Haloferax volcanii AglB and AglD are involved in N-glycosylation of the S-layer glycoprotein and proper assembly of the surface layer

In this study, the effects of deleting two genes previously implicated in Haloferax volcanii N-glycosylation on the assembly and attachment of a novel Asn-linked pentasaccharide decorating the H. volcanii S-layer glycoprotein were considered. Mass spectrometry revealed the pentasaccharide to comprise two hexoses, two hexuronic acids and an additional 190 Da saccharide. The absence of AglD prevented addition of the final hexose to the pentasaccharide, while cells lacking AglB were unable to N-glycosylate the S-layer glycoprotein. In AglD-lacking cells, the S-layer glycoprotein-based surface layer presented both an architecture and protease susceptibility different from the background strain. By contrast, the absence of AglB resulted in enhanced release of the S-layer glycoprotein. H. volcanii cells lacking these N-glycosylation genes, moreover, grew significantly less well at elevated salt levels than did cells of the background strain. Thus, these results offer experimental evidence showing that N-glycosylation endows H. volcanii with an ability to maintain an intact and stable cell envelope in hypersaline surroundings, ensuring survival in this extreme environment.     

Identification of AglE, a second glycosyltransferase involved in N glycosylation of the Haloferax volcanii S-layer glycoprotein

Archaea, like Eukarya and Bacteria, are able to N glycosylate select protein targets. However, in contrast to relatively advanced understanding of the eukaryal N glycosylation process and the information being amassed on the bacterial process, little is known of this posttranslational modification in Archaea. Toward remedying this situation, the present report continues ongoing efforts to identify components involved in the N glycosylation of the Haloferax volcanii S-layer glycoprotein. By combining gene deletion together with mass spectrometry, AglE, originally identified as a homologue of murine Dpm1, was shown to play a role in the addition of the 190-Da sugar subunit of the novel pentasaccharide decorating the S-layer glycoprotein. Topological analysis of an AglE-based chimeric reporter assigns AglE as an integral membrane protein, with its N terminus and putative active site facing the cytoplasm. These finding, therefore, contribute to the developing picture of the N glycosylation pathway in Archaea.     

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.     

Primary structure and glycosylation of the S-layer protein of Haloferax volcanii.

The outer surface of the archaebacterium Haloferax volcanii (formerly named Halobacterium volcanii) is covered with a hexagonally packed surface (S) layer. The gene coding for the S-layer protein was cloned and sequenced. The mature polypeptide is composed of 794 amino acids and is preceded by a typical signal sequence of 34 amino acid residues. A highly hydrophobic stretch of 20 amino acids at the C-terminal end probably serves as a transmembrane domain. Clusters of threonine residues are located adjacent to this membrane anchor. The S-layer protein is a glycoprotein containing both N- and O-glycosidic bonds. Glucosyl-(1----2)-galactose disaccharides are linked to threonine residues. The primary structure and the glycosylation pattern of the S-layer glycoproteins from Haloferax volcanii and from Halobacterium halobium were compared and found to exhibit distinct differences, despite the fact that three-dimensional reconstructions from electron micrographs revealed no structural differences at least to the 2.5-nm level attained so far (M. Kessel, I. Wildhaber, S. Cohe, and W. Baumeister, EMBO J. 7:1549-1554, 1988).     

A Rhomboid Protease Gene Deletion Affects a Novel Oligosaccharide N-Linked to the S-layer Glycoprotein of Haloferax volcanii

Rhomboid proteases occur in all domains of life; however, their physiological role is not completely understood, and nothing is known of the biology of these enzymes in Archaea. One of the two rhomboid homologs of Haloferax volcanii (RhoII) is fused to a zinc finger domain. Chromosomal deletion of rhoII was successful, indicating that this gene is not essential for this organism; however, the mutant strain (MIG1) showed reduced motility and increased sensitivity to novobiocin. Membrane preparations of MIG1 were enriched in two glycoproteins, identified as the S-layer glycoprotein and an ABC transporter component. The H. volcanii S-layer glycoprotein has been extensively used as a model to study haloarchaeal protein N-glycosylation. HPLC analysis of oligosaccharides released from the S-layer glycoprotein after PNGase treatment revealed that MIG1 was enriched in species with lower retention times than those derived from the parent strain. Mass spectrometry analysis showed that the wild type glycoprotein released a novel oligosaccharide species corresponding to GlcNAc-GlcNAc(Hex)₂-(SQ-Hex)₆ in contrast to the mutant protein, which contained the shorter form GlcNAc₂(Hex)₂-SQ-Hex-SQ. A glycoproteomics approach of the wild type glycopeptide fraction revealed Asn-732 peptide fragments linked to the sulfoquinovose-containing oligosaccharide. This work describes a novel N-linked oligosaccharide containing a repeating SQ-Hex unit bound to Asn-732 of the H. volcanii S-layer glycoprotein, a position that had not been reported as glycosylated. Furthermore, this study provides the first insight on the biological role of rhomboid proteases in Archaea, suggesting a link between protein glycosylation and this protease family.     

Protein glycosylation as an adaptive response in Archaea: growth at different salt concentrations leads to alterations in Haloferax volcanii S-layer glycoprotein N-glycosylation

To cope with life in hypersaline environments, halophilic archaeal proteins are enriched in acidic amino acids. This strategy does not, however, offer a response to transient changes in salinity, as would post-translational modifications. To test this hypothesis, N-glycosylation of the Haloferax volcanii S-layer glycoprotein was compared in cells grown in high (3.4 M NaCl) and low (1.75 M NaCl) salt, as was the glycan bound to dolichol phosphate, the lipid upon which the N-linked glycan is assembled. In high salt, S-layer glycoprotein Asn-13 and Asn-83 are modified by a pentasaccharide, while dolichol phosphate is modified by a tetrasaccharide comprising the first four pentasaccharide residues. When the same targets were considered from cells grown in low salt, substantially less pentasaccharide was detected. At the same time, cells grown at low salinity contain dolichol phosphate modified by a distinct tetrasaccharide absent in cells grown at high salinity. The same tetrasaccharide modified S-layer glycoprotein Asn-498 in cells grown in low salt, whereas no glycan decorated this residue in cells grown in the high-salt medium. Thus, in response to changes in environmental salinity, Hfx. volcanii not only modulates the N-linked glycans decorating the S-layer glycoprotein but also the sites of such post-translational modification.     

ATP is required for K+ active transport in the archaebacterium Haloferax volcanii

The Archaebacterium Haloferax volcanii concentrates K⁺ up to 3.6 M. This creates a very large K⁺ ion gradient of between 500- to 1,000-fold across the cell membrane. H. volcanii cells can be partially depleted of their internal K⁺ but the residual K⁺ concentration cannot be lowered below 1.5 M. In these conditions, the cells retain the ability to take up potassium from the medium and to restore a high internal K⁺ concentration (3 to 3.2 M) via an energy dependent, active transport mechanism with a K _m of between 1 to 2 mM. The driving force for K⁺ transport has been explored. Internal K⁺ concentration is not in equilibrium with m suggesting that K⁺ transport cannot be accounted for by a passive uniport process. A requirement for ATP has been found. Indeed, the depletion of the ATP pool by arsenate or the inhibition of ATP synthesis by N,N-dicyclohexylcarbodiimide inhibits by 100% K⁺ transport even though membrane potential m is maintained under these conditions. By contrast, the necessity of a m for K⁺ accumulation has not yet been clearly demonstrated. K⁺ transport in H. volcanii can be compared with K⁺ transport via the Trk system in Escherichia coli.Abbreviations CCCP Carbonylcyanide m-chlorophenyl-hydrazone - DCCD N,N-dicyclohexylcarbodiimide - MES 2-[N-morpholino] ethane sulfonic acid - MOPS 3-[N-morpholino] propane sulfonic acid - TRIS Tris (hydroxymethyl) aminomethane - TPP tetraphenyl phosphonium     

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.     

Haloferax volcanii archaeosortase is required for motility,mating, and C‐terminal processing of the S‐layer glycoprotein

Cell surfaces are decorated by a variety of proteins that facilitate interactions with their environments and support cell stability. These secreted proteins are anchored to the cell by mechanisms that are diverse, and, in archaea, poorly understood. Recently published in silico data suggest that in some species a subset of secreted euryarchaeal proteins, which includes the S‐layer glycoprotein, is processed and covalently linked to the cell membrane by enzymes referred to as archaeosortases. In silico work led to the proposal that an independent, sortase‐like system for proteolysis‐coupled, carboxy‐terminal lipid modification exists in bacteria (exosortase) and archaea (archaeosortase). Here, we provide the first in vivo characterization of an archaeosortase in the haloarchaeal model organism Haloferax volcanii. Deletion of the artA gene (HVO_0915) resulted in multiple biological phenotypes: (a) poor growth, especially under low‐salt conditions, (b) alterations in cell shape and the S‐layer, (c) impaired motility, suppressors of which still exhibit poor growth, and (d) impaired conjugation. We studied one of the ArtA substrates, the S‐layer glycoprotein, using detailed proteomic analysis. While the carboxy‐terminal region of S‐layer glycoproteins, consisting of a putative threonine‐rich O‐glycosylated region followed by a hydrophobic transmembrane helix, has been notoriously resistant to any proteomic peptide identification, we were able to identify two overlapping peptides from the transmembrane domain present in the ΔartA strain but not in the wild‐type strain. This clearly shows that ArtA is involved in carboxy‐terminal post‐translational processing of the S‐layer glycoprotein. As it is known from previous studies that a lipid is covalently attached to the carboxy‐terminal region of the S‐layer glycoprotein, our data strongly support the conclusion that archaeosortase functions analogously to sortase, mediating proteolysis‐coupled, covalent cell surface attachment.     

Protein glycosylation in Haloferax volcanii: partial characterization of a 98-kDa glycoprotein

Eubacterium ramulus, a flavonoid-degrading anaerobic bacterium from the human gastrointestinal tract, was tested for its ability to transform the isoflavonoids genistein-7-O-glucoside (genistin), genistein and daidzein. Genistein was completely degraded by E. ramulus via 6'-hydroxy-O-desmethylangolensin to 2-(4-hydroxyphenyl)-propionic acid. Dihydrogenistein was neither observed as an intermediate in this transformation nor converted itself by growing cells or cell-free extracts of E. ramulus. Genistein-7-O-glucoside was partially transformed by way of genistein to the product 2-(4-hydroxyphenyl)-propionic acid. Daidzein was in part degraded to O-desmethylangolensin, the corresponding metabolite to 6'-hydroxy-O-desmethylangolensin. The hydroxyl group in position 6' of O-desmethylangolensin is crucial for further degradation.     

A bioluminescent reporter for the halophilic archaeon Haloferax volcanii

Haloarchaea have evolved to thrive in hypersaline environments. Haloferax volcanii is of particular interest due to its genetic tractability; however, few in vivo reporters exist for halophiles. Haloarchaeal proteins evolved characteristics that promote proper folding and function at high salt concentrations, but many mesophilic reporter proteins lack these characteristics. Mesophilic proteins that acquire salt-stabilizing mutations, however, can lead to proper function in haloarchaea. Using laboratory-directed evolution, we developed and demonstrated an in vivo luciferase that functions in the hypersaline cytosol of H. volcanii.

     

All three chaperonin genes in the archaeon Haloferax volcanii are individually dispensable

The Hsp60 or chaperonin class of molecular chaperones is divided into two phylogenetic groups: group I, found in bacteria, mitochondria and chloroplasts, and group II, found in eukaryotic cytosol and archaea. Group I chaperonins are generally essential in bacteria, although when multiple copies are found one or more of these are dispensable. Eukaryotes contain eight genes for group II chaperonins, all of which are essential, and it has been shown that these proteins assemble into double-ring complexes with eightfold symmetry where all proteins occupy specific positions in the ring. In archaea, there are one, two or three genes for the group II chaperonins, but whether they are essential for growth is unknown. Here we describe a detailed genetic, structural and biochemical analysis of these proteins in the halophilic archaeon, Haloferax volcanii. This organism contains three genes for group II chaperonins, and we show that all are individually dispensable but at least one must be present for growth. Two of the three possible double mutants can be constructed, but only one of the three genes is capable of fully complementing the stress-dependent phenotypes that these double mutants show. The chaperonin complexes are made up of hetero-oligomers with eightfold symmetry, and the properties of the different combinations of subunits derived from the mutants are distinct. We conclude that, although they are more homologous to eukaryotic than prokaryotic chaperonins, archaeal chaperonins have some redundancy of function.     

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.     

Identification and characterization of the unique N-linked glycan common to the flagellins and S-layer glycoprotein of Methanococcus voltae

The flagellum of Methanococcus voltae is composed of four structural flagellin proteins FlaA, FlaB1, FlaB2, and FlaB3. These proteins possess a total of 15 potential N-linked sequons (NX(S/T)) and show a mass shift on an SDS-polyacrylamide gel indicating significant post-translational modification. We describe here the structural characterization of the flagellin glycan from M. voltae using mass spectrometry to examine the proteolytic digests of the flagellin proteins in combination with NMR analysis of the purified glycan using a sensitive, cryogenically cooled probe. Nano-liquid chromatography-tandem mass spectrometry analysis of the proteolytic digests of the flagellin proteins revealed that they are post-translationally modified with a novel N-linked trisaccharide of mass 779 Da that is composed of three sugar residues with masses of 318, 258, and 203 Da, respectively. In every instance the glycan is attached to the peptide through the asparagine residue of a typical N-linked sequon. The glycan modification has been observed on 14 of the 15 sequon sites present on the four flagellin structural proteins. The novel glycan structure elucidated by NMR analysis was shown to be a trisaccharide composed of beta-ManpNAcA6Thr-(1-4)-beta-Glc-pNAc3NAcA-(1-3)-beta-GlcpNAc linked to Asn. In addition, the same trisaccharide was identified on a tryptic peptide of the S-layer protein from this organism implicating a common N-linked glycosylation pathway.     

Novel glycoproteins of the halophilic archaeon Haloferax volcanii

Archaea possess many eukaryote-like properties, including the ability to glycosylate proteins. Using oligosaccharide staining and lectin binding, this study revealed the existence of several glycosylated Haloferax volcanii membrane proteins, besides the previously reported surface layer (S-layer) glycoprotein. While the presence of glycoproteins in archaeal S-layers and flagella is well-documented, few archaeal glycoproteins that are not part of these structures have been reported. The glycosylated 150, 98, 58 and 54 kDa protein species detected were neither precursors nor breakdown products of the 190 kDa S-layer glycoprotein. Furthermore, these novel glycoproteins were outwardly oriented and intimately associated with the membrane.