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Journal of Bacteriology, October 2003, p. 5959-5966, Vol. 185, No. 20
0021-9193/03/$08.00+0 DOI: 10.1128/JB.185.20.5959-5966.2003
Copyright © 2003, American Society for Microbiology. All Rights Reserved.
An Archaeal Chromosomal Autonomously Replicating Sequence Element from an Extreme Halophile, Halobacterium sp. Strain NRC-1
Brian R. Berquist and Shiladitya DasSarma*
Molecular and Cell Biology Program, University of Maryland, Baltimore, and Center of Marine Biotechnology, University of Maryland Biotechnology Institute, Baltimore, Maryland 21202
Received 27 May 2003/
Accepted 31 July 2003

ABSTRACT
We report on the identification and first cloning of an autonomously
replicating sequence element from the chromosome of an archaeon,
the extreme halophile
Halobacterium strain NRC-1. The putative
replication origin was identified by association with the
orc7 gene and replication ability in the host strain, demonstrated
by cloning into a nonreplicating plasmid. Deletion analysis
showed that sequences located up to 750 bp upstream of the
orc7 gene translational start, plus the
orc7 gene and 50 bp downstream,
are sufficient to endow the plasmid with replication ability,
as judged by expression of a plasmid-encoded mevinolin resistance
selectable marker and plasmid recovery after transformation.
Sequences located proximal to the two other chromosomally carried
haloarchaeal
orc genes (
orc6 and
orc8) are not able to promote
efficient autonomous replication. Located within the 750-bp
region upstream of
orc7 is a nearly perfect inverted repeat
of 31 bp, which flanks an extremely AT-rich (44%) stretch of
189 bp. The replication ability of the plasmid was lost when
one copy of the inverted repeat was deleted. Additionally, the
inverted repeat structure near
orc7 homologs in the genomic
sequences of two other halophiles,
Haloarcula marismortui and
Haloferax volcanii, is highly conserved. Our results indicate
that, in halophilic archaea, a chromosomal origin of replication
is physically linked to
orc7 homologs and that this element
is sufficient to promote autonomous replication. We discuss
the finding of a functional haloarchaeal origin in relation
to the large number of
orc1-
cdc6 homologs identified in the
genomes of all haloarchaea to date.

INTRODUCTION
Archaeal microorganisms are phylogenetically distinct from bacteria
(
38) and exhibit significant similarities to eukaryotes in their
macromolecular biosynthetic machinery, including DNA replication,
transcription, and translation systems (
11,
31). They can therefore
serve as relatively simple models for eukaryotes, although the
difficulty of culturing most archaea and their limited capability
for genetic manipulation in the laboratory have restricted the
scope of studies of archaeal molecular biology. However, recent
advances in the genomics, genetics, and biochemistry of archaea
have started to open new avenues in archaeal research. This
is especially true for the halophilic archaea (haloarchaea),
which flourish in hypersaline conditions where NaCl concentrations
can approach saturation (
8). Haloarchaea are easily cultured
in the laboratory and have well-developed genetic transformation
systems with gene replacement and knockout methodology (
6,
32).
As a result, we sought to utilize a combination of genetics
and genomics to initiate a study of DNA replication in haloarchaea.
The single complete haloarchaeal genome sequence obtained thus far, for Halobacterium strain NRC-1, revealed a dynamic 2,571,010-bp genome including 2,682 predicted genes, distributed among three replicons: a 2-Mb large chromosome and two large extrachromosomal replicons, pNRC200 (365 kb) and pNRC100 (191 kb) (30). As with other archaea, the DNA replication machinery of Halobacterium strain NRC-1 appears to be more eukaryotic than bacterial in nature (9, 10). Bioinformatic analysis surprisingly showed the presence of 10 homologs of the eukaryotic-type origin recognition proteins (Orc1 and Cdc6) in NRC-1 (P. Zhang, S. P. Kennedy, B. Berquist, and S. DasSarma, unpublished data), compared to one or two at most in other archaea. In addition, homologs of the eukaryotic-type replicative helicase proteins (MCM), single-stranded DNA binding proteins (RFA), processivity clamp loader proteins (RFC), processivity clamp proteins (PCNA), primase proteins, RNA primer removal proteins (Rad2 and RNase H), ATP-dependent DNA ligase, DNA polymerases (B family), and type IIB topoisomerase (Top6A and Top6B) were also found. A novel heterodimeric family D DNA polymerase gene found only in euryarchaea (4, 37) was also present, as were a few genes for bacterial protein-like replication proteins, a primase (DnaG), and type IA (TopA) and IIA (GyrA and GyrB) DNA topoisomerases.
The genome sequence of Halobacterium strain NRC-1 was analyzed for GC skew, (G+C)/(G-C), on a DNA strand in a sliding window (17). Typically in bacteria and other archaea, GC skew analysis will show the presence of two polarity switches, one indicating the origin of DNA replication and the other indicating the terminus. However, GC skew indicated the presence of four polarity switches for Halobacterium strain NRC-1, consistent with two chromosomal origins of replication. Further analysis of the polarity switch regions revealed the presence of two orc1-cdc6 homologs located proximal to switch points, suggesting the association of the genes with replication origins (22, 27). In many bacterial species, the dnaA gene, encoding the replication initiation protein, is also located proximal to one of the polarity switches (14, 24). Our findings led us to hypothesize that multiple origins of Halobacterium strain NRC-1 may be used to initiate DNA replication of the chromosome, suggesting that DNA replication in this haloarchaeon may be more eukaryotic than bacterial (17).
In past studies, only a single autonomously replicating sequence (ARS) was isolated for Halobacterium strain NRC-1, located within the common region of the large extrachromosomal pNRC100 and pNRC200 replicons. Extensive analysis of these replicons, which exist as inversion isomers, had also shown the presence of a B family DNA polymerase, TBP, and TFB transcription factor genes, among other important and likely essential genes, suggesting minichromosome status in Halobacterium strain NRC-1 (7, 29). Sequence analysis of the minimal replication origin (28) showed the requirement for a unique gene, repH, and an AT-rich region 5' to the gene. Elimination of either the AT-rich sequence or the repH gene was found to abolish the autonomous replication ability of plasmids.
In the present study, we have attempted to identify the Halobacterium strain NRC-1 chromosomal replication origin(s) functionally by assessing its capability to confer autonomous replication ability on nonreplicating plasmids. We have found evidence for only a single replicating sequence, located near one of the orc1-cdc6 genes (orc7) on the chromosome. We further show that both the orc7 gene and an upstream inverted repeat sequence flanking an AT-rich region are required for autonomous replication and that this region is conserved in two other distantly related haloarchaea.

MATERIALS AND METHODS
Materials.
Restriction enzymes, calf intestinal phosphatase, Vent DNA polymerase,
and T4 DNA ligase were purchased from New England Biolabs, Beverly,
Mass. The XL-PCR kit was purchased from Applied Biosystems,
Branchburg, N.J. The digoxigenin nucleic acid labeling and detection
kit was purchased from Roche Applied Science, Indianapolis,
Ind. Oligonucleotides were purchased from Sigma-Genosys, The
Woodlands, Tex. Gel extraction kits and plasmid purification
kits were purchased from Qiagen, Valencia, Calif. Mevinolin
was a gift from Merck, Rahway, N.J.
Strains and culturing.
Escherichia coli DH5
was grown in Luria-Bertani medium supplemented with 100 µg of ampicillin/ml at 37°C. Halobacterium strain NRC-1 was cultured in CM+ medium containing 4.5 M NaCl and trace metals, as well as 20 µg of mevinolin/ml where applicable, as previously described (6).
Plasmid construction.
PCR amplification under standard conditions was performed on Halobacterium strain NRC-1 genomic DNA, which was prepared as previously described (6). PCR primers used for plasmid construction were as follows: ORC1/CDC6_6.1, 5'-CCGGAATTCAATCGCTGACGGCGGCCAGG-3'; ORC6 + 750.FOR, 5'-CCGGAATTCATCGAAGGCGGGCGCAATCC-3'; ORC6 + 500.FOR, 5'-CCGGAATTCTTCGAGGCGACGCTGCGGGA-3'; ORC6 + 250.FOR, 5'-CCGGAATTCTCGACGGCATCCACGCGGCG-3'; ORC6GENE-50.REV, 5'-CCGGAATTCCACGCCACCACCTAAAAAGC-3'; ORC6-100.REV, 5'-CCGGAATTCCGTCTGCAGCTGTGACTCCC-3'; ORC1/CDC6_6.2, 5'-CCGGAATTCCATGGGAAGCCTTATAAGCGG-3'; ORC1/CDC6_7.1, 5'-CGCGGATCCTCTCGTGGGGAATGTGGCTC-3'; ORC7 + 750.FOR, 5'-CGCGGATCCTATAAAACCCCAGTGAGAGG-3'; ORC7 + 500.FOR, 5'-CGCGGATCCTAGAACTAGACAACTACCGT-3'; ORC7 + 250.FOR, 5'-CGCGGATCCCATCCCTCCCCCCTCTAACC-3'; ORC7GENE-50.REV, 5'-CGCGGATCCCTCCTCGACCGGAACCGACA-3'; ORC7-100.REV, 5'-CGCGGATCCGCTGAGCAGGTCATCGAAGA-3'; ORC1/CDC6_7.2, 5'-CGCGGATCCAACCCCGGCGTATAACTCGT-3'; ORC1/CDC6_8.1, 5'-CCGGAATTCGTAATCGAGGAAGTCGGCGT-3'; ORC8 + 750.FOR, 5'-CCGGAATTCTCGCTGCCGTGCTCGCCGTC-3'; ORC8 + 500.FOR, 5'-CCGGAATTCCACGTCGTGTTGGCGGTGGT-3'; ORC8 + 250.FOR, 5'-CCGGAATTCGGCTCTCCCACCCACCCCGT-3'; ORC8GENE-50.REV, 5'-CCGGAATTCGGCGTCCGCGATGGCCTCCT-3'; ORC8-100.REV, 5'-CCGGAATTCAGGGCGTTGGCGTACTGGTC-3'; and ORC1/CDC6_8.2, 5'-CCGGAATTCACCGCGTCGTTCAAGCCACG-3'. The PCR products were then gel purified and digested with either EcoRI or BamHI. These products were then cloned into either the EcoRI or the BamHI site of pNGMEV101 (28). Plasmids were transformed into E. coli DH5
by electroporation and recovered by alkaline lysis, as described previously (33). A description of all plasmid constructs is found in Table 1.
Transformation of Halobacterium strain NRC-1 and autonomous plasmid replication assay.
DNA-mediated transformation of
Halobacterium strain NRC-1 was
performed by the EDTA-polyethylene glycol procedure, as described
previously (
6). Mevinolin-resistant (Mev
r) transformants were
selected by plating on CM
+ solid medium containing 20 µg
of mevinolin/ml. Transformation cultures were also spotted onto
CM
+ solid medium containing 20 µg of mevinolin/ml. Plasmid
DNA was prepared by an alkaline sodium dodecyl sulfate procedure,
as described previously (
6). Plasmid DNA was prepared from at
least three separate Mev
r colonies. This DNA was fractionated
by electrophoresis on 0.5% agarose, denatured, transferred to
a nylon membrane (Roche), and probed according to the manufacturer's
instructions (Roche) with a digoxigenin-labeled PCR product
of the
bla gene as a plasmid-specific probe.
DNA sequence analysis.
Sequence data for Haloarcula marismortui were obtained from the H. marismortui genome web page at http://zdna2.umbi.umd.edu/~haloweb/hma.html. Sequence data for Haloferax volcanii were downloaded from http://zdna2.umbi.umd.edu/~haloweb/hvo.html. To identify the conserved inverted repeat in H. marismortui and H. volcanii, BLAST analysis was performed on an SGI O2 workstation with GCG computer software (Genetics Computer Group Inc.). Alignment of the conserved ARSs was done using CLUSTAL_X 1.81. Analysis of GC percentages in a sliding window was performed using the EMBOSS program DAN. Phylogenetic analysis of archaeal Orc1-Cdc6 proteins was performed using CLUSTAL_X for multiple sequence alignment and Treeview for neighbor joining tree construction (36).

RESULTS
Cloning and analysis of a chromosomal ARS element.
To identify ARS elements from the large chromosome of
Halobacterium strain NRC-1, a directed approach was used based on previous
studies implying a physical association between archaeal replication
origins and the
orc1-cdc6 gene (
22,
27) and GC skew data obtained
for the large chromosome (
17). Selected regions of the genome
proximal to the three chromosomal
orc1-cdc6 genes (
orc6,
orc7,
and
orc8 [Fig.
1]) were cloned into an
E. coli plasmid vector
which was not able to replicate in haloarchaea and assayed for
endowment with autonomous replication ability. The plasmids
were constructed to initially contain both 1 kb 5' to the respective
orc gene start and 1 kb 3' to the
orc gene stop (pBBori
n series,
with
n being 6, 7, and 8 for
orc6,
orc7, and
orc8, respectively).
Plasmid derivatives were constructed which deleted the entire
downstream 3' region 50 bp beyond the
orc gene translational
stop codon and deleted either 0, 250, 500, or 750 bp from 1
kb 5' toward the
orc gene translational start codon (pBB
nG1000,
-750, -500, or -250). Finally, constructs were made containing
the 750, 500, or 250 bp 5' to the
orc gene, but with the deletion
of the respective
orc open reading frame (pBB
n750, -500, or
-250).
The three plasmid deletion series were used to transform a
Halobacterium strain NRC-1 culture, and experiments were repeated to confirm
transformation efficiencies. Transformation efficiencies are
shown in Table
2, expressed as CFU per microgram of plasmid
DNA. Several plasmids containing the
orc7 gene, pBBori7, pBB7G1000,
and pBB7G750, showed high transformation efficiencies (>10
4 CFU/µg of transforming DNA), while those lacking more
than 500 bp of the upstream region, pBB7G500 and pBB7G250, and
those lacking the
orc7 gene, pBB7750, pBB7500, and pBB7250,
as well as all the others derived from the
orc6 and
orc8 gene
regions, had transformation efficiencies 2 orders of magnitude
lower, similar to background level. These results are consistent
with autonomous replication of plasmids containing the
orc7 gene plus either 1,000 or 750 bp of 5'-flanking sequence and
loss of replication ability when containing only 500 or 250
bp of 5'-flanking sequence or when the
orc7 gene was deleted.
These results show that the
orc7 gene plus sequence elements
between 500 and 750 bp upstream are required for autonomous
replication.
For a qualitative demonstration of plasmid autonomous replication
ability, nonselected cultures containing transformants were
spotted in 50-µl aliquots on selective CM
+ agar plates
containing mevinolin (Fig.
2). Patches of growth on plates provided
confirmation that cultures containing plasmids with the
orc7 gene plus 750 bp or more 5' to the gene transformed the host
with high efficiency. In contrast, only background colonies
were evident when only 500 or 250 bp upstream of the
orc7 gene
was included. These background colonies are also seen for the
other two
orc gene constructs. The small amount of background
growth could be attributed to two events: (i) spontaneous mutation
to mevinolin resistance, by either increased gene expression
or gene copy number of 3-hydroxy-3-methylglutaryl coenzyme A
reductase (
18), or (ii) acquisition of mevinolin resistance
by plasmid integration.
To discriminate between plasmid integration and autonomous replication,
total DNA was extracted from transformants for all of the plasmids.
This DNA was then used in Southern blot analysis with a
bla gene-specific probe for plasmid DNA (Fig.
3, lanes 1 to 5).
Plasmid bands consistent with replicative supercoiled and nicked
forms were observed in the blot for plasmid DNA for pBBori7,
pBB7G1000, and pBB7G750, but not for pBB7G500 or pBB7G250, or
other plasmids, where hybridization is to high-molecular-weight
DNA, consistent with plasmid integration (Fig.
3). For comparison,
the replicative supercoiled and nicked plasmid forms for pBBori7,
pBB7G1000, pBB7G750, pBB7G500, and pBB7G250 purified from
E. coli were visualized with ethidium bromide (Fig.
3, lanes 6
to 10). This confirms that the bands seen in lanes 1 through
3 are the replicative plasmid forms of pBBori7, pBB7G1000, and
pBB7G750. Faint bands seen at lower-molecular-weight positions
in lanes 4 and 5, for pBB7G500 and pBB7G250, are very likely
the result of sequential plasmid integration and excision events,
occurring due to large regions of homology (>1 kb) between
the plasmids. This has been previously reported for other plasmids
(
28,
32). Little or no integration is observed for plasmids
without extended regions of homology, e.g., pNGMEV101 (Table
2 and Fig.
2) (
28). These results are consistent with the presence
of an ARS element in pBBori7, pBB7G1000, and pBB7G750, where
no evidence for integration could be observed. For
orc6 and
orc8 plasmid constructs, a majority of hybridization for Mev
r transformants is seen to be associated with chromosomal DNA,
consistent with plasmid integration (data not shown). This analysis
clearly shows that the
orc7 gene region, including 750 bp of
upstream DNA, is the only one for which autonomous replication
can be demonstrated.
Analysis of the ARS element DNA sequence.
Based on the experimental replication evidence for
orc7 constructs,
a closer examination of the DNA sequence located upstream of
the
orc7 gene was undertaken. The GC percentage of the 1 kb
5' of the
orc7 gene was calculated and plotted with a sliding
window of 70 bp with 50-bp steps (Fig.
4). Immediately striking,
from this analysis, was a stretch of extreme AT richness located

300 to 500 bp from the
orc7 translational start. The GC content
of this 189-bp region is only 56%, corresponding to a substantially
higher AT content than the chromosomal average GC content of
68%. Also striking was the finding of a 31-bp nearly perfect
(with one mismatch) inverted repeat flanking the AT-rich stretch.
Significantly, autonomous replication ability is abolished when
the upstream half of the inverted repeat is deleted in pBB7G500
(see above; Table
2 and Fig.
2).
Conservation of the ARS element in other distantly related halophiles.
The availability of partial genome sequences for
H. marismortui and
H. volcanii allowed for comparative analysis to be performed
with other distantly related halophilic archaea. The 1 kb upstream
plus the
orc7 gene from
Halobacterium strain NRC-1 was used
as an initial query to identify a contig containing the
orc7 homolog and its upstream sequence in both
H. marismortui and
H. volcanii. Once the contigs were located, the 31-bp inverted
repeat sequence from
Halobacterium strain NRC-1 was used to
search for any sequence similarity in comparable regions in
H. marismortui and
H. volcanii. A nearly identical inverted
repeat was identified upstream of the
orc7 homologs in both
organisms (Fig.
5). The inverted repeat in
H. marismortui is
28 bp in length, containing two mismatches in sequence, and
is separated by 249 bp. The GC content of the sequence between
the inverted repeat is 48% compared to an average chromosomal
GC content of 61% in
H. marismortui. In
H. volcanii, the inverted
repeat is a perfect 28 bp in length, with a 2-bp insertion in
the second half. The GC content of the sequence between the
inverted repeat is 50% compared to a genomic average GC content
of 65%. This analysis indicates that a putative chromosomal
origin, containing a

30-bp inverted repeat flanking a

200-bp
AT-rich region, is conserved in halophilic archaea.
Phylogenetic analysis of archaeal chromosomally encoded Orc1-Cdc6 proteins.
The partial genomic sequences of
H. marismortui and
H. volcanii were examined to determine whether they contained a plurality
of
orc1-cdc6 genes, similar to that found in the completed genome
of
Halobacterium strain NRC-1. These two other haloarchaea were
found to contain a greater number of distinct
orc1-cdc6 genes
than even
Halobacterium strain NRC-1, 15 each in
H. marismortui and
H. volcanii. By using the three NRC-1 chromosomal Orc1-Cdc6
proteins as queries, the most similar Orc6, Orc7, and Orc8 homologs
were identified in the two other halophile sequences. To examine
the relationships between chromosomally encoded archaeal Orc1-Cdc6
proteins, an alignment was made of these Orc1-Cdc6 proteins
and a neighbor joining tree was constructed (Fig.
6). The tree
was rooted using
Saccharomyces cerevisiae Orc1p (
1) and Cdc6p
(
19) along with the
Schizosaccharomyces pombe homologs Orp1p
(
26) and Cdc18p (
16), respectively. The neighbor joining tree
displays three classes of Orc1-Cdc6, corresponding to the three
Orc1-Cdc6 proteins encoded on the
Halobacterium strain NRC-1
chromosome: Orc6, Orc7, and Orc8. Other archaeal organisms have
Orc1-Cdc6 homologs located within either one or both of the
clades that contain the haloarchaeal Orc6 and Orc7 homologs.
Interestingly, only haloarchaea contain homologs in the Orc8
clade.

DISCUSSION
Previously, our laboratory reported the cloning of a putative
replication origin from a library of the pNRC100 and pNRC200
minichromosomes of
Halobacterium sp. strain NRC-1 by its property
of conferring autonomous replication ability on nonreplicating
plasmids (
28). Now, we have cloned a putative replication origin
of the third replicon, the large chromosome from strain NRC-1,
also by virtue of its autonomous replication ability. Whereas
the minichromosomal ARS contained the
repH gene, similar to
other haloarchaeal extrachromosomal replicons, the large chromosomal
ARS contains the
orc7 gene, a relative of the eukaryotic ORC
initiator gene family (
1,
12,
13,
35). As a result of our genetic
approach, we now have in hand a haloarchaeal system with well-defined
ARS elements from each replicon.
Bioinformatic analysis of the Halobacterium strain NRC-1 genome by GC skew had suggested multiple replication origins of the large chromosome, coincident with two of the three chromosomal orc1-cdc6 genes (17). Subsequent analysis by the Z-curve method confirmed this result (39). Therefore, we cloned segments of DNA surrounding the chromosomal orc1-cdc6 genes into a plasmid which does not replicate in this haloarchaeon and tested for autonomous replication ability. Our results showed that a chromosomal region around the orc7 gene, including an upstream inverted repeat flanking an AT-rich region plus the gene itself, is sufficient to endow plasmids with replication ability. Interestingly, however, the regions surrounding two other chromosomal orc1-cdc6 genes, orc6 and orc8, were not capable of autonomous replication. These results suggest that the Halobacterium sp. strain NRC-1 large chromosome may have a single replication origin associated with orc7, similar to other archaea and bacteria (21, 22, 23, 27). However, the possibility exists that other functional chromosomal replication origins may not confer the autonomous replication ability on plasmids or may not be associated with orc1-cdc6 genes, and therefore, we cannot rule out the use of more than a single replication origin in vivo based on our present studies.
We genetically analyzed the orc7 gene region by deletion analysis. While the downstream region was dispensable for autonomous replication, the upstream region and the gene itself were found to be essential. The upstream region contained a 31-bp inverted repeat flanking a 189-bp AT-rich region. When a 500-bp region including one copy of the inverted repeat was deleted, replication ability was lost, showing the importance of this region for function. Moreover, similar inverted repeat-AT-rich structures were found to be highly conserved upstream of orc7 homologs in two other distantly related halophiles, H. marismortui and H. volcanii, consistent with a function in replication initiation for this sequence in haloarchaea. With the conservation of a large inverted repeat flanking an AT-rich region, it is tempting to speculate that these repeats serve as landing pads for archaeal Orc1-Cdc6 and other DNA replication initiation and possibly elongation proteins, with the AT-rich region acting as an initial DNA-unwinding element. All together, our results strongly support the idea that the orc7 gene and upstream region function in chromosomal replication initiation in haloarchaea.
Although DNA replication origins have been well defined for bacteria and simple eukaryotes, they have remained relatively unstudied in the archaeal domain. In general, bacterial origins of replication contain multiple DnaA boxes and an AT-rich region proximal to the dnaA gene itself. The E. coli oriC contains five such DnaA boxes and an AT-rich region over 260 bp, while the Streptomyces oriC contains 19 DnaA boxes and five short AT-rich stretches over 600 bp (25). Among eukaryotic organisms, S. cerevisiae and S. pombe are the best studied. S. cerevisiae origins are
100 bp in size and contain a conserved and essential AT-rich ARS consensus sequence, along with other essential B elements, which are less well conserved (2, 15). In S. pombe replication origins are much larger,
1,000 bp, with only short (20- to 50-bp) AT-rich stretches of variable sequence being essential for origin function (2, 5). The haloarchaeal orc7-associated replication origin appears to be quite distinct from these examples.
Among archaea, in vivo identification of an early replicating chromosomal segment of Pyrococcus abyssi indicated that this organism initiates bidirectional DNA replication from a single region, located 5' to an orc1-cdc6 gene (27). Our phylogenetic analysis indicates that the Pyrococcus gene is most closely related to the orc7 gene family. This origin region is conserved in three Pyrococcus species and contains a number of small repeats, which are also present in the genome of Methanothermobacter thermoautotrophicus (formerly Methanobacterium thermoautotrophicum) (20, 22). Recently, Pyrococcus species have also been reported to contain a large inverted repeat flanking an AT-rich region upstream of their orc7 homologs (23). However, to date, there is no report of autonomous replication of these regions or genetic analysis (3). Based on our present knowledge, it appears that a large inverted repeat and an AT-rich region are general features of archaeal replication origins and that origins in archaea are conserved in structure but not always in sequence.
In Halobacterium strain NRC-1, 10 orc1-cdc6 genes are carried within the genome, including four located on the large (2-Mb) chromosome (one is interrupted by an insertion sequence element), five on the pNRC200 replicon, and one on the pNRC100 replicon. This is in stark contrast to most other archaea, which typically carry one or two orc1-cdc6 homologs, with the exception of Sulfolobus solfataricus, which carries three (34). In systems with a few Orc1-Cdc6 homologs, these have been proposed to act as origin recognition factors, initially binding to origin DNA sequences and serving to locally unwind the DNA and nucleate formation of a replisome, akin to DnaA in bacteria and the six-membered ORC complex in eukaryotes (13). For those containing two, it would seem plausible that one might act to bind origin sequences, i.e., ORC-DnaA function, and the other might act as Cdc6 does in eukaryotes and DnaC in bacteria, namely, recruiting the replicative helicase to the origin.
For halophilic archaea, the extremely large size of the orc1-cdc6 family has been maintained throughout evolution. In addition to Halobacterium strain NRC-1, the two other halophiles examined here, H. marismortui and H. volcanii, carry at least 15 distinct orc1-cdc6 homologs each (Zhang et al., unpublished). Our phylogenetic analysis shows the existence of several classes of Orc1-Cdc6 proteins from archaeal organisms (Fig. 6). In particular two of these classes contain representatives from nonhalophilic and halophilic archaea (Orc6 and Orc7 clades). It is likely that the Orc7 clade represents the origin binding proteins in archaeal organisms, based on the requirement of this gene for autonomous replication and its association with the origin of replication in Pyrococcus sp. (22, 23, 27). The Orc6 clade may possibly represent replicative helicase-recruiting proteins for organisms which possess both, based on its homology to Cdc6, the eukaryotic replicative helicase loader, and conservation in most sequenced archaeal organisms to date. For organisms containing a single Orc1-Cdc6 protein, this protein may act for both functions. Alternatively, other yet unknown proteins may act in the process of replication initiation.
For haloarchaea, the other Orc1-Cdc6 homologs may also aid in the replication initiation process, perhaps forming multisubunit complexes akin to the six-membered eukaryotic ORC complex or recruiting the replicative helicase and other replication-associated proteins. Alternatively, the other Orc1-Cdc6 homologs may play physiological roles different from replication initiation. An expansion of orc1-cdc6 genes has occurred and is being maintained in halophilic lineages. It is possible that this may be an adaptation to living in saturating salt and containing a cytoplasm with an equally high salt concentration. This may be related to the speed or processivity of DNA polymerase or unknown activities required for life in saturating salt.
The results presented here provide a significant advance in our understanding of genetic elements essential for initiation of chromosomal DNA replication in the archaeal domain of life. We provide the first report of cloning of an ARS element from an archaeal chromosome and display genetically the DNA regions necessary to provide autonomous replication ability. We also show the sequence and structure conservation of this chromosomal origin in two other distantly related halophilic archaea. Halobacterium strain NRC-1 provides an excellent model system to study the characteristics of archaeal replication origins, and the results presented here provide the groundwork for further studies of essential elements for archaeal DNA replication initiation.

ACKNOWLEDGMENTS
This work was supported by National Science Foundation grants
MCB-0296017, -0135595, and -0196502.

FOOTNOTES
* Corresponding author. Mailing address: Center of Marine Biotechnology, University of Maryland Biotechnology Institute, 701 E. Pratt St., Baltimore, MD 21202. Phone: (410) 234-8847. Fax: (410) 234-8896. E-mail:
dassarma{at}umbi.umd.edu.


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Journal of Bacteriology, October 2003, p. 5959-5966, Vol. 185, No. 20
0021-9193/03/$08.00+0 DOI: 10.1128/JB.185.20.5959-5966.2003
Copyright © 2003, American Society for Microbiology. All Rights Reserved.
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