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Phylogeographic patterns of the Aconitum nemorum species group (Ranunculaceae) shaped by geological and climatic events in the Tianshan Mountains and their surroundings

机译:天山及其周围地区地质和气候事件形成的乌头乌头种群(毛an科)的植物志格局

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摘要

To investigate the impacts of ancient geological and climatic events on the evolutionary history of the Aconitumiu nemorum species group, including A. nemorum s. str., A. karakolicum, and A. soongoricum; a total of 18 natural populations with 146 individuals were sampled, mainly from grassy slopes or the coniferous forest understory of the Tianshan Mountain Range and its surroundings. Two cpDNA intergenic spacer regions (trnS-trnG and psbA-trnH) were sequenced and 16 haplotypes were identified. These were clustered into three divergent lineages which almost entirely corresponded to the three species. Analysis of molecular variance indicated restricted gene flow, mainly among species. High levels of genetic distance were detected among eastern populations in A. nemorum s. str. and A. karakolicum from spatial genetic landscape analysis. Neutral tests and mismatch distribution analysis suggest that A. nemorum s. str. experienced demographic expansions during interglacial periods. Based on haplotype distribution and the median-joining network, it was inferred that this species underwent two periods of eastward expansion. Our molecular dating indicates that the lineages of the complex separated during the period of the late Tertiary to late Pleistocene (11.740.064iu million years ago), which was most likely triggered by recent rapid uplift of the Tianshan Mountains, while genetic variation at the intra-specific level might be attributed to climatic cycles in the late Quaternary.
机译:调查古代地质和气候事件的影响,对乌头nemorum物种组,包括A. nemorum s的进化历史。 str。,A。karakolicum和A. earlygoricum;共采样了18个自然种群,共146个个体,主要来自天山山脉及其周围地区的草坡或针叶林。对两个cpDNA基因间隔区(trnS-trnG和psbA-trnH)进行测序,鉴定出16个单倍型。这些被分为三个不同的血统,几乎完全对应于这三个物种。分子变异分析表明受限制的基因流动,主要在物种之间。在A. nemorum s的东部人群中发现了高水平的遗传距离。海峡和A. karakolicum的空间遗传景观分析。中性检验和错配分布分析提示羊草属。海峡在冰期之间经历了人口膨胀。根据单倍型分布和中间连接网络,推断该物种经历了两个向东扩展的时期。我们的分子测年表明,在第三纪晚期至更新世末期(11,740.064iu百万年前)期间,该复合体的谱系分离,这很可能是由于天山的近期快速隆升引起的,而内部的遗传变异特定水平可能归因于第四纪晚期的气候周期。

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