Biology subjects
Publications and source records attributed to Albers, S.-V..
Natural competence requires a contractile pilus system. Here, we provide evidence that the pilus biogenesis and natural competence in cyanobacteria are regulated by the second messenger c-di-AMP. Furthermore, we show that the ComFB signaling protein is a novel c-di-AMP-receptor protein, widespread in bacterial phyla, and required for pilus biogenesis and DNA uptake.
Amongst the major archaeal filament types, several have been shown to closely resemble bacterial homologues of the Type IV pili (T4P). Within Sulfolobales, member species encode for three types of T4P, namely the archaellum, the UV-inducible pilus (Uvp) and the archaeal adhesive pilus (Aap). Whereas the archaellum functions primarily in swimming motility, and the Uvp in UV-induced cell aggregation and DNA-exchange, the Aap plays an important role in adhesion and twitching motility. All previously solved Aap appear to have almost identical helical structures. Here, we present a cryoEM structure of the Aap of the archaeal model organism Sulfolobus acidocaldarius. We identify the component subunit as AapB and find that while its structure follows the canonical T4P blueprint, it adopts three distinct conformations within the pilus. The tri-conformer Aap structure that we describe challenges our current understanding of pilus structure and sheds new light on the principles of twitching motility.
Type IV pili are ancient and widespread filamentous organelles found in most bacterial and archaeal phyla where they support a wide range of functions, including substrate adhesion, DNA uptake, self aggregation, and cell motility. In most bacteria, PilT-family ATPases disassemble adhesion pili, causing them to rapidly retract and produce twitching motility, important for surface colonization. As archaea do not possess homologs of PilT, it was thought that archaeal pili cannot retract. Here, we employ live-cell imaging under native conditions (75{degrees}C and pH 2), together with automated single-cell tracking, high-temperature fluorescence imaging, and genetic manipulation to demonstrate that S. acidocaldarius exhibits bona fide twitching motility, and that this behavior depends specifically on retractable adhesion pili. Our results demonstrate that archaeal adhesion pili are capable of retraction in the absence of a PilT retraction ATPase and suggests that the ancestral type IV pilus machinery in the last universal common ancestor (LUCA) relied on such a bifunctional ATPase for both extension and retraction.
Three GPN-loop GTPases, GPN1-GPN3, are central to the maturation and trafficking of eukaryotic RNA polymerase II. This GTPase family is widely represented in archaea but typically occurs as single paralogs. Structural analysis of the GTP- and GDP-bound states of the Sulfolobus acidocaldarius GPN enzyme (SaGPN) showed that this central GPN-loop GTPase adopts two distinct quaternary structures. In the GTP-bound form the {gamma}-phosphate induces a tensed dimeric arrangement by interacting with the GPN region that is relaxed upon hydrolysis to GDP. Consequently, a rocking-like motion of the two protomers causes a major allosteric structural change towards the roof-like helices. Using a lock-switch-rock (LSR) mechanism, homo- and heterodimeric GPN-like GTPases are locked in the GTP-bound state and undergo large conformational changes upon GTP hydrolysis. A{Delta} saGPN strain of S. acidocaldarius was characterized by impaired motility and major changes in the proteome underscoring its functional relevance for S. acidocaldarius in vivo. Significance StatementGPN-loop GTPases have been found to be crucial for eukaryotic RNA polymerase II assembly and nuclear trafficking. Despite their ubiquitous occurrence in eukaryotes and archaea the mechanism by which these self-activating GTPases mediate their function is unknown. Our study on an archaeal representative from Sulfolobus acidocaldarius showed that these dimeric GTPases undergo large-scale conformational changes upon GTP hydrolysis, which can be summarized as a lock-switch-rock mechanism. The observed requirement of SaGPN for motility appears to be due to its large footprint on the archaeal proteome.
Dividing cells into two daughter cells is a complicated process that in bacteria and eukaryotes requires many proteins to work together. For archaea that divide via an FtsZ-based mechanism, only three proteins of the cell division machinery could so far be identified. These are two tubulin homologs, FtsZ1, FtsZ2 and the membrane anchor of FtsZ2, SepF. Here, we investigate additional archaeal cell division proteins that were identified by immunoprecipitation of SepF. These proteins comprise a single PRC-barrel domain and strictly co-occur with FtsZ. Two out of three PRC-barrel domain containing proteins found in Haloferax volcanii, CdpB1 and CdpB2 localize to the site of cell division in a SepF-dependent manner. Moreover, depletions and deletions cause severe cell division defects, generating drastically enlarged cells. Fluorescence microscopy of tagged FtsZ1, FtsZ2 and SepF in CdpB1/2 deletion strains revealed that the divisome is unusually disordered and not organized into a distinct ring-like structure at the cell centre. Biochemical analysis of CdpB homologs from different archaeal species showed that SepF interacts directly with CdpB1, which in turn binds to CdpB2, forming a tripartite complex. A crystal structure of CdpB1 and B2 recapitulated these interactions and suggested how these proteins might form filaments, possibly aligning SepF and therefore the FtsZ2 ring during cell division. In summary, we demonstrate that PRC domain proteins play essential roles in FtsZ based cell division in archaea.
Biofilms represent a prevalent lifestyle of unicellular organism that confers protection to external challenges. The mechanisms by which archaea form biofilms are however not entirely clear. H. volcanii is an extremely halophilic euryarchaeon that commonly colonizes salt crust surfaces. H. volcanii produces long and thin appendages called type IV pili that are known to play a function in surface attachment and biofilm formation in archaea and bacteria. Here, we used biophysical experiments to identify critical function of type IV pili in the mechanical integrity of H. volcanii biofilms. Using interferometric scattering microscopy (iSCAT) to non-invasively visualize T4P in live cells, we find that piliation varies across mutants expressing single pilin isoforms. Using microfluidic experiments, we found that the adhesive strength of these mutants correlates with their extent of piliation. We found that in flow, H. volcanii forms clonal biofilms that extend in three dimensions. Expression of PilA2, a single pilin isoform, is sufficient to maintain normal levels of piliation and form biofilms with a structure indistinguishable from WT. Furthermore, we found that fluid flow is a crucial determinant of biofilm integrity: in the absence of flow, biofilms lose cohesion and tend to disperse in a density-dependent manner. Overall, our results demonstrate that T4P-surface and possibly T4P-T4P interactions promote biofilm formation and integrity, and that flow is a crucial ingredient regulating archaeal biofilm formation.
Pili are ubiquitous filamentous surface extensions that play crucial roles for bacterial and archaeal cellular processes such as adhesion, biofilm formation, motility, cell-cell communication, DNA uptake and horizontal gene transfer to name a few. Here we report on the discovery and structure of the archaeal thread - a remarkably stable archaeal pilus that belongs to a so-far largely unknown class of protein filaments. We find that the filament is highly glycosylated and interconnected via donor strand complementation, as well as isopeptide bonds, reminiscent of bacterial type I pili. Despite striking structural similarity with bacterial type-1 pili, archaeal threads appear to have evolved independently and are likely assembled by a markedly distinct mechanism.
CYTH is a large protein superfamily that is conserved in all three domains of life with its unique triphosphate tunnel metalloenzyme (TTM) fold. Besides phosphatase functions, e.g. as RNA triphosphatase, inorganic polyphosphatase or thiamine triphosphatase, some CYTH orthologs cyclize nucleotide triphosphates to 3,5-cyclic nucleotides. So far, archaeal CYTH proteins are annotated as adenylyl cyclases although experimental evidence is lacking. To address this gap, we characterized a CYTH ortholog, SaTTM, from the crenarchaeote Sulfolobus acidocaldarius. Our initial in silico studies suggested a close relationship between archaeal CYTH enzymes and class IV adenylyl cyclases compared to the other CYTH-subclasses, but biochemical data showed no cyclic nucleotide production. Instead, our structural and functional analyses show a classical TTM behavior. The Ca2+-inhibited Michaelis complex indicates a two-metal ion reaction mechanism analogous to other TTMs. Different co-crystal structures of SaTTM further reveal conformational dynamics in SaTTM, let us to assume feedback inhibition in TTMs due to tunnel closure in the product state. Combining our structural insights with sequence-similarity network based in silico analysis, we further set out a firm molecular basis for distinguishing CYTH orthologs with phosphatase activities from class IV adenylyl cyclases. Major highlights- CyaB-like class IV adenylyl cyclase homologs in archaea are triphosphatases. - The co-crystal structure of SaTTM in sulfate and triphosphate bound state revealed conformational transition of the TTM tunnel during catalysis. - Atomic insights into TTM inhibition by calcium and pyrophosphate. - In silico and structure-function analysis revealed the molecular determinant for functional diversification among CYTH proteins.
Motile archaea are propelled by the archaellum, whose motor complex consists of the membrane protein ArlJ, the ATPase ArlI, and the ATP-binding protein ArlH. Despite its essential function and the existence of structural and biochemical data on ArlH, the role of ArlH in archaellum assembly and function remains elusive. ArlH is a structural homolog of KaiC, the central component of the cyanobacterial circadian clock. Similar to KaiC, ArlH exhibits autophosphorylation activity, which was observed for both ArlH of the euryarchaeon Pyrococcus furiosus (PfArlH) and the crenarchaeon Sulfolobus acidocaldarius (SaArlH). Using a combination of single molecule fluorescence measurements and biochemical assays, it is shown that autophosphorylation of ArlH is closely linked to the oligomeric state of ArlH bound to ArlI. These experiments also strongly suggest that ArlH is a hexamer in its functional ArlI bound state. Mutagenesis of the putative catalytic residue Glu-57 in SaArlH results in a reduced autophosphorylation activity and abolished archaellation and motility, suggesting that optimum phosphorylation activity of ArlH is essential for both archaellation and motility.
Protein N-glycosylation is the most common posttranslational modifications found in all three domains of life. The crenarchaeal N-glycosylation begins with the synthesis of a lipid-linked chitobiose core structure, identical to that in eukaryotes. Here, we report the identification of a thermostable archaeal beta-1,4-N-acetylglucosaminyltransferase, named archaeal glycosylation enzyme 24 (Agl24), responsible for the synthesis of the N-glycan chitobiose core. Biochemical characterization confirmed the function as an inverting {beta}-D-GlcNAc-(1[->]4)--D-GlcNAc-diphosphodolichol glycosyltransferase. Substitution of a conserved histidine residue, found also in the eukaryotic and bacterial homologs, demonstrated its functional importance for Agl24. Furthermore, bioinformatics and structural modeling revealed strong similarities between Agl24 and both the eukaryotic Alg14/13 and a distant relation to the bacterial MurG, which catalyze the identical or a similar process, respectively. Our data, complemented by phylogenetic analysis of Alg13 and Alg14, revealed similar sequences in Asgardarchaeota, further supporting the hypothesis that the Alg13/14 homologs in eukaryotes have been acquired during eukaryogenesis. O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=95 SRC="FIGDIR/small/427365v2_ufig1.gif" ALT="Figure 1"> View larger version (23K): org.highwire.dtl.DTLVardef@13d1ffdorg.highwire.dtl.DTLVardef@1ff48d0org.highwire.dtl.DTLVardef@1056e75org.highwire.dtl.DTLVardef@196ff58_HPS_FORMAT_FIGEXP M_FIG C_FIG HighlightsO_LIFirst identification and characterization of a thermostable {beta}-D-GlcNAc-(1[->]4)--D-GlcNAc-diphosphodolichol glycosyltransferase (GT family 28) in Archaea. C_LIO_LIA highly conserved histidine, within a GGH motif in Agl24, Alg14, and MurG, is essential for function of Agl24. C_LIO_LIAgl24-like homologs are broadly distributed among Archaea. C_LIO_LIThe eukaryotic Alg13 and Alg14 are closely related to the Asgard homologs, suggesting their acquisition during eukaryogenesis. C_LI
Bacterial cell division has been studied for decades but reports on the different archaeal cell division systems are rare. In many archaea, cell division depends on the tubulin homolog FtsZ, but further components of the divisome in these archaea are unknown. The halophilic archaeon Haloferax volcanii encodes two FtsZ homologs with different functions in cell division and a putative SepF homolog. In bacteria, SepF is part of the divisome and is recruited early to the FtsZ ring, where it most likely stimulates FtsZ ring formation. H. volcanii SepF co-localized with FtsZ1 and FtsZ2 at midcell. Overexpression of SepF had no effect on cell morphology, but no sepF deletion mutants could be generated. SepF depletion led to a severe cell division defect, resulting in cells with a strongly increased size. Overexpression of FtsZ1- and FtsZ2-GFP in SepF-depleted cells resulted in filamentous cells with an increasing number of FtsZ1 rings depending on the cell length, whereas FtsZ2 rings were not increased. Pull-down assays with HA-tagged SepF identified an interaction with FtsZ2 but not with FtsZ1. Archaeal SepF homologs lack the conserved glycine residue important for polymerization in bacteria and the H. volcanii SepF was purified as a dimer, suggesting that in contrast to the bacterial SepF homologs, polymerization does not seem to be important for its function. A model is proposed where first the FtsZ1 ring is formed and where SepF recruits FtsZ2 to the FtsZ1 ring, resulting in the formation of the FtsZ2 ring. This study provides important novel insights into cell division in archaea and shows that SepF is an important part of the divisome in FtsZ containing archaea.
Halophilic archaea exchange DNA and proteins using a fusion-based mating mechanism. Scanning electron microscopy previously suggested that mating involves an intermediate state, where cells are connected by an intercellular bridge. To better understand this process, we used electron cryotomography and fluorescence microscopy to visualize cells forming these intercellular bridges. Electron cryo-tomography showed that the observed bridges were enveloped by an S-layer and connected mating cells via a continuous cytoplasm. Macromolecular complexes like ribosomes and unknown thin filamentous helical structures were visualized in the cytoplasm inside the bridges, demonstrating that these bridges can facilitate exchange of cellular components. We followed formation of a cell-cell bridge by fluorescence time-lapse microscopy between cells at a distance of 1.5 {micro}m. These results shed light on the process of haloarchaeal mating and highlight further mechanistic questions.
The oldest traces for planktonic lifestyle have been reported in ca. 3.4 billion years old silicified sediments from the Strelley Pool Formation in Western Australia. Observation of flange appendages suggests that Archean life motility was passive and driven by drifting of microorganisms in their surrounding environment. Until now, the oldest traces for active motility are ca. 2.1 billion years old. Whether or not active motility already existed during the Archean eon remains an open question. Here we report the discovery of new 3.4 billion years old tailed microfossils. These microfossils exhibit a lash-like appendage that likely provided them with movement capabilities. This suggests that these microfossils are the oldest remains of active motile life forms. With the ability to move in liquids and on organic and/or mineral surfaces, these microorganisms were capable of escaping from harsh environments and/or colonizing new ecological niches as early as 3.4 billion years ago. The existence of these deep-rooted Archean motile life forms offers a new picture of the Archean biodiversity, with unanticipated evolutionary innovative morphological complexities.
Cells require a sensory system and a motility structure to achieve directed movement. Bacteria and archaea both possess rotating filamentous motility structures that work in concert with the sensory chemotaxis system. This allows microorganisms to move along chemical gradients. The central response regulator protein CheY can bind to the motor of the motility structure, the flagellum in bacteria and the archaellum in archaea. Both motility structures have a fundamentally different protein composition and structural organization. Yet, both systems receive input from the chemotaxis system. We applied a fluorescent microscopy approach in the model euryarchaeon Haloferax volcanii, and shed light on the sequence order in which signals are transferred from the chemotaxis system to the archaellum. Our findings indicate that the euryarchaeal specific ArlCDE are part of the archaellum motor and that they directly receive input from the chemotaxis system via the adaptor protein CheF. Hence, ArlCDE are an important feature of the archaellum of euryarchaea, are essential for signal transduction during chemotaxis and represent the archaeal switch complex.
MinD proteins are well studied in rod-shaped bacteria such as E. coli, where they display self-organized pole-to-pole oscillations that are important for correct positioning of the Z-ring at mid-cell for cell division. Archaea also encode proteins belonging to the MinD family, but their functions are unknown. MinD homologous proteins were found to be widespread in Euryarchaeota and form a sister group to the bacterial MinD family, distinct from the ParA and other related ATPase families. We aimed to identify the function of four archaeal MinD proteins in the model archaeon Haloferax volcanii. Deletion of the minD genes did not cause cell division or size defects, and the Z-ring was still correctly positioned. Instead, one of the mutations ({Delta}minD4) reduced swimming motility, and hampered the correct formation of motility machinery at the cell poles. In {Delta}minD4 cells, there is reduced formation of the motility structure and chemosensory arrays, which are essential for signal transduction. In bacteria, several members of the ParA family can position the motility structure and chemosensory arrays via binding to a landmark protein, and consequently these proteins do not oscillate along the cell axis. However, GFP-MinD4 displayed pole-to-pole oscillation and formed polar patches or foci in H. volcanii. The MinD4 membrane targeting sequence (MTS), homologous to the bacterial MinD MTS, was essential for the oscillation. Surprisingly, MinD4 ATPase domain point-mutations did not block oscillation, but they failed to form pole-patches. Thus, MinD4 from H. volcanii combines traits of different bacterial ParA/MinD proteins.
Motility is seen across all domains of life1. Prokaryotes exhibit various types of motilities, such as gliding, swimming, and twitching, driven by supramolecular motility machinery composed of multiple different proteins2. In archaea only swimming motility is reported, driven by the archaellum (archaeal flagellum), a reversible rotary motor consisting of a torque-generating motor and a helical filament which acts as a propeller3,4. Unlike the bacterial flagellar motor (BFM), adenosine triphosphate (ATP) hydrolysis probably drives both motor rotation and filamentous assembly in the archaellum5,6. However, direct evidence is still lacking due to the lack of a versatile model system. Here we present a membrane-permeabilized ghost system that enables the manipulation of intracellular contents, analogous to the triton model in eukaryotic flagella7 and gliding Mycoplasma8,9. We observed high nucleotide selectivity for ATP driving motor rotation, negative cooperativity in ATP hydrolysis and the energetic requirement for at least 12 ATP molecules to be hydrolyzed per revolution of the motor. The response regulator CheY increased motor switching from counterclockwise (CCW) to clockwise (CW) rotation, which is the opposite of a previous report10. Finally, we constructed the torque-speed curve at various [ATP]s and discuss rotary models in which the archaellum has characteristics of both the BFM and F1-ATPase. Because archaea share similar cell division and chemotaxis machinery with other domains of life11,12, our ghost model will be an important tool for the exploration of the universality, diversity, and evolution of biomolecular machinery.
The UV-inducible pili system of Sulfolobales (Ups) mediates the formation of species-specific cellular aggregates. Within these aggregates, cells exchange DNA in order to repair DNA double strand breaks via homologous recombination. Substitution of the S. acidocaldarius pilin subunits UpsA and UpsB with their homologs from Sulfolobus tokodaii showed that these subunits facilitate species-specific aggregation. A region of low conservation within the UpsA homologs is primarily important for this specificity. Aggregation assays in the presence of different sugars showed the importance of N-glycosylation in the recognition process. In addition, the N-glycan decorating the S-layer of S. tokodaii is different from the one of S. acidocaldarius. Therefore, each Sulfolobus species seems to have developed a unique UpsA binding pocket and unique N-glycan composition to ensure aggregation and consequently also DNA exchange with cells from only the same species, which is essential for DNA repair by homologous recombination.\n\nImportanceType IV pili can be found on the cell surface of many archaea and bacteria where they play important roles in different processes. The Ups-pili from the crenarchaeal Sulfolobales species are essential in establishing species-specific mating partners, ensuring genome stability. With this work, we show that different Sulfolobus species have species-specific regions in their Ups-pilin subunits, which allow them to interact only with cells from the same species. Additionally, different Sulfolobus species all have unique S-layer N-glycosylation patterns. We propose that the unique features of each species allow the recognition of specific mating partners. This knowledge for the first time gives insights into the molecular basis of archaeal self-recognition.