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黎凡特旧石器时代晚期早期在非洲的线粒体DNA遗产。

The mtDNA legacy of the Levantine early Upper Palaeolithic in Africa.

作者信息

Olivieri Anna, Achilli Alessandro, Pala Maria, Battaglia Vincenza, Fornarino Simona, Al-Zahery Nadia, Scozzari Rosaria, Cruciani Fulvio, Behar Doron M, Dugoujon Jean-Michel, Coudray Clotilde, Santachiara-Benerecetti A Silvana, Semino Ornella, Bandelt Hans-Jürgen, Torroni Antonio

机构信息

Dipartimento di Genetica e Microbiologia, Università di Pavia, Via Ferrata 1, 27100 Pavia, Italy.

出版信息

Science. 2006 Dec 15;314(5806):1767-70. doi: 10.1126/science.1135566.

Abstract

Sequencing of 81 entire human mitochondrial DNAs (mtDNAs) belonging to haplogroups M1 and U6 reveals that these predominantly North African clades arose in southwestern Asia and moved together to Africa about 40,000 to 45,000 years ago. Their arrival temporally overlaps with the event(s) that led to the peopling of Europe by modern humans and was most likely the result of the same change in climate conditions that allowed humans to enter the Levant, opening the way to the colonization of both Europe and North Africa. Thus, the early Upper Palaeolithic population(s) carrying M1 and U6 did not return to Africa along the southern coastal route of the "out of Africa" exit, but from the Mediterranean area; and the North African Dabban and European Aurignacian industries derived from a common Levantine source.

摘要

对属于单倍群M1和U6的81条完整人类线粒体DNA(mtDNA)进行测序后发现,这些主要分布在北非的分支起源于亚洲西南部,并在约4万至4.5万年前一起迁移至非洲。它们的到来在时间上与现代人类进入欧洲的事件重叠,很可能是由于气候条件发生了同样的变化,使得人类得以进入黎凡特地区,为欧洲和北非的殖民开辟了道路。因此,携带M1和U6的早期旧石器时代晚期人群并非沿着“走出非洲”路线的南部沿海返回非洲,而是从地中海地区返回;北非的达班文化和欧洲的奥瑞纳文化都源自黎凡特地区的同一个源头。

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