Raff Jennifer A, Rzhetskaya Margarita, Tackney Justin, Hayes M Geoffrey
Division of Endocrinology, Metabolism and Molecular Medicine, Department of Medicine, Northwestern University Feinberg School of Medicine, Chicago, IL, 60611.
Department of Anthropology, University of Utah, Salt Lake City, UT, 84112.
Am J Phys Anthropol. 2015 Aug;157(4):603-14. doi: 10.1002/ajpa.22750. Epub 2015 Apr 17.
All modern Iñupiaq speakers share a common origin, the result of a recent (∼800 YBP) and rapid trans-Arctic migration by the Neo-Eskimo Thule, who replaced the previous Paleo-Eskimo inhabitants of the region. Reduced mitochondrial haplogroup diversity in the eastern Arctic supports the archaeological hypothesis that the migration occurred in an eastward direction. We tested the hypothesis that the Alaskan North Slope served as the origin of the Neo- and Paleo-Eskimo populations further east.
We sequenced HVR I and HVR II of the mitochondrial D-loop from 151 individuals in eight Alaska North Slope communities, and compared genetic diversity and phylogenetic relationships between the North Slope Inupiat and other Arctic populations from Siberia, the Aleutian Islands, Canada, and Greenland.
Mitochondrial lineages from the North Slope villages had a low frequency (2%) of non-Arctic maternal admixture, and all haplogroups (A2, A2a, A2b, D2a, and D4b1a-formerly known as D3) found in previously sequenced Neo- and Paleo-Eskimos and living Inuit and Eskimo peoples from across the North American Arctic. Lineages basal for each haplogroup were present in the North Slope. We also found the first occurrence of two haplogroups in contemporary North American Arctic populations: D2a, previously identified only in Aleuts and Paleo-Eskimos, and the pan-American C4.
Our results yield insight into the maternal population history of the Alaskan North Slope and support the hypothesis that this region served as an ancestral pool for eastward movements to Canada and Greenland, for both the Paleo-Eskimo and Neo-Eskimo populations.
所有现代因纽皮阿特语使用者都有共同的起源,这是新爱斯基摩图勒人近期(约800年前)迅速跨北极迁移的结果,他们取代了该地区先前的古爱斯基摩居民。北极东部线粒体单倍群多样性的减少支持了迁移是向东发生的这一考古假说。我们检验了阿拉斯加北坡是更东部新爱斯基摩人和古爱斯基摩人群体起源地的假说。
我们对阿拉斯加北坡八个社区的151个人的线粒体D环高变区I和高变区II进行了测序,并比较了北坡因纽皮阿特人与来自西伯利亚、阿留申群岛、加拿大和格陵兰的其他北极人群之间的遗传多样性和系统发育关系。
北坡村庄的线粒体谱系中非北极母系混合的频率较低(2%),并且在先前测序的新爱斯基摩人和古爱斯基摩人以及来自北美北极地区的现存因纽特人和爱斯基摩人群体中发现的所有单倍群(A2、A2a、A2b、D2a和D4b1a,以前称为D3)都存在。每个单倍群的基部谱系都出现在北坡。我们还首次在当代北美北极人群体中发现了两个单倍群:D2a,以前仅在阿留申人和古爱斯基摩人中发现;以及泛美C4。
我们的结果深入了解了阿拉斯加北坡的母系群体历史,并支持了该地区是古爱斯基摩人和新爱斯基摩人群体向东迁移至加拿大和格陵兰的祖先库的假说。