The replication origin of archaea is finally revealed

Archaeal DNA replication and repair: new genetic, biophysical and molecular tools for discovering and characterizing enzymes, pathways and mechanisms

DNA replication and repair are essential biological processes needed for the survival of all organisms. Although these processes are fundamentally conserved in the three domains, archaea, bacteria and eukarya, the proteins and complexes involved differ. The genetic and biophysical tools developed for archaea in the last several years have accelerated the study of DNA replication and repair in this domain. In this review, the current knowledge of DNA replication and repair processes in archaea will be summarized, with emphasis on the contribution of genetics and other recently developed biophysical and molecular tools, including capillary gel electrophoresis, next-generation sequencing and single-molecule approaches. How these new tools will continue to drive archaeal DNA replication and repair research will also be discussed.

Do Archaea Need an Origin of Replication?

Chromosomal DNA replication starts at a specific region called an origin of replication. Until recently, all organisms were thought to require origins to replicate their chromosomes. It was recently discovered that some archaeal species do not utilize origins of replication under laboratory growth conditions.

Archaeal DNA replication

DNA replication is essential for all life forms. Although the process is fundamentally conserved in the three domains of life, bioinformatic, biochemical, structural, and genetic studies have demonstrated that the process and the proteins involved in archaeal DNA replication are more similar to those in eukaryal DNA replication than in bacterial DNA replication, but have some archaeal-specific features. The archaeal replication system, however, is not monolithic, and there are some differences in the replication process between different species. In this review, the current knowledge of the mechanisms governing DNA replication in Archaea is summarized. The general features of the replication process as well as some of the differences are discussed.

Thermococcus kodakarensis DNA replication

DNA replication plays an essential role in all life forms. Research on archaeal DNA replication began approximately 20 years ago. Progress was hindered, however, by the lack of genetic tools to supplement the biochemical and structural studies. This has changed, however, and genetic approaches are now available for several archaeal species. One of these organisms is the thermophilic euryarchaeon Thermococcus kodakarensis. In the present paper, the recent developments in the biochemical, structural and genetic studies on the replication machinery of T. kodakarensis are summarized.

Genomic analysis of the uncultivated marine crenarchaeote Cenarchaeum symbiosum

Crenarchaeota are ubiquitous and abundant microbial constituents of soils, sediments, lakes, and ocean waters. To further describe the cosmopolitan nonthermophilic Crenarchaeota, we analyzed the genome sequence of one representative, the uncultivated sponge symbiont Cenarchaeum symbiosum. C. symbiosum genotypes coinhabiting the same host partitioned into two dominant populations, corresponding to previously described a- and b-type ribosomal RNA variants. Although they were syntenic, overlapping a- and b-type ribotype genomes harbored significant variability. A single tiling path comprising the dominant a-type genotype was assembled and used to explore the genomic properties of C. symbiosum and its planktonic relatives. Of 2,066 ORFs, 55.6% matched genes with predicted function from previously sequenced genomes. The remaining genes partitioned between functional RNAs (2.4%) and hypotheticals (42%) with limited homology to known functional genes. The latter category included some genes likely involved in the archaeal-sponge symbiotic association. Conversely, 525 C. symbiosum ORFs were most highly similar to sequences from marine environmental genomic surveys, and they apparently represent orthologous genes from free-living planktonic Crenarchaeota. In total, the C. symbiosum genome was remarkably distinct from those of other known Archaea and shared many core metabolic features in common with its free-living planktonic relatives.

Identification of replication origins in archaeal genomes based on the Z-curve method

The Z-curve is a three-dimensional curve that constitutes a unique representation of a DNA sequence, i.e., both the Z-curve and the given DNA sequence can be uniquely reconstructed from the other. We employed Z-curve analysis to identify one replication origin in the Methanocaldococcus jannaschii genome, two replication origins in the Halobacterium species NRC-1 genome and one replication origin in the Methanosarcina mazei genome. One of the predicted replication origins of Halobacterium species NRC-1 is the same as a replication origin later identified by in vivo experiments. The Z-curve analysis of the Sulfolobus solfataricus P2 genome suggested the existence of three replication origins, which is also consistent with later experimental results. This review aims to summarize applications of the Z-curve in identifying replication origins of archaeal genomes, and to provide clues about the locations of as yet unidentified replication origins of the Aeropyrum pernix K1, Methanococcus maripaludis S2, Picrophilus torridus DSM 9790 and Pyrobaculum aerophilum str. IM2 genomes.

The DNA primase of Sulfolobus solfataricus is activated by substrates containing a thymine-rich bubble and has a 3'-terminal nucleotidyl-transferase activity

DNA primases are responsible for the synthesis of the short RNA primers that are used by the replicative DNA polymerases to initiate DNA synthesis on the leading- and lagging-strand at the replication fork. In this study, we report the purification and biochemical characterization of a DNA primase (Sso DNA primase) from the thermoacidophilic crenarchaeon Sulfolobus solfataricus. The Sso DNA primase is a heterodimer composed of two subunits of 36 kDa (small subunit) and 38 kDa (large subunit), which show sequence similarity to the eukaryotic DNA primase p60 and p50 subunits, respectively. The two polypeptides were co-expressed in Escherichia coli and purified as a heterodimeric complex, with a Stokes radius of about 39.2 A and a 1:1 stoichiometric ratio among its subunits. The Sso DNA primase utilizes poly-pyrimidine single-stranded DNA templates with low efficiency for de novo synthesis of RNA primers, whereas its synthetic function is specifically activated by thymine-containing synthetic bubble structures that mimic early replication intermediates. Interestingly, the Sso DNA primase complex is endowed with a terminal nucleotidyl-transferase activity, being able to incorporate nucleotides at the 3' end of synthetic oligonucleotides in a non-templated manner.

Identification of replication origins in the genome of the methanogenic archaeon, Methanocaldococcus jannaschii

Methanocaldococcus jannaschii has been notorious as an archaeon in which the replication origins are difficult to identify. Although extensive efforts have been exerted on this issue, the locations of replication origins still remain elusive 7 years after the publication of its complete genome sequence in 1996. Ambiguous results were obtained in identifying the replication origins of M. jannaschii based on all theoretical and experimental approaches. In the genome of M. jannaschii, we found that an ORF (MJ0774), annotated as a hypothetical protein, is a homologue of the Cdc6 protein. The position of the gene is at a global minimum of the x component of the Z curve, i.e., RY disparity curve, which has been used to identify replication origins in other Archaea. In addition, an intergenic region (694,540-695,226 bp) that is between the cdc6 gene and an adjacent ORF shows almost all the characteristics of known replication origins, i.e., it is highly rich in AT composition (80%) and contains multiple copies of repeat elements and AT stretches. Therefore, these lines of evidence strongly suggest that the identified region is a replication origin, which is designated as oriC1. The analysis of the y component of the Z curve, i.e., MK disparity curve, suggests the presence of another replication origin corresponding to one of the peaks in the MK disparity curve at around 1,388 kb of the genome.

Archeal DNA replication: eukaryal proteins in a bacterial context

Genome sequences of a number of archaea have revealed an apparent paradox in the phylogenies of the bacteria, archaea, and eukarya, as well as an intriguing set of problems to be resolved in the study of DNA replication. The archaea, long thought to be bacteria, are not only different enough to merit their own domain but also appear to be an interesting mosaic of bacterial, eukaryal, and unique features. Most archaeal proteins participating in DNA replication are more similar in sequence to those found in eukarya than to analogous replication proteins in bacteria. However, archaea have only a subset of the eukaryal replication machinery, apparently needing fewer polypeptides and structurally simpler complexes. The archaeal replication apparatus also contains features not found in other organisms owing, in part, to the broad range of environmental conditions, some extreme, in which members of this domain thrive. In this review the current knowledge of the mechanisms governing DNA replication in archaea is summarized and the similarities and differences of those of bacteria and eukarya are highlighted.

Thymine-rich single-stranded DNA activates Mcm4/6/7 helicase on Y-fork and bubble-like substrates

The presence of multiple clusters of runs of asymmetric adenine or thymine is a feature commonly found in eukaryotic replication origins. Here we report that the helicase and ATPase activities of the mammalian Mcm4/6/7 complex are activated specifically by thymine stretches. The Mcm helicase is specifically activated by a synthetic bubble structure which mimics an activated replication origin, as well as by a Y-fork structure, provided that a single-stranded DNA region of sufficient length is present in the unwound segment or 3' tail, respectively, and that it carries clusters of thymines. Sequences derived from the human lamin B2 origin can serve as a potent activator for the Mcm helicase, and substitution of its thymine clusters with guanine leads to loss of this activation. At the fork, Mcm displays marked processivity, expected for a replicative helicase. These findings lead us to propose that selective activation by stretches of thymine sequences of a fraction of Mcm helicases loaded onto chromatin may be the determinant for selection of initiation sites on mammalian genomes.

Helicase and nuclease activities of hyperthermophile Pyrococcus horikoshii Dna2 inhibited by substrates with RNA segments at 5'-end

Dna2 protein plays an important role in Okazaki fragment maturation on the lagging strand and also participates in DNA repair in Eukarya. Herein, we report the first biochemical characterization of a Dna2 homologue from Archaea, the hyperthermophile Pyrococcus horikoshii (Dna2Pho). Dna2Pho has both a RecB-like nuclease motif and seven conserved helicase motifs similar to Dna2 from Saccharomyces cerevisiae. Dna2Pho has single-stranded (ss) DNA-stimulated ATPase activity, DNA helicase activity (5' to 3' direction) requiring ATP, and nuclease activity, which prefers free 5'-ends of ssDNA as substrate. These activities depend on MgCl(2) concentrations. Dna2Pho requires a higher concentration of MgCl(2) for the nuclease than helicase activity. Both the helicase and nuclease activities of Dna2Pho were inhibited by substrates with RNA segments at the 5'-end of flap DNA, whereas the nuclease activity of Dna2 from S. cerevisiae was reported to be stimulated by RNA segments in the 5'-tail (Bae, S.-H., and Seo, Y. S. (2000) J. Biol. Chem. 38022-38031).

Archaea: an archetype for replication initiation studies?

Whereas the process of DNA replication is fundamentally conserved in the three domains of life, the archaeal system is closer to that of eukarya than bacteria. In the time since the complete genome sequences of several members of the archaeal domain became available, there has been a burst of research on archaeal DNA replication. These studies have led to both expected and surprising findings. This review summarizes the search for origins of replication in archaea, and our current knowledge of initiation, the process by which replication origins are recognized, the DNA molecule is unwound and the replicative helicase is loaded onto the DNA in preparation for DNA synthesis. The similarities and differences of the initiation process in archea, bacteria and eukarya are also summarized.

Multiple replication origins of the archaeon Halobacterium species NRC-1

The genomic sequence of the halophilic archaeon Halobacterium NRC-1 has been analyzed by the Z curve method. The Z curve is a three-dimensional curve that uniquely represents a given DNA sequence. Based on the known behaviors of the Z curves for the archaea whose replication origins have been identified, the analysis of the Z curve for the genome of Halobacterium NRC-1 strongly suggests that the large genome has two replication origins, oriC1 (921,863-922,014) and oriC2 (1,806,444-1,807,229), which are located at two sharp peaks of the Z curve. These two regions are next to the cdc6 genes and contain multiple copies of stretches of G and C, i.e., ggggtgggg and ccccacccc, which may also be regarded as direct and inverted repeats. Based on the above analysis, a model of replication of Halobacterium NRC-1 with two replication origins and two termini has been proposed. The experimental confirmation of this model would constitute the first example of multiple replication origins of archaea, which will finally provide much insight into the understanding of replication mechanisms of eukaryotic organisms, including human. In addition, the potential multiple replication origins of the archaeon Sulfolobus solfataricus are suggested by the analysis based on the Z curve method.

Molecular structure and novel DNA binding sites located in loops of flap endonuclease-1 from Pyrococcus horikoshii

The crystal structure of flap endonuclease-1 from Pyrococcus horikoshii (phFEN-1) was determined to a resolution of 3.1 A. The active cleft of the phFEN-1 molecule is formed with one large loop and four small loops. We examined the function of the conserved residues and positively charged clusters on these loops by kinetic analysis with 45 different mutants. Arg(40) and Arg(42) on small loop 1, a cluster Lys(193)-Lys(195) on small loop 2, and two sites, Arg(94) and Arg(118)-Lys(119), on the large loop were identified as binding sites. Lys(87) on the large loop may play significant roles in catalytic reaction. Furthermore, we successfully elucidated the function of the four DNA binding sites that form productive ES complexes specific for each endo- or exo-type hydrolysis, probably by bending the substrates. For the endo-activity, Arg(94) and Lys(193)-Lys(195) located at the top and bottom of the molecule were key determinants. For the exo-activity, all four sites were needed, but Arg(118)-Lys(119) was dominant. The major binding sites for both the nick substrate and double-stranded DNA might be the same.

Single replication origin of the archaeon Methanosarcina mazei revealed by the Z curve method

The genomic sequence of the archaeon Methanosarcina mazei has been analyzed by the Z curve method. The Z curve is a three-dimensional curve that uniquely represents the given DNA sequence. The three-dimensional Z curve and its x and y components for the genome of M. mazei show a sharp peak and relatively broad peak, respectively. The cdc6 gene is located exactly at the position of the sharp peak. Based on the known behavior of the Z curves for the archaea whose replication origins have been identified, we hypothesize that the replication origin and termination sites correspond to the positions of the sharp peak and broad peak, respectively. We have located an intergenic region that is between the cdc6 gene (MM1314) and the gene for an adjacent protein (MM1315), which shows strong characteristics of the known replication origins. This region is highly rich in AT and contains multiple copies of consecutive repeats. Our results strongly suggest that the single replication origin of M. mazei is situated at the intergenic region between the cdc6 gene and the gene for the adjacent protein, from 1,564,657 to 1,566,241 bp of the genome.

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

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

The genome of M. acetivorans reveals extensive metabolic and physiological diversity

Methanogenesis, the biological production of methane, plays a pivotal role in the global carbon cycle and contributes significantly to global warming. The majority of methane in nature is derived from acetate. Here we report the complete genome sequence of an acetate-utilizing methanogen, Methanosarcina acetivorans C2A. Methanosarcineae are the most metabolically diverse methanogens, thrive in a broad range of environments, and are unique among the Archaea in forming complex multicellular structures. This diversity is reflected in the genome of M. acetivorans. At 5,751,492 base pairs it is by far the largest known archaeal genome. The 4524 open reading frames code for a strikingly wide and unanticipated variety of metabolic and cellular capabilities. The presence of novel methyltransferases indicates the likelihood of undiscovered natural energy sources for methanogenesis, whereas the presence of single-subunit carbon monoxide dehydrogenases raises the possibility of nonmethanogenic growth. Although motility has not been observed in any Methanosarcineae, a flagellin gene cluster and two complete chemotaxis gene clusters were identified. The availability of genetic methods, coupled with its physiological and metabolic diversity, makes M. acetivorans a powerful model organism for the study of archaeal biology. [Sequence, data, annotations and analyses are available at http://www-genome.wi.mit.edu/.]

Characterization of two DNA polymerases from the hyperthermophilic euryarchaeon Pyrococcus abyssi

The complete genome sequence of the hyperthermophilic archaeon Pyrococcus abyssi revealed the presence of a family B DNA polymerase (Pol I) and a family D DNA polymerase (Pol II). To extend our knowledge about euryarchaeal DNA polymerases, we cloned the genes encoding these two enzymes and expressed them in Escherichia coli. The DNA polymerases (Pol I and Pol II) were purified to homogeneity and characterized. Pol I had a molecular mass of approximately 90 kDa, as estimated by SDS/PAGE. The optimum pH and Mg(2+) concentration of Pol I were 8.5-9.0 and 3 mm, respectively. Pol II is composed of two subunits that are encoded by two genes arranged in tandem on the P. abyssi genome. We cloned these genes and purified the Pol II DNA polymerase from an E. coli strain coexpressing the cloned genes. The optimum pH and Mg(2+) concentration of Pol II were 6.5 and 15-20 mm, respectively. Both P. abyssi Pol I and Pol II have associated 3'-->5' exonuclease activity although the exonuclease motifs usually found in DNA polymerases are absent in the archaeal family D DNA polymerase sequences. Sequence analysis has revealed that the small subunit of family D DNA polymerase and the Mre11 nucleases belong to the calcineurin-like phosphoesterase superfamily and that residues involved in catalysis and metal coordination in the Mre11 nuclease three-dimensional structure are strictly conserved in both families. One hypothesis is that the phosphoesterase domain of the small subunit is responsible for the 3'-->5' exonuclease activity of family D DNA polymerase. These results increase our understanding of euryarchaeal DNA polymerases and are of importance to push forward the complete understanding of the DNA replication in P. abyssi.