Area de Antropología, Facultad de Biología, Universidad de Santiago de Compostela, Campus Sur s/n, 15782, Santiago de Compostela, Spain.
BIOMICs Research Group, Dpto. Z. y Biologia Celular A., Lascaray Research Centre, University of the Basque Country, UPV/EHU, Vitoria-Gasteiz, Spain.
Sci Rep. 2023 Jan 23;13(1):1268. doi: 10.1038/s41598-023-28384-8.
It is thought that Paleo-Inuit were the first people that settled the American Arctic about 5000 BP (before the present) from a migration that crossed Beringia from Northeast Asia. It is theorized that this group initially migrated to the North Slopes of Alaska and subsequently expanded eastward, eventually reaching Greenland. A second circumpolar dispersal of Neo-Inuit from the North Slopes associated with the Thule-Inuk culture has been postulated to have extended eastward around 800 BP, totally replacing the original Paleo-Inuit without admixing. Although generally accepted, this migration scenario is incompatible with previously reported indications of east to west gene flow across the American Arctic. Here we report on the Y-chromosome haplogroup and Y-STR diversity of the four circumpolar populations of the Tuva Republic (N = 24), Northeast Siberia (N = 9), Bethel, Alaska (N = 40), and Barrow, Alaska (N = 31). Four haplogroup lineages (Q-NWT01, Q-M3, Q-M346, and Q-M120) were detected, Q-NWT01 and Q-M3 being the most abundant at 11.11 and 66.67% in Northeast Siberia, 32.50 and 65.00% in Bethel, and 67.74 and 32.26% in Barrow, respectively. The same samples genotyped for Y-chromosome SNPs were typed for 17 Y-STYR loci using the AmpFlSTR Yfiler system. Age estimates and diversity values for the Q-NWT01 and Q-M3 mutations suggest extensive movement of male individuals along the entire longitudinal stretch of the American circumpolar region. Throughout the entire region, Q-M3 exhibits a west to east decreasing gradient in age and diversity while Q-NWT01 indicates the opposite with older TMRCA and higher diversity values running from east to west with the most recent estimates in Canada and Alaska. The high age and diversity values in Greenland are congruent with an origin of the Q-NWT01 mutation in the east of the circumpolar range about 2000-3000 ya. This scenario is incompatible with a complete biological replacement starting about 700 BP of Paleo-Inuit like the Dorset by the Thule-Inuit (Neo-Inuit), as is currently thought, and more parsimonious with gene flow carrying the NWT01 mutation from a pre-Thule population to the ancestors of the present-day Inuit.
据推测,大约在 5000 年前(即现在之前),古因纽特人从东北亚穿越白令海峡迁徙到美洲北极地区,成为第一批在此定居的人。据推测,这群人最初迁徙到阿拉斯加北坡,然后向东扩张,最终到达格陵兰岛。另一个与图勒因纽特文化相关的新因纽特人在北坡的环极扩散,据推测在 800 年前向东延伸,完全取代了没有混合的原始古因纽特人。尽管这种迁徙情景已被普遍接受,但它与之前报道的横跨美洲北极地区的东西向基因流的指示不符。在这里,我们报告了图瓦共和国(N=24)、东北西伯利亚(N=9)、贝塞尔(N=40)和巴罗(N=31)这四个环极人群的 Y 染色体单倍群和 Y-STR 多样性。检测到四个单倍群谱系(Q-NWT01、Q-M3、Q-M346 和 Q-M120),在东北西伯利亚,Q-NWT01 和 Q-M3 的丰度最高,分别为 11.11%和 66.67%;在贝塞尔,分别为 32.50%和 65.00%;在巴罗,分别为 67.74%和 32.26%。用 AmpFlSTR Yfiler 系统对同一批 Y 染色体 SNP 进行基因分型的样本,对 17 个 Y-STR 位点进行了基因分型。Q-NWT01 和 Q-M3 突变的年龄估计和多样性值表明,男性个体沿着美洲环极地区的整个纵向区域进行了大量迁移。在整个地区,Q-M3 表现出从西向东的年龄和多样性递减梯度,而 Q-NWT01 则相反,其 TMRCA 较老,多样性值从东向西增加,在加拿大和阿拉斯加的最新估计中达到最大值。格陵兰岛的高年龄和高多样性值与 Q-NWT01 突变的起源相一致,该突变起源于环极地区的东部,约在 2000-3000 年前。这种情况与目前认为的大约 700 年前由图勒因纽特人(新因纽特人)完全取代古因纽特人(如多塞特人)的情况不一致,更合理的情况是,带有 NWT01 突变的基因流从图勒前的种群携带到当今因纽特人的祖先那里。