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喜马拉雅山从青藏高原东南部的植物再殖民化:地理隔离导致种群高度分化。

Plant recolonization in the Himalaya from the southeastern Qinghai-Tibetan Plateau: Geographical isolation contributed to high population differentiation.

机构信息

State Key Laboratory of Systematic and Evolutionary Botany, Institute of Botany, The Chinese Academy of Sciences, Beijing 100093, China.

出版信息

Mol Phylogenet Evol. 2010 Sep;56(3):972-82. doi: 10.1016/j.ympev.2010.05.007. Epub 2010 May 21.

Abstract

The Himalaya-Hengduan Mountains region (HHM) in the southern and southeastern Qinghai-Tibetan Plateau (QTP) is considered an important reservoir and a differentiation center for temperate and alpine plants in the Cenozoic. To reveal how plants responded to the Quaternary climatic oscillations in the QTP, the phylogeographical histories of a few subalpine and alpine plants have been investigated, but nearly all studies used only uniparentally inherited cytoplasmic DNA markers, and only a couple of them included sampling from the Himalaya. In this study, range-wide genetic variation of the Himalayan hemlock (Tsuga dumosa), an important forest species in the HHM, was surveyed using DNA markers from three genomes. All markers revealed genetic depauperation in the Himalaya and richness in the Hengduan Mountains populations. Surprisingly, population differentiation of this wind-pollinated conifer is very high in all three genomes, with few common and many private nuclear gene alleles. These results, together with fossil evidence, clearly indicate that T. dumosa recolonized the Himalaya from the Hengduan Mountains before the Last Glacial Maximum (LGM), accompanied with strong founder effects, and the influence of the earlier glaciations on demographic histories of the QTP plants could be much stronger than that of the LGM. The strong population differentiation in T. dumosa could be attributed to restricted gene flow caused by the complicated topography in the HHM that formed during the uplift of the QTP, and thus sheds lights on the importance of geographical isolation in the development of high plant species diversity in this biodiversity hotspot.

摘要

横断山脉(HHM)位于青藏高原(QTP)的南部和东南部,被认为是新生代温带和高山植物的重要库和分化中心。为了揭示青藏高原第四纪气候振荡中植物的响应方式,已经研究了一些亚高山和高山植物的系统地理学历史,但几乎所有研究都仅使用单亲遗传的细胞质 DNA 标记,而且只有少数研究包括喜马拉雅山的采样。在这项研究中,使用来自三个基因组的 DNA 标记调查了喜马拉雅铁杉(Tsuga dumosa)的广泛遗传变异,喜马拉雅铁杉是 HHM 中的一种重要森林物种。所有标记均显示喜马拉雅地区的遗传枯竭和横断山脉种群的丰富。令人惊讶的是,这种风媒传粉针叶树在所有三个基因组中的种群分化都非常高,只有少数常见的和许多私人的核基因等位基因。这些结果与化石证据一起清楚地表明,Tsuga dumosa 在末次冰盛期(LGM)之前从横断山脉重新殖民喜马拉雅山脉,伴随着强烈的奠基者效应,早期冰川对青藏高原植物的种群历史的影响可能比 LGM 强得多。Tsuga dumosa 中强烈的种群分化可能归因于青藏高原抬升期间形成的 HHM 复杂地形导致的基因流受限,这表明地理隔离在这个生物多样性热点地区高山物种多样性的发展中的重要性。

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