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Ancient Solomon Islands mtDNA: assessing Holocene settlement and the impact of European contact

机译:所罗门群岛古代mtDNA:评估全新世定居和欧洲接触的影响

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Archaeologists, linguists and geneticists generally agree that Near Oceania was subject to two major pulses of human dispersal: a Pleistocene occupation around 40,000 BP and a Late-Holocene migration at 3500 BP commonly associated with the Austronesian expansion out of Taiwan. The latter led to the development of the Lapita cultural complex in the Bismarck Archipelago which resulted in the settlement of Remote Oceania and there are a variety of competing models (express train, slow boat, entangled bank, etc.) used to explain this. Recent genetic studies have focused on this issue, but none of them have taken into consideration the bias possibly introduced by 19th-century historically reported population decline caused by European contact. In this paper we present a case study to test the effect of 19th-20th century colonial impact on the mitochondrial DNA diversity of Solomon Islanders and to investigate the complex stratigraphy of settlement in this archipelago during and after the Lapita period. We extracted DNA from hairs and teeth belonging to 21 individuals collected by the Somerville expedition during the late 19th-century, and typed them for mitochondrial DNA (mtDNA) hypervariable region I (HVS-I) and the intergenic COII/tRNALys 9-base pair deletion (9 bp-del). Comparison of these genetic data with those available from the modern Solomon Islanders and Southeast Asian and Oceanic populations conflicts with the hypothesis of drastic changes in Solomon maternal genepool diversity, indicating that the last century putative bottleneck is not detectable through our genetic data. In addition, the ancient and modern Solomon haplogroup distribution (e.g. M27 haplogroup) suggests, in agreement with some archaeological and linguistic models, that Early Lapita populations expanding out of the Bismarck Archipelago had little or no contact with indigenous non-Austronesian populations in Bougainville and the Solomon Islands. This finding indicates smaller scale analyses reveal a more complex reality of genetic admixture in some parts of Oceania than is often assumed in current debates.
机译:考古学家,语言学家和遗传学家普遍认为,近大洋洲受人类散布的两个主要推动力:更新世占领约40,000 BP和晚全新世在3500 BP迁移,这通常与南岛从台湾的扩张有关。后者导致了the斯麦群岛拉皮塔(Lapita)文化综合体的发展,从而导致了偏远大洋洲的定居,并且有各种各样的竞争模式(快车,慢船,纠结的银行等)来解释这一点。最近的遗传研究集中在这个问题上,但是它们都没有考虑到19世纪历史上报道的欧洲接触人口减少所引起的偏见。在本文中,我们提供了一个案例研究,以测试19-20世纪殖民地影响对所罗门群岛居民线粒体DNA多样性的影响,并调查拉皮塔时期及其后该群岛的复杂地层学。我们从19世纪末萨默维尔(Somerville)探险队收集的21个人的头发和牙齿中提取了DNA,并为线粒体DNA(mtDNA)高变区I(HVS-I)和基因间COII / tRNALys 9碱基对进行了分类。缺失(9bp-del)。将这些遗传数据与现代所罗门群岛人以及东南亚和海洋人口获得的数据进行比较,与所罗门产妇基因库多样性发生急剧变化的假说相矛盾,这表明通过我们的遗传数据无法检测到上个世纪的假定瓶颈。此外,古代和现代的所罗门单倍群分布(例如M27单倍群)表明,与某些考古和语言模型相一致,从La斯麦群岛扩展而来的早期Lapita种群与布干维尔和布干维尔的非南岛土著种群几乎没有接触。所罗门群岛。这一发现表明,与目前的辩论相比,较小规模的分析揭示了大洋洲某些地区的遗传混合现实。

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