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Climate change underlies global demographic genetic and cultural transitions in pre-Columbian southern Peru

机译:气候变化是秘鲁前哥伦布时期南部南部全球人口遗传和文化转型的基础

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摘要

Several archaeological studies in the Central Andes have pointed at the temporal coincidence of climatic fluctuations (both long- and short-term) and episodes of cultural transition and changes of socioeconomic structures throughout the pre-Columbian period. Although most scholars explain the connection between environmental and cultural changes by the impact of climatic alterations on the capacities of the ecosystems inhabited by pre-Columbian cultures, direct evidence for assumed demographic consequences is missing so far. In this study, we address directly the impact of climatic changes on the spatial population dynamics of the Central Andes. We use a large dataset of pre-Columbian mitochondrial DNA sequences from the northern Rio Grande de Nasca drainage (RGND) in southern Peru, dating from ∼840 BC to 1450 AD. Alternative demographic scenarios are tested using Bayesian serial coalescent simulations in an approximate Bayesian computational framework. Our results indicate migrations from the lower coastal valleys of southern Peru into the Andean highlands coincident with increasing climate variability at the end of the Nasca culture at ∼640 AD. We also find support for a back-migration from the highlands to the coast coincident with droughts in the southeastern Andean highlands and improvement of climatic conditions on the coast after the decline of the Wari and Tiwanaku empires (∼1200 AD), leading to a genetic homogenization in the RGND and probably southern Peru as a whole.
机译:安第斯中部地区的一些考古研究指出,在整个哥伦布时期之前,气候波动(长期和短期)的时间重合,文化过渡和社会经济结构的变化都在发生。尽管大多数学者通过气候变化对哥伦布前文化所居住的生态系统的能力的影响来解释环境与文化变化之间的联系,但到目前为止,尚缺乏假定的人口后果的直接证据。在这项研究中,我们直接解决了气候变化对安第斯中部空间人口动态的影响。我们使用了秘鲁南部里奥格兰德纳斯卡河北部排水区(RGND)的大量哥伦比亚前线粒体DNA序列,其历史可追溯至公元前840年至1450年。在近似的贝叶斯计算框架中,使用贝叶斯串行合并模拟来测试其他人口统计方案。我们的结果表明,从秘鲁南部较低的沿海山谷向安第斯山脉的高地迁移与公元640年左右的纳斯卡(Nasca)文化结束时的气候变异性增加是同时发生的。我们还发现,在瓦里帝国和蒂瓦纳库帝国衰落(公元1200年左右)之后,伴随着安第斯东南部东南高地的干旱以及沿海气候条件的改善,人们从高地向沿海地区回迁, RGND甚至整个秘鲁南部地区均质化。

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