Izagirre N, de la Rúa C
Euskal Herriko Unibertsitatea, Animali Biologia eta Genetika Saila, Zientzi Fakultatea, Bilbao, Spain.
Am J Hum Genet. 1999 Jul;65(1):199-207. doi: 10.1086/302442.
mtDNA sequence variation was studied in 121 dental samples from four Basque prehistoric sites, by high-resolution RFLP analysis. The results of this study are corroborated by (1) parallel analysis of 92 bone samples, (2) the use of controls during extraction and amplification, and (3) typing by both positive and negative restriction of the linked sites that characterize each haplogroup. The absence of haplogroup V in the prehistoric samples analyzed conflicts with the hypothesis proposed by Torroni et al., in which haplogroup V is considered as an mtDNA marker for a major Paleolithic population expansion from southwestern Europe, occurring approximately 10,000-15,000 years before the present (YBP). Our samples from the Basque Country provide a valuable tool for checking the previous hypothesis, which is based on genetic data from present-day populations. In light of the available data, the most realistic scenario to explain the origin and distribution of haplogroup V suggests that the mutation defining that haplogroup (4577 NlaIII) appeared at a time when the effective population size was small enough to allow genetic drift to act-and that such drift is responsible for the heterogeneity observed in Basques, with regard to the frequency of haplogroup V (0%-20%). This is compatible with the attributed date for the origin of that mutation (10,000-15, 000 YBP), because during the postglacial period (the Mesolithic, approximately 11,000 YBP) there was a major demographic change in the Basque Country, which minimized the effect of genetic drift. This interpretation does not rely on migratory movements to explain the distribution of haplogroup V in present-day Indo-European populations.
通过高分辨率限制性片段长度多态性(RFLP)分析,对来自四个巴斯克史前遗址的121个牙齿样本的线粒体DNA(mtDNA)序列变异进行了研究。这项研究的结果得到了以下几点的证实:(1)对92个骨骼样本进行的平行分析;(2)在提取和扩增过程中使用对照;(3)通过对表征每个单倍群的连锁位点进行正向和负向限制分型。在所分析的史前样本中没有单倍群V,这与托罗尼等人提出的假设相矛盾,在该假设中,单倍群V被认为是旧石器时代主要人口从欧洲西南部扩张的线粒体DNA标记,大约发生在距今10000 - 15000年前(YBP)。我们从巴斯克地区采集的样本为检验基于现代人群遗传数据的先前假设提供了一个有价值的工具。根据现有数据,解释单倍群V起源和分布的最现实情况表明,定义该单倍群的突变(4577 NlaIII)出现在有效种群规模足够小以至于允许遗传漂变起作用的时候,并且这种漂变是导致巴斯克人群中观察到的单倍群V频率(0% - 20%)异质性的原因。这与该突变起源的归因日期(10000 - 15000 YBP)相符,因为在冰后期(中石器时代,大约11000 YBP),巴斯克地区发生了重大的人口变化,这使遗传漂变的影响最小化。这种解释不依赖于迁徙运动来解释单倍群V在当今印欧语系人群中的分布。