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晚更新世小型仓鼠在古北界的扩张与过去环境变化的关系。

Late Pleistocene Expansion of Small Murid Rodents across the Palearctic in Relation to the Past Environmental Changes.

机构信息

Department of Genetics, Wrocław University of Environmental and Life Sciences, Kożuchowska 7, 51-631 Wrocław, Poland.

BIOCEV Group, Department of Zoology, Faculty of Science, Charles University, Viničná 7, 128 44 Prague, Czech Republic.

出版信息

Genes (Basel). 2021 Apr 26;12(5):642. doi: 10.3390/genes12050642.

Abstract

We investigated the evolutionary history of the striped field mouse to identify factors that initiated its past demographic changes and to shed light on the causes of its current genetic structure and trans-Eurasian distribution. We sequenced mitochondrial cyt b from 184 individuals, obtained from 35 sites in central Europe and eastern Mongolia. We compared genetic analyses with previously published historical distribution models and data on environmental and climatic changes. The past demographic changes displayed similar population trends in the case of recently expanded clades C1 and C3, with the glacial (MIS 3-4) expansion and postglacial bottleneck preceding the recent expansion initiated in the late Holocene and were related to environmental changes during the upper Pleistocene and Holocene. The past demographic trends of the eastern Asian clade C3 were correlated with changes in sea level and the formation of new land bridges formed by the exposed sea shelf during the glaciations. These data were supported by reconstructed historical distribution models. The results of our genetic analyses, supported by the reconstruction of the historical spatial distributions of the distinct clades, confirm that over time the local populations mixed as a consequence of environmental and climatic changes resulting from cyclical glaciation and the interglacial period during the Pleistocene.

摘要

我们研究了条纹田鼠的进化历史,以确定引发其过去种群变化的因素,并阐明其当前遗传结构和跨欧亚分布的原因。我们从中欧和蒙古东部的 35 个地点采集了 184 只个体的线粒体 cyt b 进行测序。我们将遗传分析与先前发表的历史分布模型和环境及气候变化数据进行了比较。最近扩张的支系 C1 和 C3 的过去种群变化显示出相似的趋势,冰川(MIS 3-4)扩张和冰后期瓶颈发生在全新世晚期的最近扩张之前,与上新世和全新世的环境变化有关。东亚支系 C3 的过去种群变化与海平面变化以及冰川期间暴露的海架形成的新陆桥的形成有关。这些数据得到了重建的历史分布模型的支持。我们的遗传分析结果以及不同支系历史空间分布的重建都证实,随着时间的推移,当地种群由于冰期和间冰期的循环引起的环境和气候变化而混合。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/cfe9/8145813/e3aedbe75385/genes-12-00642-g001.jpg

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