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Phylogeography of Orinus (Poaceae), a dominant grass genus on the Qinghai-Tibet Plateau

机译:orinus(poaceae),青藏高原的主要草属植物(Poaceae)

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To better understand the responses of arid-adapted, alpine plants to Quaternary climatic oscillations, we investigated the genetic variation and phylogeographic history of Orinus, an endemic genus of Poaceae comprising three species from the dry grasslands of the Qinghai-Tibet Plateau (QTP) in China. We measured the genetic variation of 476 individuals from 88 populations using three maternally inherited plastid DNA markers (matK, rbcL and psbA-trnH), the biparentally inherited nuclear ribosomal internal transcribed spacer (nrITS) and amplified fragment length polymorphisms (AFLPs). We found that the plastid DNA, nrITS and AFLPs show considerable, recent differentiation among the species. We detected 14 plastid haplotypes (H1-H14), of which only three were shared among all species, and 30 nrITS ribotypes (S1-S30), of which one (S10) was shared between two species, O. kokonoricus and O. intermedius, but absent in O. thoroldii. The nrITS types formed clades that were inconsistent with species boundaries. Based on these data, we propose and illustrate a complex hypothesis for the evolutionary history of Orinus involving lineage sorting and introgression, the latter of which may explain the shared S10 nrITS type. The AFLP results showed clades corresponding to current species delineation and suggest that lineage sorting in the genus is probably complete. We estimated the crown age of Orinus to be 2.85 (95% highest posterior density: 0.58-12.45) Mya (late Pliocene), and subsequent divergence occurred in the Quaternary. Early divergences were allopatric. More recently, Orinus probably underwent regional expansions corresponding to Quaternary climatic changes, especially glaciation, which is consistent with our divergence time estimates. These climatic changes could have facilitated the S10 event and other hybridization events. Our data also suggest that species of this small genus of grasses survived the Quaternary glacial period in the extremely adverse habitats of the QTP.
机译:为了更好地了解干旱适应的高山植物到第四季气候振荡的响应,我们研究了矿物质的遗传变异和神话史,矿石的地方性属,包括来自青藏高原(QTP)的干草原(QTP)的三种物种中国。通过使用三种母生遗传血管DNA标记物(MATK,RBCL和PSBA-TNH),分脂性脑膜核糖体内转录的间隔件(NRITS)和扩增的片段长度多态性(AFLP)测量了来自88个群体的476个体群体的遗传变异。我们发现塑性DNA,NRITS和AFLP显示了该物种的相当大的,最近的分化。我们检测到14个体积单倍型(H1-H14),其中只有三种在所有物种中共用,并且30个NRITS核糖型(S1-S30),其中一个(S10)在两个物种,O.Kokonicus和O.中学,但在O. Thoroldii中缺席。 NRITS类型形成与物种边界不一致的片状。基于这些数据,我们提出并说明了涉及谱系分类和迟发的orinus进化历史的复杂假设,其后者可以解释共享的S10 nrits类型。 AFLP结果表明,与当前物种描绘相对应的片状,并表明属属中的谱系分类可能完成。我们估计orinus的皇冠年龄为2.85(最高后密度:0.58-12.45)mya(晚期全烯),随后发生在第四纪的发散。早期分歧都是疾病。最近,奥林斯可能经历了对应于第四纪气候变化的区域扩张,特别是冰川,这与我们的分歧时间估计一致。这些气候变化可以促进S10事件和其他杂交事件。我们的数据还表明,这种小属的草地的种类在QTP的极其不利栖息地中幸存下季节冰川。

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