Molecular Ecology (2003) 12, 859–868 Nuclear gene sequences and DNA variation of Cryptomeria japonica samples from the postglacial period Blackwell Publishing Ltd. N A O K I T A N I ,* Y O S H I H I K O T S U M U R A * and H I T O S H I S A T O † *Department of Forest Genetics, Forestry and Forest Products Research Institute, Matsunosato, Tsukuba, Ibaraki 305–8687 Japan, †Landscape and Natural Reservation Section, Environment and Life Division, Shimane Prefecture, Matsue, Shimane 690–8501 Japan Abstract Genomic DNA was extracted from heartwood blocks of six Cryptomeria japonica individuals that had been buried (in an area now covered by rice fields) for about 3600 years. Attempts were made to determine the sequences of five nuclear genes following polymerase chain reaction amplification, using previously obtained C. japonica expressed sequence tag (EST) information. We detected 15 nucleotide substitutions and four insertion/deletions (indels) in a partial GapC gene sequence among 13 individuals of the buried and an extant population, which allowed us to estimate the extent of DNA variation within the buried populations, and the level of genetic differentiation between the buried population and the extant population growing in a neighbouring area. For the entire haplotypes of the GapC region, π and θ nucleotide diversity estimates were 0.0063 and 0.0010, respectively, when both populations were included, while corresponding figures for the buried population alone were 0.0009 and 0.0017. Estimates of DNA divergence statistics (dXY = 0.0062, dA = 0.0005, FST = 0.0832 and KST = 0.0935) suggest that differentiation between the two populations was not great. However, permutation tests gave FST and KST values rejecting the null hypothesis (that populations were not differentiated) at the 5% and 1% probability levels, respectively. The significant genetic differentiation between the two populations was mainly caused by differences in haplotype diversity. The significant level of haplotype diversity in the extant population compared to the buried population might be the result of gene flow from neighbouring artificial forests. Alternatively, it is possible that we failed to detect all the DNA variation in the buried population because of clonal growth in the buried population. Keywords: ancient DNA, buried forest, Cryptomeria japonica, DNA variation, GapC, PCR Received 15 August 2002; revision received 10 December 2002; accepted 10 December 2002 Introduction The most common use of ancient DNA has been directed at the systematics of extinct species (reviewed in Wayne et al. 1999). For example, cytochrome b sequences demonstrated that the extinct Tasmanian wolf was closely related to other Australian marsupials (Thomas et al. 1989). Krings et al. (1997) demonstrated that Neanderthals were phylogenetically divergent from recent humans. In contrast, little interest has been shown in less ancient DNA, isolated from fossils of extant species, for studies of systematics, although it has been used to distinguish species or to help probe their geographical origins. For Correspondence: Yoshihiko Tsumura. Fax: 81–29–8743720; E-mail: [email protected] © 2003 Blackwell Publishing Ltd instance, spacer regions and genes on the chloroplast genome have been used in two studies (Suyama et al. 1996; Poinar et al. 2001) for identifying species, because we can seek which chloroplast sequences on public databases are identical with the fossil chloroplast sequences. These sequences are the most useful for identifying species following successful polymerase chain reaction (PCR) amplification from fossil sources. Thus, sequencing chloroplast DNA offers enormous research possibilities in the fields of molecular evolution and systematics. However, it is not useful for population genetic analysis related to aspects such as genetic differentiation between extant and extinct populations, or for probing the genetic structures of several hierarchic levels of extinct populations because of the low nucleotide substitution rate of chloroplast DNA (Curtis & Clegg 1984; Palmer 1985). For these purposes, 860 N . T A N I , Y . T S U M U R A and H . S A T O the amplification and subsequent sequencing of genes on the nuclear genome would be more desirable, because nucleotide and haplotype diversities of each gene between individuals and/or populations could then be obtained, allowing efficient evaluation of genetic diversity in terms of population genetics and molecular evolution. Natural populations of Cryptomeria japonica D. Don. are discontinuously distributed from the northern part of Honshu (the main Japanese island) to Yaku Island, which is located 100 km off the coast of southern Kyushu (Hayashi 1960). Although C. japonica covers a vertical range from 0 to 1850 m above sea level, dense natural forests of C. japonica are restricted to a montane zone. However, the cool period following the hypsithermal climatic interval (2000–5000 years ago) allowed the habitat of C. japonica to be extended to alluvial plains, as evidenced by a buried forest found under rice fields at the foothill of Sanbe volcano, Shimane prefecture in November 1998. The cause of the burial was a pyroclastic flow (about 3600 years ago) that dammed the Azukihara River, leading to the forest being rapidly covered by water, earth and sand. The wood of the trees has been well preserved to the present day. Hence, it is possible to investigate the genetic structure of the buried population and assess genetic differentiation between the buried and extant populations. Here, we describe the successful isolation of ancient DNA from wood tissues of the buried trees, PCR amplification and sequencing of nuclear genes. We also studied the differentiation between the buried and extant populations, and considered the genetic structure within the buried population. This is the first report of successful sequencing analysis of nuclear genic regions of fossil trees. Materials and methods Plant materials and molecular methods The buried forest at Sanbe–Azukihara was discovered in 1998 (Figs 1, 2). Some trees buried under rice fields have been exhumed for investigation and an exhibition has been mounted at Sanbe Natural History Museum by Shimane prefecture, Japan. In our study, blocks of these trees were taken, and immediately stored at −30 °C, until genomic DNA was isolated using a DNeasy plant mini-kit (Qiagen GmbH) from 400 mg of each individual wood chip (Dumolin-Lapègue et al. 1999). The DNA samples were then diluted 1 : 20 with water. In addition, needles were sampled from an extant population located on the hillside of Sanbe Volcano, at a considerably higher altitude (≈ 600– 800 m) than the level of the excavation (≈ 250 m; Fig. 1), because no natural Cryptomeria forests currently occur at lower elevations. Needles were collected individually, with more than 30 m between sampled trees to avoid erroneous sampling of half-sib and/or identical ramet individuals. Genomic DNA of these samples was also isolated from 5 g portions of fresh leaf tissues using the modified CTAB method of Murray & Thompson (1980). For preliminary screening, we tried to amplify 17 nuclear genes that give PCR product sizes of less than 600 base pairs (bp), because the DNA isolated from buried wood tissues tends to be degraded. The primer pairs for these 17 nuclear genes yielded a single band when genomic DNA extracted from extant samples were used as template samples for PCR. The sequences of the primers were derived from expressed sequence tag (EST) information generated by the Sugi genome project (Iwata et al. 2001) or supplied by Professor Tachida, Kyushu University, Japan (Table 1). Attempts were made to amplify these genes from nine DNA samples of buried trees and eight DNA samples of natural trees from a sympatric region under the following PCR conditions: initial denaturing at 94 °C for 5 min, followed by 40 cycles of 94 °C for 1 min, 55 °C to 60 °C (depending on primer pair) for 1 min and 72 °C for 1 min 30 s, with a final extension step of 72 °C for 5 min. All reactions were performed in a Perkin Elmer thermal cycler with a Mg2+ concentration of 1.5 mm. Subsequently, PCR products that were confirmed as single bands in 2.0% agarose gel electrophoresis were cleaned up using a QIAquick PCR Purification kit (QIAGEN GmbH) to remove primers and residual dNTPs. Purified PCR products were sequenced using a Big dye deoxy-terminator cycle sequence kit (Perkin Elmer), following the manufacturer’s recommendations, and the corresponding primer for each gene on an Applied Biosystems Model 377 automated sequencer (Applied Biosystems). When heterozygotes were detected, PCR products were cloned into the pCRTOPO vector using TOPO™ TA Cloning® Kits (Invitrogen). Plasmids from single colonies were prepared as templates for cycle sequencing using Quantum prep plasmid purification kits (Bio-Rad Laboratories Inc.), and eight plasmids per heterozygote were independently sequenced with the M13 reverse primer, following the manufacturer’s method for the Big dye deoxy-terminator cycle sequence kit (Perkin Elmer). Sequences were analysed on an ABI 377 sequencer. Newly determined sequences were deposited in the EMBL data bank under nos AJ517805–AJ517812. Sequence analysis Sequences used in this study were aligned by clustal w version 1.6 computer software (Thompson et al. 1994), followed by manual adjustment to reduce further the number of insertions and deletions. The polymorphism data were analysed by dnasp version 3.50 computer software (Rozas & Rozas 1999). To assess genetic variation within the populations we estimated the following genetic diversity statistics: haplotype (gene) diversity using the methods of Nei (1973) and Nei & Chesser (1983), the © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859 –868 D N A V A R I A T I O N O F A N C I E N T C R Y P T O M E R I A J A P O N I C A 861 Fig. 1 Contour map showing the location of Sanbe buried forest and the sampling area of the natural extant population of Cryptomeria japonica. Fig. 2 Locations of buried trees at the excavation site of Sanbe buried forest. Solid circles indicate buried trees from which genomic DNA was isolated and successfully sequenced. Shaded circles indicate buried trees from which it was impossible to isolate genomic DNA. Open circles indicate buried trees that have not been investigated. © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859–868 Polymophism © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859 –868 Index of EST marker* Putative function Primer CC0254 Thaumatin-like protein precursor CC0256 No match on database CC0257 Ephrin type-B receptor 6 precursor CC0288 (R)-mandelonitrile lyase isoform 1 precursor CC0349 Harpin induced gene 1 homologue CC0392 Eukaryotic translation initiation factor 3 p42 subunit CC0411 Homeobox protein BIX3 CC0420 Ribose 5 phosphate isomerase CC0498 Peptidyl-prolyl cis-trans isomerase CC1333 GTP-binding protein CC1348 Peptidylprolyl isomerase CC1439 Nine-cis-epoxycarotenoid dioxygenase CC1522 Alpha-glucosidase precursor CC1606 R2R3-MYB transcription factor CD1514† Chalconsintase CD1706† Fedoroxine CC2241† Glyceraldehyde-3-phosphate dehydrogenase 5′-GGCCACAACGTTCTGCTAAAT-3′ 5′-GGCGGGCGTAACCATC-3′ 5′-GGCATGCCCTTCTTCAAT-3′ 5′-ATGACCGGATAAAGCCAAAT-3′ 5′-GCCCTCGACGATGTGTGGAC-3′ 5′-CACGAAACCTTCCGCCAGTG-3′ 5′-TTTGTGATTTCATGCCTGCTA-3′ 5′-GAAATCCAAGCTTGCCCTAC-3′ 5′-GCGGATGCCTGATGTTCTTGA-3′ 5′-CAGGACGCCGGTCTGTTGAT-3′ 5′-CGCGATAAACCTAAGCTACAA-3′ 5′-AATGGACCAGAAGACAGGAG-3′ 5′-GATGAGCCGAGTATTGGTTAT-3′ 5′-GATTTCATCGCCTTGGTT-3′ 5′-TGGCGGCAGCAGCATTTA-3′ 5′-GCCAGGTCAATCTTCGGATGA-3′ 5′-GGCCGAATCGTGATGGA-3′ 5′-GGGCAACTTAGAAGGGCATTA-3′ 5′-CTCCTAGATCAGCGTATCACA-3′ 5′-CCCTTTCTTGACCAGCAG-3′ 5′-GCCGAATCGTGATGGA-3′ 5′-GCAACTTAGAAGAGGGCAACT-3′ 5′-GCATGGGAGTGGCGAATG-3′ 5′-AGCTGAGCTTCACCGCAGAAT-3′ 5′-GGACTCTGTAGCCAAATCAG-3′ 5′-AAGTTAATGTCTTGCCGAATA-3′ 5′-TAACCAGCTTTGCCCTCAG-3′ 5′-ATACAATTCGCGGCTACCATA-3′ 5′-GGTCGGTCTGACATTCCATT-3′ 5′-CGAGAAGCGTCCAAACATTA-3′ 5′-ATAGGCGACGCAGGTCAAAA 5′-TCTGCGGCTGTAGTTCCAGT-3′ 5′-CAGATTTCATTGGAGACAGC-3′ 5′-CAAATCTATGACTCGTGAAC-3′ *For details of primers with CC and CD initials see Iwata et al. (2001). †Primer pair supplied by Dr Tachida, Kyushu University. ‡Estimated product size was deduced by 2.0% agarose gel electrophoresis. Expected product size‡ Amplification Sequencing Buried population Extant population 250 bp Amplified Success Monomorphic 1 polymorphic site 380 bp Amplified Success Monomorphic 1 polymorphic site 420 bp Multiple — — 450 bp Impossible — — 320 bp Impossible — — 450 bp Multiple — — 500 bp Multiple — — 400 bp Amplified Success Monomorphic 600 bp Impossible — — 600 bp Amplified Success Monomorphic 600 bp Multiple — — 1300 bp Multiple — — 900 bp Impossible — — 900 bp Impossible — — 500 bp Impossible — — 400 bp Impossible — — 400 bp Amplified Success Polymorphic 1 polymorphic site 1 polymorphic site 15 polymorphic sites 862 N . T A N I , Y . T S U M U R A and H . S A T O Table 1 Screened EST markers and results of PCR amplification and subsequent sequencing D N A V A R I A T I O N O F A N C I E N T C R Y P T O M E R I A J A P O N I C A 863 Fig. 3 A 0.8% agarose gel following genomic DNA electrophoresis and ethidium bromide staining. No DNA molecules were detected in lanes 1–3, while fragmented DNA molecules were visible in lanes 4 and 5. number of pairwise differences between sequences (per base estimates of nucleotide diversity, π; Nei & Li 1979; Tajima & Nei 1984) and scaled neutral mutation rate (θ = 4Neµ; Watterson 1975; Nei 1987; Tajima 1993). The extent of DNA divergence between the buried and extant populations was estimated as the average number of nucleotide substitutions per site between populations (dXY), and the number of net nucleotide substitutions between the two populations (dA; Nei 1987). When statistics of nucleotide diversity were estimated, insertions and deletions were ignored. To test for population differentiation between the two populations, we used permutations described by Hudson et al. (1992a). FST (Hudson et al. 1992b) and KST (Hudson et al. 1992a) statistics are based on the frequencies of individual segregation sites in two populations. For each test, 10 000 permutations of the data were carried out, and proseq version 2.9 software was used (Filatov 2001). To visualize relationships among haplotypes of both buried and extant trees, a minimum spanning network was constructed using tcs version 1.13 (Clement et al. 2000). All indels were ignored when the network was constructed. Results Isolation, PCR amplification and sequencing of DNA from buried wood Although 0.8% agarose gel electrophoresis showed the isolated genomic DNAs to be severely degraded (Fig. 3), fragmented DNA molecules could be recovered from six out of nine excavated trees, designated nos. A-2, A-3, A-4, A-5, A-9 and A-10, from the buried population. It was impossible to isolate genomic DNA from the remaining three excavated trees (A-1, A-7, A-19; Fig. 2). Single bands in subsequent 2.0% agarose gel electrophoresis were generated by each of five pairs of primers (CC0254, © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859–868 CC0256, CC0420, CC1333 and GapC exon 4 to exon 6), and multiple bands by another five (CC0257, CC0392, CC0411, CC1348 and CC1439) out of 17 pairs tested (Table 1). The other seven did not amplify any detectable fragments (Table 1). Each PCR product from the five pairs of primers that gave single bands was subsequently sequenced, but no nucleotide substitutions among samples from the six individuals in the buried forest were detected in four of the five genes. We observed only one nucleotide substitution (CC0254 and CC1333) or indel (CC0256 and CC0420) between individuals within the extant population with four of the five genes. One of the haplotypes detected in each gene was identical with the sequence of each gene of the buried population. Another haplotype is newly detected with low frequency. On the other hand, DNA polymorphisms were detected in the 391-bp GapC gene sequence among the buried tree haplotypes. Gene diversity and DNA variation within buried and extant populations The 391-bp fragment comprises two introns and one exon, defined by comparison with the glyceraldehyde-phosphate dehydrogenase mRNA sequence of Taxus baccata (GenBank Acc. No. L26922; Jansson et al. 1994) and the GapC2 gene sequence of Zea mays (GenBank Acc. No. X73151). We found only two synonymous substitutions in exon 5, which is 80 bp long (Fig. 4). Because we detected sufficient polymorphisms concerning only GapC gene sequence, we only measured gene diversity and DNA variation statistics in this gene. In the exon 4 to exon 6 region of the GapC gene we found 19 variations within the buried and extant populations of Cryptomeria japonica: 15 nucleotide substitutions and four indels (Fig. 4). Three nucleotide substitutions and one indel were singletons, and there were 15 nonsingleton variations (12 nucleotide substitutions and three indels). Of the 864 N . T A N I , Y . T S U M U R A and H . S A T O Fig. 4 Alignment of partial GapC region of Cryptomeria japonica. Dots indicate identical nucleotides to haplotype 1. Bars indicate deletions. nonsingleton variations, six nucleotide variations and two indels (at positions 21, 47, 49, 67, 77, 81, 83 and 107) were uniquely detected in haplotypes 4 and 5, creating a bimorphic pattern of DNA variation (Fig. 4). All of the buried trees were homozygotes with respect to the GapC sequence, except A4, which was heterozygous. Two nucleotide substitutions at 361 bp and 376 bp and one indel at 372 bp to 373 bp were responsible for differences between haplotype 2 (detected in A4) and haplotype 1 (typical buried tree type; Fig. 4). In contrast, seven distinct haplotypes were observed in the seven extant trees collected from the hillside of Sanbe volcano. Of the seven extant trees, five and two were heterozygous and homozygous, respectively. Table 2 summarizes estimates of DNA variation at the GapC gene of the buried C. japonica population and the extant population. Estimates of nucleotide diversity of the GapC region for the entire haplotypes, including both buried and extant populations, were 0.0063 (π) and 0.0010 (θ), while the corresponding figures were 0.0009 and 0.0017 © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859 –868 0.4083 NS −1.7204 NS 0.8070 NS −0.6890 NS — −0.4457 NS 0.4083 NS −1.7204 NS 0.6167 NS Tajima’s D‡ −1.3709 NS −1.4514 NS −0.5401 NS −1.2239 NS — −0.9592 NS −1.3709 NS −1.4514 NS −0.6672 NS θ 0.0104 0.0017 0.0142 0.0057 0.0000 0.0068 0.0010 0.0017 0.0125 π 0.0063 0.0009 0.0123 0.0024 0.0000 0.0044 0.0063 0.0009 0.0104 0.665 (0.010) 0.167 (0.134) 0.890 (0.055) 0.151 (0.093) 0.000 (0.000) 0.275 (0.148) 0.665 (0.010) 0.167 (0.134) 0.890 (0.055) DNA divergence between the buried and extant populations and phylogenetic relationships of the haplotypes Three individuals of the extant population displayed the most common haplotype of the buried population, haplotype 1, while haplotype 6 detected in the extant population differed only at the 261st nucleotide position from a unique haplotype of the buried population, haplotype 2 (Fig. 4). Thus, DNA polymorphism within the extant population included nearly all of the range of DNA polymorphisms found within the buried population. The estimates of DNA divergence statistics (dXY = 0.0062, dA = 0.0005, FST = 0.0832 and KST = 0.0935) suggest that there was not much differentiation between the two populations (Table 3). When we treated indels as single mutations, the levels of population differentiation rose a little. When we estimated population differentiation levels solely for the intronic region, the values also rose. FST and KST values derived from permutation tests rejected the null hypothesis, that populations were not differentiated, at the 5% and 1% probability levels, respectively. Because 11 0 11 1 0 1 12 0 12 Table 3 DNA divergence in the GapC partial seqence between buried and extant populations of Cryptomeria japonica Entire region *Number of sampled accessions. †Number of polymorphic sites. ‡ns, not significant. 2 2 2 1 0 1 3 2 3 13 2 13 2 0 2 15 2 15 Intronic region Intronic region Intronic region Exonic region Exonic region Exonic region Entire region Entire region Entire region 26 12 14 26 12 14 26 12 14 Buried and extant Buried Extant Buried and extant Buried Extant Buried and extant Buried Extant Region n* Population for the buried population, respectively, and those for the extant population were 0.0104 and 0.0125. Most of the DNA variations occurred in the intronic region, so nucleotide diversity in this region was greater than in the exon (Table 2). Table 2 also summarizes results of the Tajima’s (1989) and Fu & Li’s (1993) tests. All Tajima’s D-values were negative, but not significantly so, against the null hypotheses of neutrality and population equilibrium. Fu and Li’s test also gave results that were not statistically significant. However, while Tajima’s D statistics were negative for the pool of buried and extant populations, Fu and Li’s D statistics were positive for these populations. The conflict between Tajima’s and Fu and Li’s Ds showed that the D-values were almost equal to expectations in the tests. 4 1 4 0 0 0 4 1 4 Fu and Li’s D‡ Neutrality test Haplotype diversity Singleton site Polymorphic site Informative site No. of indels Nucleotide diversity S† Table 2 DNA polymorphisms, nucleotide diversity and neutrality tests of GapC partial sequence in C. japonica populations D N A V A R I A T I O N O F A N C I E N T C R Y P T O M E R I A J A P O N I C A 865 © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859–868 dXY dA FST† KST† Intronic region Indels ignored Indels as single mutation Indels ignored Indels as single mutation Exon 0.0062 0.0005 0.0832* 0.0935** 0.0078 0.0007 0.0834 0.0935* 0.0074 0.0006 0.0846* 0.0978** 0.0090 0.0011 0.1197* 0.1332** 0.0023 0.0001 0.0513 0.0232 †The significance of these statistics was tested by 10 000 permutation tests following Hudson et al. (1992a). *P < 0.05, **P < 0.01. 866 N . T A N I , Y . T S U M U R A and H . S A T O fragments of at most a few hundred nucleotides (Pääbo 1985, 1989; Pääbo et al. 1988; Hagelberg et al. 1989; Lawlor et al. 1991). Our samples were exhumed from a 3600-yearold layer, and agarose gel electrophoresis showed that the extracted DNA was fragmented. We successfully amplified PCR fragments less than about 500 bp long, which is consistent with previous PCR amplifications of nuclear genomic regions using ancient DNA. Fig. 5 Haplotype network (cladogram) of partial GapC sequences of the buried and extant Cryptomeria japonica constructed under the statistical parsimony criterion. Haplotype numbers (Hap 1 and so on) correspond to those given in Fig. 4. Each line in the network represents a single mutational change between haplotypes. Small solid circles indicate a haplotype not present in the sample, but inferred to be intermediate between two nearest-neighbour haplotypes. The size of each circle and the number at the lower right side of the circle indicate number of individuals retaining each haplotype. All haplotypes within the buried population are included in Haplotype 1 and 2. the major haplotype within the buried population was also detected in the extant population and the extant population retained the very similar haplotype as another haplotype within the buried population (Fig. 4), significant population differentiation was caused by differences in haplotype diversity between the extant and buried populations. An estimation of genetic relationships among eight haplotypes was obtained by the minimum spanning network based on nucleotide substitutions in the 391-bp region of the GapC gene. Haplotypes 4 and 5 were located furthest from the centre of the network. Seven nucleotide substitutions were required to evolve haplotypes 4 and 5 from the major haplotype 1 located at the centre. The two haplotypes observed in the buried population were not greatly differentiated (two steps), and were similar to four extant haplotypes around haplotypes 1 and 2 that were detected in the buried population (Fig. 5) Discussion Successful PCR amplification of nuclear DNA from fossils Based on in vitro analysis of the rate of DNA degradation, it has been suggested that the molecule could not persist for more than 104−105 years in most geological settings (Pääbo & Wilson 1991; Lindahl 1993). To date, only small fragments of nuclear DNAs (including the HLA gene and a long nucleotide tandem repeat) have been amplified, from fossils up to about 7500 years old (Lawlor et al. 1991; Kurosaki et al. 1993; Fischer et al. 2001). This is because ancient DNA is usually only available in low quantities in Population history, from the buried population to the extant population Haplotype 1 was the major type of the buried population, and it was also detected in the extant population, while haplotype 2 was detected only in the buried population. No other haplotypes were observed in the buried population (Fig. 4). We believe there are two possible reasons for several haplotypes being detected only in the extant population. Firstly, clonal growth in the buried population may have been responsible for the limited DNA variation detected within the buried population. In support of this hypothesis, clonal growth has been shown to be responsible for some propagation of Cryptomeria japonica, according to allozyme and DNA marker analysis in a high-altitude region with heavy snow (Taira et al. 1997; Moriguchi et al. 2001). Global warming in the postglacial period caused sea levels to rise, and led to the inflow of a warm current into the Sea of Japan about 8000 years ago. Subsequent increases in the temperature of the Sea of Japan caused snowfall on that side of southwestern Japan to rise (Yasuda 1982). Many pollen analyses of core samples have shown that C. japonica forest developed on the Sea of Japan side of southwestern Japan from 4000 years to 2000 years ago (Miyoshi & Hada 1975; Hatanaka & Miyoshi 1980; Tsukada 1982; Sugita & Tsukada 1983; Miyoshi & Yano 1986). Moreover, it was observed that a tree with a thin diameter (A19) was connected to a neighbouring tree with large diameter (A9) in the ground (Fig. 2). Therefore, clonal growth may have occurred, in an environment with moist and heavy snow at this time, which may have led to extension of clonal growth in the buried population. Such clonal growth would have hindered detection of the total DNA variation within the buried population. If so, all the haplotypes detected in the extant population might also have existed in the buried population. Alternatively, the unique haplotypes in the extant population may have originated from migration from surrounding populations. Japanese people have been clearing forest lands to construct artificial C. japonica forests for about 400 years (Ohba 1991), and the extant population is currently surrounded by artificial forests of C. japonica. Tomaru et al. (1994) made an indirect estimate of the mean number of migrants exchanged per generation (Nm) based on allozyme data derived from 17 natural populations of © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859 –868 D N A V A R I A T I O N O F A N C I E N T C R Y P T O M E R I A J A P O N I C A 867 C. japonica, obtaining a mean value of 7.1. The estimates of Nm suggest that gene flow may have occurred frequently, probably even between natural and artificial forests. The minimum spanning network indicated that haplotype 1 is the most common allele and arguably the oldest in the samples, because haplotype 1 became central and had the most connections. The remaining haplotypes were connected to haplotype 1 within fewer than three steps of mutations except for haplotypes 4 and 5 (Fig. 5). Because seven mutations were needed to evolve the remote haplotypes 4 and 5 from the central haplotype 1 in the network and four intermediate haplotypes were missed from haplotype 7 to haplotypes 4 and 5, a reasonable speculation was that these haplotypes had migrated from some other populations. The origin of unique haplotypes in the extant population is unknown, so further extensive study of population genetic analysis using DNA sequences will focus on defining the intensity and extent of gene flow and genetic structure of C. japonica. Acknowledgements The authors are particularly grateful to Dr H. Tachida, Ms J. Kusumi, Mr T. Kado, Dr Y. Suyama, Dr H. Yoshimaru and Dr H. Iwata for their help in collecting samples, and to Dr H. Tachida for supplying primers to amplify the GapC gene. We also thank two anonymous referees for their perceptive suggestions on the latest version of the manuscript. This study was supported by a grant from the Programme for Promotion of Basic Research Activities for Innovative Biosciences (PROBRAIN). References Clement M, Posada D, Crandall KA (2000) TCS: a computer program to estimate gene genealogies. Molecular Ecology, 9, 1657–1659. Curtis SE, Clegg MT (1984) Molecular evolution of chloroplast DNA sequences. Molecular Biology and Evolution, 4, 291–301. Dumolin-Lapègue S, Pegmonge M, Gielly L, Taberlet P, Petit R (1999) Amplification of oak DNA from ancient and modern wood. Molecular Ecology, 8, 2137–2140. Filatov D (2001) Processor of Sequences Manual. University of Birmingham, Birmingham UK. Fischer GF, Fae I, Mann D et al. (2001) An HLA class-II allele frequent in Eskimos and Amerindians is found in the Tyrolean Ice Man. Annals of Human Genetics, 65, 363–369. Fu Y-X, Li W-H (1993) Statistical tests of neutrality of mutations. Genetics, 133, 693–709. Hagelberg E, Sykes B, Hedges R (1989) Ancient bone DNA amplified. Nature, 342, 485. Hatanaka K, Miyoshi N (1980) History of the late Pleistocene and Holocene vegetation in the Ubuka basin, southwestern Japan. Japanese Journal of Ecology, 30, 239–244 (In Japanese). Hayashi Y (1960) Taxonomical and phytogeographical study of Japanese conifers. Norin-Shuppan, Tokyo. (In Japanese). Hudson RR, Boos DD, Kaplan NF (1992a) A statistical test for detecting geographic subdivision. Molecular Biology and Evolution, 9, 138–151. © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859–868 Hudson RR, Slatkin M, Maddison WP (1992b) Estimating levels of gene flow from DNA sequence data. Genetics, 116, 153–159. Iwata H, Ujino-Ihara T, Yoshimura K, Nagasaka K, Mukai Y, Tsumura Y (2001) Cleaved amplified polymorphic sequence markers in sugi, Cryptomeria japonica D. Don, and their locations on a linkage map. Theoretical and Applied Genetics, 103, 881–895. Jansson S, Meyer-Gauen G, Cerff R, Martin W (1994) Nucleotide distribution in gymnosperm nuclear sequences suggests a model for GC-content change in land-plant nuclear genomes. Journal of Molecular Evolution, 39, 34–46. Krings M, Stone A, Schmitz RW, Krainitski H, Stoneking M, Pääbo S (1997) Neanderthal DNA sequences and the origin of modern humans. Cell, 90, 19–30. Kurosaki K, Matsushita T, Ueda S (1993) Individual DNA identification from ancient human remains. American Journal of Human Genetics, 53, 638–643. Lawlor DA, Dickel CD, Hauswirth WW, Parham P (1991) Ancient HLA genes from 7500-year-old archaeological remains. Nature, 349, 785–787. Lindahl T (1993) Instability and decay in the primary structure of DNA. Nature, 362, 709–715. Miyoshi N, Hada Y (1975) Pollen analytical studies of moor sediments in Chugoku, Japan. I. Orogatawa moor. Quaternary Research, 14, 161–168 (In Japanese). Miyoshi N, Yano N (1986) Late Pleistocene and Holocene vegetation history of the Ohnuma moor in the Chugoku mountains, western Japan. Review of Palaeobotany and Palynology, 46, 355–376. Moriguchi Y, Matsumoto A, Saito M, Tsumura Y, Taira H (2001) DNA analysis of clonal structure of an old growth, isolated forest of Cryptomeria japonica in a snowy region. Canadian Journal of Forest Research, 31, 377–383. Murray MG, Thompson WF (1980) Rapid isolation of high molecular weight plant DNA. Nucleic Acids Research, 8, 4321–4325. Nei M (1973) Analysis of gene diversity in subdivided populations. Proceedings of the National Academy of Sciences of the USA, 70, 3321–3323. Nei M (1987) Molecular Evolutionary Genetics. Columbia University Press, New York. Nei M, Li WS (1979) Mathematical model for studying genetic variation in terms of restriction endonuclease. Proceedings of the National Academy of Sciences of the USA, 76, 5269–5273. Nei M, Chesser RK (1983) Estimation of fixation indices and gene diversities. Annals of Human Genetics, 47, 253–259. Ohba K (1991) The history of forest breeding. In: Forest Breeding (eds Ohba K, Katsuta M), pp. 32–43. Buneido, Tokyo. Pääbo S (1985) Molecular cloning of ancient Egyptian mummy DNA. Nature, 314, 644–645. Pääbo S (1989) Ancient DNA: extraction, characterization, molecular cloning, and enzymatic amplification. Proceedings of the National Academy of Sciences of the USA, 86, 1939–1943. Pääbo S, Wilson AC (1991) Miocene DNA sequences a dream come true? Current Biology, 1, 45–46. Pääbo S, Gifford JA, Wilson AC (1988) Mitochondrial DNA sequence from a 7000 year old brain. Nucleic Acid Research, 16, 9775–9787. Palmer JD (1985) Evolution of chloroplast and mitochondrial DNA in plants and algae. In: Molecular Evolutionary Genetics (ed. MacIntyre RJ), pp. 131–240. Plenum Press, New York. Poinar HN, Melanie K, Sobolik KD et al. (2001) A molecular analysis of dietary diversity for three archaic native Americans. Proceedings of the National Academy of Sciences of the USA, 98, 4317–4322. 868 N . T A N I , Y . T S U M U R A and H . S A T O Rozas J, Rozas R (1999) DnaSP, Version 3: an integrated program for molecular population genetics and molecular evolution analysis. Bioinformatics, 15, 174 –175. Sugita S, Tsukada M (1983) Vegetation history around Nonbara bog in the San’in district for the past 17,000 years. Japanese Journal of Ecology, 33, 225 –230 (In Japanese). Suyama Y, Kawamuro K, Kinoshita I, Yoshimura K, Tsumura Y, Takahara H (1996) DNA sequence from a fossil pollen of Abies spp from Pleistocene peat. Genes and Genetic Systems, 71, 145 –149. Taira H, Tsumura Y, Tomaru N, Ohba K (1997) Regeneration system and genetic diversity of Cryptomeria japonica growing at different altitudes. Canadian Journal of Forest Research, 27, 447– 452. Tajima F (1989) Statistical method for testing the neutral mutation hypothesis by DNA polymorphism. Genetics, 123, 585–595. Tajima F (1993) Measurement of DNA polymorphism. In: Mechanisms of Molecular Evolution (eds Takahata N. Clark AG), pp. 37–59. Sinauer Associates, Inc., Sunderland. Tajima F, Nei M (1984) Estimation of evolutionary distance between nucleotide sequences. Molecular Biology and Evolution, 1, 269–285. Thomas R, Schaffner W, Wilson A, Pääbo S (1989) DNA phylogeny of the extinct marsupial wolf. Nature, 340, 465– 467. Thompson JD, Higgins DG, Gibson TJ (1994) CLUSTAL W: improving the sensitivity of progressive multiple sequence alignment through sequence weighting, position specific gap penalties and weight matrix choice. Nucleic Acid Research, 22, 4673–4680. Tomaru N, Tsumura Y, Ohba K (1994) Genetic variation and population differentiation in natural populations of Cryptomeria japonica. Plant Species Biology, 9, 191–199. Tsukada M (1982) Cryptomeria japonica: glacial refugia and lateglacial and postglacial migration. Ecology, 63, 1091–1105. Watterson GA (1975) On the number of segregating sites in genetical models without recombination. Theoretical Population Biology, 7, 256–276. Wayne RK, Leonard JA, Cooper A (1999) Full of sound and fury: the recent history of ancient DNA. Annual Review of Ecology and Systematics, 30, 457–477. Yasuda Y (1982) Pollen analytical study of the sediment from the lake Mikata in Fukui prefecture, central Japan, especially on the fluctuation of precipitation since the last glacial age on the side of sea of Japan. Quaternary Research, 21, 255 –271. (In Japanese). N. Tani is working on the sugi (Cryptomeria japonica) genome project. His other current research interests are a population genetic study of five-needle pines and conservation genetics for endangered species in oceanic islands. Y. Tsumura is the leader of the sugi genome project, whose other current research interests include the population genetics of C. japonica and conservation genetics for tropical tree species. H. Sato is working on environmental policy in Shimane prefecture and is directing the excavation and exhibition of Sanbe buried forest. © 2003 Blackwell Publishing Ltd, Molecular Ecology, 12, 859 –868
© Copyright 2026 Paperzz