Regulation of minichromosome maintenance helicase activity by Cdc6

Genetic studies, together with amino acid and structural similarities to the clamp loaders of DNA polymerase sliding clamps, have suggested that the Cdc6 protein may function as a loader for the eukaryotic replicative helicase, the minichromosome maintenance (MCM) complex. Thus, Cdc6 may act as the functional homologue of the bacterial DnaC that utilizes ATP hydrolysis to assemble the DnaB helicase at the origin. This report shows that the helicase activity of an MCM homologue from the archaeon Methanothermobacter thermautotrophicus is inhibited in the presence of the Cdc6 homologues. This inhibitory activity is dependent, as for DnaC, on ATP binding to Cdc6. Moreover, an intact Cdc6 winged helix domain is required for efficient inhibition. Two-hybrid analyses indicated that MCM and Cdc6 interact and that the interaction is mediated by the winged helix domain. Analysis of Cdc6 and MCM homologues from several archaea exhibited differences in the inhibitory activity suggesting divergence in function in Cdc6 and MCM homologues among the archaea.     

Characterization of the Replication Initiator Orc1/Cdc6 from the Archaeon Picrophilus torridus

Eukaryotic DNA replication is preceded by the assembly of prereplication complexes (pre-RCs) at or very near origins in G₁ phase, which licenses origin firing in S phase. The archaeal DNA replication machinery broadly resembles the eukaryal apparatus, though simpler in form. The eukaryotic replication initiator origin recognition complex (ORC), which serially recruits Cdc6 and other pre-RC proteins, comprises six components, Orc1-6. In archaea, a single gene encodes a protein similar to both the eukaryotic Cdc6 and the Orc1 subunit of the eukaryotic ORC, with most archaea possessing one to three Orc1/Cdc6 orthologs. Genome sequence analysis of the extreme acidophile Picrophilus torridus revealed a single Orc1/Cdc6 (PtOrc1/Cdc6). Biochemical analyses show MBP-tagged PtOrc1/Cdc6 to preferentially bind ORB (origin recognition box) sequences. The protein hydrolyzes ATP in a DNA-independent manner, though DNA inhibits MBP-PtOrc1/Cdc6-mediated ATP hydrolysis. PtOrc1/Cdc6 exists in stable complex with PCNA in Picrophilus extracts, and MBP-PtOrc1/Cdc6 interacts directly with PCNA through a PIP box near its C terminus. Furthermore, PCNA stimulates MBP-PtOrc1/Cdc6-mediated ATP hydrolysis in a DNA-dependent manner. This is the first study reporting a direct interaction between Orc1/Cdc6 and PCNA in archaea. The bacterial initiator DnaA is converted from an active to an inactive form by ATP hydrolysis, a process greatly facilitated by the bacterial ortholog of PCNA, the β subunit of Pol III. The stimulation of PtOrc1/Cdc6-mediated ATP hydrolysis by PCNA and the conservation of PCNA-interacting protein motifs in several archaeal PCNAs suggest the possibility of a similar mechanism of regulation existing in archaea. This mechanism may involve other yet to be identified archaeal proteins.     

Genomewide and biochemical analyses of DNA-binding activity of Cdc6/Orc1 and Mcm proteins in Pyrococcus sp

The origin of DNA replication (oriC) of the hyperthermophilic archaeon Pyrococcus abyssi contains multiple ORB and mini-ORB repeats that show sequence similarities to other archaeal ORB (origin recognition box). We report here that the binding of Cdc6/Orc1 to a 5kb region containing oriC in vivo was highly specific both in exponential and stationary phases, by means of chromatin immunoprecipitation coupled with hybridization on a whole genome microarray (ChIP-chip). The oriC region is practically the sole binding site for the Cdc6/Orc1, thereby distinguishing oriC in the 1.8M bp genome. We found that the 5kb region contains a previously unnoticed cluster of ORB and mini-ORB repeats in the gene encoding the small subunit (dp1) for DNA polymerase II (PolD). ChIP and the gel retardation analyses further revealed that Cdc6/Orc1 specifically binds both of the ORB clusters in oriC and dp1. The organization of the ORB clusters in the dp1 and oriC is conserved during evolution in the order Thermococcales, suggesting a role in the initiation of DNA replication. Our ChIP-chip analysis also revealed that Mcm alters the binding specificity to the oriC region according to the growth phase, consistent with its role as a licensing factor.     

Molecular determinants of origin discrimination by Orc1 initiators in archaea

Unlike bacteria, many eukaryotes initiate DNA replication from genomic sites that lack apparent sequence conservation. These loci are identified and bound by the origin recognition complex (ORC), and subsequently activated by a cascade of events that includes recruitment of an additional factor, Cdc6. Archaeal organisms generally possess one or more Orc1/Cdc6 homologs, belonging to the Initiator clade of ATPases associated with various cellular activities (AAA(+)) superfamily; however, these proteins recognize specific sequences within replication origins. Atomic resolution studies have shown that archaeal Orc1 proteins contact double-stranded DNA through an N-terminal AAA(+) domain and a C-terminal winged-helix domain (WHD), but use remarkably few base-specific contacts. To investigate the biochemical effects of these associations, we mutated the DNA-interacting elements of the Orc1-1 and Orc1-3 paralogs from the archaeon Sulfolobus solfataricus, and tested their effect on origin binding and deformation. We find that the AAA(+) domain has an unpredicted role in controlling the sequence selectivity of DNA binding, despite an absence of base-specific contacts to this region. Our results show that both the WHD and ATPase region influence origin recognition by Orc1/Cdc6, and suggest that not only DNA sequence, but also local DNA structure help define archaeal initiator binding sites.     

Interactions between the archaeal Cdc6 and MCM proteins modulate their biochemical properties

The origin recognition complex, Cdc6 and the minichromosome maintenance (MCM) complex play essential roles in the initiation of eukaryotic DNA replication. Homologs of these proteins may play similar roles in archaeal replication initiation. While the interactions among the eukaryotic initiation proteins are well documented, the protein–protein interactions between the archaeal proteins have not yet been determined. Here, an extensive structural and functional analysis of the interactions between the Methanothermobacter thermautotrophicus MCM and the two Cdc6 proteins (Cdc6-1 and -2) identified in the organism is described. The main contact between Cdc6 and MCM occurs via the N-terminal portion of the MCM protein. It was found that Cdc6–MCM interaction, but not Cdc6–DNA binding, plays the predominant role in regulating MCM helicase activity. In addition, the data showed that the interactions with MCM modulate the autophosphorylation of Cdc6-1 and -2. The results also suggest that MCM and DNA may compete for Cdc6-1 protein binding. The implications of these observations for the initiation of archaeal DNA replication are discussed.     

Cdc6 ATPase activity regulates ORC x Cdc6 stability and the selection of specific DNA sequences as origins of DNA replication

DNA replication, as with all macromolecular synthesis steps, is controlled in part at the level of initiation. Although the origin recognition complex (ORC) binds to origins of DNA replication, it does not solely determine their location. To initiate DNA replication ORC requires Cdc6 to target initiation to specific DNA sequences in chromosomes and with Cdt1 loads the ring-shaped mini-chromosome maintenance (MCM) 2-7 DNA helicase component onto DNA. ORC and Cdc6 combine to form a ring-shaped complex that contains six AAA+ subunits. ORC and Cdc6 ATPase mutants are defective in MCM loading, and ORC ATPase mutants have reduced activity in ORC x Cdc6 x DNA complex formation. Here we analyzed the role of the Cdc6 ATPase on ORC x Cdc6 complex stability in the presence or absence of specific DNA sequences. Cdc6 ATPase is activated by ORC, regulates ORC x Cdc6 complex stability, and is suppressed by origin DNA. Mutations in the conserved origin A element, and to a lesser extent mutations in the B1 and B2 elements, induce Cdc6 ATPase activity and prevent stable ORC x Cdc6 formation. By analyzing ORC x Cdc6 complex stability on various DNAs, we demonstrated that specific DNA sequences control the rate of Cdc6 ATPase, which in turn controls the rate of Cdc6 dissociation from the ORC x Cdc6 x DNA complex. We propose a mechanism explaining how Cdc6 ATPase activity promotes origin DNA sequence specificity; on DNA that lacks origin activity, Cdc6 ATPase promotes dissociation of Cdc6, whereas origin DNA down-regulates Cdc6 ATPase resulting in a stable ORC x Cdc6 x DNA complex, which can then promote MCM loading. This model has relevance for origin specificity in higher eukaryotes.     

The regulatory function of N-terminal AAA+ ATPase domain of eukaryote-like archaeal Orc1/Cdc6 protein during DNA replication initiation

Archaeal replication machinery represents a core version of this in eukaryotes. The crenarchaeon Sulfolobus solfataricus has the potential to be a powerful model system to understand the central mechanism of eukaryotic DNA replication because it contains three active origins of replication and three eukaryote-like Orc1/Cdc6 proteins (SsoCdc6-1, SsoCdc6-2, and SsoCdc6-3). In this study, we investigate the DNA-binding activities of the N-terminal AAA⁺ ATPase domains of these Orc1/Cdc6 proteins, including their functional interactions with the other SsoCdc6 proteins, on duplex DNA substrates derived from the origins of S. solfataricus. We showed that the ATPase domain of SsoCdc6-2 retained to a great extent the origin DNA-binding activity, and likewise maintained its stimulating effect on SsoCdc6-3. Second, the ATPase domain of SsoCdc6-1, which also stimulated the DNA-binding ability of SsoCdc6-3, demonstrated a significantly improved DNA-binding activity at the forked substrate, but only showed a very weak ability towards the blunt DNA. Third, the ATPase domain of SsoCdc6-3, although having lost much of its DNA-binding activity from the origin, inhibited both SsoCdc6-1 and SsoCdc6-2. These imply that the N-terminal AAA⁺ ATPase domain of archaeal Orc1/Cdc6 protein could be differentially involved in origin recognition during DNA replication initiation even if lacking conventional C-terminal winged helix DNA-binding elements. Our findings further propose that conserved AAA⁺ ATPase domains of Orc1/Cdc6 proteins determine their defined and coordinated functions not only in the archaeon species but also in eukaryotes during the early events of DNA replication.     

The structure of bacterial DnaA: implications for general mechanisms underlying DNA replication initiation

The initiation of DNA replication is a key event in the cell cycle of all organisms. In bacteria, replication initiation occurs at specific origin sequences that are recognized and processed by an oligomeric complex of the initiator protein DnaA. We have determined the structure of the conserved core of the Aquifex aeolicus DnaA protein to 2.7 A resolution. The protein comprises an AAA+ nucleotide-binding fold linked through a long, helical connector to an all-helical DNA-binding domain. The structure serves as a template for understanding the physical consequences of a variety of DnaA mutations, and conserved motifs in the protein suggest how two critical aspects of origin processing, DNA binding and homo-oligomerization, are mediated. The spatial arrangement of these motifs in DnaA is similar to that of the eukaryotic-like archaeal replication initiation factor Cdc6/Orc1, demonstrating that mechanistic elements of origin processing may be conserved across bacterial, archaeal and eukaryotic domains of life.     

DNA binding properties in vivo and target recognition domain sequence alignment analyses of wild-type and mutant RsrI [N6-adenine] DNA methyltransferases

A genetic selection method, the P22 challenge-phage assay, was used to characterize DNA binding in vivo by the prokaryotic beta class [N:6-adenine] DNA methyltransferase M.RSR:I. M.RSR:I mutants with altered binding affinities in vivo were isolated. Unlike the wild-type enzyme, a catalytically compromised mutant, M.RSR:I (L72P), demonstrated site-specific DNA binding in vivo. The L72P mutation is located near the highly conserved catalytic motif IV, DPPY (residues 65-68). A double mutant, M.RSR:I (L72P/D173A), showed less binding in vivo than did M.RSR:I (L72P). Thus, introduction of the D173A mutation deleteriously affected DNA binding. D173 is located in the putative target recognition domain (TRD) of the enzyme. Sequence alignment analyses of several beta class MTases revealed a TRD sequence element that contains the D173 residue. Phylogenetic analysis suggested that divergence in the amino acid sequences of these methyltransferases correlated with differences in their DNA target recognition sequences. Furthermore, MTases of other classes (alpha and gamma) having the same DNA recognition sequence as the beta class MTases share related regions of amino acid sequences in their TRDs.     

Biochemical characterization of Cdc6/Orc1 binding to the replication origin of the euryarchaeon Methanothermobacter thermoautotrophicus

Archaeal cell division cycle protein 6 (Cdc6)/Origin Replication Complex subunit 1 (Orc1) proteins share sequence homology with eukaryotic DNA replication initiation factors but are also structurally similar to the bacterial initiator DnaA. To better understand whether Cdc6/Orc1 functions in an eukaryotic or bacterial-like manner, we have characterized the interaction of two Cdc6/Orc1 paralogs (mthCdc6-1 and mthCdc6-2) with the replication origin from Methanothermobacter thermoautotrophicus. We show that while both proteins display a low affinity for a small dsDNA of random sequence, mthCdc6-1 binds tightly to a short duplex containing a single copy of a 13 bp sequence that is repeated throughout the origin. Surprisingly, sequence comparisons show that this 13 bp sequence is a minimized version of the Origin Recognition Box element found in many euryarchaeotal origins. Analysis of mthCdc6-1 mutants demonstrates that the helix–turn–helix motif in the winged-helix domain mediates the interaction with this sequence. Association of both mthCdc6/Orc1 paralogs with the duplex containing the minimized Origin Recognition Box fits to an independent binding sites model, but their interaction with longer DNA ligands is cooperative. Together, our data provide the first detailed biophysical characterization of the association of an archaeal DNA replication initiator with its origin. Our observations also indicate that the origin-binding properties of Cdc6/Orc1 proteins closely resemble those of bacterial DnaA.     

Cryo-EM structure of the archaeal 50S ribosomal subunit in complex with initiation factor 6 and implications for ribosome evolution

Translation of mRNA into proteins by the ribosome is universally conserved in all cellular life. The composition and complexity of the translation machinery differ markedly between the three domains of life. Organisms from the domain Archaea show an intermediate level of complexity, sharing several additional components of the translation machinery with eukaryotes that are absent in bacteria. One of these translation factors is initiation factor 6 (IF6), which associates with the large ribosomal subunit. We have reconstructed the 50S ribosomal subunit from the archaeon Methanothermobacter thermautotrophicus in complex with archaeal IF6 at 6.6?? resolution using cryo-electron microscopy (EM). The structure provides detailed architectural insights into the 50S ribosomal subunit from a methanogenic archaeon through identification of the rRNA expansion segments and ribosomal proteins that are shared between this archaeal ribosome and eukaryotic ribosomes but are mostly absent in bacteria and in some archaeal lineages. Furthermore, the structure reveals that, in spite of highly divergent evolutionary trajectories of the ribosomal particle and the acquisition of novel functions of IF6 in eukaryotes, the molecular binding of IF6 on the ribosome is conserved between eukaryotes and archaea. The structure also provides a snapshot of the reductive evolution of the archaeal ribosome and offers new insights into the evolution of the translation system in archaea.     

Archaeal cell cycle progress

The discovery of multiple chromosome replication origins in Sulfolobus species has added yet another eukaryotic trait to the archaea, and brought new levels of complexity to the cell cycle in terms of initiation of chromosome replication, replication termination and chromosome decatenation. Conserved repeated DNA elements--origin recognition boxes--have been identified in the origins of replication, and shown to bind the Orc1/Cdc6 proteins involved in cell cycle control. The origin recognition boxes aid in the identification and characterization of new origins, and their conservation suggests that most archaea have a similar replication initiation mechanism. Cell-cycle-dependent variation in Orc1/Cdc6 levels has been demonstrated, reminiscent of variations in cyclin levels during the eukaryotic cell cycle. Information about archaeal chromosome segregation is also accumulating, including the identification of a protein that binds to short regularly spaced repeats that might constitute centromere-like elements. In addition, studies of cell-cycle-specific gene expression have potential to reveal, in the near future, missing components in crenarchaeal chromosome replication, genome segregation and cell division. Together with an increased number of physiological and cytological investigations of the overall organization of the cell cycle, rapid progress of the archaeal cell cycle field is evident, and archaea, in particular Sulfolobus species, are emerging as simple and powerful models for the eukaryotic cell cycle.     

Four chromosome replication origins in the archaeon Pyrobaculum calidifontis

Replication origins were mapped in hyperthermophilic crenarchaea, using high‐throughput sequencing‐based marker frequency analysis. We confirm previous origin mapping in Sulfolobus acidocaldarius, and demonstrate that the single chromosome of Pyrobaculum calidifontis contains four replication origins, the highest number detected in a prokaryotic organism. The relative positions of the origins in both organisms coincided with regions enriched in highly conserved (core) archaeal genes. We show that core gene distribution provides a useful tool for origin identification in archaea, and predict multiple replication origins in a range of species. One of the P. calidifontis origins was mapped in detail, and electrophoretic mobility shift assays demonstrated binding of the Cdc6/Orc1 replication initiator protein to a repeated sequence element, denoted Orb‐1, within the origin. The high‐throughput sequencing approach also allowed for an annotation update of both genomes, resulting in the restoration of open reading frames encoding proteins involved in, e.g., sugar, nitrate and energy metabolism, as well as in glycosylation and DNA repair.     

An ALS disease mutation in Cdc48/p97 impairs 20S proteasome binding and proteolytic communication

Cdc48 (also known as p97 or VCP) is an essential and highly abundant, double-ring AAA+ ATPase, which is ubiquitous in archaea and eukaryotes. In archaea, Cdc48 ring hexamers play a direct role in quality control by unfolding and translocating protein substrates into the degradation chamber of the 20S proteasome. Whether Cdc48 and 20S cooperate directly in protein degradation in eukaryotic cells is unclear. Two regions of Cdc48 are important for 20S binding, the pore-2 loop at the bottom of the D2 AAA+ ring and a C-terminal tripeptide. Here, we identify an aspartic acid in the pore-2 loop as an important element in 20S recognition. Importantly, mutation of this aspartate in human Cdc48 has been linked to familial amyotrophic lateral sclerosis (ALS). In archaeal or human Cdc48 variants, we find that mutation of this pore-2 residue impairs 20S binding and proteolytic communication but does not affect the stability of the hexamer or rates of ATP hydrolysis and protein unfolding. These results suggest that human Cdc48 interacts functionally with the 20S proteasome.     

Structural and Dynamical Studies of Humanin in Water and TFE/Water Mixture: A Molecular Dynamics Simulation

Summary

Proline-rich peptides are known to adopt preferentially the extended polyproline II (PPII) helical conformation, which is involved in several protein-protein recognition events. By resorting to molecular modelling techniques, we wished to investigate the extent to which PPII helices could be used for the formation of isohelical peptide-DNA complexes leading to the selective recognition of the major groove of B-DNA. For that purpose, we have grafted to a cationic intercalator, 9-amino-acridine, an oligopeptide having the sequence: Pro-Arg-Pro-Pro-Arg-Pro-Pro-Arg-Pro-Pro-Asp-Pro-Pro. Each residue in the sequence was set in the D configuration, to prevent enzymatic hydrolysis, and each Arg residue was designed to target O6/N7 of a guanine base following the intercalation site. The Asp residue was designed to target a cytosine base, whilst simultaneously forming a bidentate complex with the Arg three residues upstream. Energy-minimization, using the JUMNA procedure, led to the following conclusions: 1) major groove binding is favoured over minor groove or exclusive binding to the phosphates by large energy differences, of over 50 and 90 kcal/mole, respectively; 2) the two best bound sequences are those having three successive guanine bases on the same DNA strand, immediately adjacent to the intercalation site. Sequence d(CGGGC G), encountered in the Primer Binding Site of the HIV retrovirus, thus ranks amongst the best-bound sequences; 3) replacement of an individual guanine amongst the three ones upstream of the intercalation site, by an adenine base, weakens by > 6 kcal/mole the binding energetics; 4) the conformational rigidity of the DNA-bound PPII helix should enable for a modulation of the base sequence selectivity, by appropriate replacements of the Arg and Asp residues. Thus sequence CGGCAAG, also encountered in the HIV genome, could be targeted by an oligopeptide having the sequence Pro-Arg-Pro-Pro-Asp-Pro-Pro- Asn-Pro-Pro-Asn-Pro-Pro-Arg-Ala.     

How does a DNA interacting enzyme change its specificity during molecular evolution? A site-directed mutagenesis study at the DNA binding site of the DNA-(adenine-N6)-methyltransferase EcoRV

The EcoRV DNA-(adenine-N6)-methyltransferase (MTase) recognizes GATATC sequences and modifies the first adenine residue within this site. Parts of its DNA interface show high sequence homology to DNA MTases of the dam family which recognize and modify GATC sequences. A phylogenetic analysis of M.EcoRV and dam-MTases suggests that EcoRV arose in evolution from a primordial dam-MTase in agreement to the finding that M.EcoRV also methylates GATC sites albeit at a strongly reduced rate. GATCTC sites that deviate in only one position from the EcoRV sequence are preferred over general dam sites. We have investigated by site-directed mutagenesis the function of 17 conserved and nonconserved residues within three loops flanking the DNA binding cleft of M.EcoRV. M.EcoRV contacts the GATATC sequence with two highly cooperative recognition modules. The contacts to the GAT-part of the recognition sequence are formed by residues conserved between dam MTases and M.EcoRV. Mutations at these positions lead to an increase in the discrimination between GATATC and GATC substrates. Our data show that the change in sequence specificity from dam (GATC) to EcoRV (GATATC) was accompanied by the generation of a second recognition module that contacts the second half of the target sequence. The new DNA contacts are formed by residues from all three loops that are not conserved between M.EcoRV and dam MTases. Mutagenesis at important residues within this module leads to variants that show a decreased ability to recognize the TC-part of the GATATC sequence.     

DNA binding by the Methanothermobacter thermautotrophicus Cdc6 protein is inhibited by the minichromosome maintenance helicase

The Cdc6 proteins from the archaeon Methanothermobacter thermautotrophicus were previously shown to bind double-stranded DNA. It is shown here that the proteins also bind single-stranded DNA. Using minichromosome maintenance (MCM) helicase mutant proteins unable to bind DNA, it was found that the interaction of MCM with Cdc6 inhibits the DNA binding activity of Cdc6.     

Conserved structural motifs governing the stoichiometric repair of alkylated DNA by O(6)-alkylguanine-DNA alkyltransferase

O(6)-alkylguanine-DNA alkyltransferase (AGT) directly repairs alkylation damage at the O(6)-position of guanine in a unique, stoichiometric reaction. Crystal structures of AGT homologs from the three kingdoms of life reveal that despite their extremely low primary sequence homology, the topology and overall structure of AGT has been remarkably conserved. The C-terminal domain of the two-domain, alpha/beta fold bears a helix-turn-helix (HTH) motif that has been implicated in DNA-binding by structural and mutagenic studies. In the second helix of the HTH, the recognition helix, lies a conserved RAV[A/G] motif, whose "arginine finger" promotes flipping of the target nucleotide from the base stack. Recognition of the extrahelical guanine is likely predominantly through interactions with the protein backbone, while hydrophobic sidechains line the alkyl-binding pocket, as defined by product complexes of human AGT. The irreversible dealkylation reaction is accomplished by an active-site cysteine that participates in a hydrogen bond network with invariant histidine and glutamic acid residues, reminiscent of the serine protease catalytic triad. Structural and biochemical results suggest that cysteine alkylation opens the domain-interfacing "Asn-hinge", which couples the active-site to the recognition helix, providing both a mechanism for release of repaired DNA and a signal for the observed degradation of alkylated AGT.