首页> 外文期刊>Journal of Neurochemistry: Offical Journal of the International Society for Neurochemistry >Prevalence gradients of Friedreich's Ataxia and R1b haplotype in Europe co-localize, suggesting a common Palaeolithic origin in the Franco-Cantabrian ice age refuge
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Prevalence gradients of Friedreich's Ataxia and R1b haplotype in Europe co-localize, suggesting a common Palaeolithic origin in the Franco-Cantabrian ice age refuge

机译:欧洲弗里德里希共济失调和R1b单倍体的患病率梯度共存,表明弗朗哥-坎塔布连冰期避难所是一个常见的旧石器时代起源

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摘要

Combining data from epidemiological studies in Friedreich's Ataxia (FRDA) and patient organization membership lists, shows that FRDA prevalence exhibits large regional differences in Europe with a prevalence gradient from west to east. Highest levels are observed in northern Spain, south of France and Ireland, lowest levels in Scandinavia and Russia. The observed distribution of FRDA in Europe co-localizes with the gradient of the chromosomal R1b marker as detected within west Europe. This gradient is either derived from Palaeolithic migrations out of the Franco-Cantabrian Ice age refuge or from Neolithic migrations entering west Europe with the advance of agriculture. FRDA prevalence may have been increased in this population anytime after its separation from the closely related R1a carrying group. East European populations with a high frequency of the R1a marker show 10 fold lower prevalence of FRDA, indicating that the FRDA mutation was present in the common ancestor and was increased in the R1b carrying group. The FRDA carrying population went through a Palaeolithic population bottleneck supporting the view that the observed FRDA distribution and potentially the R1b distribution are derived from Palaeolithic migrations out of the Franco-Cantabrian ice age refuge.
机译:结合弗里德赖希共济失调(FRDA)和患者组织成员名单中的流行病学研究数据,发现FRDA患病率在欧洲表现出较大的地区差异,患病率从西向东倾斜。西班牙北部,法国和爱尔兰南部观察到最高水平,斯堪的纳维亚和俄罗斯观察到最低水平。在欧洲观察到的FRDA分布与在西欧发现的染色体R1b标记的梯度共定位。这种梯度要么来自弗朗哥-坎塔布连冰期避难所的旧石器时代迁徙,要么源自随着农业发展而进入西欧的新石器时代迁徙。与密切相关的R1a携带者分离后,该人群中的FRDA患病率可能随时增加。 R1a标记频率较高的东欧人群显示FRDA的患病率低10倍,这表明FRDA突变存在于共同祖先中,并在R1b携带组中增加。携带FRDA的人口经历了旧石器时代的人口瓶颈,这支持了以下观点:观察到的FRDA分布以及可能的R1b分布是从旧石器时代从佛朗哥-坎塔布连冰期避难所迁出的。

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