Why Are There So Many Diverse Replication Machineries?

The replicon model has initiated a major research line in molecular biology: the study of DNA replication mechanisms. Until now, the majority of studies have focused on a limited set of model organisms, mainly from Bacteria or Opisthokont eukaryotes (human, yeasts) and a few viral systems. However, molecular evolutionists have shown that the living world is more complex and diverse than believed when the operon model was proposed. Comparison of DNA replication proteins in the three domains, Archaea, Bacteria, and Eukarya, have surprisingly revealed the existence of two distinct sets of non-homologous cellular DNA replication proteins, one in Bacteria and the other in Archaea and Eukarya, suggesting that the last universal common ancestor possibly still had an RNA genome. A major puzzle is the presence in eukaryotes of the unfaithful DNA polymerase alpha (Pol α) to prime Okazaki fragments. Interestingly, Pol α is specifically involved in telomere biosynthesis, and its absence in Archaea correlates with the absence of telomeres. The recent discovery of telomere-like GC quartets in eukaryotic replication origins suggests a link between Pol α and the overall organization of the eukaryotic chromosome. As previously proposed by Takemura, Pol α might have originated from a mobile element of viral origin that played a critical role in the emergence of the complex eukaryotic genomes. Notably, most large DNA viruses encode DNA replication proteins very divergent from their cellular counterparts. The diversity of viral replication machineries compared to cellular ones suggests that DNA and DNA replication mechanisms first originated and diversified in the ancient virosphere, possibly explaining why they are so many different types of replication machinerie.     

The Roles of Family B and D DNA Polymerases in Thermococcus Species 9°N Okazaki Fragment Maturation

During replication, Okazaki fragment maturation is a fundamental process that joins discontinuously synthesized DNA fragments into a contiguous lagging strand. Efficient maturation prevents repeat sequence expansions, small duplications, and generation of double-stranded DNA breaks. To address the components required for the process in Thermococcus, Okazaki fragment maturation was reconstituted in vitro using purified proteins from Thermococcus species 9°N or cell extracts. A dual color fluorescence assay was developed to monitor reaction substrates, intermediates, and products. DNA polymerase D (polD) was proposed to function as the replicative polymerase in Thermococcus replicating both the leading and the lagging strands. It is shown here, however, that it stops before the previous Okazaki fragments, failing to rapidly process them. Instead, Family B DNA polymerase (polB) was observed to rapidly fill the gaps left by polD and displaces the downstream Okazaki fragment to create a flap structure. This flap structure was cleaved by flap endonuclease 1 (Fen1) and the resultant nick was ligated by DNA ligase to form a mature lagging strand. The similarities to both bacterial and eukaryotic systems and evolutionary implications of archaeal Okazaki fragment maturation are discussed.     

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.     

Size distribution of DNA replicative intermediates in bacteriophage P4 and in Escherichia coli.

We have tested the hypothesis that Okazaki fragment replicative intermediates have defined termini using as a model system the in vivo DNA replication of the tiny bacteriophage P4. The kinetics of formation of intermediates in P4 DNA replication have been investigated. P4 DNA replication in DNA polymerase I-deficient mutants generates Okazaki fragments with a size distribution similar to that in uninfected cells. When P4-derived Okazaki fragments are resolved by agarose gel electrophoresis, no discrete size classes appear. This finding is incompatible with sequence-specific models of Okazaki fragment formation but supports the view that these replication intermediates are initiated and terminated at random locations on the P4 chromosome.     

Helicobacter pylori oriC��the first bipartite origin of chromosome replication in Gram-negative bacteria

Binding of the DnaA protein to oriC leads to DNA melting within the DNA unwinding element (DUE) and initiates replication of the bacterial chromosome. Helicobacter pylori oriC was previously identified as a region localized upstream of dnaA and containing a cluster of DnaA boxes bound by DnaA protein with a high affinity. However, no unwinding within the oriC sequence has been detected. Comprehensive in silico analysis presented in this work allowed us to identify an additional region (oriC2), separated from the original one (oriC1) by the dnaA gene. DnaA specifically binds both regions, but DnaA-dependent DNA unwinding occurs only within oriC2. Surprisingly, oriC2 is bound exclusively as supercoiled DNA, which directly shows the importance of the DNA topology in DnaA-oriC interactions, similarly as previously presented only for initiator-origin interactions in Archaea and some Eukaryota. We conclude that H. pylori oriC exhibits bipartite structure, being the first such origin discovered in a Gram-negative bacterium. The H. pylori mode of initiator-oriC interactions, with the loop formation between the subcomplexes of the discontinuous origin, resembles those discovered in Bacillus subtilis chromosome and in many plasmids, which might suggest a similar way of controlling initiation of replication.     

DNA Repair Systems in Archaea: Mementos from the Last Universal Common Ancestor?

DNA repair in the Archaea is relevant to the consideration of genome maintenance and replication fidelity in the last universal common ancestor (LUCA) from two perspectives. First, these prokaryotes embody a mix of bacterial and eukaryal molecular features. Second, DNA repair proteins would have been essential in LUCA to maintain genome integrity, regardless of the environmental temperature. Yet we know very little of the basic molecular mechanisms of DNA damage and repair in the Archaea in general. Many studies on DNA repair in archaea have been conducted with hyperthermophiles because of the additional stress imposed on their macromolecules by high temperatures. In addition, of the six complete archaeal genome sequences published so far, five are thermophilic archaea. We have recently shown that the hyperthermophile Pyrococcus furiosus has an extraordinarily high capacity for repair of radiation-induced double-strand breaks and we have identified and sequenced several genes involved in DNA repair in P. furiosus. At the sequence level, only a few genes share homology with known bacterial repair genes. For instance, our phylogenetic analysis indicates that archaeal recombinases occur in two paralogous gene families, one of which is very deeply branched, and both recombinases are more closely related to the eukaryotic RAD51 and Dmc1 gene families than to the Escherichia coli recA gene. We have also identified a gene encoding a repair endo/exonuclease in the genomes of several Archaea. The archaeal sequences are highly homologous to those of the eukaryotic Rad2 family and they cluster with genes of the FEN-1 subfamily, which are known to be involved in DNA replication and repair in eukaryotes. We argue that there is a commonality of mechanisms and protein sequences, shared between prokaryotes and eukaryotes for several modes of DNA repair, reflecting diversification from a minimal set of genes thought to represent the genome of the LUCA.     

Identification of a mismatch-specific endonuclease in hyperthermophilic Archaea

The common mismatch repair system processed by MutS and MutL and their homologs was identified in Bacteria and Eukarya. However, no evidence of a functional MutS/L homolog has been reported for archaeal organisms, and it is not known whether the mismatch repair system is conserved in Archaea. Here, we describe an endonuclease that cleaves double-stranded DNA containing a mismatched base pair, from the hyperthermophilic archaeon Pyrococcus furiosus. The corresponding gene revealed that the activity originates from PF0012, and we named this enzyme Endonuclease MS (EndoMS) as the mismatch-specific Endonuclease. The sequence similarity suggested that EndoMS is the ortholog of NucS isolated from Pyrococcus abyssi, published previously. Biochemical characterizations of the EndoMS homolog from Thermococcus kodakarensis clearly showed that EndoMS specifically cleaves both strands of double-stranded DNA into 5′-protruding forms, with the mismatched base pair in the central position. EndoMS cleaves G/T, G/G, T/T, T/C and A/G mismatches, with a more preference for G/T, G/G and T/T, but has very little or no effect on C/C, A/C and A/A mismatches. The discovery of this endonuclease suggests the existence of a novel mismatch repair process, initiated by the double-strand break generated by the EndoMS endonuclease, in Archaea and some Bacteria.     

Synthesis of small polynucleotide chains in thymine-depleted bacteria

Bacteria that are depleted of intracellular thymidine nucleotide pools incorporate [³H]thymine at full specific activity, allowing the detection of early intermediates in DNA replication. A short pulse of [³H]thymine is incorporated almost exclusively into very small DNA chains which, during further incorporation of thymine, are converted into larger chains and high molecular weight DNA. The synthesis of these small DNA chains depends on the products of dna genes B, E and G. Analysis of the DNA by gel filtration on Sepharose 2B revealed an abundance of extremely short DNA chains while the frequency of larger chains decreased exponentially with increasing size. This size distribution of small DNA chains suggests a mechanism of DNA replication in which larger chains (Okazaki pieces, Okazaki et al., 1968a) arise through joining of extremely short polynucleotide chains in a process resembling crystallization rather than unidirectional chain elongation.     

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.     

Localized melting of duplex DNA by Cdc6/Orc1 at the DNA replication origin in the hyperthermophilic archaeon Pyrococcus furiosus

The initiation step is a key process to regulate the frequency of DNA replication. Although recent studies in Archaea defined the origin of DNA replication (oriC) and the Cdc6/Orc1 homolog as an origin recognition protein, the location and mechanism of duplex opening have remained unclear. We have found that Cdc6/Orc1 binds to oriC and unwinds duplex DNA in the hyperthermophilic archaeon Pyrococcus furiosus, by means of a P1 endonuclease assay. A primer extension analysis further revealed that this localized unwinding occurs in the oriC region at a specific site, which is 12-bp long and rich in adenine and thymine. This site is different from the predicted duplex unwinding element (DUE) that we reported previously. We also discovered that Cdc6/Orc1 induces topological changes in supercoiled oriC DNA, and that this process is dependent on the AAA+ domain. These results indicate that topological alterations of oriC DNA by Cdc6/Orc1 introduce a single-stranded region at the 12-mer site, that could possibly serve as an entry point for Mcm helicase.     

Archaeal chromatin proteins

Archaea, along with Bacteria and Eukarya, are the three domains of life. In all living cells, chromatin proteins serve a crucial role in maintaining the integrity of the structure and function of the genome. An array of small, abundant and basic DNA-binding proteins, considered candidates for chromatin proteins, has been isolated from the Euryarchaeota and the Crenarchaeota, the two major phyla in Archaea. While most euryarchaea encode proteins resembling eukaryotic histones, crenarchaea appear to synthesize a number of unique DNA-binding proteins likely involved in chromosomal organization. Several of these proteins (e.g., archaeal histones, Sac10b homologs, Sul7d, Cren7, CC1, etc.) have been extensively studied. However, whether they are chromatin proteins and how they function in vivo remain to be fully understood. Future investigation of archaeal chromatin proteins will lead to a better understanding of chromosomal organization and gene expression in Archaea and provide valuable information on the evolution of DNA packaging in cellular life.     

Roles of DNA polymerase I in leading and lagging-strand replication defined by a high-resolution mutation footprint of ColE1 plasmid replication

DNA polymerase I (pol I) processes RNA primers during lagging-strand synthesis and fills small gaps during DNA repair reactions. However, it is unclear how pol I and pol III work together during replication and repair or how extensive pol I processing of Okazaki fragments is in vivo. Here, we address these questions by analyzing pol I mutations generated through error-prone replication of ColE1 plasmids. The data were obtained by direct sequencing, allowing an accurate determination of the mutation spectrum and distribution. Pol I’s mutational footprint suggests: (i) during leading-strand replication pol I is gradually replaced by pol III over at least 1.3 kb; (ii) pol I processing of Okazaki fragments is limited to ∼20 nt and (iii) the size of Okazaki fragments is short (∼250 nt). While based on ColE1 plasmid replication, our findings are likely relevant to other pol I replicative processes such as chromosomal replication and DNA repair, which differ from ColE1 replication mostly at the recruitment steps. This mutation footprinting approach should help establish the role of other prokaryotic or eukaryotic polymerases in vivo, and provides a tool to investigate how sequence topology, DNA damage, or interactions with protein partners may affect the function of individual DNA polymerases.     

A primordial RNA modification enzyme: the case of tRNA (m1A) methyltransferase

The modified nucleoside 1-methyladenosine (m¹A) is found in the T-loop of many tRNAs from organisms belonging to the three domains of life (Eukaryota, Bacteria, Archaea). In the T-loop of eukaryotic and bacterial tRNAs, m¹A is present at position 58, whereas in archaeal tRNAs it is present at position(s) 58 and/or 57, m¹A57 being the obligatory intermediate in the biosynthesis of 1-methylinosine (m¹I57). In yeast, the formation of m¹A58 is catalysed by the essential tRNA (m¹A58) methyltransferase (MTase), a tetrameric enzyme that is composed of two types of subunits (Gcd14p and Gcd10p), whereas in the bacterium Thermus thermophilus the enzyme is a homotetramer of the TrmI polypeptide. Here, we report that the TrmI enzyme from the archaeon Pyrococcus abyssi is also a homotetramer. However, unlike the bacterial site-specific TrmI MTase, the P.abyssi enzyme is region-specific and catalyses the formation of m¹A at two adjacent positions (57 and 58) in the T-loop of certain tRNAs. The stabilisation of P.abyssi TrmI at extreme temperatures involves intersubunit disulphide bridges that reinforce the tetrameric oligomerisation, as revealed by biochemical and crystallographic evidences. The origin and evolution of m¹A MTases is discussed in the context of different hypotheses of the tree of life.     

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.     

DNA topoisomerase VIII: a novel subfamily of type IIB topoisomerases encoded by free or integrated plasmids in Archaea and Bacteria

Type II DNA topoisomerases are divided into two families, IIA and IIB. Types IIA and IIB enzymes share homologous B subunits encompassing the ATP-binding site, but have non-homologous A subunits catalyzing DNA cleavage. Type IIA topoisomerases are ubiquitous in Bacteria and Eukarya, whereas members of the IIB family are mostly present in Archaea and plants. Here, we report the detection of genes encoding type IIB enzymes in which the A and B subunits are fused into a single polypeptide. These proteins are encoded in several bacterial genomes, two bacterial plasmids and one archaeal plasmid. They form a monophyletic group that is very divergent from archaeal and eukaryotic type IIB enzymes (DNA topoisomerase VI). We propose to classify them into a new subfamily, denoted DNA topoisomerase VIII. Bacterial genes encoding a topoisomerase VIII are present within integrated mobile elements, most likely derived from conjugative plasmids. Purified topoisomerase VIII encoded by the plasmid pPPM1a from Paenibacillus polymyxa M1 had ATP-dependent relaxation and decatenation activities. In contrast, the enzyme encoded by mobile elements integrated into the genome of Ammonifex degensii exhibited DNA cleavage activity producing a full-length linear plasmid and that from Microscilla marina exhibited ATP-independent relaxation activity. Topoisomerases VIII, the smallest known type IIB enzymes, could be new promising models for structural and mechanistic studies.     

DNA replication in Escherichia coli: physical and kinetic studies of the replication point

DNA replication in Escherichia coli was followed using analytical composite agarose-acrylamide gel electrophoresis of native and denatured DNA samples from cells that had been pulse-labeled in vivo. The results obtained with samples of native DNA, combined with the different sensitivities of the various electrophoretic fractions of native DNA to enzymatic attack, led us to conclude that a significant amount of single-strandedness exists in the region of the replication site. Data obtained from kinetic analyses of the labeling of both the high molecular weight DNA and the fragments formed on denaturation of native DNA samples were consistent with the Okazaki model (Okazaki et al., 1968a,b) of DNA replication. Furthermore, the data indicated that eight to ten precursor fragments are present per fork during bacterial growth at both 20 and 37 °C, under the conditions used in this study.     

Dynamics of enzymatic interactions during short flap human Okazaki fragment processing by two forms of human DNA polymerase δ

Lagging strand DNA replication requires the concerted actions of DNA polymerase δ, Fen1 and DNA ligase I for the removal of the RNA/DNA primers before ligation of Okazaki fragments. To better understand this process in human cells, we have reconstituted Okazaki fragment processing by the short flap pathway in vitro with purified human proteins and oligonucleotide substrates. We systematically characterized the key events in Okazaki fragment processing: the strand displacement, Pol δ/Fen1 combined reactions for removal of the RNA/DNA primer, and the complete reaction with DNA ligase I. Two forms of human DNA polymerase δ were studied: Pol δ4 and Pol δ3, which represent the heterotetramer and the heterotrimer lacking the p12 subunit, respectively. Pol δ3 exhibits very limited strand displacement activity in contrast to Pol δ4, and stalls on encounter with a 5′-blocking oligonucleotide. Pol δ4 and Pol δ3 exhibit different characteristics in the Pol δ/Fen1 reactions. While Pol δ3 produces predominantly 1 and 2 nt cleavage products irrespective of Fen1 concentrations, Pol δ4 produces cleavage fragments of 1–10 nts at low Fen1 concentrations. Pol δ3 and Pol δ4 exhibit comparable formation of ligated products in the complete system. While both are capable of Okazaki fragment processing in vitro, Pol δ3 exhibits ideal characteristics for a role in Okazaki fragment processing. Pol δ3 readily idles and in combination with Fen1 produces primarily 1 nt cleavage products, so that nick translation predominates in the removal of the blocking strand, avoiding the production of longer flaps that require additional processing. These studies represent the first analysis of the two forms of human Pol δ in Okazaki fragment processing. The findings provide evidence for the novel concept that Pol δ3 has a role in lagging strand synthesis, and that both forms of Pol δ may participate in DNA replication in higher eukaryotic cells.     

DNA replication: archaeal oriGINS

GINS is an essential eukaryotic DNA replication factor that is found in a simplified form in Archaea. A new study in this issue of BMC Biology reveals the first structure of the archaeal GINS complex. The structure reveals the anticipated similarity to the previously determined eukaryotic complex but also has some intriguing differences in the relative disposition of subunit domains.