Mitochondrial DNA Analysis of Hokkaido Jomon Skeletons: Remnants of Archaic Maternal Lineages at the Southwestern Edge of Former Beringia

被引:56
|
作者
Adachi, Noboru [1 ]
Shinoda, Ken-ichi [2 ]
Umetsu, Kazuo [3 ]
Kitano, Takashi [4 ]
Matsumura, Hirofumi [5 ]
Fujiyama, Ryuzo [6 ]
Sawada, Junmei [7 ]
Tanaka, Masashi [8 ]
机构
[1] Univ Yamanashi, Interdisciplinary Grad Sch Med & Engn, Dept Legal Med, Yamanashi 4093898, Japan
[2] Natl Museum Nat & Sci, Dept Anthropol, Tokyo, Japan
[3] Yamagata Univ, Dept Forens Med, Fac Med, Yamagata 990, Japan
[4] Ibaraki Univ, Coll Engn, Dept Biomol Funct Engn, Ibaraki, Japan
[5] Sapporo Med Univ, Dept Anat, Sch Med, Sapporo, Hokkaido, Japan
[6] Keio Univ, Archaeol Res Off, Kanagawa, Japan
[7] St Marianna Univ, Sch Med, Dept Anat, Kanagawa, Japan
[8] Tokyo Metropolitan Inst Gerontol, Dept Genom Longev & Hlth, Tokyo, Japan
关键词
ancient DNA; single nucleotide polymorphisms; Jomon; Siberia; last glacial maximum; USU-MOSHIRI SITE; GENETIC-ANALYSIS; CONTROL REGION; INTEGRATED SOFTWARE; DOUBLE BURIAL; AFFINITIES; DIVERSITY; SEQUENCE; HISTORY; ORIGINS;
D O I
10.1002/ajpa.21561
中图分类号
Q98 [人类学];
学科分类号
030303 ;
摘要
To clarify the colonizing process of East/Northeast Asia as well as the peopling of the Americas, identifying the genetic characteristics of Paleolithic Siberians is indispensable. However, no genetic information on the Paleolithic Siberians has hitherto been reported. In the present study, we analyzed ancient DNA recovered from Jomon skeletons excavated from the northernmost island of Japan, Hokkaido, which was connected with southern Siberia in the Paleolithic period. Both the control and coding regions of their mitochondrial DNA (mtDNA) were analyzed in detail, and we confidently assigned 54 mtDNAs to relevant haplogroups. Haplogroups N9b, D4h2, G1b, and M7a were observed in these individuals, with N9b being the predominant one. The fact that all these haplogroups, except M7a, were observed with relatively high frequencies in the southeastern Siberians, but were absent in southeastern Asian populations, implies that most of the Hokkaido Jomon people were direct descendants of Paleolithic Siberians. The coalescence time of N9b (ca. 22,000 years) was before or during the last glacial maximum, implying that the initial trigger for the Jomon migration in Hokkaido was increased glaciations during this period. Interestingly, Hokkaido Jomons lack specific haplogroups that are prevailing in present-day native Siberians, implying that diffusion of these haplogroups in Siberia might have been after the beginning of the Jomon era, about 15,000 years before present. Am J Phys Anthropol 146:346-360, 2011. (C) 2011 Wiley-Liss, Inc.
引用
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页码:346 / 360
页数:15
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