Differential regulation of the PanA and PanB proteasome-activating nucleotidase and 20S proteasomal proteins of the haloarchaeon Haloferax volcanii

CdrS Is a Global Transcriptional Regulator Influencing Cell Division in Haloferax volcanii

Transcriptional regulators that integrate cellular and environmental signals to control cell division are well known in bacteria and eukaryotes, but their existence is poorly understood in archaea. We identified a conserved gene (cdrS) that encodes a small protein and is highly transcribed in the model archaeon Haloferax volcanii. The cdrS gene could not be deleted, but CRISPR interference (CRISPRi)-mediated repression of the cdrS gene caused slow growth and cell division defects and changed the expression of multiple genes and their products associated with cell division, protein degradation, and metabolism. Consistent with this complex regulatory network, overexpression of cdrS inhibited cell division, whereas overexpression of the operon encoding both CdrS and a tubulin-like cell division protein (FtsZ2) stimulated division. Chromatin immunoprecipitation-DNA sequencing (ChIP-Seq) identified 18 DNA-binding sites of the CdrS protein, including one upstream of the promoter for a cell division gene, ftsZ1, and another upstream of the essential gene dacZ, encoding diadenylate cyclase involved in c-di-AMP signaling, which is implicated in the regulation of cell division. These findings suggest that CdrS is a transcription factor that plays a central role in a regulatory network coordinating metabolism and cell division. IMPORTANCE Cell division is a central mechanism of life and is essential for growth and development. Members of the Bacteria and Eukarya have different mechanisms for cell division, which have been studied in detail. In contrast, cell division in members of the Archaea is still understudied, and its regulation is poorly understood. Interestingly, different cell division machineries appear in members of the Archaea, with the Euryarchaeota using a cell division apparatus based on the tubulin-like cytoskeletal protein FtsZ, as in bacteria. Here, we identify the small protein CdrS as essential for survival and a central regulator of cell division in the euryarchaeon Haloferax volcanii. CdrS also appears to coordinate other cellular pathways, including synthesis of signaling molecules and protein degradation. Our results show that CdrS plays a sophisticated role in cell division, including regulation of numerous associated genes. These findings are expected to initiate investigations into conditional regulation of division in archaea.

The Role of Stress Proteins in Haloarchaea and Their Adaptive Response to Environmental Shifts

Over the years, in order to survive in their natural environment, microbial communities have acquired adaptations to nonoptimal growth conditions. These shifts are usually related to stress conditions such as low/high solar radiation, extreme temperatures, oxidative stress, pH variations, changes in salinity, or a high concentration of heavy metals. In addition, climate change is resulting in these stress conditions becoming more significant due to the frequency and intensity of extreme weather events. The most relevant damaging effect of these stressors is protein denaturation. To cope with this effect, organisms have developed different mechanisms, wherein the stress genes play an important role in deciding which of them survive. Each organism has different responses that involve the activation of many genes and molecules as well as downregulation of other genes and pathways. Focused on salinity stress, the archaeal domain encompasses the most significant extremophiles living in high-salinity environments. To have the capacity to withstand this high salinity without losing protein structure and function, the microorganisms have distinct adaptations. The haloarchaeal stress response protects cells against abiotic stressors through the synthesis of stress proteins. This includes other heat shock stress proteins (Hsp), thermoprotectants, survival proteins, universal stress proteins, and multicellular structures. Gene and family stress proteins are highly conserved among members of the halophilic archaea and their study should continue in order to develop means to improve for biotechnological purposes. In this review, all the mechanisms to cope with stress response by haloarchaea are discussed from a global perspective, specifically focusing on the role played by universal stress proteins.

Molecular Factors of Hypochlorite Tolerance in the Hypersaline Archaeon Haloferax volcanii

Halophilic archaea thrive in hypersaline conditions associated with desiccation, ultraviolet (UV) irradiation and redox active compounds, and thus are naturally tolerant to a variety of stresses. Here, we identified mutations that promote enhanced tolerance of halophilic archaea to redox-active compounds using Haloferax volcanii as a model organism. The strains were isolated from a library of random transposon mutants for growth on high doses of sodium hypochlorite (NaOCl), an agent that forms hypochlorous acid (HOCl) and other redox acid compounds common to aqueous environments of high concentrations of chloride. The transposon insertion site in each of twenty isolated clones was mapped using the following: (i) inverse nested two-step PCR (INT-PCR) and (ii) semi-random two-step PCR (ST-PCR). Genes that were found to be disrupted in hypertolerant strains were associated with lysine deacetylation, proteasomes, transporters, polyamine biosynthesis, electron transfer, and other cellular processes. Further analysis revealed a ΔpsmA1 (α1) markerless deletion strain that produces only the α2 and β proteins of 20S proteasomes was hypertolerant to hypochlorite stress compared with wild type, which produces α1, α2, and β proteins. The results of this study provide new insights into archaeal tolerance of redox active compounds such as hypochlorite.

Proteolytic systems of archaea: slicing, dicing, and mincing in the extreme

Archaea are phylogenetically distinct from bacteria, and some of their proteolytic systems reflect this distinction. Here, the current knowledge of archaeal proteolysis is reviewed as it relates to protein metabolism, protein homeostasis, and cellular regulation including targeted proteolysis by proteasomes associated with AAA-ATPase networks and ubiquitin-like modification. Proteases and peptidases that facilitate the recycling of peptides to amino acids as well as membrane-associated and integral membrane proteases are also reviewed.

Conformational switching in the coiled-coil domains of a proteasomal ATPase regulates substrate processing

Protein degradation in all domains of life requires ATPases that unfold and inject proteins into compartmentalized proteolytic chambers. Proteasomal ATPases in eukaryotes and archaea contain poorly understood N-terminally conserved coiled-coil domains. In this study, we engineer disulfide crosslinks in the coiled-coils of the archaeal proteasomal ATPase (PAN) and report that its three identical coiled-coil domains can adopt three different conformations: (1) in-register and zipped, (2) in-register and partially unzipped, and (3) out-of-register. This conformational heterogeneity conflicts with PAN's symmetrical OB-coiled-coil crystal structure but resembles the conformational heterogeneity of the 26S proteasomal ATPases' coiled-coils. Furthermore, we find that one coiled-coil can be conformationally constrained even while unfolding substrates, and conformational changes in two of the coiled-coils regulate PAN switching between resting and active states. This switching functionally mimics similar states proposed for the 26S proteasome from cryo-EM. These findings thus build a mechanistic framework to understand regulation of proteasome activity.

Ubiquitin-Like Proteasome System Represents a Eukaryotic-Like Pathway for Targeted Proteolysis in Archaea

The molecular mechanisms of targeted proteolysis in archaea are poorly understood, yet they may have deep evolutionary roots shared with the ubiquitin-proteasome system of eukaryotic cells. Here, we demonstrate in archaea that TBP2, a TATA-binding protein (TBP) modified by ubiquitin-like isopeptide bonds, is phosphorylated and targeted for degradation by proteasomes. Rapid turnover of TBP2 required the functions of UbaA (the E1/MoeB/ThiF homolog of archaea), AAA ATPases (Cdc48/p97 and Rpt types), a type 2 JAB1/MPN/MOV34 metalloenzyme (JAMM/MPN+) homolog (JAMM2), and 20S proteasomes. The ubiquitin-like protein modifier small archaeal modifier protein 2 (SAMP2) stimulated the degradation of TBP2, but SAMP2 itself was not degraded. Analysis of the TBP2 fractions that were not modified by ubiquitin-like linkages revealed that TBP2 had multiple N termini, including Met1-Ser2, Ser2, and Met1-Ser2(p) [where (p) represents phosphorylation]. The evidence suggested that the Met1-Ser2(p) form accumulated in cells that were unable to degrade TBP2. We propose a model in archaea in which the attachment of ubiquitin-like tags can target proteins for degradation by proteasomes and be controlled by N-terminal degrons. In support of a proteolytic mechanism that is energy dependent and recycles the ubiquitin-like protein tags, we find that a network of AAA ATPases and a JAMM/MPN+ metalloprotease are required, in addition to 20S proteasomes, for controlled intracellular proteolysis.

This study advances the fundamental knowledge of signal-guided proteolysis in archaea and sheds light on components that are related to the ubiquitin-proteasome system of eukaryotes. In archaea, the ubiquitin-like proteasome system is found to require function of an E1/MoeB/ThiF homolog, a type 2 JAMM/MPN+ metalloprotease, and a network of AAA ATPases for the targeted destruction of proteins. We provide evidence that the attachment of the ubiquitin-like protein is controlled by an N-terminal degron and stimulates proteasome-mediated proteolysis.

Global role of the membrane protease LonB in Archaea: Potential protease targets revealed by quantitative proteome analysis of a lonB mutant in Haloferax volcanii

The membrane-associated LonB protease is essential for viability in Haloferax volcanii, however, the cellular processes affected by this protease in archaea are unknown. In this study, the impact of a lon conditional mutation (down-regulation) on H. volcanii physiology was examined by comparing proteomes of parental and mutant cells using shotgun proteomics. A total of 1778 proteins were identified (44% of H. volcanii predicted proteome) and 142 changed significantly in amount (≥2 fold). Of these, 66 were augmented in response to Lon deficiency suggesting they could be Lon substrates. The "Lon subproteome" included soluble and predicted membrane proteins expected to participate in diverse cellular processes. The dramatic stabilization of phytoene synthase (57 fold) in concert with overpigmentation of lon mutant cells suggests that Lon controls carotenogenesis in H. volcanii. Several hypothetical proteins, which may reveal novel functions and/or be involved in adaptation to extreme environments, were notably increased (300 fold). This study, which represents the first proteome examination of a Lon deficient archaeal cell, shows that Lon has a strong impact on H. volcanii physiology evidencing the cellular processes controlled by this protease in Archaea. Additionally, this work provides a platform for the discovery of novel targets of Lon proteases.

BIOLOGICAL SIGNIFICANCE

The proteome of a Lon-deficient archaeal cell was examined for the first time showing that Lon has a strong impact on H. volcanii physiology and evidencing the proteins and cellular processes controlled by this protease in Archaea. This work will facilitate future investigations aiming to address Lon function in archaea and provides a platform for the discovery of endogenous targets of the archaeal-type Lon as well as novel targets/processes regulated by Lon proteases. This knowledge will advance the understanding on archaeal physiology and the biological function of membrane proteases in microorganisms.

Archaeal Tuc1/Ncs6 homolog required for wobble uridine tRNA thiolation is associated with ubiquitin-proteasome, translation, and RNA processing system homologs

While cytoplasmic tRNA 2-thiolation protein 1 (Tuc1/Ncs6) and ubiquitin-related modifier-1 (Urm1) are important in the 2-thiolation of 5-methoxycarbonylmethyl-2-thiouridine (mcm⁵s²U) at wobble uridines of tRNAs in eukaryotes, the biocatalytic roles and properties of Ncs6/Tuc1 and its homologs are poorly understood. Here we present the first report of an Ncs6 homolog of archaea (NcsA of Haloferax volcanii) that is essential for maintaining cellular pools of thiolated tRNA^Lys_UUU and for growth at high temperature. When purified from Hfx. volcanii, NcsA was found to be modified at Lys204 by isopeptide linkage to polymeric chains of the ubiquitin-fold protein SAMP2. The ubiquitin-activating E1 enzyme homolog of archaea (UbaA) was required for this covalent modification. Non-covalent protein partners that specifically associated with NcsA were also identified including UbaA, SAMP2, proteasome activating nucleotidase (PAN)-A/1, translation elongation factor aEF-1α and a β-CASP ribonuclease homolog of the archaeal cleavage and polyadenylation specificity factor 1 family (aCPSF1). Together, our study reveals that NcsA is essential for growth at high temperature, required for formation of thiolated tRNA^Lys_UUU and intimately linked to homologs of ubiquitin-proteasome, translation and RNA processing systems.

The LonB protease controls membrane lipids composition and is essential for viability in the extremophilic haloarchaeon Haloferax volcanii

Although homologs of the ATP-dependent Lon protease exist in all domains of life, the relevance of this protease in archaeal physiology remains a mystery. In this study, we have constructed and phenotypically characterized deletion and conditional lon mutants in the model haloarchaeon Haloferax volcanii to elucidate the role of the unusual membrane-bound LonB protease in archaea. Hvlon could be deleted from the chromosome only when a copy of the wild type gene was provided in trans suggesting that Lon is essential for survival in this archaeon. Successful complementation of the lethal phenotype of ΔHvlon was attained by expression of the heterologous protease gene Nmlon from the haloalkaliphilic archaeon Natrialba magadii, meaning that the biological function of Lon is conserved in these organisms. Suboptimal cellular levels of Lon protein affected growth rate, cell shape, cell pigmentation, lipid composition and sensitivity to various antibiotics. The contents of bacterioruberins and some polar lipids were increased in the lon mutants suggesting that Lon is linked to maintenance of membrane lipid balance which likely affects cell viability in this archaeon. The phenotypes associated to a membrane-bound LonB protease mutant were examined for the first time providing insight on the relevance of this protease in archaeal physiology.

Structural and biochemical properties of an extreme 'salt-loving' proteasome activating nucleotidase from the archaeon Haloferax volcanii

In eukaryotes, the 26S proteasome degrades ubiquitinylated proteins in an ATP-dependent manner. Archaea mediate a form of post-translational modification of proteins termed sampylation that resembles ubiquitinylation. Sampylation was identified in Haloferax volcanii, a moderate halophilic archaeon that synthesizes homologs of 26S proteasome subunits including 20S core particles and regulatory particle triple-A ATPases (Rpt)-like proteasome-associated nucleotidases (PAN-A/1 and PAN-B/2). To determine whether sampylated proteins associate with the Rpt subunit homologs, PAN-A/1 was purified to homogeneity from Hfx. volcanii and analyzed for its subunit stoichiometry, nucleotide-hydrolyzing activity and binding to sampylated protein targets. PAN-A/1 was found to be associated as a dodecamer (630 kDa) with a configuration in TEM suggesting a complex of two stacked hexameric rings. PAN-A/1 had high affinity for ATP (K m of ~0.44 mM) and hydrolyzed this nucleotide with a specific activity of 0.33 ± 0.1 μmol Pi/h per mg protein and maximum at 42 °C. PAN-A1 was stabilized by 2 M salt with a decrease in activity at lower concentrations of salt that correlated with dissociation of the dodecamer into trimers to monomers. Binding of PAN-A/1 to a sampylated protein was demonstrated by modification of a far Western blotting technique (derived from the standard Western blot method to detect protein-protein interaction in vitro) for halophilic proteins. Overall, our results support a model in which sampylated proteins associate with the PAN-A/1 AAA+ ATPase in proteasome-mediated proteolysis and/or protein remodeling and provide a method for assay of halophilic protein-protein interactions.

Prokaryotic proteasomes: nanocompartments of degradation

Proteasomes are self-compartmentalized energy-dependent proteolytic machines found in Archaea, Actinobacteria species of bacteria and eukaryotes. Proteasomes consist of two separate protein complexes, the core particle that hydrolyzes peptide bonds and an AAA+ ATPase domain responsible for the binding, unfolding and translocation of protein substrates into the core particle for degradation. Similarly to eukaryotes, proteasomes play a central role in protein degradation and can be essential in Archaea. Core particles associate with and utilize a variety of ATPase complexes to carry out protein degradation in Archaea. In actinobacterial species, such as Mycobacterium tuberculosis, proteasome-mediated degradation is associated with pathogenesis and does not appear to be essential. Interestingly, both actinobacterial species and Archaea use small proteins to covalently modify proteins, prokaryotic ubiquitin-like proteins (Pup) in Actinobacteria and ubiquitin-like small archaeal modifier proteins (SAMP) in Archaea. These modifications may play a role in proteasome targeting similar to the ubiquitin-proteasome system in eukaryotes.

Ionic strength-dependent conformations of a ubiquitin-like small archaeal modifier protein (SAMP1) from Haloferax volcanii

Eukaryotic ubiquitin and ubiquitin-like systems play crucial roles in various cellular biological processes. In this work, we determined the solution structure of SAMP1 from Haloferax volcanii by NMR spectroscopy. Under low ionic conditions, SAMP1 presented two distinct conformations, one folded β-grasp and the other disordered. Interestingly, SAMP1 underwent a conformational conversion from disorder to order with ion concentration increasing, indicating that the ordered conformation is the functional form of SAMP1 under the physiological condition of H. volcanii. Furthermore, SAMP1 could interact with proteasome-activating nucleotidase B, supposing a potential role of SAMP1 in the protein degradation pathway mediated by proteasome.

Archaeal proteasomes and sampylation

Archaea contain, both a functional proteasome and an ubiquitin-like protein conjugation system (termed sampylation) that is related to the ubiquitin proteasome system (UPS) of eukaryotes. Archaeal proteasomes have served as excellent models for understanding how proteins are degraded by the central energy-dependent proteolytic machine of eukaryotes, the 26S proteasome. While sampylation has only recently been discovered, it is thought to be linked to proteasome-mediated degradation in archaea. Unlike eukaryotes, sampylation only requires an E1 enzyme homolog of the E1-E2-E3 ubiquitylation cascade to mediate protein conjugation. Furthermore, recent evidence suggests that archaeal and eurkaryotic E1 enzyme homologs can serve dual roles in mediating protein conjugation and activating sulfur for incorporation into biomolecules. The focus of this book chapter is the energy-dependent proteasome and sampylation systems of Archaea.

Post-translation modification in Archaea: lessons from Haloferax volcanii and other haloarchaea

As an ever-growing number of genome sequences appear, it is becoming increasingly clear that factors other than genome sequence impart complexity to the proteome. Of the various sources of proteomic variability, post-translational modifications (PTMs) most greatly serve to expand the variety of proteins found in the cell. Likewise, modulating the rates at which different proteins are degraded also results in a constantly changing cellular protein profile. While both strategies for generating proteomic diversity are adopted by organisms across evolution, the responsible pathways and enzymes in Archaea are often less well described than are their eukaryotic and bacterial counterparts. Studies on halophilic archaea, in particular Haloferax volcanii, originally isolated from the Dead Sea, are helping to fill the void. In this review, recent developments concerning PTMs and protein degradation in the haloarchaea are discussed.

AglS, a novel component of the Haloferax volcanii N-glycosylation pathway, is a dolichol phosphate-mannose mannosyltransferase

In Haloferax volcanii, a series of Agl proteins mediates protein N-glycosylation. The genes encoding all but one of the Agl proteins are sequestered into a single gene island. The same region of the genome includes sequences also suspected but not yet verified as serving N-glycosylation roles, such as HVO_1526. In the following, HVO_1526, renamed AglS, is shown to be necessary for the addition of the final mannose subunit of the pentasaccharide N-linked to the surface (S)-layer glycoprotein, a convenient reporter of N-glycosylation in Hfx. volcanii. Relying on bioinformatics, topological analysis, gene deletion, mass spectrometry, and biochemical assays, AglS was shown to act as a dolichol phosphate-mannose mannosyltransferase, mediating the transfer of mannose from dolichol phosphate to the tetrasaccharide corresponding to the first four subunits of the pentasaccharide N-linked to the S-layer glycoprotein.

The archaeal proteasome is regulated by a network of AAA ATPases

The proteasome is the central machinery for targeted protein degradation in archaea, Actinobacteria, and eukaryotes. In its basic form, it consists of a regulatory ATPase complex and a proteolytic core particle. The interaction between the two is governed by an HbYX motif (where Hb is a hydrophobic residue, Y is tyrosine, and X is any amino acid) at the C terminus of the ATPase subunits, which stimulates gate opening of the proteasomal α-subunits. In archaea, the proteasome-interacting motif is not only found in canonical proteasome-activating nucleotidases of the PAN/ARC/Rpt group, which are absent in major archaeal lineages, but also in proteins of the CDC48/p97/VAT and AMA groups, suggesting a regulatory network of proteasomal ATPases. Indeed, Thermoplasma acidophilum, which lacks PAN, encodes one CDC48 protein that interacts with the 20S proteasome and activates the degradation of model substrates. In contrast, Methanosarcina mazei contains seven AAA proteins, five of which, both PAN proteins, two out of three CDC48 proteins, and the AMA protein, function as proteasomal gatekeepers. The prevalent presence of multiple, distinct proteasomal ATPases in archaea thus results in a network of regulatory ATPases that may widen the substrate spectrum of proteasomal protein degradation.

Diversity in prokaryotic glycosylation: an archaeal-derived N-linked glycan contains legionaminic acid

VP4, the major structural protein of the haloarchaeal pleomorphic virus, HRPV-1, is glycosylated. To define the glycan structure attached to this protein, oligosaccharides released by β-elimination were analysed by mass spectrometry and nuclear magnetic resonance spectroscopy. Such analyses showed that the major VP4-derived glycan is a pentasaccharide comprising glucose, glucuronic acid, mannose, sulphated glucuronic acid and a terminal 5-N-formyl-legionaminic acid residue. This is the first observation of legionaminic acid, a sialic acid-like sugar, in an archaeal-derived glycan structure. The importance of this residue for viral infection was demonstrated upon incubation with N-acetylneuraminic acid, a similar monosaccharide. Such treatment reduced progeny virus production by half 4 h post infection. LC-ESI/MS analysis confirmed the presence of pentasaccharide precursors on two different VP4-derived peptides bearing the N-glycosylation signal, NTT. The same sites modified by the native host, Halorubrum sp. strain PV6, were also recognized by the Haloferax volcanii N-glycosylation apparatus, as determined by LC-ESI/MS of heterologously expressed VP4. Here, however, the N-linked pentasaccharide was the same as shown to decorate the S-layer glycoprotein in this species. Hence, N-glycosylation of the haloarchaeal viral protein, VP4, is host-specific. These results thus present additional examples of archaeal N-glycosylation diversity and show the ability of Archaea to modify heterologously expressed proteins.

Molecular architecture of the 26S proteasome holocomplex determined by an integrative approach

The 26S proteasome is at the executive end of the ubiquitin-proteasome pathway for the controlled degradation of intracellular proteins. While the structure of its 20S core particle (CP) has been determined by X-ray crystallography, the structure of the 19S regulatory particle (RP), which recruits substrates, unfolds them, and translocates them to the CP for degradation, has remained elusive. Here, we describe the molecular architecture of the 26S holocomplex determined by an integrative approach based on data from cryoelectron microscopy, X-ray crystallography, residue-specific chemical cross-linking, and several proteomics techniques. The "lid" of the RP (consisting of Rpn3/5/6/7/8/9/11/12) is organized in a modular fashion. Rpn3/5/6/7/9/12 form a horseshoe-shaped heterohexamer, which connects to the CP and roofs the AAA-ATPase module, positioning the Rpn8/Rpn11 heterodimer close to its mouth. Rpn2 is rigid, supporting the lid, while Rpn1 is conformationally variable, positioned at the periphery of the ATPase ring. The ubiquitin receptors Rpn10 and Rpn13 are located in the distal part of the RP, indicating that they were recruited to the complex late in its evolution. The modular structure of the 26S proteasome provides insights into the sequence of events prior to the degradation of ubiquitylated substrates.

Stress regulation of the PAN-proteasome system in the extreme halophilic archaeon Halobacterium

In Archaea, the importance of the proteasome system for basic biological processes is only poorly understood. Proteasomes were partially purified from Halobacterium by native gradient density ultracentrifugation. The peptidase activity profiles showed that the 20S proteasome accumulation is altered depending on the physiological state of the cells. The amount of active 20S particles increases in Halobacterium cells as a response to thermal and low salt stresses. In the same conditions, Northern experiments showed a positive transcriptional regulation of the alpha and beta proteasome subunits as well as of the two proteasome regulatory ATPases, PANA and PANB. Co-immunoprecipitation experiments demonstrated the existence of a physical interaction between the two Proteasome Activating Nucleotidase (PAN) proteins in cell extracts. Thus, a direct regulation occurs on the PAN-proteasome components to adjust the protein degradation activity to growth and environmental constraints. These results also indicate that, in extreme halophiles, proteasome mediated proteolysis is an important aspect of low salt stress response. The tri-peptide vinyl sulfone inhibitor NLVS was used in cell cultures to study the in vivo function of proteasome in Halobacterium. The chemical inhibition of proteasomes was measured in the cellular extracts. It has no effect on cell growth and mortality under normal growth conditions as well as under heat shock conditions. These results suggest that the PAN activators or other proteases compensate for loss of proteasome activity in stress conditions.

Localization of the proteasomal ubiquitin receptors Rpn10 and Rpn13 by electron cryomicroscopy

Two canonical subunits of the 26S proteasome, Rpn10 and Rpn13, function as ubiquitin (Ub) receptors. The mutual arrangement of these subunits--and all other non-ATPase subunits--in the regulatory particle is unknown. Using electron cryomicroscopy, we calculated difference maps between wild-type 26S proteasome from Saccharomyces cerevisiae and deletion mutants (rpn10Δ, rpn13Δ, and rpn10Δrpn13Δ). These maps allowed us to localize the two Ub receptors unambiguously. Rpn10 and Rpn13 mapped to the apical part of the 26S proteasome, above the N-terminal coiled coils of the AAA-ATPase heterodimers Rpt4/Rpt5 and Rpt1/Rpt2, respectively. On the basis of the mutual positions of Rpn10 and Rpn13, we propose a model for polyubiquitin binding to the 26S proteasome.

Proteasomes and protein conjugation across domains of life

Like other energy-dependent proteases, proteasomes, which are found across the three domains of life, are self-compartmentalized and important in the early steps of proteolysis. Proteasomes degrade improperly synthesized, damaged or misfolded proteins and hydrolyse regulatory proteins that must be specifically removed or cleaved for cell signalling. In eukaryotes, proteins are typically targeted for proteasome-mediated destruction through polyubiquitylation, although ubiquitin-independent pathways also exist. Interestingly, actinobacteria and archaea also covalently attach small proteins (prokaryotic ubiquitin-like protein (Pup) and small archaeal modifier proteins (Samps), respectively) to certain proteins, and this may serve to target the modified proteins for degradation by proteasomes.

Phosphorylation and methylation of proteasomal proteins of the haloarcheon Haloferax volcanii

Proteasomes are composed of 20S core particles (CPs) of alpha- and beta-type subunits that associate with regulatory particle AAA ATPases such as the proteasome-activating nucleotidase (PAN) complexes of archaea. In this study, the roles and additional sites of post-translational modification of proteasomes were investigated using the archaeon Haloferax volcanii as a model. Indicative of phosphorylation, phosphatase-sensitive isoforms of alpha1 and alpha2 were detected by 2-DE immunoblot. To map these and other potential sites of post-translational modification, proteasomes were purified and analyzed by tandem mass spectrometry (MS/MS). Using this approach, several phosphosites were mapped including alpha1 Thr147, alpha2 Thr13/Ser14 and PAN-A Ser340. Multiple methylation sites were also mapped to alpha1, thus, revealing a new type of proteasomal modification. Probing the biological role of alpha1 and PAN-A phosphorylation by site-directed mutagenesis revealed dominant negative phenotypes for cell viability and/or pigmentation for alpha1 variants including Thr147Ala, Thr158Ala and Ser58Ala. An H. volcanii Rio1p Ser/Thr kinase homolog was purified and shown to catalyze autophosphorylation and phosphotransfer to alpha1. The alpha1 variants in Thr and Ser residues that displayed dominant negative phenotypes were significantly reduced in their ability to accept phosphoryl groups from Rio1p, thus, providing an important link between cell physiology and proteasomal phosphorylation.

SAMPyling proteins in archaea

For some time, post-translational small protein modifications were found only in eukaryotes; much later, such modifications were identified in some species of bacteria. The recent discovery of ubiquitin-like proteins that form polymeric chains and covalently modify proteins in archaea finally closes the evolutionary gap among the domains of life.

Ubiquitin-like small archaeal modifier proteins (SAMPs) in Haloferax volcanii

Archaea, one of three major evolutionary lineages of life, encode proteasomes highly related to those of eukaryotes. In contrast, archaeal ubiquitin-like proteins are less conserved and not known to function in protein conjugation. This has complicated our understanding of the origins of ubiquitination and its connection to proteasomes. Here we report two small archaeal modifier proteins, SAMP1 and SAMP2, with a β-grasp fold and C-terminal diglycine motif similar to ubiquitin, that form protein-conjugates in the archaeon Haloferax volcanii. SAMP-conjugates were altered by nitrogen-limitation and proteasomal gene knockout and spanned various functions including components of the Urm1 pathway. LC-MS/MS-based collision-induced dissociation demonstrated isopeptide bonds between the C-terminal glycine of SAMP2 and the ε-amino group of lysines from a number of protein targets and Lys58 of SAMP2 itself, revealing poly-SAMP chains. The widespread distribution and diversity of pathways modified by SAMPylation suggest this type of protein-conjugation is central to the archaeal lineage.

LccA, an archaeal laccase secreted as a highly stable glycoprotein into the extracellular medium by Haloferax volcanii

Laccases couple the oxidation of phenolic compounds to the reduction of molecular oxygen and thus span a wide variety of applications. While laccases of eukaryotes and bacteria are well characterized, these enzymes have not been described in archaea. Here, we report the purification and characterization of a laccase (LccA) from the halophilic archaeon Haloferax volcanii. LccA was secreted at high levels into the culture supernatant of a recombinant H. volcanii strain, with peak activity (170 +/- 10 mU.ml(-)(1)) at stationary phase (72 to 80 h). LccA was purified 13-fold to an overall yield of 72% and a specific activity of 29.4 U.mg(-)(1) with an absorbance spectrum typical of blue multicopper oxidases. The mature LccA was processed to expose an N-terminal Ala after the removal of 31 amino acid residues and was glycosylated to 6.9% carbohydrate content. Purified LccA oxidized a variety of organic substrates, including bilirubin, syringaldazine (SGZ), 2,2,-azino-bis-(3-ethylbenzothiazoline-6-sulfonic acid) (ABTS), and dimethoxyphenol (DMP), with DMP oxidation requiring the addition of CuSO(4). Optimal oxidation of ABTS and SGZ was at 45 degrees C and pH 6 and pH 8.4, respectively. The apparent K(m) values for SGZ, bilirubin, and ABTS were 35, 236, and 670 muM, with corresponding k(cat) values of 22, 29, and 10 s(-)(1), respectively. The purified LccA was tolerant of high salt, mixed organosolvents, and high temperatures, with a half-life of inactivation at 50 degrees C of 31.5 h.

Hydrophobic carboxy-terminal residues dramatically reduce protein levels in the haloarchaeon Haloferax volcanii

Proteolysis is important not only to cell physiology but also to the successful development of biocatalysts. While a wide-variety of signals are known to trigger protein degradation in bacteria and eukaryotes, these mechanisms are poorly understood in archaea, known for their ability to withstand harsh conditions. Here we present a systematic study in which single C-terminal amino acid residues were added to a reporter protein and shown to influence its levels in an archaeal cell. All 20 amino acid residues were examined for their impact on protein levels, using the reporter protein soluble modified red-shifted GFP (smRS-GFP) expressed in the haloarchaeon Haloferax volcanii as a model system. Addition of hydrophobic residues, including Leu, Cys, Met, Phe, Ala, Tyr, Ile and Val, gave the most pronounced reduction in smRS-GFP levels compared with the addition of either neutral or charged hydrophilic residues. In contrast to the altered protein levels, the C-terminal alterations had no influence on smRS-GFP-specific transcript levels, thus revealing that the effect is post-transcriptional.

The N-terminal penultimate residue of 20S proteasome alpha1 influences its N(alpha) acetylation and protein levels as well as growth rate and stress responses of Haloferax volcanii

Proteasomes are energy-dependent proteolytic machines. We elaborate here on the previously observed N(alpha) acetylation of the initiator methionine of the alpha1 protein of 20S core particles (CPs) of Haloferax volcanii proteasomes. Quantitative mass spectrometry revealed this was the dominant N-terminal form of alpha1 in H. volcanii cells. To further examine this, alpha1 proteins with substitutions in the N-terminal penultimate residue as well as deletion of the CP "gate" formed by the alpha1 N terminus were examined for their N(alpha) acetylation. Both the "gate" deletion and Q2A substitution completely altered the N(alpha)-acetylation pattern of alpha1, with the deletion rendering alpha1 unavailable for N(alpha) acetylation and the Q2A modification apparently enhancing cleavage of alpha1 by methionine aminopeptidase (MAP), resulting in acetylation of the N-terminal alanine. Cells expressing these two alpha1 variants were less tolerant of hypoosmotic stress than the wild type and produced CPs with enhanced peptidase activity. Although alpha1 proteins with Q2D, Q2P, and Q2T substitutions were N(alpha) acetylated in CPs similar to the wild type, cells expressing these variants accumulated unusually high levels of alpha1 as rings in N(alpha)-acetylated, unmodified, and/or MAP-cleaved forms. More detailed examination of this group revealed that while CP peptidase activity was not impaired, cells expressing these alpha1 variants displayed higher growth rates and were more tolerant of hypoosmotic and high-temperature stress than the wild type. Overall, these results suggest that N(alpha) acetylation of alpha1 is important in CP assembly and activity, high levels of alpha1 rings enhance cell proliferation and stress tolerance, and unregulated opening of the CP "gate" impairs the ability of cells to overcome salt stress.

Stabilization of an archaeal DNA-sliding clamp protein, PCNA, by proteasome-activating nucleotidase gene knockout in Haloferax volcanii

Many details of structure, function and substrate specificity of eukaryotic proteasomal systems have been elucidated. This information far-exceeds that available for the archaeal and bacterial counterparts. While structural and functional studies have provided some insight into the workings of prokaryotic proteasomes, the question of substrate targeting and global cellular influence remain largely unaddressed. In this communication, we report an over 720-fold increase in the half-life of the DNA-sliding clamp protein proliferating cell nuclear antigen after knockout of the panA gene, encoding a proteasome-activating nucleotidase A, on the chromosome of the halophilic archaeon Haloferax volcanii. This discovery marks the first identification of a protein stabilized by an archaeal proteasome mutation and provides a starting point for investigations into substrate recognition mechanisms. The findings also begin to address the functional role of proteasomal systems within the scope of the archaeal cell.

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.

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.

The two PAN ATPases from Halobacterium display N-terminal heterogeneity and form labile complexes with the 20S proteasome

The PAN (proteasome-activating nucleotidase) proteins from archaea represent homologues of the eukaryotic 26S proteasome regulatory ATPases. In vitro the PAN complex has been previously shown to have a stimulatory effect on the peptidase activities of the 20S core. By using gradient ultracentrifugation we found that, in cellular extracts, the two PAN proteins from Halobacterium do not form stable high-molecular-mass complexes. Only PAN B was found to associate transiently with the 20S proteasome, thus suggesting that the two PAN proteins are not functionally redundant. The PAN B-20S proteasome complexes associate in an ATP-dependent manner and are stabilized upon nucleotide binding. The two PAN proteins were immunodetected in cellular extracts as N-terminal-truncated polypeptides. RNA-mapping experiments and sequence analysis indicated that this process involved transcript heterogeneities and dual translational initiation mechanisms. Taken together, our results suggest that PAN N-terminal modifications and their intracellular dynamics of assembly/association may constitute important determinants of proteolysis regulation.

Transcriptional linkage of Haloferax volcanii proteasomal genes with non-proteasomal gene neighbours including RNase P, MOSC domain and SAM-methyltransferase homologues

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.

Genetic and proteomic analyses of a proteasome-activating nucleotidase A mutant of the haloarchaeon Haloferax volcanii

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.

Protein biogenesis in Archaea: addressing translation initiation using an in vitro protein synthesis system for Haloferax volcanii

Translation initiation in Archaea combines aspects of the parallel process in Eukarya and Bacteria alongside traits unique to this domain. To better understand translation initiation in Archaea, an in vitro translation system from the haloarchaeon Haloferax volcanii has been developed. The ability to translate individual mRNAs both under the conditions used in previously developed poly(U)-dependent poly(Phe) synthesis systems as well as under physiological conditions was shown. Using the H. volcanii system, mRNAs proceeded by either 'strong' or 'weak' Shine-Dalgarno (SD) motifs, or completely lacking leader sequences were effectively translated. The in vitro haloarchaeal system also successfully translated mRNA from Bacteria, again either presenting a SD initiation motif or completely lacking a leader sequence. Thus, the ability to translate individual mRNAs in vitro offers a system to address translation initiation as well as other aspects of protein biogenesis in Archaea.

Role of the beta1 subunit in the function and stability of the 20S proteasome in the hyperthermophilic archaeon Pyrococcus furiosus

The hyperthermophilic archaeon Pyrococcus furiosus genome encodes three proteasome component proteins: one alpha protein (PF1571) and two beta proteins (beta1-PF1404 and beta2-PF0159), as well as an ATPase (PF0115), referred to as proteasome-activating nucleotidase. Transcriptional analysis of the P. furiosus dynamic heat shock response (shift from 90 to 105 degrees C) showed that the beta1 gene was up-regulated over twofold within 5 minutes, suggesting a specific role during thermal stress. Consistent with transcriptional data, two-dimensional sodium dodecyl sulfate-polyacrylamide gel electrophoresis revealed that incorporation of the beta1 protein relative to beta2 into the 20S proteasome (core particle [CP]) increased with increasing temperature for both native and recombinant versions. For the recombinant enzyme, the beta2/beta1 ratio varied linearly with temperature from 3.8, when assembled at 80 degrees C, to 0.9 at 105 degrees C. The recombinant alpha+beta1+beta2 CP assembled at 105 degrees C was more thermostable than either the alpha+beta1+beta2 version assembled at 90 degrees C or the alpha+beta2 version assembled at either 90 degrees C or 105 degrees C, based on melting temperature and the biocatalytic inactivation rate at 115 degrees C. The recombinant CP assembled at 105 degrees C was also found to have different catalytic rates and specificity for peptide hydrolysis, compared to the 90 degrees C assembly (measured at 95 degrees C). Combination of the alpha and beta1 proteins neither yielded a large proteasome complex nor demonstrated any significant activity. These results indicate that the beta1 subunit in the P. furiosus 20S proteasome plays a thermostabilizing role and influences biocatalytic properties, suggesting that beta subunit composition is a factor in archaeal proteasome function during thermal stress, when polypeptide turnover is essential to cell survival.

Posttranslational modification of the 20S proteasomal proteins of the archaeon Haloferax volcanii

20S proteasomes are large, multicatalytic proteases that play an important role in intracellular protein degradation. The barrel-like architecture of 20S proteasomes, formed by the stacking of four heptameric protein rings, is highly conserved from archaea to eukaryotes. The outer two rings are composed of alpha-type subunits, and the inner two rings are composed of beta-type subunits. The halophilic archaeon Haloferax volcanii synthesizes two different alpha-type proteins, alpha1 and alpha2, and one beta-type protein that assemble into at least two 20S proteasome subtypes. In this study, we demonstrate that all three of these 20S proteasomal proteins (alpha1, alpha2, and beta) are modified either post- or cotranslationally. Using electrospray ionization quadrupole time-of-flight mass spectrometry, a phosphorylation site of the beta subunit was identified at Ser129 of the deduced protein sequence. In addition, alpha1 and alpha2 contained N-terminal acetyl groups. These findings represent the first evidence of acetylation and phosphorylation of archaeal proteasomes and are one of the limited examples of post- and/or cotranslational modification of proteins in this unusual group of organisms.

Rooting the tree of life by transition analyses

BACKGROUND

Despite great advances in clarifying the family tree of life, it is still not agreed where its root is or what properties the most ancient cells possessed--the most difficult problems in phylogeny. Protein paralogue trees can theoretically place the root, but are contradictory because of tree-reconstruction artefacts or poor resolution; ribosome-related and DNA-handling enzymes suggested one between neomura (eukaryotes plus archaebacteria) and eubacteria, whereas metabolic enzymes often place it within eubacteria but in contradictory places. Palaeontology shows that eubacteria are much more ancient than eukaryotes, and, together with phylogenetic evidence that archaebacteria are sisters not ancestral to eukaryotes, implies that the root is not within the neomura. Transition analysis, involving comparative/developmental and selective arguments, can polarize major transitions and thereby systematically exclude the root from major clades possessing derived characters and thus locate it; previously the 20 shared neomuran characters were thus argued to be derived, but whether the root was within eubacteria or between them and archaebacteria remained controversial.

RESULTS

I analyze 13 major transitions within eubacteria, showing how they can all be congruently polarized. I infer the first fully resolved prokaryote tree, with a basal stem comprising the new infrakingdom Glidobacteria (Chlorobacteria, Hadobacteria, Cyanobacteria), which is entirely non-flagellate and probably ancestrally had gliding motility, and two derived branches (Gracilicutes and Unibacteria/Eurybacteria) that diverged immediately following the origin of flagella. Proteasome evolution shows that the universal root is outside a clade comprising neomura and Actinomycetales (proteates), and thus lies within other eubacteria, contrary to a widespread assumption that it is between eubacteria and neomura. Cell wall and flagellar evolution independently locate the root outside Posibacteria (Actinobacteria and Endobacteria), and thus among negibacteria with two membranes. Posibacteria are derived from Eurybacteria and ancestral to neomura. RNA polymerase and other insertions strongly favour the monophyly of Gracilicutes (Proteobacteria, Planctobacteria, Sphingobacteria, Spirochaetes). Evolution of the negibacterial outer membrane places the root within Eobacteria (Hadobacteria and Chlorobacteria, both primitively without lipopolysaccharide): as all phyla possessing the outer membrane beta-barrel protein Omp85 are highly probably derived, the root lies between them and Chlorobacteria, the only negibacteria without Omp85, or possibly within Chlorobacteria.

CONCLUSION

Chlorobacteria are probably the oldest and Archaebacteria the youngest bacteria, with Posibacteria of intermediate age, requiring radical reassessment of dominant views of bacterial evolution. The last ancestor of all life was a eubacterium with acyl-ester membrane lipids, large genome, murein peptidoglycan walls, and fully developed eubacterial molecular biology and cell division. It was a non-flagellate negibacterium with two membranes, probably a photosynthetic green non-sulphur bacterium with relatively primitive secretory machinery, not a heterotrophic posibacterium with one membrane.

Functional and structural characterization of the Methanosarcina mazei proteasome and PAN complexes

We have cloned the proteasome and the proteasome activating nucleotidase (PAN) genes from the mesophilic archaeon Methanosarcina mazei and produced the respective proteins in Escherichia coli cultures. The recombinant complexes were purified to homogeneity and characterized biochemically, structurally, and by mass spectrometry. We found that the degradation of Bodipy-casein by Methanosarcina proteasomes was activated by Methanosarcina PAN. Notably, the Methanosarcina PAN unfolded GFP-SsrA only in the presence of Methanosarcina proteasomes. Structural analysis by 2D averaging electron microscopy of negatively stained complexes displayed the typical structure for the proteasome, namely four-striped side-views and sevenfold-symmetric top-views, with 15 nm height and 11 nm diameter. The structural analysis of the PAN preparation revealed also four-striped side-views, albeit with a height of 18 nm and sixfold-symmetric top-views with a diameter of 15 nm, which corresponds most likely to a dimer of two hexameric complexes. Mass spectrometric analysis of both the Methanosarcina and the Methanocaldococcus PAN proteins indicated hexameric complexes. In summary, we performed a functional and structural characterization of the PAN and proteasome complexes from the archaeon M. mazei and described unique new structural and functional features.

20S Proteasomes Have the Potential to Keep Substrates in Store for Continual Degradation

The 20S core of the proteasome, which together with the regulatory particle plays a major role in the degradation of proteins in eukaryotic cells, is traversed by an internal system of cavities, namely two antechambers and one central proteolytic chamber. Little is known about the mechanisms underlying substrate binding and translocation of polypeptide chains into the interior of 20S proteasomes. Specifically, the role of the antechambers is not fully understood, and the number of substrate molecules sequestered within the internal cavities at any one time is unknown. Here we have shown that by applying both electron microscopy and tandem mass spectrometry (MS) approaches to this multisubunit complex we obtain precise information regarding the stoichiometry and location of substrates within the three chambers. The dissociation pattern in tandem MS allows us to conclude that a maximum of three green fluorescent protein and four cytochrome c substrate molecules are bound within the cavities. Our results also show that >95% of the population of proteasome molecules contain the maximum number of partially folded substrates. Moreover, we deduce that one green fluorescent protein or two cytochrome c molecules must reside within the central proteolytic chamber while the remaining substrate molecules occupy, singly, both antechambers. The results imply therefore an additional role for 20S proteasomes in the storage of substrates prior to their degradation, specifically in cases where translocation rates are slower than proteolysis. More generally, the ability to locate relatively small protein ligands sequestered within the 28-subunit core particle highlights the tremendous potential of tandem MS for deciphering substrate binding within large macromolecular assemblies.

Haloarchaeal proteases and proteolytic systems

Proteases play key roles in many biological processes and have numerous applications in biotechnology and industry. Recent advances in the genetics, genomics and biochemistry of the halophilic Archaea provide a tremendous opportunity for understanding proteases and their function in the context of an archaeal cell. This review summarizes our current knowledge of haloarchaeal proteases and provides a reference for future research.

Proteasomes from Structure to Function: Perspectives from Archaea

Insight into the world of proteolysis has expanded considerably over the past decade. Energy-dependent proteases, such as the proteasome, are no longer viewed as nonspecific degradative enzymes associated solely with protein catabolism but are intimately involved in controlling biological processes that span life to death. The proteasome maintains this exquisite control by catalyzing the precisely timed and rapid turnover of key regulatory proteins. Proteasomes also interplay with chaperones to ensure protein quality and to readjust the composition of the proteome following stress. Archaea encode proteasomes that are highly related to those of eukaryotes in basic structure and function. Investigations of archaeal proteasomes coupled with those of eukaryotes has greatly facilitated our understanding of the molecular mechanisms that govern regulated protein degradation by this elaborate nanocompartmentalized machine.

From replication to cultivation: hot news from Haloarchaea

Haloarchaea have developed into model organisms that are utilized to study many biological processes. Examples are the mechanisms of chromosome maintenance, gene expression and its regulation, protein export and degradation, and motility and sensing. In addition to the analysis of model species like Halobacterium salinarum and Haloferax volcanii, natural communities have been characterized. Halophilic Archaea were found in low-salt environments and are thus more widespread than previously thought.

Archaeal proteasomes and other regulatory proteases

Numerous proteases have been shown to catalyze the precisely-timed and rapid turnover of key cellular proteins. Often these regulatory proteases are either energy-dependent or intramembrane-cleaving. In archaea, two different types of energy-dependent proteases have been characterized: 20S proteasomes associated with proteasome-activating nucleotidases and membrane-associated Lon proteases. Interestingly, homologs of all three mechanistic classes of intramembrane-cleaving proteases are widely distributed in archaea. Similar to their eucaryal and bacterial counterparts, members of these uncharacterized proteases might promote the controlled release of membrane-anchored regulatory proteins or liberate small peptide reporters and/or effectors that function in cell signaling.

Recombinant production of Zymomonas mobilis pyruvate decarboxylase in the haloarchaeon Haloferax volcanii

The unusual physiological properties of archaea (e.g., growth in extreme salt concentration, temperature and pH) make them ideal platforms for metabolic engineering. Towards the ultimate goal of modifying an archaeon to produce bioethanol or other useful products, the pyruvate decarboxylase gene of Zymomonas mobilis (Zm pdc) was expressed in Haloferax volcanii. This gene has been used successfully to channel pyruvate to ethanol in various Gram-negative bacteria, including Escherichia coli. Although the ionic strength of the H. volcanii cytosol differs over 15-fold from that of E. coli, gel filtration and circular dichroism revealed no difference in secondary structure between the ZmPDC protein isolated from either of these hosts. Like the E. coli purified enzyme, ZmPDC from H. volcanii catalyzed the nonoxidative decarboxylation of pyruvate. A decrease in the amount of soluble ZmPDC protein was detected as H. volcanii transitioned from log phase to late stationary phase that was inversely proportional to the amount of pdc-specific mRNA. Based on these results, proteins from non-halophilic organisms can be actively synthesized in haloarchaea; however, post-transcriptional mechanisms present in stationary phase appear to limit the amount of recombinant protein expressed.

Analysis of proteasome-dependent proteolysis in Haloferax volcanii cells, using short-lived green fluorescent proteins

Proteasomes are energy-dependent proteases that are central to the quality control and regulated turnover of proteins in eukaryotic cells. Dissection of this proteolytic pathway in archaea, however, has been hampered by the lack of substrates that are easily detected in whole cells. In the present study, we developed a convenient reporter system by functional expression of a green fluorescent protein variant with C-terminal fusions in the haloarchaeon Haloferax volcanii. The levels of this reporter protein correlated with whole-cell fluorescence that was readily detected in culture. Accumulation of the reporter protein was dependent on the sequence of the C-terminal amino acid fusion, as well as the presence of an irreversible, proteasome-specific inhibitor (clasto-lactacystin beta-lactone). This inhibitor was highly specific for H. volcanii 20S proteasomes, with a Ki of approximately 40 nM. In contrast, phenylmethanesulfonyl fluoride did not influence the levels of fluorescent reporter protein or inhibit 20S proteasomes. Together, these findings provide a powerful tool for the elucidation of protein substrate recognition motifs and the identification of new genes which may be involved in the proteasome pathway of archaea.