State Key Laboratory of Genetic Resources and Evolution, Kunming Institute of Zoology, Chinese Academy of Sciences, Kunming 650223, Yunnan Province, China.
Proc Natl Acad Sci U S A. 2009 Dec 15;106(50):21230-5. doi: 10.1073/pnas.0907844106. Epub 2009 Dec 2.
Due to its numerous environmental extremes, the Tibetan Plateau--the world's highest plateau--is one of the most challenging areas of modern human settlement. Archaeological evidence dates the earliest settlement on the plateau to the Late Paleolithic, while previous genetic studies have traced the colonization event(s) to no earlier than the Neolithic. To explore whether the genetic continuity on the plateau has an exclusively Neolithic time depth, we studied mitochondrial DNA (mtDNA) genome variation within 6 regional Tibetan populations sampled from Tibet and neighboring areas. Our results confirm that the vast majority of Tibetan matrilineal components can trace their ancestry to Epipaleolithic and Neolithic immigrants from northern China during the mid-Holocene. Significantly, we also identified an infrequent novel haplogroup, M16, that branched off directly from the Eurasian M founder type. Its nearly exclusive distribution in Tibetan populations and ancient age (>21 kya) suggest that M16 may represent the genetic relics of the Late Paleolithic inhabitants on the plateau. This partial genetic continuity between the Paleolithic inhabitants and the contemporary Tibetan populations bridges the results and inferences from archaeology, history, and genetics.
由于其众多的环境极端条件,青藏高原——世界上最高的高原——是现代人类定居的最具挑战性的地区之一。考古证据将高原上最早的定居时间追溯到旧石器时代晚期,而之前的遗传研究表明,殖民事件最早发生在新石器时代。为了探索高原上的遗传连续性是否仅限于新石器时代,我们研究了从西藏和邻近地区采集的 6 个地区藏族人群的线粒体 DNA(mtDNA)基因组变异。我们的研究结果证实,绝大多数藏族母系遗传成分可以追溯到中全新世时期来自中国北方的旧石器时代晚期和新石器时代移民。值得注意的是,我们还发现了一个罕见的新单倍群 M16,它直接从欧亚大陆的 M 创始类型分支出来。它在藏族人群中的几乎排他性分布和古老的年龄(>21 kya)表明,M16 可能代表了高原上旧石器时代居民的遗传遗迹。这种旧石器时代居民与当代藏族人群之间的部分遗传连续性,连接了考古学、历史学和遗传学的研究结果和推论。