Shotgun proteomics of the haloarchaeon Haloferax volcanii

Haloferax volcanii, an extreme halophile originally isolated from the Dead Sea, is used worldwide as a model organism for furthering our understanding of archaeal cell physiology. In this study, a combination of approaches was used to identify a total of 1296 proteins, representing 32% of the theoretical proteome of this haloarchaeon. This included separation of (phospho)proteins/peptides by 2-dimensional gel electrophoresis (2-D), immobilized metal affinity chromatography (IMAC), metal oxide affinity chromatography (MOAC), and Multidimensional Protein Identification Technology (MudPIT) including strong cation exchange (SCX) chromatography coupled with reversed phase (RP) HPLC. Proteins were identified by tandem mass spectrometry (MS/MS) using nanoelectrospray ionization hybrid quadrupole time-of-flight (QSTAR XL Hybrid LC/MS/MS System) and quadrupole ion trap (Thermo LCQ Deca). Results indicate that a SCX RP HPLC fractionation coupled with MS/MS provides the best high-throughput workflow for overall protein identification.     

Improvement of two-dimensional gel electrophoresis proteome maps of the haloarchaeon Haloferax volcanii

Proteins of haloarchaea are remarkably unstable in low-ionic-strength solvents and tend to aggregate under standard two-dimensional (2-D) gel electrophoresis conditions, causing strong horizontal streaking. We have developed a new approach to generate 2-D maps of halophilic proteins which included washing cells with 1.5 M Tris-HCl buffer. In addition, proteins were precipitated with acetone, solubilized with urea and thiourea in the presence of the sulfobetaine detergent 3-[(3-cholamidopropyl)dimethylamino]-1-propanesulfonate (CHAPS), reduced with tributylphosphine (TBP), and separated with microrange strips of immobilized pH gradients (pH 3.9-5.1). This combination enabled the construction of highly reproducible 2-D maps of Haloferax volcanii proteins.     

Gene conversion results in the equalization of genome copies in the polyploid haloarchaeon Haloferax volcanii

Haloferax volcanii is highly polyploid and contains about 20 copies of the major chromosome. A heterozygous strain was constructed that contained two different types of genomes: the leuB locus contained either the wild-type leuB gene or a leuB:trpA gene introduced by gene replacement. As the trpA locus is devoid of the wild-type trpA gene, growth in the absence of both amino acids is only possible when both types of genomes are simultaneously present, exemplifying gene redundancy and the potential to form heterozygous cells as one possible evolutionary advantage of polyploidy. The heterozygous strain was grown (i) in the presence of tryptophan, selecting for the presence of leuB, (ii) in the presence of leucine selecting for leuB:trpA and (iii) in the absence of selection. Both types of genomes were quantified with real-time PCR. The first condition led to a complete loss of leuB:trpA-containing genomes, while under the second condition leuB-containing genomes were lost. Also in the absence of selection gene conversion led to a fast equalization of genomes and resulted in homozygous leuB-containing cells. Gene conversion leading to genome equalization can explain the escape from 'Muller's ratchet' as well as the ease of mutant construction using polyploid haloarchaea.     

Proteasomal components required for cell growth and stress responses in the haloarchaeon Haloferax volcanii

Little is known regarding the biological roles of archaeal proteases. The haloarchaeon Haloferax volcanii is an ideal model for understanding these enzymes, as it is one of few archaea with an established genetic system. In this report, a series of H. volcanii mutant strains with markerless and/or conditional knockouts in each known proteasome gene was systematically generated and characterized. This included single and double knockouts of genes encoding the 20S core alpha1 (psmA), beta (psmB), and alpha2 (psmC) subunits as well as genes (panA and panB) encoding proteasome-activating nucleotidase (PAN) proteins closely related to the regulatory particle triple-A ATPases (Rpt) of eukaryotic 26S proteasomes. Our results demonstrate that 20S proteasomes are required for growth. Although synthesis of 20S proteasomes containing either alpha1 or alpha2 could be separately abolished via gene knockout with little to no impact on growth, conditional depletion of either beta alone or alpha1 and alpha2 together rendered the cells inviable. In contrast, the PAN proteins were not essential based on the robust growth of the panA panB double knockout strain. Deletion of genes encoding either alpha1 or PanA did, however, render cells more sensitive to growth on organic versus inorganic nitrogen sources and hypo-osmotic stress and limited growth in the presence of l-canavanine. Abolishment of alpha1 synthesis also had a severe impact on the ability of cells to withstand thermal stress. This contrasted with what was seen for panA knockouts, which displayed enhanced thermotolerance. Together, these results provide new and important insight into the biological role of proteasomes in archaea.     

The 2-oxoacid dehydrogenase multienzyme complex of Haloferax volcanii

Those aerobic archaea whose genomes have been sequenced possess four adjacent genes that, by sequence comparisons with bacteria and eukarya, appear to encode the component enzymes of a 2-oxoacid dehydrogenase multienzyme complex. However, no catalytic activity of any such complex has ever been detected in the archaea. In Thermoplasma acidophilum, evidence has been presented that the heterologously expressed recombinant enzyme possesses activity with the branched chain 2-oxoacids and, to a lesser extent, with pyruvate. In the current paper, we demonstrate that in Haloferax volcanii the four genes are transcribed as an operon in vivo. However, no functional complex or individual enzyme, except for the dihydrolipoamide dehydrogenase component, could be detected in this halophile grown on a variety of carbon sources. Dihydrolipoamide dehydrogenase is present at low catalytic activities, the level of which is increased three to fourfold when Haloferax volcanii is grown on the branched-chain amino acids valine, leucine and isoleucine.     

Functional role for a 2-oxo acid dehydrogenase in the halophilic archaeon Haloferax volcanii

The archaeon Haloferax volcanii was previously shown to contain and transcribe the genes for a 2-oxo acid dehydrogenase (OADH) complex, but their presence remained a mystery because no enzymatic activity with any of the known OADH substrates could be found, and an inactivation of one of the genes did not lead to any phenotype. Here we report the identification of an additional oadh gene cluster in the genome of H. volcanii. In contrast to previously known oadh loci, it contains three genes, oadh2A1, oadh2A2, and oadh2ld, with coding capacity for the E1alpha and E1beta subunits and an unattached lipoyl domain, but it is devoid of the genes for a complete E2 and an E3. The genes were isolated by complementation of a nitrate respiration-deficient mutant of H. volcanii and therefore were shown to be functional in vivo. Phylogenetic analyses revealed that the deduced E1alpha and E1beta subunits of OADH2 group with bacterial acetoin dehydrogenases but not with the OADH1 subunits, and thus, H. volcanii has obtained the two gene groups independently. Comparison of the wild type and the mutant allowed us to exclude a function of OADH2 in the aerobic or anaerobic degradation of acetoin or glucose. Instead, it could be shown that OADH2 is important during nitrate-respirative growth on Casamino Acids. Many physiological and biochemical experiments failed to indicate that OADH2 uses any of the previously known OADH substrates. Growth potentials of the mutant were markedly different in media with a single carbon source versus media with mixed carbon sources.     

Defining the topology of the N-glycosylation pathway in the halophilic archaeon Haloferax volcanii

In Eukarya, N glycosylation involves the actions of enzymes working on both faces of the endoplasmic reticulum membrane. The steps of bacterial N glycosylation, in contrast, transpire essentially on the cytoplasmic side of the plasma membrane, with only transfer of the assembled glycan to the target protein occurring on the external surface of the cell. For Archaea, virtually nothing is known about the topology of enzymes involved in assembling those glycans that are subsequently N linked to target proteins on the external surface of the cell. To remedy this situation, subcellular localization and topology predictive algorithms, protease accessibility, and immunoblotting, together with cysteine modification following site-directed mutagenesis, were enlisted to define the topology of Haloferax volcanii proteins experimentally proven to participate in the N-glycosylation process. AglJ and AglD, involved in the earliest and latest stages, respectively, of assembly of the pentasaccharide decorating the H. volcanii S-layer glycoprotein, were shown to present their soluble N-terminal domain, likely containing the putative catalytic site of each enzyme, to the cytosol. The same holds true for Alg5-B, Dpm1-A, and Mpg1-D, proteins putatively involved in this posttranslational event. The results thus point to the assembly of the pentasaccharide linked to certain Asn residues of the H. volcanii S-layer glycoprotein as occurring within the cell.     

Post-translational modification of the S-layer glycoprotein occurs following translocation across the plasma membrane of the haloarchaeon Haloferax volcanii.

The halophilic archaeon Haloferax volcanii is surrounded by a protein shell solely comprised of the S-layer glycoprotein. While the gene sequence and glycosylation pattern of the protein and indeed the three-dimensional structure of the surface layer formed by the protein have been described, little is known of the biosynthesis of the S-layer glycoprotein. In the following, pulse-chase radiolabeling and cell-fractionation studies were employed to reveal that newly synthesized S-layer glycoprotein undergoes a maturation step following translocation of the protein across the plasma membrane. The processing step, detected as an increase in the apparent molecular mass of the S-layer glycoprotein, is unaffected by inhibition of protein synthesis and is apparently unrelated to glycosylation of the protein. Maturation requires the presence of magnesium ions, involved in membrane association of the S-layer glycoprotein, and results in increased hydrophobicity of the protein as revealed by enhanced detergent binding. Thus, along with protein glycosylation, additional post-translational modifications apparently occur on the external face of the haloarchaeal plasma membrane, the proposed topological homologue of the lumenal face of the eukaryal endoplasmic reticulum membrane.     

Membrane binding of SRP pathway components in the halophilic archaea Haloferax volcanii.

Across evolution, the signal recognition particle pathway targets extra-cytoplasmic proteins to membranous translocation sites. Whereas the pathway has been extensively studied in Eukarya and Bacteria, little is known of this system in Archaea. In the following, membrane association of FtsY, the prokaryal signal recognition particle receptor, and SRP54, a central component of the signal recognition particle, was addressed in the halophilic archaea Haloferax volcanii. Purified H. volcanii FtsY, the FtsY C-terminal GTP-binding domain (NG domain) or SRP54, were combined separately or in different combinations with H. volcanii inverted membrane vesicles and examined by gradient floatation to differentiate between soluble and membrane-bound protein. Such studies revealed that both FtsY and the FtsY NG domain bound to H. volcanii vesicles in a manner unaffected by proteolytic pretreatment of the membranes, implying that in Archaea, FtsY association is mediated through the membrane lipids. Indeed, membrane association of FtsY was also detected in intact H. volcanii cells. The contribution of the NG domain to FtsY binding in halophilic archaea may be considerable, given the low number of basic charges found at the start of the N-terminal acidic domain of haloarchaeal FtsY proteins (the region of the protein thought to mediate FtsY-membrane association in Bacteria). Moreover, FtsY, but not the NG domain, was shown to mediate membrane association of H. volcanii SRP54, a protein that did not otherwise interact with the membrane.     

Genomic stability in the archaeae Haloferax volcanii and Haloferax mediterranei.

Through hybridization of available probes, we have added nine genes to the macrorestriction map of the Haloferax mediterranei chromosome and five genes to the contig map of Haloferax volcanii. Additionally, we hybridized 17 of the mapped cosmid clones from H. volcanii to the H. mediterranei genome. The resulting 35-point chromosomal comparison revealed only two inversions and a few translocations. Forces known to promote rearrangement, common in the haloarchaea, have been ineffective in changing global gene order throughout the nearly 10(7) years of these species' divergent evolution.     

Chemical cross-linking, mass spectrometry, and in silico modeling of proteasomal 20S core particles of the haloarchaeon Haloferax volcanii

A fast and accurate method is reported to generate distance constraints between juxtaposited amino acids and to validate molecular models of halophilic protein complexes. Proteasomal 20S core particles (CPs) from the haloarchaeon Haloferax volcanii were used to investigate the quaternary structure of halophilic proteins based on their symmetrical, yet distinct subunit composition. Proteasomal CPs are cylindrical barrel-like structures of four-stacked homoheptameric rings of α- and β-type subunits organized in α(7)β(7) β(7)α(7) stoichiometry. The CPs of H. volcanii are formed from a single type of β subunit associated with α1 and/or α2 subunits. Tandem affinity chromatography and new genetic constructs were used to separately isolate α1(7)β(7)β(7)α1(7) and α2(7)β(7)β(7)α2(7) CPs from H. volcanii. Chemically cross-linked peptides of the H. volcanii CPs were analyzed by high-performance mass spectrometry and an open modification search strategy to first generate and then to interpret the resulting tandem mass spectrometric data. Distance constraints obtained by chemical cross-linking mass spectrometry, together with the available structural data of nonhalophilic CPs, facilitated the selection of accurate models of H. volcanii proteasomal CPs composed of α1-, α2-, and β-homoheptameric rings from several different possible structures from Protein Data Bank.