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末次冰期期间多个避难所对红松(Pinus koraiensis)当前大陆种群的贡献。

Contributions of multiple refugia during the last glacial period to current mainland populations of Korean pine (Pinus koraiensis).

作者信息

Bao Lei, Kudureti Ayijiamali, Bai Weining, Chen Rongzhang, Wang Tianming, Wang Hongfang, Ge Jianping

机构信息

State Key Laboratory of Earth Surface Processes and Resource Ecology, Ministry of Education Key Laboratory for Biodiversity Science and Engineering &College of Life Sciences, Beijing Normal University, Beijing, China.

出版信息

Sci Rep. 2015 Dec 22;5:18608. doi: 10.1038/srep18608.

Abstract

The northern microrefugia that existed during the Last Glacial Maximum (LGM) are a key factor in the demographic history of species. Pinus koraiensis has a unique distribution in northeast Asia. The Changbai Mountains and the Korean peninsula (CM/KP) are usually considered to be the LGM refugia for P. koraiensis. However, the Xiaoxingan Range (XR), at the northern part of this species' distribution, is another possible refugium. We used chloroplast sequencing and ten nuclear single-copy gene loci to calculate the genetic diversity pattern of P. koraiensis. The probabilities of a single LGM refugium and of multiple LGM refugia were calculated based on approximate Bayesian computation. The effect of the latitudinal gradient on genetic diversity was not significant. However, unique alleles occurred at low frequencies in CM/KP and XR. A conservative estimate of the coalescence time between CM/KP and XR is 0.4 million years ago, a time prior to the LGM. Gene flow between CM/KP and XR was estimated to be more than one in per generation, an amount that may be sufficient to limit genetic divergence between the regions. Our study strongly supports the hypothesis that XR was another LGM refugium in addition to CM/KP.

摘要

末次盛冰期(LGM)期间存在的北方微避难所是物种种群历史的关键因素。红松在东北亚有着独特的分布。长白山和朝鲜半岛(CM/KP)通常被认为是红松的末次盛冰期避难所。然而,该物种分布区北部的小兴安岭(XR)是另一个可能的避难所。我们使用叶绿体测序和十个核单拷贝基因座来计算红松的遗传多样性模式。基于近似贝叶斯计算,计算了单一末次盛冰期避难所和多个末次盛冰期避难所的概率。纬度梯度对遗传多样性的影响不显著。然而,在CM/KP和XR中低频出现了独特的等位基因。CM/KP和XR之间合并时间的保守估计是40万年前,早于末次盛冰期。CM/KP和XR之间的基因流估计每代超过一次,这一数量可能足以限制区域间的遗传分化。我们的研究有力地支持了这样的假设,即除了CM/KP之外,XR也是另一个末次盛冰期避难所。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9df3/4686996/873ed171c217/srep18608-f1.jpg

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