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线粒体 DNA 单倍群 L3 在非洲内部和外部的扩张。

The Expansion of mtDNA Haplogroup L3 within and out of Africa.

机构信息

IPATIMUP (Instituto de Patologia e Imunologia Molecular da Universidade do Porto), Porto, Portugal.

出版信息

Mol Biol Evol. 2012 Mar;29(3):915-27. doi: 10.1093/molbev/msr245. Epub 2011 Nov 16.

Abstract

Although fossil remains show that anatomically modern humans dispersed out of Africa into the Near East ∼100 to 130 ka, genetic evidence from extant populations has suggested that non-Africans descend primarily from a single successful later migration. Within the human mitochondrial DNA (mtDNA) tree, haplogroup L3 encompasses not only many sub-Saharan Africans but also all ancient non-African lineages, and its age therefore provides an upper bound for the dispersal out of Africa. An analysis of 369 complete African L3 sequences places this maximum at ∼70 ka, virtually ruling out a successful exit before 74 ka, the date of the Toba volcanic supereruption in Sumatra. The similarity of the age of L3 to its two non-African daughter haplogroups, M and N, suggests that the same process was likely responsible for both the L3 expansion in Eastern Africa and the dispersal of a small group of modern humans out of Africa to settle the rest of the world. The timing of the expansion of L3 suggests a link to improved climatic conditions after ∼70 ka in Eastern and Central Africa rather than to symbolically mediated behavior, which evidently arose considerably earlier. The L3 mtDNA pool within Africa suggests a migration from Eastern Africa to Central Africa ∼60 to 35 ka and major migrations in the immediate postglacial again linked to climate. The largest population size increase seen in the L3 data is 3-4 ka in Central Africa, corresponding to Bantu expansions, leading diverse L3 lineages to spread into Eastern and Southern Africa in the last 3-2 ka.

摘要

虽然化石遗迹表明,解剖学上的现代人类大约在 10 万至 13 万年前从非洲扩散到近东地区,但来自现存人群的遗传证据表明,非非洲人主要来自一次成功的后期迁徙。在人类线粒体 DNA(mtDNA)树中,L3 单倍群不仅包含许多撒哈拉以南非洲人,还包含所有古代非非洲谱系,因此其年龄为非洲以外的扩散提供了一个上限。对 369 个完整的非洲 L3 序列的分析将这个最大值定在大约 7 万年前,几乎排除了在 74000 年前成功离开的可能性,即苏门答腊多巴火山超级喷发的日期。L3 的年龄与其两个非非洲子单倍群 M 和 N 的相似性表明,同样的过程可能导致了 L3 在东非的扩张以及一小群现代人离开非洲散布到世界其他地方。L3 的扩张时间表明,大约在 7 万年前,东非和中非的气候条件有所改善,而不是与象征性的行为有关,这种行为显然发生得更早。非洲内部的 L3 mtDNA 池表明,大约在 6 万至 3.5 万年前从东非向中非发生了一次迁徙,而在冰期后的立即迁徙再次与气候有关。在 L3 数据中看到的最大人口增长是中非的 3-4 千年前,与班图扩张相对应,导致不同的 L3 谱系在过去 3-2 千年前传播到东非和南非。

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