Department of Anthropology, University of Kansas, Lawrence, Kansas.
UIC Science LLC, Barrow, Alaska.
Am J Phys Anthropol. 2019 Feb;168(2):303-317. doi: 10.1002/ajpa.23746.
The North American archaeological record supports a Holocene origin of Arctic Indigenous peoples. Although the Paleo-Inuit were present for millennia, archaeological and genetic studies suggest that modern peoples descend from a second, more recent tradition known as the Neo-Inuit. Origins of the Neo-Inuit and their relations to the earlier and later Indigenous peoples are an area of active study. Here, we genetically analyze the maternal lineages present at Nuvuk, once the northernmost community in Alaska and located in a region identified as a possible origin point of the Neo-Inuit Thule. The cemetery at Nuvuk contains human remains representing a nearly one thousand year uninterrupted occupation from early Thule to post-contact Iñupiat.
We selected 44 individuals from Nuvuk with calibrated dates between 981 AD and 1885 AD for molecular analysis. We amplified and sequenced the hypervariable segment I of the mitogenome. We compared the Nuvuk data with previously published sequences from 68 modern and ancient communities from across Asia and North America. Phylogeographic analyses suggest possible scenarios of Holocene Arctic and sub-Arctic population movements.
We successfully retrieved sequence data from 39 individuals. Haplogroup frequencies in Nuvuk were typed as 66.7% A2b1, 25.6% A2a, and 7.7% D4b1a2a1a. These results suggest that the population at Nuvuk was closest to the ancient Thule and modern Inuit of Canada, and to the Siberian Naukan people. We confirm that haplogroups A2a, A2b1, D2a, and D4b1a2a1a appear at high frequency in Arctic and sub-Arctic populations of North America and Chukotka. Sister clades D2b and D4b1a2a1b are present in Asian and Eastern European populations.
The ancient mitochondrial sequences from Nuvuk confirm the link between the North Slope and the Thule who later spread east, and the maternal discontinuity between the Neo-Inuit and Paleo-Inuit. We suggest haplogroups A2a, A2b, and D4b1a2a1a are linked to the ancestors of the Thule in eastern Beringia, whereas the D2 and D4b1a2a1 clades appear to have Asian Holocene origins. Further Siberian and Alaskan genomes are necessary to clarify these population migrations beyond a simple two-wave scenario of Neo-Inuit and Paleo-Inuit.
北美考古记录支持全新世时期北极地区的土著人民起源。尽管古因纽特人已经存在了数千年,但考古学和遗传学研究表明,现代人类是来自第二个更近期的传统,即新因纽特人。新因纽特人的起源及其与更早和更晚的土著人民的关系是一个活跃的研究领域。在这里,我们从努武克进行了母系血统的基因分析,努武克曾是阿拉斯加最北部的社区,位于被认为是新因纽特人图勒的可能起源地的一个地区。努武克的墓地中有人类遗骸,代表了从早期图勒到接触后因纽特人近 1000 年的不间断居住。
我们选择了 44 名来自努武克的个体,其校准日期在公元 981 年至 1885 年之间进行分子分析。我们扩增并测序了线粒体基因组的高变区 I。我们将努武克的数据与来自亚洲和北美的 68 个现代和古代社区的先前公布的序列进行了比较。系统地理学分析表明,全新世北极和亚北极地区人口迁移的可能情景。
我们成功地从 39 个人中检索到了序列数据。努武克的单倍群频率被分为 66.7% A2b1、25.6% A2a 和 7.7% D4b1a2a1a。这些结果表明,努武克的人口与古代图勒和现代加拿大因纽特人以及西伯利亚的 Naukan 人最为接近。我们确认 A2a、A2b1、D2a 和 D4b1a2a1a 等单倍群在北美和楚科奇的北极和亚北极地区的人口中出现频率较高。姐妹枝系 D2b 和 D4b1a2a1b 存在于亚洲和东欧人口中。
努武克的古老线粒体序列证实了北坡与后来向东传播的图勒之间的联系,以及新因纽特人和古因纽特人之间的母系连续性。我们认为 A2a、A2b 和 D4b1a2a1a 等单倍群与东部白令海峡的图勒祖先有关,而 D2 和 D4b1a2a1 枝系似乎具有全新世的亚洲起源。需要进一步的西伯利亚和阿拉斯加基因组来澄清这些人口迁移,而不仅仅是新因纽特人和古因纽特人的简单两波情景。