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分子标记为广泛分布的钙质草原物种小地榆从南部和隐秘的北部避难所进行广泛前沿重新定殖提供了证据。

Molecular markers provide evidence for a broad-fronted recolonisation of the widespread calcareous grassland species Sanguisorba minor from southern and cryptic northern refugia.

作者信息

Tausch S, Leipold M, Poschlod P, Reisch C

机构信息

University of Regensburg, Institute of Plant Sciences, Regensburg, Germany.

出版信息

Plant Biol (Stuttg). 2017 Jul;19(4):562-570. doi: 10.1111/plb.12570. Epub 2017 May 2.

Abstract

Calcareous grasslands belong to the most species-rich and endangered habitats in Europe. However, little is known about the origin of the species typically occurring in these grasslands. In this study we analysed the glacial and post-glacial history of Sanguisorba minor, a typical plant species frequently occurring in calcareous grasslands. The study comprised 38 populations throughout the whole distribution range of the species across Europe. We used molecular markers (AFLP) and applied Bayesian cluster analysis as well as spatial principal components analysis (sPCA) to identify glacial refugia and post-glacial migration routes to Central Europe. Our study revealed significant differences in the level of genetic variation and the occurrence of rare fragments within populations of S. minor and a distinct separation of eastern and western lineages. The analyses uncovered traditional southern but also cryptic northern refugia and point towards a broad fronted post-glacial recolonisation. Based on these results we postulate that incomplete lineage sorting may have contributed to the detected pattern of genetic variation and that S. minor recolonised Central Europe post-glacially from Iberia and northern glacial refugia in France, Belgium or Germany. Our results highlight the importance of refugial areas for the conservation of intraspecific variation in calcareous grassland species.

摘要

钙质草原是欧洲物种最为丰富且濒危的栖息地之一。然而,对于这些草原中常见物种的起源却知之甚少。在本研究中,我们分析了小地榆(Sanguisorba minor)的冰川期和冰后期历史,小地榆是钙质草原中常见的典型植物物种。该研究涵盖了该物种在欧洲整个分布范围内的38个种群。我们使用分子标记(AFLP),并应用贝叶斯聚类分析以及空间主成分分析(sPCA)来确定冰川避难所和冰后期向中欧的迁移路线。我们的研究揭示了小地榆种群在遗传变异水平和稀有片段出现情况上的显著差异,以及东部和西部谱系的明显分离。分析发现了传统的南部避难所,也发现了隐秘的北部避难所,并表明冰后期重新定殖是从广阔前沿开始的。基于这些结果,我们推测不完全的谱系分选可能导致了所检测到的遗传变异模式,并且小地榆在冰后期从伊比利亚以及法国、比利时或德国的北部冰川避难所向中欧重新定殖。我们的结果凸显了避难区域对于保护钙质草原物种种内变异的重要性。

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