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.     

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 β-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.     

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.     

Unwinding the structure and function of the archaeal MCM helicase

During chromosomal DNA replication, the replicative helicase unwinds the duplex DNA to provide the single-stranded DNA substrate for the polymerase. In archaea, the replicative helicase is the minichromosome maintenance (MCM) complex. The enzyme utilizes the energy of ATP hydrolysis to translocate along one strand of the duplex and unwind the complementary strand. Much progress has been made in elucidating structure and function since the first report on the biochemical properties of an archaeal MCM protein in 1999. We now know the biochemical and structural properties of the enzyme from several archaeal species and some of the mechanisms by which the enzyme is regulated. This review summarizes recent studies on the archaeal MCM protein and discusses the implications for helicase function and DNA replication in archaea.     

Hexameric ring structure of the full-length archaeal MCM protein complex

In eukaryotes, a family of six homologous minichromosome maintenance (MCM) proteins has a key function in ensuring that DNA replication occurs only once before cell division. Whereas all eukaryotes have six paralogues, in some Archaea a single protein forms a homomeric assembly. The complex is likely to function as a helicase during DNA replication. We have used electron microscopy to obtain a three-dimensional reconstruction of the full-length MCM from Methanobacterium thermoautotrophicum. Six monomers are arranged around a sixfold axis, generating a ring-shaped molecule with a large central cavity and lateral holes. The channel running through the molecule can easily accommodate double-stranded DNA. The crystal structure of the amino-terminal fragment of MCM and a model for the AAA+ hexamer have been docked into the map, whereas additional electron density suggests that the carboxy-terminal domain is located at the interface between the two domains. The structure suggests that the MCM complex is likely to act in a different manner to traditional hexameric helicases and is likely to bear more similarity to the SV40 large T antigen or to double-stranded DNA translocases.     

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.     

The structure and function of MCM from archaeal M. Thermoautotrophicum

Eukaryotic chromosomal DNA is licensed for replication precisely once in each cell cycle. The mini-chromosome maintenance (MCM) complex plays a role in this replication licensing. We have determined the structure of a fragment of MCM from Methanobacterium thermoautotrophicum (mtMCM), a model system for eukaryotic MCM. The structure reveals a novel dodecameric architecture with a remarkably long central channel. The channel surface has an unusually high positive charge and binds DNA. We also show that the structure of the N-terminal fragment is conserved for all MCMs proteins despite highly divergent sequences, suggesting a common architecture for a similar task: gripping/remodeling DNA and regulating MCM activity. An mtMCM mutant protein equivalent to a yeast MCM5 (CDC46) protein with the bob1 mutation at its N terminus has only subtle structural changes, suggesting a Cdc7-bypass mechanism by Bob1 in yeast. Yeast bypass experiments using MCM5 mutant proteins support the hypothesis for the bypass mechanism.     

Substrate requirements for duplex DNA translocation by the eukaryal and archaeal minichromosome maintenance helicases

Replicative DNA helicases are ring-shaped hexamers that play an essential role in DNA synthesis by separating the two strands of chromosomal DNA to provide the single-stranded (ss) substrate for replicative polymerases. Biochemical and structural studies suggest that these helicases translocate along one strand of the duplex, which passes through and interacts with the central channel of these ring-shaped hexamers, and displace the complementary strand. A number of these helicases were shown to also encircle both strands simultaneously and then translocate along double-stranded (ds)DNA. In this report it is shown that the Schizosaccharomyces pombe Mcm4,6,7 complex and archaeal minichromosome maintenance (MCM) helicase from Methanothermobacter thermautotrophicus move along duplex DNA. These two helicases, however, differ in the substrate required to support dsDNA translocation. Although the S. pombe Mcm4,6,7 complex required a 3'-overhang ssDNA region to initiate its association with the duplex, the archaeal protein initiated its transit along dsDNA in the absence of a 3'-overhang region, as well. Furthermore, DNA substrates containing a streptavidin-biotin steric block inhibited the movement of the eukaryotic helicase along ss and dsDNAs but not of the archaeal enzyme. The M. thermautotrophicus MCM helicase, however, was shown to displace a streptavidin-biotin complex from ss, as well as dsDNAs. The possible roles of dsDNA translocation by the MCM proteins during the initiation and elongation phases of chromosomal replication are discussed.     

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.     

Organization of the archaeal MCM complex on DNA and implications for the helicase mechanism

The homomultimeric archaeal mini-chromosome maintenance (MCM) complex serves as a simple model for the analogous heterohexameric eukaryotic complex. Here we investigate the organization and orientation of the MCM complex of the hyperthermophilic archaeon Sulfolobus solfataricus (Sso) on model DNA substrates. Sso MCM binds as a hexamer and slides on the end of a 3'-extended single-stranded DNA tail of a Y-shaped substrate; binding is oriented so that the motor domain of the protein faces duplex DNA. Two candidate beta-hairpin motifs within the MCM monomer have partially redundant roles in DNA binding. Notably, however, conserved basic residues within these motifs have nonequivalent roles in the helicase activity of MCM. On the basis of these findings, we propose a model for the mechanism of the helicase activity of MCM and note parallels with SV40 T antigen.     

Structural and kinetic characterization of an archaeal beta-class carbonic anhydrase

The beta-class carbonic anhydrase from the archaeon Methanobacterium thermoautotrophicum (Cab) was structurally and kinetically characterized. Analytical ultracentrifugation experiments show that Cab is a tetramer. Circular dichroism studies of Cab and the Spinacia oleracea (spinach) beta-class carbonic anhydrase indicate that the secondary structure of the beta-class enzymes is predominantly alpha-helical, unlike that of the alpha- or gamma-class enzymes. Extended X-ray absorption fine structure results indicate the active zinc site of Cab is coordinated by two sulfur and two O/N ligands, with the possibility that one of the O/N ligands is derived from histidine and the other from water. Both the steady-state parameters k(cat) and k(cat)/K(m) for CO(2) hydration are pH dependent. The steady-state parameter k(cat) is buffer-dependent in a saturable manner at both pH 8.5 and 6.5, and the analysis suggested a ping-pong mechanism in which buffer is the second substrate. At saturating buffer conditions and pH 8.5, k(cat) is 2.1-fold higher in H(2)O than in D(2)O, consistent with an intramolecular proton transfer step being rate contributing. The steady-state parameter k(cat)/K(m) is not dependent on buffer, and no solvent hydrogen isotope effect was observed. The results suggest a zinc hydroxide mechanism for Cab. The overall results indicate that prokaryotic beta-class carbonic anhydrases have fundamental characteristics similar to the eukaryotic beta-class enzymes and firmly establish that the alpha-, beta-, and gamma-classes are convergently evolved enzymes that, although structurally distinct, are functionally equivalent.     

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.     

Primary structure of selected archaeal mesophilic and extremely thermophilic outer surface layer proteins

The archaea are recognized as a separate third domain of life together with the bacteria and eucarya. The archaea include the methanogens, extreme halophiles, thermoplasmas, sulfate reducers and sulfur metabolizing thermophiles, which thrive in different habitats such as anaerobic niches, salt lakes, and marine hydrothermals systems and continental solfataras. Many of these habitats represent extreme environments in respect to temperature, osmotic pressure and pH-values and remind on the conditions of the early earth. The cell envelope structures were one of the first biochemical characteristics of archaea studied in detail. The most common archaeal cell envelope is composed of a single crystalline protein or glycoprotein surface layer (S-layer), which is associated with the outside of the cytoplasmic membrane. The S-layers are directly exposed to the extreme environment and can not be stabilized by cellular components. Therefore, from comparative studies of mesophilic and extremely thermophilic S-layer proteins hints can be obtained about the molecular mechanisms of protein stabilization at high temperatures. First crystallization experiments of surface layer proteins under microgravity conditions were successful. Here, we report on the biochemical features of selected mesophilic and extremely archaeal S-layer (glyco-) proteins.     

Comparative analysis of thermoadaptation within the archaeal glyceraldehyde-3-phosphate dehydrogenases from mesophilic Methanobacterium bryantii and thermophilic Methanothermus fervidus

To gain insight into the molecular determinants of thermoadaptation within the family of archaeal glyceraldehyde-3-phosphate dehydrogenases (GAPDH), a homology-based 3-D model of the mesophilic GAPDH from Methanobacterium bryantii was built and compared with the crystal structure of the thermophilic GAPDH from Methanothermus fervidus. The homotetrameric model of the holoenzyme was initially assembled from identical subunits completed with NADP molecules. The structure was then refined by energy minimization and simulated-annealing procedures. PROCHECK and the 3-D profile method were used to appraise the model reliability. Striking molecular features underlying the difference in stability between the enzymes were deduced from their structural comparison. First, both the increase in hydrophobic contacts and the decrease in accessibility to the protein core were shown to discriminate in favor of the thermophilic enzyme. Besides, but to a lesser degree, the number of ion pairs involved in cooperative clusters appeared to correlate with thermostability. Finally, the decreased stability of the mesophilic enzyme was also predicted to proceed from both the lack of charge-dipole interactions within alpha-helices and the enhanced entropy of unfolding due to an increase in chain flexibility. Thus, archaeal GAPDHs appear to be governed by thermoadaptation rules that differ in some aspects from those previously observed within their eubacterial counterparts.     

The interplay of DNA binding, ATP hydrolysis and helicase activities of the archaeal MCM helicase

The MCM (minichromosome maintenance) proteins of archaea are widely believed to be the replicative DNA helicase of these organisms. Most archaea possess a single MCM orthologue that forms homo-multimeric assemblies with a single hexamer believed to be the active form. In the present study we characterize the roles of highly conserved residues in the ATPase domain of the MCM of the hyperthermophilic archaeon Sulfolobus solfataricus. Our results identify a potential conduit for communicating DNA-binding information to the ATPase active site.     

Probing the archaeal diversity of a mixed thermophilic bioleaching culture by TGGE and FISH

The archaeal community present in a sample of Mixed Thermophilic Culture-B (MTC-B) from a laboratory-scale thermophilic bioleaching reactor was investigated by temperature gradient gel electrophoresis (TGGE) and fluorescence in situ hybridisation (FISH). Both techniques were specifically adapted for use on native state bioleaching samples, with a view to establishing convenient means for monitoring culture composition. Using the TGGE protocol developed, the relative species composition of the thermophilic bioleaching sample was analysed, and included four phylotypes belonging to the Sulfolobales, which were related to Stygiolobus azoricus, Metallosphaera sp. J1, Acidianus infernus and Sulfurisphaera ohwakuensis. However, the St. azoricus-like phylotype was difficult to resolve and some micro-heterogeneity was observed within this phylotype. Specific FISH probes were designed to qualitatively assess the presence of the phylotypes in MTC-B. The sample was dominated by Sf. ohwakuensis-like Archaea. In addition, the St. azoricus-like, Metallosphaera species-like and Acidianus species-like cells appeared in similar low abundance in the community. Most strikingly, FISH identified Sulfolobus shibatae-like cells present in low numbers in the sample even though these were not detected by PCR-dependent TGGE. These results highlight the importance of using more than one molecular technique when investigating the archaeal diversity of complex bioleaching reactor samples.     

The MCM8/9 complex: A recent recruit to the roster of helicases involved in genome maintenance

There are several DNA helicases involved in seemingly overlapping aspects of homologous and homoeologous recombination. Mutations of many of these helicases are directly implicated in genetic diseases including cancer, rapid aging, and infertility. MCM8/9 are recent additions to the catalog of helicases involved in recombination, and so far, the evidence is sparse, making assignment of function difficult. Mutations in MCM8/9 correlate principally with primary ovarian failure/insufficiency (POF/POI) and infertility indicating a meiotic defect. However, they also act when replication forks collapse/break shuttling products into mitotic recombination and several mutations are found in various somatic cancers. This review puts MCM8/9 in context with other replication and recombination helicases to narrow down its genomic maintenance role. We discuss the known structure/function relationship, the mutational spectrum, and dissect the available cellular and organismal data to better define its role in recombination.