Physical and functional interaction between the mini-chromosome maintenance-like DNA helicase and the single-stranded DNA binding protein from the crenarchaeon Sulfolobus solfataricus

The canonical single-stranded DNA-binding protein is not an essential replication factor but an RNA chaperon in Saccharolobus islandicus

Single-stranded DNA-binding proteins (SSBs) have been regarded as indispensable replication factors. Herein, we report that the genes encoding the canonical SSB (SisSSB) and the non-canonical SSB (SisDBP) in Saccharolobus islandicus REY15A are not essential for cell viability. Interestingly, at a lower temperature (55°C), the protein level of SisSSB increases and the growth of ΔSisssb and ΔSisssbΔSisdbp is retarded. SisSSB exhibits melting activity on dsRNA and DNA/RNA hybrid in vitro and is able to melt RNA hairpin in Escherichia coli. Furthermore, the core SisSSB domain is able to complement the absence of cold-shock proteins in E. coli. Importantly, these activities are conserved in the canonical SSBs from Crenarchaeota species that lack bacterial Csp homologs. Overall, our study has clarified the function of the archaeal canonical SSBs which do not function as a DNA-processing factor, but play a role in the processes requiring melting of dsRNA or DNA/RNA hybrid.

Arabidopsis thaliana MCM3 single subunit of MCM2-7 complex functions as 3' to 5' DNA helicase

Minichromosome maintenance 2-7 (MCM2-7) proteins are conserved eukaryotic replicative factors essential for the DNA replication at its initiation and elongation step, and act as a licensing factor. The MCM2-7 and MCM4/6/7subcomplex exhibit DNA helicase activity, and are therefore regarded as the replicative helicase. The MCM proteins have not been studied in detail in plant system. Here, we present the biochemical characterization of Arabidopsis thaliana MCM3 single subunit and show that it exhibits in vitro unwinding and ATPase activities. AtMCM3 shows a greater unwinding activity with 5' forked partial DNA duplex substrate as compared to 3' forked and non-forked substrates. ATP and magnesium ion are indispensable for its DNA helicase activity. Specifically, ATP and dATP are the preferred nucleotides for its unwinding activity. The directionality of the AtMCM3 has been determined to be in 3' to 5' direction. The oligomerization status of AtMCM3 single subunit protein indicates that it is present in different multimeric forms. The unraveling of the helicase activity of AtMCM3 will provide better insights into the plant DNA replication.

MCM ring hexamerization is a prerequisite for DNA-binding

The hexameric Minichromosome Maintenance (MCM) protein complex forms a ring that unwinds DNA at the replication fork in eukaryotes and archaea. Our recent crystal structure of an archaeal MCM N-terminal domain bound to single-stranded DNA (ssDNA) revealed ssDNA associating across tight subunit interfaces but not at the loose interfaces, indicating that DNA-binding is governed not only by the DNA-binding residues of the subunits (MCM ssDNA-binding motif, MSSB) but also by the relative orientation of the subunits. We now extend these findings by showing that DNA-binding by the MCM N-terminal domain of the archaeal organism Pyrococcus furiosus occurs specifically in the hexameric oligomeric form. We show that mutants defective for hexamerization are defective in binding ssDNA despite retaining all the residues observed to interact with ssDNA in the crystal structure. One mutation that exhibits severely defective hexamerization and ssDNA-binding is at a conserved phenylalanine that aligns with the mouse Mcm4(Chaos3) mutation associated with chromosomal instability, cancer, and decreased intersubunit association.

The Sulfolobus solfataricus GINS Complex Stimulates DNA Binding and Processive DNA Unwinding by Minichromosome Maintenance Helicase

GINS is a key component of the eukaryotic Cdc45-minichromosome maintenance (MCM)-GINS (CMG) complex, which unwinds duplex DNA at the moving replication fork. Archaeal GINS complexes have been shown to stimulate the helicase activity of their cognate MCM mainly by elevating its ATPase activity. Here, we report that GINS from the thermoacidophilic crenarchaeon Sulfolobus solfataricus (SsoGINS) is capable of DNA binding and binds preferentially to single-stranded DNA (ssDNA) over double-stranded DNA (dsDNA). Notably, SsoGINS binds more strongly to dsDNA with a 5' ssDNA tail than to dsDNA with a 3' tail and more strongly to an ssDNA fragment blocked at the 3' end than to one at the 5' end with a biotin-streptavidin (SA) complex, suggesting the ability of the protein complex to slide in a 5'-to-3' direction along ssDNA. DNA-bound SsoGINS enhances DNA binding by SsoMCM. Furthermore, SsoGINS increases the helicase activity of SsoMCM. However, the ATPase activity of SsoMCM is not affected by SsoGINS. Our results suggest that SsoGINS facilitates processive DNA unwinding by SsoMCM by enhancing the binding of the helicase to DNA. We propose that SsoGINS stabilizes the interaction of SsoMCM with the replication fork and moves along with the helicase as the fork progresses.

IMPORTANCE

GINS is a key component of the eukaryotic Cdc45-MCM-GINS complex, a molecular motor that drives the unwinding of DNA in front of the replication fork. Archaea also encode GINS, which interacts with MCM, the helicase. But how archaeal GINS serves its role remains to be understood. In this study, we show that GINS from the hyperthermophilic archaeon Sulfolobus solfataricus is able to bind to DNA and slide along ssDNA in a 5'-to-3' direction. Furthermore, Sulfolobus GINS enhances DNA binding by MCM, which slides along ssDNA in a 3'-to-5' direction. Taken together, these results suggest that Sulfolobus GINS may stabilize the interaction of MCM with the moving replication fork, facilitating processive DNA unwinding.

Regulation of gene expression in rats with spinal cord injury based on microarray data

The present study aimed to investigate the molecular mechanisms of spinal cord injury (SCI) in rats. First, the differentially expressed genes (DGEs) were screened based on GSE45006 microarray data downloaded from Gene Expression Omnibus using the significant analysis of microarray (SAM) method. Screening was performed for DEGs which were negatively or possibly correlated with time and subsequently subjected to gene ontology (GO) functional annotation. Furthermore, pathway enrichment analysis using the Kyoto Encyclopedia of Genes and Genomes was also performed. In addition, a protein-protein interaction (PPI) network was constructed using the Search Tool for the Retrieval of Interacting Genes/Proteins database. Finally, GeneCodis was used to seek transcription factors and microRNAs that are involved in the regulation of DEGs. A total of 806 DEGs were upregulated and 549 DEGs were downregulated in the rats with SCI. Cholesterol metabolism-associated genes (e.g. HMGCS1, FDFT1 and IDI1) were negatively correlated with time, while injury genes (e.g. SERPING1, C1S and RAB27A) were positively correlated with time after SCI. PCNA, MCM2, JUN and SNAP25 were the hub proteins of the PPI network. The transcription factors LEF1 and SP1 were observed to be associated with the regulation of two DEGs that were involved in the cholesterol-associated metabolism as well as injury responses. A number of microRNAs (e.g. miR210, miR-487b and miR-16) were observed to target cholesterol metabolism-associated DGEs. The hub genes PCNA, MCM2, JUN and SNAP25 presumably have critical roles in rats with SCI, and the transcription factors LEF1 and SP1 may be important for the regulation of cholesterol metabolism and injury responses following SCI.

Characterization of the MCM homohexamer from the thermoacidophilic euryarchaeon Picrophilus torridus

The typical archaeal MCM exhibits helicase activity independently invitro. This study characterizes MCM from the euryarchaeon Picrophilus torridus. While PtMCM hydrolyzes ATP in DNA-independent manner, it displays very poor ability to unwind DNA independently, and then too only under acidic conditions. The protein exists stably in complex with PtGINS in whole cell lysates, interacting directly with PtGINS under neutral and acidic conditions. GINS strongly activates MCM helicase activity, but only at low pH. In consonance with this, PtGINS activates PtMCM-mediated ATP hydrolysis only at low pH, with the amount of ATP hydrolyzed during the helicase reaction increasing more than fifty-fold in the presence of GINS. While the stimulation of MCM-mediated helicase activity by GINS has been reported in MCMs from P.furiosus, T.kodakarensis, and very recently, T.acidophilum, to the best of our knowledge, this is the first report of an MCM helicase demonstrating DNA unwinding activity only at such acidic pH, across all archaea and eukaryotes. PtGINS may induce/stabilize a conducive conformation of PtMCM under acidic conditions, favouring PtMCM-mediated DNA unwinding coupled to ATP hydrolysis. Our findings underscore the existence of divergent modes of replication regulation among archaea and the importance of investigating replication events in more archaeal organisms.

Structure and regulatory role of the C-terminal winged helix domain of the archaeal minichromosome maintenance complex

The minichromosome maintenance complex (MCM) represents the replicative DNA helicase both in eukaryotes and archaea. Here, we describe the solution structure of the C-terminal domains of the archaeal MCMs of Sulfolobus solfataricus (Sso) and Methanothermobacter thermautotrophicus (Mth). Those domains consist of a structurally conserved truncated winged helix (WH) domain lacking the two typical ‘wings’ of canonical WH domains. A less conserved N-terminal extension links this WH module to the MCM AAA+ domain forming the ATPase center. In the Sso MCM this linker contains a short α-helical element. Using Sso MCM mutants, including chimeric constructs containing Mth C-terminal domain elements, we show that the ATPase and helicase activity of the Sso MCM is significantly modulated by the short α-helical linker element and by N-terminal residues of the first α-helix of the truncated WH module. Finally, based on our structural and functional data, we present a docking-derived model of the Sso MCM, which implies an allosteric control of the ATPase center by the C-terminal domain.

MCM Paradox: Abundance of Eukaryotic Replicative Helicases and Genomic Integrity

As a crucial component of DNA replication licensing system, minichromosome maintenance (MCM) 2–7 complex acts as the eukaryotic DNA replicative helicase. The six related MCM proteins form a heterohexamer and bind with ORC, CDC6, and Cdt1 to form the prereplication complex. Although the MCMs are well known as replicative helicases, their overabundance and distribution patterns on chromatin present a paradox called the “MCM paradox.” Several approaches had been taken to solve the MCM paradox and describe the purpose of excess MCMs distributed beyond the replication origins. Alternative functions of these MCMs rather than a helicase had also been proposed. This review focuses on several models and concepts generated to solve the MCM paradox coinciding with their helicase function and provides insight into the concept that excess MCMs are meant for licensing dormant origins as a backup during replication stress. Finally, we extend our view towards the effect of alteration of MCM level. Though an excess MCM constituent is needed for normal cells to withstand stress, there must be a delineation of the threshold level in normal and malignant cells. This review also outlooks the future prospects to better understand the MCM biology.

Interaction of T4 UvsW helicase and single-stranded DNA binding protein gp32 through its carboxy-terminal acidic tail

Bacteriophage T4 UvsW helicase contains both unwinding and annealing activities and displays some functional similarities to bacterial RecG and RecQ helicases. UvsW is involved in several DNA repair pathways, playing important roles in recombination-dependent DNA repair and the reorganization of stalled replication forks. The T4 single-stranded DNA (ssDNA) binding protein gp32 is a central player in nearly all DNA replication and repair processes and is thought to facilitate their coordination by recruiting and regulating the various proteins involved. Here, we show that the activities of the UvsW protein are modulated by gp32. UvsW-catalyzed unwinding of recombination intermediates such as D-loops and static X-DNA (Holliday junction mimic) to ssDNA products is enhanced by the gp32 protein. The enhancement requires the presence of the protein interaction domain of gp32 (the acidic carboxy-terminus), suggesting that a specific interaction between UvsW and gp32 is required. In the absence of this interaction, the ssDNA annealing and ATP-dependent translocation activities of UvsW are severely inhibited when gp32 coats the ssDNA lattice. However, when UvsW and gp32 do interact, UvsW is able to efficiently displace the gp32 protein from the ssDNA. This ability of UvsW to remove gp32 from ssDNA may explain its ability to enhance the strand invasion activity of the T4 recombinase (UvsX) and suggests a possible new role for UvsW in gp32-mediated DNA transactions.

Physical and functional interaction between yeast Pif1 helicase and Rim1 single-stranded DNA binding protein

Pif1 helicase plays various roles in the maintenance of nuclear and mitochondrial genome integrity in most eukaryotes. Here, we used a proteomics approach called isotopic differentiation of interactions as random or targeted to identify specific protein complexes of Saccharomyces cerevisiae Pif1. We identified a stable association between Pif1 and a mitochondrial SSB, Rim1. In vitro co-precipitation experiments using recombinant proteins indicated a direct interaction between Pif1 and Rim1. Fluorescently labeled Rim1 was titrated with Pif1 resulting in an increase in anisotropy and a K_d value of 0.69 µM. Deletion mutagenesis revealed that the OB-fold domain and the C-terminal tail of Rim1 are both involved in interaction with Pif1. However, a Rim1 C-terminal truncation (Rim1ΔC18) exhibited a nearly 4-fold higher K_d value. Rim1 stimulated Pif1 DNA helicase activity by 4- to 5-fold, whereas Rim1ΔC18 stimulated Pif1 by 2-fold. Hence, two regions of Rim1, the OB-fold domain and the C-terminal domain, interact with Pif1. One of these interactions occurs through the N-terminal domain of Pif1 because a deletion mutant of Pif1 (Pif1ΔN) retained interaction with Rim1 but did not exhibit stimulation of helicase activity. In light of our in vivo and in vitro data, and previous work, it is likely that the Rim1–Pif1 interaction plays a role in coordination of their functions in mtDNA metabolism.

Biochemical and genetical analyses of the three mcm genes from the hyperthermophilic archaeon, Thermococcus kodakarensis

In eukaryotes, the replicative DNA helicase 'core' is the minichromosome maintenance (Mcm) complex (MCM), forming a heterohexameric complex consisting of six subunits (Mcm2-7). Recent studies showed that the CMG (Cdc45-MCM-GINS) complex is the actual helicase body in the replication fork progression complex. In Archaea, Thermococcus kodakarensis harbors three genes encoding the Mcm homologs on its genome, contrary to most archaea, which have only one homolog. It is thus, of high interest, whether and how these three Mcms share their functions in DNA metabolism in this hyperthermophile. Here, we report the biochemical properties of two of these proteins, TkoMcm1 and TkoMcm3. In addition, their physical and functional interactions with GINS, possibly an essential factor for the initiation and elongation process of DNA replication, are presented through in vitro ATPase and helicase assays, and an in vivo immunoprecipitation assay. Gene disruption and product quantification analyses suggested that TkoMcm3 is essential for cell growth and plays a key role as the main DNA helicase in DNA replication, whereas TkoMcm1 also shares some function in the cells.

Molecular architecture of a multifunctional MCM complex

DNA replication is strictly regulated through a sequence of steps that involve many macromolecular protein complexes. One of them is the replicative helicase, which is required for initiation and elongation phases. A MCM helicase found as a prophage in the genome of Bacillus cereus is fused with a primase domain constituting an integrative arrangement of two essential activities for replication. We have isolated this helicase–primase complex (BcMCM) showing that it can bind DNA and displays not only helicase and primase but also DNA polymerase activity. Using single-particle electron microscopy and 3D reconstruction, we obtained structures of BcMCM using ATPγS or ADP in the absence and presence of DNA. The complex depicts the typical hexameric ring shape. The dissection of the unwinding mechanism using site-directed mutagenesis in the Walker A, Walker B, arginine finger and the helicase channels, suggests that the BcMCM complex unwinds DNA following the extrusion model similarly to the E1 helicase from papillomavirus.

Steric exclusion and wrapping of the excluded DNA strand occurs along discrete external binding paths during MCM helicase unwinding

The minichromosome maintenance (MCM) helicase complex is essential for the initiation and elongation of DNA replication in both the eukaryotic and archaeal domains. The archaeal homohexameric MCM helicase from Sulfolobus solfataricus serves as a model for understanding mechanisms of DNA unwinding. In this report, the displaced 5'-tail is shown to provide stability to the MCM complex on DNA and contribute to unwinding. Mutations in a positively charged patch on the exterior surface of the MCM hexamer destabilize this interaction, alter the path of the displaced 5'-tail DNA and reduce unwinding. DNA footprinting and single-molecule fluorescence experiments support a previously unrecognized wrapping of the 5'-tail. This mode of hexameric helicase DNA unwinding is termed the steric exclusion and wrapping (SEW) model, where the 3'-tail is encircled by the helicase while the displaced 5'-tail wraps around defined paths on the exterior of the helicase. The novel wrapping mechanism stabilizes the MCM complex in a positive unwinding mode, protects the displaced single-stranded DNA tail and prevents reannealing.

The GINS complex from the thermophilic archaeon, Thermoplasma acidophilum may function as a homotetramer in DNA replication

The eukaryotic GINS heterotetramer, consisting of Sld5, Psf1, Psf2, and Psf3, participates in "CMG complex" formation with mini-chromosome maintenance (MCM) and Cdc45 as a key component of a replicative helicase. There are only two homologs of the GINS proteins in Archaea, and these proteins, Gins51 and Gins23, form a heterotetrameric GINS with a 2:2 molar ratio. The Pyrococcus furiosus GINS stimulates the ATPase and helicase activities of its cognate MCM, whereas the Sulfolobus solfataricus GINS does not affect those activities of its cognate MCM, although the proteins bind each other. Intriguingly, Thermoplasma acidophilum, as well as many euryarchaea, have only one gene encoding the sequence homologous to that of archaeal Gins protein (Gins51) on the genome. In this study, we investigated the biochemical properties of the gene product (TaGins51). A gel filtration and electron microscopy revealed that TaGins51 forms a homotetramer. A physical interaction between TaGins51 and TaMcm was detected by a surface plasmon resonance analysis. Unexpectedly, TaGins51 inhibited the ATPase activity, but did not affect the helicase activity of its cognate MCM. These results suggest that another factor is required to form a stable helicase complex with MCM and GINS at the replication fork in T. acidophilum cells.

Protein-protein interactions in the archaeal core replisome

Most of the core components of the archaeal chromosomal DNA replication apparatus share significant protein sequence similarity with eukaryotic replication factors, making the Archaea an excellent model system for understanding the biology of chromosome replication in eukaryotes. The present review summarizes current knowledge of how the core components of the archaeal chromosome replication apparatus interact with one another to perform their essential functions.

Insights into the MCM functional mechanism: lessons learned from the archaeal MCM complex

The helicase function of the minichromosome maintenance protein (MCM) is essential for genomic DNA replication in archaea and eukaryotes. There has been rapid progress in studies of the structure and function of MCM proteins from different organisms, leading to better understanding of the MCM helicase mechanism. Because there are a number of excellent reviews on this topic, we will use this review to summarize some of the recent progress, with particular focus on the structural aspects of MCM and their implications for helicase function. Given the hexameric and double hexameric architecture observed by X-ray crystallography and electron microscopy of MCMs from archaeal and eukaryotic cells, we summarize and discuss possible unwinding modes by either a hexameric or a double hexameric helicase. Additionally, our recent crystal structure of a full length archaeal MCM has provided structural information on an intact, multi-domain MCM protein, which includes the salient features of four unusual beta-hairpins from each monomer, and the side channels of a hexamer/double hexamer. These new structural data enable a closer examination of the structural basis of the unwinding mechanisms by MCM.

Evolution of DNA replication protein complexes in eukaryotes and Archaea

Background

The replication of DNA in Archaea and eukaryotes requires several ancillary complexes, including proliferating cell nuclear antigen (PCNA), replication factor C (RFC), and the minichromosome maintenance (MCM) complex. Bacterial DNA replication utilizes comparable proteins, but these are distantly related phylogenetically to their archaeal and eukaryotic counterparts at best.

Methodology/Principal Findings

While the structures of each of the complexes do not differ significantly between the archaeal and eukaryotic versions thereof, the evolutionary dynamic in the two cases does. The number of subunits in each complex is constant across all taxa. However, they vary subtly with regard to composition. In some taxa the subunits are all identical in sequence, while in others some are homologous rather than identical. In the case of eukaryotes, there is no phylogenetic variation in the makeup of each complex—all appear to derive from a common eukaryotic ancestor. This is not the case in Archaea, where the relationship between the subunits within each complex varies taxon-to-taxon. We have performed a detailed phylogenetic analysis of these relationships in order to better understand the gene duplications and divergences that gave rise to the homologous subunits in Archaea.

Conclusion/Significance

This domain level difference in evolution suggests that different forces have driven the evolution of DNA replication proteins in each of these two domains. In addition, the phylogenies of all three gene families support the distinctiveness of the proposed archaeal phylum Thaumarchaeota.

The Mcm complex: unwinding the mechanism of a replicative helicase

The Mcm2-7 complex serves as the eukaryotic replicative helicase, the molecular motor that both unwinds duplex DNA and powers fork progression during DNA replication. Consistent with its central role in this process, much prior work has illustrated that Mcm2-7 loading and activation are landmark events in the regulation of DNA replication. Unlike any other hexameric helicase, Mcm2-7 is composed of six unique and essential subunits. Although the unusual oligomeric nature of this complex has long hampered biochemical investigations, recent advances with both the eukaryotic as well as the simpler archaeal Mcm complexes provide mechanistic insight into their function. In contrast to better-studied homohexameric helicases, evidence suggests that the six Mcm2-7 complex ATPase active sites are functionally distinct and are likely specialized to accommodate the regulatory constraints of the eukaryotic process.

An archaeal order with multiple minichromosome maintenance genes

In eukaryotes, a complex of six highly related minichromosome maintenance (MCM) proteins is believed to function as the replicative helicase. Until recently, systems for exploring the molecular mechanisms underlying eukaryotic MCM function have been biochemically intractable. To overcome this, molecular studies of MCM function have been carried out using MCM homologues from the archaea. Archaeal MCM systems studied to date possess a single functional MCM, which forms a homohexameric complex that displays DNA binding, ATPase and helicase activities. We have identified an archaeal order that possesses multiple MCM homologues. blast searches of available Methanococcales genomes reveal that members of this order possess between two and eight MCM homologues. Phylogenetic analysis suggests that an ancient duplication in the Methanococcales gave rise to two major groups of MCMs. One group contains Methanococcus maripaludis S2 McmD and possesses a conserved C-terminal insert similar to one observed in eukaryotic MCM3, while the other group contains McmA, -B and -C. Analysis of the genome context of MCMs in the latter group indicates that these genes could have arisen from phage-mediated events. When co-expressed in Escherichia coli, the four MCMs from M. maripaludis co-purify, indicating the formation of heteromeric complexes in vitro. The presence of homologues from both groups in all Methanococcales indicates that there could be functionally important differences between these proteins and that Methanococcales MCMs may therefore provide an interesting additional model for eukaryotic MCM function.

A superfamily 3 DNA helicase encoded by plasmid pSSVi from the hyperthermophilic archaeon Sulfolobus solfataricus unwinds DNA as a higher-order oligomer and interacts with host primase

Replication proteins encoded by nonconjugative plasmids from the hyperthermophilic archaea of the order Sulfolobales show great diversity in amino acid sequence. We have biochemically characterized ORF735, a replication protein from pSSVi, an integrative nonconjugative plasmid from Sulfolobus solfataricus P2. We show that ORF735 is a DNA helicase of superfamily 3. It unwound double-stranded DNA (dsDNA) in a 3'-to-5' direction in the presence of ATP over a wide range of temperatures, from 37 degrees C to 75 degrees C, and possessed DNA-stimulated ATPase activity. ORF735 existed in solution as a salt-stable dimer and was capable of assembling into a salt-sensitive oligomer that was significantly larger than a hexamer in the presence of a divalent cation (Mg(2+)) and an adenine nucleotide (ATP, dATP, or ADP) or its analog (ATPgammaS or AMPPNP). Both N-terminal and C-terminal portions of ORF735 (87 and 160 amino acid residues, respectively, in size) were required for protein dimerization but dispensable for the formation of the higher-order oligomer. The protein unwound DNA only as a large oligomer. Yeast two-hybrid and coimmunoprecipitation assays revealed that ORF735 interacted with the noncatalytic subunit of host primase. These findings provide clues to the functional role of ORF735 in pSSVi DNA replication.

Structural biology of MCM helicases

The eukaryotic MCM2-7 complex is recruited onto origins of replication during the G1 phase of the cell cycle and acts as the main helicase at the replication fork during the S phase. Over the last few years a number of structural reports on MCM proteins using both electron microscopy and protein crystallography have been published. The crystal structures of two (almost) full-length archaeal homologs provide the first atomic pictures of a MCM helicase. However one of the structures is at low resolution and the other is of an inactive MCM. Moreover, both proteins are monomeric in the crystal, whereas the activity of the complex is critically dependent on oligomerization. Lower resolution structures derived from electron microscopy studies are therefore crucial to complement the crystallographic analysis and to assemble the multimeric complex that is active in the cell. A critical analysis of all the structural results elucidates the potential conformational changes and dynamic behavior of MCM helicase to provide a first insight into the gamut of molecular configurations adopted during the processes of DNA melting and unwinding.

Mutations in subdomain B of the minichromosome maintenance (MCM) helicase affect DNA binding and modulate conformational transitions

Minichromosome maintenance (MCM) proteins are believed to provide the replicative helicase activity in eukaryotes and archaea. The single MCM orthologue from Methanothermobacter thermautotrophicus (MthMCM) has been extensively characterized as a model of the eukaryotic heterohexameric MCM complex. MthMCM forms high molecular weight complexes in solution consistent with a dodecamer. Visualization of this complex by electron microscopy suggests that single and double heptameric or hexameric rings can form. We have mutated two arginine residues (Arg-137, Arg-160) in the N-terminal subdomain B of MthMCM based on their apparent potential to form inter-ring hydrogen bonds. Both the single R137A and the double R137A,R160A mutants were characterized by a combination of biophysical, biochemical, and electron microscopy techniques. Biophysical analysis coupled with electron microscopy studies shows that the R137A mutant forms a double heptameric ring, whereas the R137A,R160A protein assembles as a single heptamer. They both show a defect in DNA binding and a concomitant conformational change in subdomain A, with the double mutant displaying significant defects in helicase activity as well. We propose a model in which MCM loading and the subsequent activation of the helicase activity involve a conformational transition that is connected to a DNA binding event.

Methanococcus maripaludis: an archaeon with multiple functional MCM proteins?

There are a large number of proteins involved in the control of eukaryotic DNA replication, which act together to ensure DNA is replicated only once every cell cycle. Key proteins involved in the initiation and elongation phases of DNA replication include the MCM (minchromosome maintenance) proteins, MCM2-MCM7, a family of six related proteins believed to act as the replicative helicase. Genome sequencing has revealed that the archaea possess a simplified set of eukaryotic replication homologues. The complexity of the DNA replication machinery in eukaryotes has led to a number of archaeal species being adapted as model organisms for the study of the DNA replication process. Most archaea sequenced to date possess a single MCM homologue that forms a hexameric complex. Recombinant MCMs from several archaea have been used in the biochemical characterization of the protein, revealing that the MCM complex has ATPase, DNA-binding and -unwinding activities. Unusually, the genome of the methanogenic archaeon Methanococcus maripaludis contains four MCM homologues, all of which contain the conserved motifs required for function. The availability of a wide range of genetic tools for the manipulation of M. maripaludis and the relative ease of growth of this organism in the laboratory makes it a good potential model for studying the role of multiple MCMs in DNA replication.

Biochemical characterization of the minichromosome maintenance (MCM) protein of the crenarchaeote Aeropyrum pernix and its interactions with the origin recognition complex (ORC) proteins

Replication in archaea is carried out by proteins that are homologues of eukaryotic counterparts. However, the archaeal systems tend to be much simpler with fewer different genes encoding the core functions than in eukaryotic counterparts. In many archaea, there is a single minichromosome maintenance (MCM) homologue, presumed to be the replicative helicase and between one and three origin recognition complex (ORC) homologues involved in binding to the replication origins. Here we describe the cloning and characterization of the MCM protein from the crenarchaeote Aeropyrum pernix. Like other eukaryotic and archaeal MCM proteins, it is found to be an ATP-dependent DNA helicase, and the putative active site residues involved in ATP binding and hydrolysis are confirmed by mutation. Deletion of the N-terminal 256 amino acids yielded a protein with higher ATPase activity in the absence of DNA and retained robust helicase activity. Interactions with the ORC proteins of A. pernix were examined, and it was found that both ORC homologues could inhibit the helicase activity of MCM. Further it was found that ORC2 could autophosphorylate in the presence of ATP and more remarkably could phosphorylate MCM in a species-specific manner.

Crystal structure of a near-full-length archaeal MCM: functional insights for an AAA+ hexameric helicase

The minichromosome maintenance protein (MCM) complex is an essential replicative helicase for DNA replication in Archaea and Eukaryotes. Whereas the eukaryotic complex consists of 6 homologous proteins (MCM2-7), the archaeon Sulfolobus solfataricus has only 1 MCM protein (ssoMCM), 6 subunits of which form a homohexamer. Here, we report a 4.35-A crystal structure of the near-full-length ssoMCM. The structure shows an elongated fold, with 5 subdomains that are organized into 2 large N- and C-terminal domains. A near-full-length ssoMCM hexamer generated based on the 6-fold symmetry of the N-terminal Methanothermobacter thermautotrophicus (mtMCM) hexamer shows intersubunit distances suitable for bonding contacts, including the interface around the ATP pocket. Four unusual beta-hairpins of each subunit are located inside the central channel or around the side channels in the hexamer. Additionally, the hexamer fits well into the double-hexamer EM map of mtMCM. Our mutational analysis of residues at the intersubunit interfaces and around the side channels demonstrates their critical roles for hexamerization and helicase function. These structural and biochemical results provide a basis for future study of the helicase mechanisms of the archaeal and eukaryotic MCM complexes in DNA replication.

Biochemical characterization of the minichromosome maintenance protein from the archaeon Thermoplasma acidophilum

Minichromosome maintenance (MCM) proteins are thought to function as the replicative helicases in archaea. Studies have shown that the MCM complex from the thermoacidophilic euryarchaeon Thermoplasma acidophilum (TaMCM) has some properties not reported in other archaeal MCM helicases. Here, the biochemical properties of the TaMCM are studied. The protein binds single-stranded DNA, has DNA-dependent ATPase activity and ATP-dependent 3' --> 5' helicase activity. The optimal helicase conditions with regard to temperature, pH and salinity are similar to the intracellular conditions in T. acidophilum. It is also found that about 1,000 molecules of TaMCM are present per actively growing cell.

The Methanothermobacter thermautotrophicus MCM helicase is active as a hexameric ring

The minichromosome maintenance (MCM) complex is thought to function as the replicative helicase in archaea and eukarya. The structure of the single MCM protein homologue from the archaeon Methanothermobacter thermautotrophicus is not yet clear, and hexameric, heptameric, octameric, and dodecameric structures, open rings, and filamentous structures have been reported. Using a combination of biochemical and structural analysis, it is shown here that the M. thermautotrophicus MCM helicase is active as a hexamer.

Cryo-electron microscopy reveals a novel DNA-binding site on the MCM helicase

The eukaryotic MCM2-7 complex is recruited at origins of replication during the G1 phase and acts as the main helicase at the replication fork during the S phase of the cell cycle. To characterize the interplay between the MCM helicase and DNA prior to the melting of the double helix, we determined the structure of an archaeal MCM orthologue bound to a 5.6-kb double-stranded DNA segment, using cryo-electron microscopy. DNA wraps around the N-terminal face of a single hexameric ring. This interaction requires a conformational change within the outer belt of the MCM N-terminal domain, exposing a previously unrecognized helix-turn-helix DNA-binding motif. Our findings provide novel insights into the role of the MCM complex during the initiation step of DNA replication.

Structural analysis of the Sulfolobus solfataricus MCM protein N-terminal domain

The Mini-Chromosome Maintenance (MCM) proteins are candidates of replicative DNA helicase in eukarya and archaea. Here we report a 2.8 Å crystal structure of the N-terminal domain (residues 1–268) of the Sulfolobus solfataricus MCM (Sso MCM) protein. The structure reveals single-hexameric ring-like architecture, at variance from the protein of Methanothermobacter thermoautotrophicus (Mth). Moreover, the central channel in Sso MCM seems significantly narrower than the Mth counterpart, which appears to more favorably accommodate single-stranded DNA than double-stranded DNA, as supported by DNA-binding assays. Structural analysis also highlights the essential role played by the zinc-binding domain in the interaction with nucleic acids and allows us to speculate that the Sso MCM N-ter domain may function as a molecular clamp to grasp the single-stranded DNA passing through the central channel. On this basis possible DNA unwinding mechanisms are discussed.

Functional differentiation and cooperative interaction between two eukaryote-like archaeal Orc1/Cdc6 proteins on the replication origin

The DNA replication apparatus of archaea represents a core version of that in eukaryotes. Archaeal Orc1/Cdc6s can be an integral component in the replication machineries cooperatively regulating DNA replication. We investigated the DNA-binding activities of two eukaryote-like Orc1/Cdc6 proteins (SsoCdc6-1 and -2) and interactions between them on the different structural duplex DNA substrates derived from oriC1 of Sulfolobus solfataricus. The results showed that two Orc1/Cdc6 proteins stimulated mutual DNA-binding activities at lower concentrations and formed bigger SsoCdc6-1/SsoCdc6-2/DNA complex at higher concentrations. Furthermore, SsoCdc6-2 stimulated the DNA-binding activity of SsoMCM and demonstrated a high affinity to the 5-forked DNA. In contrast, SsoCdc6-1 inhibited the binding of SsoMCM and demonstrated better affinity to the sequence-specific blunt DNA substrate. Finally, we found that the two proteins physically interacted with each other and with SsoMCM. Thus, the two Orc1/Cdc6 proteins were functionally different, but they may keep the coordinated interaction on the replication origin.

A novel DNA helicase with strand-annealing activity from the crenarchaeon Sulfolobus solfataricus

To protect their genetic material cells adopt different mechanisms linked to DNA replication, recombination and repair. Several proteins function at the interface of these DNA transactions. In the present study, we report on the identification of a novel archaeal DNA helicase. BlastP searches of the Sulfolobus solfataricus genome database allowed us to identify an open reading frame (SSO0112, 875 amino acid residues) having sequence similarity with the human RecQ5beta. The corresponding protein, termed Hel112 by us, was produced in Escherichia coli in soluble form, purified to homogeneity and characterized. Gel-filtration chromatography and glycerol-gradient sedimentation analyses revealed that Hel112 forms monomers and dimers in solution. Biochemical characterization of the two oligomeric species revealed that only the monomeric form has an ATP-dependent 3'-5' DNA-helicase activity, whereas, unexpectedly, both the monomeric and dimeric forms possess DNA strand-annealing capability. The Hel112 monomeric form is able to unwind forked and 3'-tailed DNA structures with high efficiency, whereas it is almost inactive on blunt-ended duplexes and bubble-containing molecules. This analysis reveals that S. solfataricus Hel112 shares some enzymatic features with the RecQ-like DNA helicases and suggests potential cellular functions of this protein.

The GINS complex from Pyrococcus furiosus stimulates the MCM helicase activity

Pyrococcus furiosus, a hyperthermophilic Archaea, has homologs of the eukaryotic MCM (mini-chromosome maintenance) helicase and GINS complex. The MCM and GINS proteins are both essential factors to initiate DNA replication in eukaryotic cells. Many biochemical characterizations of the replication-related proteins have been reported, but it has not been proved that the homologs of each protein are also essential for replication in archaeal cells. Here, we demonstrated that the P. furiosus GINS complex interacts with P. furiosus MCM. A chromatin immunoprecipitation assay revealed that the GINS complex is detected preferentially at the oriC region on Pyrococcus chromosomal DNA during the exponential growth phase but not in the stationary phase. Furthermore, the GINS complex stimulates both the ATPase and DNA helicase activities of MCM in vitro. These results strongly suggest that the archaeal GINS is involved in both the initiation and elongation processes of DNA replication in P. furiosus, as observed in eukaryotic cells.

Single strand binding proteins increase the processivity of DNA unwinding by the hepatitis C virus helicase

The nonstructural NS3 protein of the hepatitis C virus is a multifunctional enzyme with an N-terminal serine protease activity and a C-terminal helicase activity. The helicase is capable of unwinding both DNA and RNA duplexes; however, the overall processivity of the helicase is fairly low. We show here that single-strand binding (SSB) proteins enhance the unwinding processivity of both the NS3 helicase domain (NS3h) and the full-length protease-helicase NS3-4A. The detailed study of the effect of SSB on the DNA unwinding activity of NS3h indicates that the SSB stabilizes the helicase at the unwinding junction and prevents its dissociation. These results suggest a potential role for either cellular or virus-encoded SSB protein in improving the processivity of the NS3 in vivo.

ATPase site architecture and helicase mechanism of an archaeal MCM

The subunits of the presumptive replicative helicase of archaea and eukaryotes, the MCM complex, are members of the AAA+ (ATPase-associated with various cellular activities) family of ATPases. Proteins within this family harness the chemical energy of ATP hydrolysis to perform a broad range of cellular processes. Here, we investigate the function of the AAA+ site in the mini-chromosome maintenance (MCM) complex of the archaeon Sulfolobus solfataricus (SsoMCM). We find that SsoMCM has an unusual active-site architecture, with a unique blend of features previously found only in distinct families of AAA+ proteins. We additionally describe a series of mutant doping experiments to investigate the mechanistic basis of intersubunit coordination in the generation of helicase activity. Our results indicate that MCM can tolerate catalytically inactive subunits and still function as a helicase, leading us to propose a semisequential model for helicase activity of this complex.

MCM forked substrate specificity involves dynamic interaction with the 5'-tail

The archaeal minichromosome maintenance protein MCM forms a homohexameric complex that functions as the DNA replicative helicase and serves as a model system for its eukaryotic counterpart. Here, we applied single molecule fluorescence resonance energy transfer methods to probe the substrate specificity and binding mechanism of MCM from the hyperthermophilic Archaea Sulfolobus solfataricus on various DNA substrates. S. solfataricus MCM displays a binding preference for forked substrates relative to partial or full duplex substrates. Moreover, the nature of MCM binding to Y-shaped substrates is distinct in that MCM loads on the 3'-tail while interacting with the 5'-tail likely via the MCM surface. These results provide the first elucidation of a dynamic nature of interaction between a ring-shaped helicase interacting with an opposing single-stranded DNA tail. This interaction contributes to substrate selectivity and increases the stability of the forked DNA-MCM complex, with possible implications for the MCM unwinding mechanism.

Three eukaryote-like Orc1/Cdc6 proteins functionally interact and mutually regulate their activities of binding to the replication origin in the hyperthermophilic archaeon Sulfolobus solfataricus P2

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. However, it is not known whether these SsoCdc6 proteins can functionally interact and collectively contribute to DNA replication initiation. In the current work, we found that SsoCdc6-1 stimulates DNA-binding activities of SsoCdc6-3. In contrast, SsoCdc6-3 inhibits those of both SsoCdc6-1 and SsoCdc6-2. These regulatory functions are differentially affected by the C-terminal domains of these SsoCdc6 proteins. These data, in conjunction with studies on physical interactions between these replication initiators by bacterial two-hybrid and pull-down/Western blot assays, lead us to propose the possibility that multiple SsoCdc6 proteins might coordinately regulate DNA replication in the archaeon species. This is the first report on the functional interaction among the archaeal multiple Cdc6 proteins to regulate DNA replication.

Divergent functions of multiple eukaryote-like Orc1/Cdc6 proteins on modulating the loading of the MCM helicase onto the origins of the hyperthermophilic archaeon Sulfolobus solfataricus P2

The Cdc6 protein has been suggested as a loader for the eukaryotic MCM helicase. Archaeal replication machinery represents a core version of that in eukaryotes. In the current work, three eukaryotic Orc1/Cdc6 homologs (SsoCdc6-1, -2, and -3) from crenarchaeon Sulfolobus solfataricus were shown to have totally different effects on the interactions with SsoMCM helicase. SsoCdc6-2 stimulates the binding of the SsoMCM onto the origin DNA, but SsoCdc6-1 and SsoCdc6-3 significantly inhibit the loading activities, and these inhibitive effects can not be reversed by the stimulation of SsoCdc6-2. Using pull-down assays, we showed that three SsoCdc6 proteins interacted physically with the SsoMCM. Furthermore, the C-terminal domains of SsoCdc6 proteins were shown to physically and functionally affect the interactions with SsoMCM. This is the first report on the divergent functions of multiple eukaryote-like Orc1/Cdc6 proteins on regulating the loading of the MCM helicase onto the origins in the archaeon.

Modular organization of the Sulfolobus solfataricus mini-chromosome maintenance protein

Mini-chromosome maintenance (MCM) proteins form ring-like hexameric complexes that are commonly believed to act as the replicative DNA helicase at the eukaryotic/archaeal DNA replication fork. Because of their simplified composition with respect to the eukaryotic counterparts, the archaeal MCM complexes represent a good model system to use in analyzing the structural/functional relationships of these important replication factors. In this study the domain organization of the MCM-like protein from Sulfolobus solfataricus (Sso MCM) has been dissected by trypsin partial proteolysis. Three truncated derivatives of Sso MCM corresponding to protease-resistant domains were produced as soluble recombinant proteins and purified: the N-terminal domain (N-ter, residues 1-268); a fragment comprising the AAA+ and C-terminal domains (AAA+-C-ter, residues 269-686); and the C-terminal domain (C-ter, residues 504-686). All of the purified recombinant proteins behaved as monomers in solution as determined by analytical gel filtration chromatography, suggesting that the polypeptide chain integrity is required for stable oligomerization of Sso MCM. However, the AAA+-C-ter derivative, which includes the AAA+ motor domain and retains ATPase activity, was able to form dimers in solution when ATP was present, as analyzed by size exclusion chromatography and glycerol gradient sedimentation analyses. Interestingly, the AAA+-C-ter protein could displace oligonucleotides annealed to M13 single-stranded DNA although with a reduced efficiency in comparison with the full-sized Sso MCM. The implications of these findings for understanding the DNA helicase mechanism of the MCM complex are discussed.

DNA replication in the archaea

The archaeal DNA replication machinery bears striking similarity to that of eukaryotes and is clearly distinct from the bacterial apparatus. In recent years, considerable advances have been made in understanding the biochemistry of the archaeal replication proteins. Furthermore, a number of structures have now been obtained for individual components and higher-order assemblies of archaeal replication factors, yielding important insights into the mechanisms of DNA replication in both archaea and eukaryotes.

Stimulation of MCM helicase activity by a Cdc6 protein in the archaeon Thermoplasma acidophilum

Replicative DNA helicases are ring-shaped hexamers that play an essential role in chromosomal DNA replication. They unwind the two strands of the duplex DNA and provide the single-stranded (ss) DNA substrate for the polymerase. The minichromosome maintenance (MCM) proteins are thought to function as the replicative helicases in eukarya and archaea. The proteins of only a few archaeal organisms have been studied and revealed that although all have similar amino acid sequences and overall structures they differ in their biochemical properties. In this report the biochemical properties of the MCM protein from the archaeon Thermoplasma acidophilum is described. The enzyme has weak helicase activity on a substrate containing only a 3′-ssDNA overhang region and the protein requires a forked DNA structure for efficient helicase activity. It was also found that the helicase activity is stimulated by one of the two T.acidophilum Cdc6 homologues. This is an interesting observation as it is in sharp contrast to observations made with MCM and Cdc6 homologues from other archaea in which the helicase activity is inhibited when bound to Cdc6.

Structural basis of the Methanothermobacter thermautotrophicus MCM helicase activity

The MCM complex from the archaeon Methanother-mobacter thermautotrophicus is a model for the eukaryotic MCM2-7 helicase. We present electron-microscopy single-particle reconstructions of a DNA treated M.thermautotrophicus MCM sample and a ADP.AlF(x) treated sample, respectively assembling as double hexamers and double heptamers. The electron-density maps display an unexpected asymmetry between the two rings, suggesting that large conformational changes can occur within the complex. The structure of the MCM N-terminal domain, as well as the AAA+ and the C-terminal HTH dom-ains of ZraR can be fitted into the reconstructions. Distinct configurations can be modelled for the AAA+ and the HTH domains, suggesting the nature of the conformational change within the complex. The pre-sensor 1 and the helix 2 insertions, important for the activity, can be located pointing towards the centre of the channel in the presence of DNA. We propose a mechanistic model for the helicase activity, based on a ligand-controlled rotation of the AAA+ subunits.

Structural studies of the archaeal MCM complex in different functional states

The primary candidate for the eukaryotic replicative helicase is the MCM2-7 complex, a hetero-oligomer formed by six AAA+ paralogous polypeptides. A simplified model for structure-function studies is the homo-oligomeric orthologue from the archaeon Methanothermobacter thermoautotrophicus. The crystal structure of the DNA-interacting N-terminal domain of this homo-oligomer revealed a double hexamer in a head-to-head configuration; single-particle electron microscopy studies have shown that the full-length protein complex can form both single and double rings, in which each ring can consist of a cyclical arrangement of six or seven subunits. Using single-particle techniques and especially multivariate statistical symmetry analysis, we have assessed the changes in stoichiometry that the complex undergoes when treated with various nucleotide analogues or when binding a double-stranded DNA fragment. We found that the binding of nucleotides or of double-stranded DNA leads to the preferred formation of double-ring structures. Specifically, the protein complex is present as a double heptamer when treated with a nucleotide analogue, but it is rather found as a double hexamer when complexed with double-stranded DNA. The possible physiological role of the various stoichiometries of the complex is discussed in the light of the proposed mechanisms of helicase activity.

Influence of Chromatin and Single Strand Binding Proteins on the Activity of an Archaeal MCM

The mini-chromosome maintenance (MCM) complex is the presumptive replicative helicase in archaea and eukaryotes. In archaea, the MCM is a homo-multimer, in eukaryotes a heterohexamer composed of six related subunits, MCM 2-7. Biochemical studies using naked DNA templates have revealed that archaeal MCMs and a sub-complex of eukaryotic MCM 4, 6 and 7 have 3' to 5' helicase activity. Here, we investigate the influence of the major chromatin proteins, Alba and Sul7d, of Sulfolobus solfataricus (Sso) on the ability of the MCM complex to melt partial duplex DNA substrates. In addition, we test the effect of Sso SSB on MCM activity. We reveal that Alba represents a formidable barrier to MCM activity and further demonstrate that acetylation of Alba alleviates repression of MCM activity.

The chromosome replication machinery of the archaeon Sulfolobus solfataricus

In the three domains of life, the archaea, bacteria, and eukarya, there are two general lineages of DNA replication proteins: the bacterial and the eukaryal/archaeal lineages. The hyperthermophilic archaeon Sulfolobus solfataricus provides an attractive model for biochemical study of DNA replication. Its relative simplicity in both genomic and biochemical contexts, together with high protein thermostability, has already provided insight into the function of the more complex yet homologous molecules of the eukaryotic domain. Here, we provide an overview of recent insights into the functioning of the chromosome replication machinery of S. solfataricus, focusing on some of the relatively well characterized core components that act at the DNA replication fork.

Archaeal DNA replication and repair

Since the first archaeal genome was sequenced, much attention has been focused on the study of these unique microorganisms. We have learnt that although archaeal DNA metabolic processes (replication, recombination and repair) are more similar to the metabolic processes of Eukarya than those of Bacteria, Archaea are not simply 'mini Eukarya'. They are, in fact, a mosaic of the eukaryal and bacterial systems that also possess archaeal-specific features. Recent biochemical and structural studies of the proteins that participate in archaeal DNA replication and repair have increased our understanding of these processes.

Biochemical characterization of two Cdc6/ORC1-like proteins from the crenarchaeon Sulfolobus solfataricus

The biological role of archaeal proteins, homologous to the eukaryal replication initiation factors of cell division control (Cdc6) and origin recognition complex (ORC1), has not yet been clearly established. The hyperthermophilic crenarchaeon Sulfolobus solfataricus (referred to as Sso) possesses three Cdc6/ORC1-like factors, which are named Sso Cdc6-1, Cdc6-2 and Cdc6-3. This study is a report on the biochemical characterization of Sso Cdc6-1 and Cdc6-3. It has been found that either Sso Cdc6-1 or Cdc6-3 behave as monomers in solutions by gel filtration analyses. Both factors are able to bind to various single-stranded and double-stranded DNA ligands, but Sso Cdc6-3 shows a higher DNA-binding affinity. It has also been observed that either Sso Cdc6-1 or Cdc6-3 inhibit the DNA unwinding activity of the S. solfataricus homo-hexameric mini-chromosome maintenance (MCM)-like DNA helicase (Sso MCM); although they strongly stimulate the interaction of the Sso MCM with bubble-containing synthetic oligonucleotides. The study has also showed, with surface plasmon resonance measurements, that Sso Cdc6-2 physically interacts with either Sso Cdc6-1 or Sso Cdc6-3. These findings may provide important clues needed to understand the biological role that is played by each of these three Cdc6 factors during the DNA replication initiation process in the S. solfataricus cells.

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.