the Fe-S cluster assembly, protein-folding, DNA binding and repair, oxidative and osmotic stress, phosphorus assimilation, and polyphosphate synthesis systems were enriched and identified as unique to the panA mutant. The cumulative proteomic data not only furthered our understanding of the archaeal proteasome system but also facilitated the assembly of the first subproteome map of H. volcanii.  (+info)

Overlapping activator sequences determined for two oppositely oriented promoters in halophilic Archaea. (46/150)

Transcription of the genomic region involved in gas vesicle formation in Halobacterium salinarum (p-vac) and Haloferax mediterranei (mc-vac) is driven by two divergent promoters, P(A) and P(D), separated by only 35 nt. Both promoters are activated by the transcription activator GvpE which in the case of P(mcA) requires a 20-nt sequence (UAS) consisting of two conserved 8-nt sequence portions located upstream of BRE. Here, we determined the two UAS elements in the promoter region of p-vac by scanning mutageneses using constructs containing P(pD) (without P(pA)) fused to the bgaH reporter gene encoding an enzyme with beta-galactosidase activity, or the dual reporter construct pApD with P(pD) fused to bgaH and P(pA) to an altered version of gvpA. The two UAS elements found exhibited a similar extension and distance to BRE as previously determined for the UAS in P(mcA). Their distal 8-nt portions almost completely overlapped in the centre of P(pD)-P(pA), and mutations in this region negatively affected the GvpE-mediated activation of both promoters. Any alteration of the distance between BRE and UAS resulted in the loss of the GvpE activation, as did a complete substitution of the proximal 8-nt portion, underlining that a close location of UAS and BRE was very important.  (+info)

Experimental characterization of Cis-acting elements important for translation and transcription in halophilic archaea. (47/150)

The basal transcription apparatus of archaea is well characterized. However, much less is known about the mechanisms of transcription termination and translation initation. Recently, experimental determination of the 5'-ends of ten transcripts from Pyrobaculum aerophilum revealed that these are devoid of a 5'-UTR. Bioinformatic analysis indicated that many transcripts of other archaeal species might also be leaderless. The 5'-ends and 3'-ends of 40 transcripts of two haloarchaeal species, Halobacterium salinarum and Haloferax volcanii, have been determined. They were used to characterize the lengths of 5'-UTRs and 3'-UTRs and to deduce consensus sequence-elements for transcription and translation. The experimental approach was complemented with a bioinformatics analysis of the H. salinarum genome sequence. Furthermore, the influence of selected 5'-UTRs and 3'-UTRs on transcript stability and translational efficiency in vivo was characterized using a newly established reporter gene system, gene fusions, and real-time PCR. Consensus sequences for basal promoter elements could be refined and a novel element was discovered. A consensus motif probably important for transcriptional termination was established. All 40 haloarchaeal transcripts analyzed had a 3'-UTR (average size 57 nt), and their 3'-ends were not posttranscriptionally modified. Experimental data and genome analyses revealed that the majority of haloarchaeal transcripts are leaderless, indicating that this is the predominant mode for translation initiation in haloarchaea. Surprisingly, the 5'-UTRs of most leadered transcripts did not contain a Shine-Dalgarno (SD) sequence. A genome analysis indicated that less than 10% of all genes are preceded by a SD sequence and even most proximal genes in operons lack a SD sequence. Seven different leadered transcripts devoid of a SD sequence were efficiently translated in vivo, including artificial 5'-UTRs of random sequences. Thus, an interaction of the 5'-UTRs of these leadered transcripts with the 16S rRNA could be excluded. Taken together, either a scanning mechanism similar to the mechanism of translation initiation operating in eukaryotes or a novel mechanism must operate on most leadered haloarchaeal transcripts.  (+info)

Identification of AglE, a second glycosyltransferase involved in N glycosylation of the Haloferax volcanii S-layer glycoprotein. (48/150)

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