Sandy Y. M. Ng

Archaeal Flagella, Bacterial Flagella and Type IV Pili: A Comparison of Genes and Posttranslational Modifications

The archaeal flagellum is a unique motility organelle. While superficially similar to the bacterial flagellum, several similarities have been reported between the archaeal flagellum and the bacterial type IV pilus system. These include the multiflagellin nature of the flagellar filament, N-terminal sequence similarities between archaeal flagellins and bacterial type IV pilins, as well as the presence of homologous proteins in the two systems. Recent advances in archaeal flagella research add to the growing list of similarities. First, the preflagellin peptidase that is responsible for processing the N-terminal signal peptide in preflagellins has been identified. The preflagellin peptidase is a membrane-bound enzyme topologically similar to its counterpart in the type IV pilus system (prepilin peptidase); the two enzymes are demonstrated to utilize the same catalytic mechanism. Second, it has been suggested that the archaeal flagellum and the bacterial type IV pilus share a similar mode of assembly. While bacterial flagellins and type IV pilins can be modified with O-linked glycans, N-linked glycans have recently been reported on archaeal flagellins. This mode of glycosylation, as well as the observation that the archaeal flagellum lacks a central channel, are both consistent with the proposed assembly model. On the other hand, the failure to identify other genes involved in archaeal flagellation by homology searches likely implies a novel aspect of the archaeal flagellar system. These interesting features remain to be deciphered through continued research. Such knowledge would be invaluable to motility and protein export studies in the Archaea.

Systematic deletion analyses of the fla genes in the flagella operon identify several genes essential for proper assembly and function of flagella in the archaeon, Methanococcus maripaludis

The archaeal flagellum is a unique motility apparatus in the prokaryotic domain, distinct from the bacterial flagellum. Most of the currently recognized archaeal flagella‐associated genes fall into a single fla operon that contains the genes for the flagellin proteins (two or more genes designated as flaA or flaB), some variation of a set of conserved proteins of unknown function (flaC, flaD, flaE, flaF, flaG and flaH), an ATPase (flaI) and a membrane protein (flaJ). In addition, the flaD gene has been demonstrated to encode two proteins: a full‐length gene product and a truncated product derived from an alternate, internal start site. A systematic deletion approach was taken using the methanogen Methanococcus maripaludis to investigate the requirement and a possible role for these proposed flagella‐associated genes. Markerless in‐frame deletion strains were created for most of the genes in the M. maripaludis fla operon. In addition, a strain lacking the truncated FlaD protein [FlaD M(191)I] was also created. DNA sequencing and Southern blot analysis confirmed each mutant strain, and the integrity of the remaining operon was confirmed by immunoblot. With the exception of the ΔFlaB3 and FlaD M(191)I strains, all mutants were non‐motile by light microscopy and non‐flagellated by electron microscopy. A detailed examination of the ΔFlaB3 mutant flagella revealed that these structures had no hook region, while the FlaD M(191)I strain appeared identical to wild type. Each deletion strain was complemented, and motility and flagellation was restored. Collectively, these results demonstrate for first time that these fla operon genes are directly involved and critically required for proper archaeal flagella assembly and function.

Genetic and Mass Spectrometry Analyses of the Unusual Type IV-Like Pili of the Archaeon Methanococcus maripaludis

The structure of pili from the archaeon Methanococcus maripaludis is unlike that of any bacterial pili. However, genetic analysis of the genes involved in the formation of these pili has been lacking until this study. Pili were isolated from a nonflagellated (ΔflaK) mutant and shown by sodium dodecyl sulfate-polyacrylamide gel electrophoresis to consist primarily of subunits with an apparent molecular mass of 17 kDa. In-frame deletions were created in three genes, MMP0233, MMP0236, and MMP0237, which encode proteins with bacterial type IV pilin-like signal peptides previously identified by in silico methodology as likely candidates for pilus structural proteins. Deletion of MMP0236 or MMP0237 resulted in mutant cells completely devoid of pili on the cell surface, while deletion of the third pilin-like gene, MMP0233, resulted in cells greatly reduced in the number of pili on the surface. Complementation with the deleted gene in each case returned the cells to a piliated state. Surprisingly, mass spectrometry analysis of purified pili identified the major structural pilin as another type IV pilin-like protein, MMP1685, whose gene is located outside the first pilus locus. This protein was found to be glycosylated with an N-linked branched pentasaccharide glycan. Deletion and complementation analysis confirmed that MMP1685 is required for piliation.

The Structure of an Archaeal Pilus

Bacterial pili are involved in a host of activities, including motility, adhesion, transformation, and immune escape. Structural studies of these pili have shown that several distinctly different classes exist, with no common origin. Remarkably, it is now known that the archaeal flagellar filament appears to have a common origin with the bacterial type IV pilus, and assembly in both systems involves hydrophobic N-terminal alpha-helices that form three-stranded coils in the center of these filaments. Recent work has identified further genes in archaea as being similar to bacterial type IV pilins, but the function or structures formed by such gene products was unknown. Using electron cryo-microscopy, we show that an archaeal pilus from Methanococcus maripaludis has a structure entirely different from that of any of the known bacterial pili. Two subunit packing arrangements were identified: one has rings of four subunits spaced by approximately 44 A and the other has a one-start helical symmetry with approximately 2.6 subunits per turn of a approximately 30 A pitch helix. Remarkably, these schemes appear to coexist within the same filaments. For the segments composed of rings, the twist between adjacent rings is quite variable, while for the segments having a one-start helix there is a large variability in both the axial rise and the twist per subunit. Since this pilus appears to be assembled from a type IV pilin-like protein with a hydrophobic N-terminal helix, it provides yet another example of how different quaternary structures can be formed from similar building blocks. This result has many implications for understanding the evolutionary divergence of bacteria and archaea.

Cell Surface Structures of Archaea

Prokaryotes possess various kinds of cell surface organelles serving versatile biological roles depending on the environmental niche of the organism. The formation of these structures involves fascinating machineries, as not only do the protein components need to travel across the cytoplasmic

Recent advances in the structure and assembly of the archaeal flagellum.

Archaeal motility occurs through the rotation of flagella that are distinct from the flagella found on bacteria. The differences between the two structures include the multi-flagellin nature of the archaeal filament, the widespread posttranslational modification of the flagellins and the presence of a short signal peptide on each flagellin that is cleaved by a specific signal peptidase prior to the incorporation of the mature flagellin into the flagellar filament. Research has revealed similarities between the archaeal flagellum and the type IV pilus, including the presence of similar unusual signal peptides on the flagellins and pilins, similarities in the amino acid sequences of the major structural proteins themselves, as well as similarities between potential assembly and processing components. The recent suggestion that type IV pili are part of a family of cell surface complexes, coupled with the similarities between type IV pili and archaeal flagella, raise questions about the evolution of these systems and possible inclusion of archaeal flagella into this surface complex family.

Identification of a Putative Acetyltransferase Gene, MMP0350, Which Affects Proper Assembly of both Flagella and Pili in the Archaeon Methanococcus maripaludis

Glycosylation is a posttranslational modification utilized in all three domains of life. Compared to eukaryotic and bacterial systems, knowledge of the archaeal processes involved in glycosylation is limited. Recently, Methanococcus voltae flagellin proteins were found to have an N-linked trisaccharide necessary for proper flagellum assembly. Current analysis by mass spectrometry of Methanococcus maripaludis flagellin proteins also indicated the attachment of an N-glycan containing acetylated sugars. To identify genes involved in sugar biosynthesis in M. maripaludis, a putative acetyltransferase was targeted for in-frame deletion. Deletion of this gene (MMP0350) resulted in a flagellin molecular mass shift to a size comparable to that expected for underglycosylated or completely nonglycoslyated flagellins, as determined by immunoblotting. Assembled flagellar filaments were not observed by electron microscopy. Interestingly, the deletion also resulted in defective pilus anchoring. Mutant cells with a deletion of MMP0350 had very few, if any, pili attached to the cell surface compared to a nonflagellated but piliated strain. However, pili were obtained from culture supernatants of this strain, indicating that the defect was not in pilus assembly but in stable attachment to the cell surface. Complementation of MMP0350 on a plasmid restored pilus attachment, but it was unable to restore flagellation, likely because the mutant ceased to make detectable flagellin. These findings represent the first report of a biosynthetic gene involved in flagellin glycosylation in archaea. Also, it is the first gene to be associated with pili, linking flagellum and pilus structure and assembly through posttranslational modifications.

Different Minimal Signal Peptide Lengths Recognized by the Archaeal Prepilin-Like Peptidases FlaK and PibD

In Archaea, the preflagellin peptidase (a type IV prepilin-like peptidase designated FlaK in Methanococcus voltae and Methanococcus maripaludis) is the enzyme that cleaves the N-terminal signal peptide from preflagellins. In methanogens and several other archaeal species, the typical flagellin signal peptide length is 11 to 12 amino acids, while in other archaea preflagellins possess extremely short signal peptides. A systematic approach to address the signal peptide length requirement for preflagellin processing is presented in this study. M. voltae preflagellin FlaB2 proteins with signal peptides 3 to 12 amino acids in length were generated and used as a substrate in an in vitro assay utilizing M. voltae membranes as an enzyme source. Processing by FlaK was observed in FlaB2 proteins containing signal peptides shortened to 5 amino acids; signal peptides 4 or 3 amino acids in length were unprocessed. In the case of Sulfolobus solfataricus, where the preflagellin peptidase PibD has broader substrate specificity, some predicted substrates have predicted signal peptides as short as 3 amino acids. Interestingly, the shorter signal peptides of the various mutant FlaB2 proteins not processed by FlaK were processed by PibD, suggesting that some archaeal preflagellin peptidases are likely adapted toward cleaving shorter signal peptides. The functional complementation of signal peptidase activity by FlaK and PibD in an M. maripaludis DeltaflaK mutant indicated that processing of preflagellins was detected by complementation with either FlaK or PibD, yet only FlaK-complemented cells were flagellated. This suggested that a block in an assembly step subsequent to signal peptide removal occurred in the PibD complementation.

Cloning and Characterization of Archaeal Type I Signal Peptidase from Methanococcus voltae

Archaeal protein trafficking is a poorly characterized process. While putative type I signal peptidase genes have been identified in sequenced genomes for many archaea, no biochemical data have been presented to confirm that the gene product possesses signal peptidase activity. In this study, the putative type I signal peptidase gene in Methanococcus voltae was cloned and overexpressed in Escherichia coli, the membranes of which were used as the enzyme source in an in vitro peptidase assay. A truncated, His-tagged form of the M. voltae S-layer protein was generated for use as the substrate to monitor the signal peptidase activity. With M. voltae membranes as the enzyme source, signal peptidase activity in vitro was optimal between 30 and 40 degrees C; it was dependent on a low concentration of KCl or NaCl but was effective over a broad concentration range up to 1 M. Processing of the M. voltae S-layer protein at the predicted cleavage site (confirmed by N-terminal sequencing) was demonstrated with the overexpressed archaeal gene product. Although E. coli signal peptidase was able to correctly process the signal peptide during overexpression of the M. voltae S-layer protein in vivo, the contribution of the E. coli signal peptidase to cleavage of the substrate in the in vitro assay was minimal since E. coli membranes alone did not show significant activity towards the S-layer substrate in in vitro assays. In addition, when the peptidase assays were performed in 1 M NaCl (a previously reported inhibitory condition for E. coli signal peptidase I), efficient processing of the substrate was observed only when the E. coli membranes contained overexpressed M. voltae signal peptidase. This is the first proof of expressed type I signal peptidase activity from a specific archaeal gene product.

Site-Directed Mutagenesis Analysis of Amino Acids Critical for Activity of the Type I Signal Peptidase of the Archaeon Methanococcus voltae

Site-directed mutagenesis studies of the signal peptidase of the methanogenic archaeon Methanococcus voltae identified three conserved residues (Ser52, His122, and Asp148) critical for activity. The requirement for one conserved aspartic acid residue distinguishes the archaeal enzyme from both the Escherichia coli and yeast Sec11 enzymes.