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Applied and Environmental Microbiology, April 2008, p. 2023-2031, Vol. 74, No. 7
0099-2240/08/$08.00+0 doi:10.1128/AEM.02411-07
Copyright © 2008, American Society for Microbiology. All Rights Reserved.

Akiyoshi Yamada,3 and
Akira Ohta4
Department of Applied Microbiology and Mushroom Sciences, Forestry and Forest Products Research Institute, Tsukuba, Ibaraki 305-8687, Japan,1 Central Customs Laboratory, Ministry of Finance, Kashiwa-shi, Chiba 277-0882, Japan,2 Department of Bioscience and Biotechnology, Faculty of Agriculture, Shinshu University, Minami-minowa, Nagano 399-4598, Japan,3 Shiga Forest Research Center, Yasu, Shiga 520-2321, Japan4
Received 26 October 2007/ Accepted 29 January 2008
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Traceability is one of the most serious issues faced in the market for matsutake in Japan. In general, domestic matsutake and South Korean matsutake are traded at a premium and at a semipremium, respectively. For example, the former products are traded at the price of approximately $500/kg and the latter are traded at $250/kg recently, while the Chinese counterpart is traded at $100/kg. Tariffs are imposed depending upon exporting countries. For example, as of the year 2007, products from China and Bhutan are free of extra charge, whereas those from South and North Korea are subjected to customs duties of 4 and 5%, respectively (Ministry of Finance of Japan). Food safety is another concern, for safety regulations vary among countries. To prevent falsification of the geographical origin of matsutake, a simple method, such as a PCR-based analytical system, to efficiently differentiate among Asian isolates of T. matsutake has been demanded.
Retroelements are retrovirus-like DNA parasites associated with host eukaryotic genomes, which replicate through an RNA intermediate and integrate into multiple genomic loci, exerting great influence on the genome structure and function (4, 5, 7, 8, 23, 26, 28, 31). Such a transposition process through copy-and-paste, rather than through cut-and-paste, leaves stable positive markers of genome evolution that are inherited by the host's descendants (4, 5, 7, 8, 23, 26, 28, 31). We previously reported that interretrotransposon amplified polymorphism (IRAP) analysis using as a genetic marker the long terminal repeat (LTR) of the gypsy-type retroelement marY1, designated
marY1, which is accumulated in the genome of T. matsutake, could specify strains of the symbiont by exhibiting highly polymorphic fingerprints (16, 18, 20). The analysis, however, fails to inform us of subtle differences among biogeographical groups of individual Asian isolates of T. matsutake (18). The failure of biogeographical typing, or geotyping, through IRAP may be attributed to highly polymorphic fingerprints that may obscure some
marY1-associated markers generated upon the occurrence of biogeographical diversification of T. matsutake. In the present study, we explored the structure of
marY1 insertion sites for use as genetic markers useful in tracing the geographical origin of Asian matsutake.
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TABLE 1. Tricholoma matsutake strains used in this study
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FIG. 1. Primer design to differentiate among individual Asian isolates of T. matsutake. Locations and directions of primers are indicated by arrows: solid arrows, primers designed for IRAP previously (18); open arrows, primers designed to be used with pS48 in this study.
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TABLE 2. Specifications of the marY1-based T. matsutake geotypes in Asia
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Nucleotide sequencing.
Desired fragments were extracted from the agarose gels after separation by gel electrophoresis using the Wizard DNA purification system (Promega, Madison, WI), ligated with pCR2.1 vector (Invitrogen, Carlsbad, CA), and introduced into Escherichia coli JM109 competent cells. The plasmids containing the target inserts were isolated from the E. coli transformants using the Wizard Plus SV miniprep DNA purification system (Promega). After confirmation of the presence of appropriate DNA inserted in the plasmids, nucleotide sequencing was carried out in both directions using the 3130xl Genetic Analyzer (Applied Biosystems/Hitachi) with Big Dye Terminator FS core kit, version 3.1 (Applied Biosystems). Sequence data were analyzed with Genetix Mac version 13.1 and ATSQ (Software Development Inc., Tokyo, Japan), and homology search analysis was conducted with the BLASTN program provided by DDBJ.
Nucleotide sequence accession numbers.
Nucleotide sequences have been deposited in the DDBJ database under the accession numbers AB330884-96, AB360715-40, and AB363821-38.
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marY1 as described previously (Fig. 1) (18). The PCR amplicons, ranging from approximately 140 bp to 700 bp, were extracted, ligated into pCR2.1, and sequenced. While the sequences associated with pS48 are conserved carrying the 5'-terminal (bp 1 to 47) sequence of
marY1 in all the fragments analyzed, those with pL281 are diversified (AB330884-96). Therefore, we fixed pS48 for one end of the primer and designed primers to be used with pS48 for the other end based on the sequence data (Fig. 1). Two primers, pDGSL313-1 and pDGSL719-2, were selected (Fig. 1). pDGSL313-1 was designed based on a sequence of a 313-bp DNA segment from Y1 (Fig. 1; AB330894 [bp 41 to 67]). The 313-bp DNA segment consists of sequences of a putative coat protein gene throughout (AB160897). pDGSL719-2 was designed based on a sequence of a 719-bp DNA segment from Tm-31 (Fig. 1; AB330884 [bp 263 to 288]). The 719-bp DNA segment has sequences of the non-LTR retroelement marY2N cluster at bp 101 to 596 (19) (AB047280).
pDGSL313-1/pS48 system.
Table 1 shows the
marY1-based geotypes of individual T. matsutake isolates, and Fig. 2 shows the relevant biogeographical map of Asian matsutake. PCR with pDGSL313-1/pS48 (Ta = 64.0°C) overall conferred two types of polymorphisms: one designated geotype A exclusively sharing the 493-bp and the 337-bp bands as the basic characteristic feature among isolates from the Far East including Japan, South Korea, and North Korea (Table 2; Fig. 3A, lanes 1 to 26 and 37 to 44) and the other designated geotype B composed solely of the 273-bp band that is specific to the isolates from the area of China through Bhutan (Table 2; Fig. 3A, lanes 27 to 36). In geotype A, subgeotype A2 was assigned to the DNA profile with the 450-bp and the 299-bp bands that are conserved among isolates from the far western part of the main island (Honshu) of Japan (Table 2; Fig. 3A, lanes 9 to 13), while subgeotype A1 and subgeotype A3, which should allow us to differentiate between Japanese and Korean isolates, were assigned to the profile based on the other analytical system with pDGSL719-2/pS48 (see below).
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FIG. 2. Biogeography of T. matsutake in Asia based on the marY1-based typing. The predominant distribution of T. matsutake geotypes is given. The blank map was obtained from Freemap.jp (http://www.freemap.jp/ or http://english.freemap.jp/world_paint/world_paint.html).
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FIG. 3. PCR profiles of Asian isolates of T. matsutake. After electrophoresis, the 26-cm by 30-cm agarose gel, which was enough to run 37 samples simultaneously, was cut into pieces large enough to observe the result on a 20-cm by 20-cm transilluminator. Photographs of lanes 1 to 36 and lanes 37 to 44 were taken after gel electrophoresis that was separately carried out. The molecular size (bp) of a relevant DNA band is indicated by arrowheads to the right. Geographical origins of specimens are given at the bottom. (A) pDGSL313-1/pS48 primer system. (B) pDGSL719-2/pS48 primer system. Lanes M, molecular markers (200 to 1,000 bp); lanes 1 to 44, T. matsutake strains (Table 1 shows assigned geotypes): 1, TM15; 2, Y1; 3, Y4; 4, F1; 5, Tm-8; 6, MR32; 7, Tm029; 8, OK-T4; 9, Tm-T4; 10, Tm-507; 11, Tm-H102; 12, Tm-Y59ABF; 13, Tm-Y62B; 14, K1; 15, Tm-K2; 16, Tm-31; 17, Tm-156; 18, Tm-157; 19, Tm-158; 20, SKR02; 21, SKR03; 22, NK1; 23, NKR02; 24, NKR03; 25, NKR04; 26, NKR05; 27, CN01; 28, CHI1; 29, Tm-9; 30, CH381; 31, CH382; 32, CH383; 33, CH384; 34, CH385; 35, CH387; 36, BH1; 37, Tm-31; 38, K3; 39, K4; 40, Tm-159; 41, SKR01; 42, SKR04; 43, SKR05; 44, NKR01.
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Geotyping of T. matsutake from three representative localities in Japan.
Since the Japanese commodities are the most probable target for counterfeiting, we attempted to confirm the reliability of the test to specify the Japanese subgeotypes with additional samples that we had picked by ourselves in Pinus densiflora woodlands, i.e., samples with no risk of contamination (Table 2). We assayed samples from study sites representing three major localities distantly located from each other: the Khonan-Minakuchi study site in Shiga prefecture, the Morigane site in Ibaraki, and the Yokkaichi site in Iwate (Table 1; Fig. 2) (20). The results clearly showed that isolates from all three locations in Japan, as well as domestic ones examined earlier, shared the genotypic identity of either A1 or A2 that was distinct from isolates from the continent (Fig. 4; Tables 1 and 2). It is noteworthy that Iwate and North Korea are at the same distance from Shiga, located on the same latitude and with almost similar longitudinal spans from Shiga (Fig. 2). Such is also the case with Ibaraki and South Korea (Fig. 2). Note that the Korean isolates examined earlier also include samples that we had picked by ourselves in P. densiflora woodlands in Gyeongsangbuk-do, South Korea, as well as those obtained by the Japanese Customs Service at ports and airports prior to circulation (see above) (Table 1; Fig. 3).
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FIG. 4. PCR profiles of T. matsutake from three representative localities in Japan. The molecular size (bp) of a relevant DNA band is indicated by arrowheads to the right. Geographical origins of specimens are given at the bottom. (A) pDGSL313-1/pS48 primer system. (B) pDGSL719-2/pS48 primer system. Lane M, molecular markers (300 to 1,000 bp); lanes 1 to 33, T. matsutake strains (Table 1 shows assigned geotypes): 1, Tm027; 2, Tm029; 3, Tm040; 4, Tm043; 5, Tm050; 6, Tm068; 7, Tm077; 8, Tm078; 9, Tm082; 10, Tm069; 11, Tm072; 12, Tm074; 13, Tm100; 14, Tm127; 15, Tm172; 16, Tm195; 17, Tm196; 18, AT634; 19, AT636; 20, AT639; 21, AT640; 22, AT641; 23, AT642; 24, AT635; 25, AT637; 26, AT638; 27, IW-92602-1; 28, IW-92602-2; 29, IW-92602-4; 30, IW-100702-2; 31, IW-100702-4; 32, I-84; 33, I-114.
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DNA was extracted from gills of the specimens at the stage prior to breaking the veil. The pDGSL313-1/pS48 system conferred polymorphisms that clearly specify T. matsutake isolates as being either from the southwestern provinces or from the northeastern provinces (Fig. 5A; Tables 1 and 2). All the isolates from the southwestern provinces examined were geotype B (Fig. 5A, lanes 15 to 25), and those that we had obtained as Chinese matsutake at local markets in Japan were proven to be from the same region (Fig. 3A, lanes 28 to 35). In contrast, the isolates from the northeastern provinces showed a 573-bp band unique to the Asian population examined while exhibiting the profile of geotype A characterizing the Far East isolates (Fig. 5A, lanes 5 to 14). These isolates also showed a close relationship with those from the Korean peninsula as revealed by the pDGSL719-2/pS48 system (Fig. 5B, lanes 5 to 14). We, therefore, assigned subgeotype A4 to the profile featuring the northeastern provinces of China (Table 2).
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FIG. 5. PCR profiles of T. matsutake from northeastern and southwestern provinces of China. The molecular size (bp) of a relevant DNA band is indicated by arrowheads in the right column. Geographical origins of specimens are given at the bottom. (A) pDGSL313-1/pS48 primer system. (B) pDGSL719-2/pS48 primer system. Lane M, molecular markers (300 to 1,000 bp); lanes 1 to 25, T. matsutake strains (Table 1 shows assigned geotypes): 1, Tm-Y62B; 2, Tm-158; 3, NK1; 4, NKR02; 5, CH-HE1; 6, CH-HE2; 7, CH-HE3; 8, CH-HE4; 9, CH-HE5; 10, CH-JI1; 11, CH-JI2; 12, CH-JI3; 13, CH-JI4; 14, CH-JI5; 15, CH-SI1; 16, CH-SI3; 17, CH-SI4; 18, CH-SI5; 19, CH-SI2; 20, CH-YU1; 21, CH-YU2; 22, CH-YU3; 23, CH-YU4; 24, CH-YU-5; 25, CN01.
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Nucleotide sequence analysis of the geotype determinants.
Representative DNA segments that feature geotypes assigned in this study were cloned into pCR2.1 and analyzed by nucleotide sequencing (AB360715-40 and AB363821-38). The sequences of the 493-bp and the 337-bp fragments, which determine geotype A, are 99% identical at bp 1 to 337 in the direction from pS48 to pDGSL313-1, and so are those of the 450-bp and the 299-bp fragments, which determine subgeotype A2, at bp 1 to 299. Therefore, we classified isolates exhibiting one of the former fragments into geotype A and one of the latter into subgeotype A2 (Fig. 4, lane 32; Table 1 [I-84]). The sequence of the 573-bp fragment, which specifies subgeotype A4, is related to neither that of the geotype A determinant nor that of the A2 determinant. None of these fragments is the homolog of the 313-bp DNA segment whose sequence was used for designing the primer pDGSL313-1. Rather, the sequence of the 273-bp DNA segment, which is the marker of geotype B, is 99% identical to that of the 313-bp DNA segment at bp 1 to 273 in the direction from pS48 to pDGSL313-1. Although we found that some strains belonging to geotype A have the 273-bp fragment shared with geotype B, we dared to establish another subtype in geotype A (Fig. 3A, lanes 1 to 2, 9, 15, 19, 21, 23, 25, 38 to 40, and 42). Similarly, although some isolates from North Korea and the Jilin province of China exhibited fragments smaller than the 273-bp fragment, such as 255-bp and 265-bp fragments that are recognized as deletion derivatives of the 273-bp fragment, their significance in biogeography is yet to be clarified (Fig. 3A, lanes 22 to 25 and 44; Fig. 5A, lanes 10, 12, and 14). The sequence of the 457-bp fragment which determines subgeotype A3 is 99% identical among isolates belonging to this geotype but is not the homolog of the 719-bp DNA segment used for designing the primer pDGSL719-2. This phenomenon may be attributed to the preference of sequences for PCR amplification among repetitive sequences dispersed throughout the genome (16, 19, 33) (AB047280).
Conclusion.
We demonstrated for the first time that two PCR systems concurrently carried out differentiate among individual Asian isolates of T. matsutake by their geographical origins, allowing us to trace them back to Japan, the area of South Korea through North Korea, the northeastern provinces of China, and the area of the southwestern provinces of China through Bhutan (Table 2; Fig. 2). The results presented here are consistent with our hypothesis that the genome of T. matsutake could have dramatically evolved during a rather later evolutionary stage by the involvement of retroelements (16, 17). This study strongly suggests that some retroelement integrations have occurred during the course of biogeographical diversification.
The results are reproducible. Note that Japanese isolates were collected from various locations between 1983 and 2005, Korean isolates were collected between 1997 and 2006, and Chinese and Bhutanese isolates were collected between 1992 and 2007 (Table 1). The occurrence of local diversification at the level of isolates has been reported in T. matsutake (14, 20, 33), and diversification through mosaicism has been documented as a general phenomenon in mushroom-producing basidiomycetes (1, 2, 9, 25, 27, 29, 30). Therefore, the retroelement-based geotyping markers are recognized as highly conserved over generations. Retroelements are mobile with copy-and-paste rather than with cut-and-paste processes. This unique transposition process allows the original copy and copies once amplified and integrated to remain in the genomic loci as footprints of genome evolution (4, 5, 7, 8, 23, 26, 28, 31). In this view, it is not surprising that the retroelement-based analytical system unearthed for the first time the significant biogeographical diversification of Chinese matsutake, in which the isolates from northeastern provinces are not only distinct among the population of Asian matsutake tested but also closely related to the Korean and Japanese isolates, while isolates from the southeastern provinces of China through Bhutan, a high-altitude area distant from the Far East, are unique among the population.
In biogeographical studies of mushroom species, the sequence of ribosomal DNA (rDNA) has been regarded as a reliable genetic marker, as in the typical case with species of Pleurotus (32, 36). In T. matsutake, however, the sequences of both intergenic spacer 1 (IGS1) and the interspacer regions (ITS1 and ITS2) are highly conserved among isolates from all over the world (10, 15). We previously demonstrated that T. matsutake has megB1, an approximately 500-bp DNA segment that is the major component of IGS1 from many mushroom species including species of Pleurotus, in a genomic region out of rDNA (3) (AB304914 and AB304915). The sequence of megB1 is also too conserved as a marker to classify T. matsutake isolates (unpublished data; AB293550 and AB298297 to AB298306).
The system developed in this study offers us a simple but highly reliable polymorphism analysis system, enabling rapid assay of Asian matsutake geotypes without requiring dendrogram calculation of a number of DNA fragments (Table 2). The situation contrasts with IRAP, which generates tremendous numbers of DNA segments as the fingerprint of each strain, making their classification very difficult (18, 20). Since matsutake is a fresh food and should be consumed within a week after harvest, the availability of a rapid analytical system is extremely important. By the same token, it could be a practical method suitable for identifying the geographical origin of matsutake at the Customs and Consumer Services. Also, the demonstration presented here opens a new horizon in the scope of molecular ecology and the evolution of mushroom-producing basidiomycetes, a research area that has seldom explored mobile DNA as genetic markers that should inform us of the dynamics of molecular ecology and the evolution of eukaryotes (4, 5, 7, 8, 23, 26, 28, 31).
Like any other traceability methods designed to examine agricultural products, including the elemental composition analysis widely used, the PCR-based analytical system is not always perfectly accurate. In fact, some Korean isolates exhibited the same subgeotype A1 as Japanese isolates. However, the analytical system met a reliability standard with an average misjudgment rate of approximately 5% and, therefore, is useful in the primary screening of products traded all over Japan to be followed by tracing back the geographical origin through the in-depth examination of trading records. Such a primary screening method not only facilitates traceability but also deters counterfeiting. In the summer of 2007, Scandinavian matsutake mushrooms were imported for the first time and traded at a price of $400/kg, which is equivalent to an average price for Japanese matsutake in a high season, while early crops harvested in the northern part of Japan were traded at the record high price of $4,000/kg. We hope that the traceability method presented here contributes to mutual trust among consumers, trading authorities, and exporting countries, as well as to conservation of natural resources through rationalizing international trading in the field of ectomycorrhizal specialty mushrooms.
Published ahead of print on 15 February 2008. ![]()
Present address: Customs Laboratory Clearance Division of Tokyo Customs, Koto-ku Aomi 2-56, Tokyo 135-8615, Japan. ![]()
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marY1, the long terminal repeat of gypsy-type retroelement marY1. Mycorrhiza 15:179-186.[CrossRef][Medline]
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