Zhang Dong-Ru, Hui Hong, Yu Guo-Hua, Song Xin-Qiang, Liu Shuo, Yuan Si-Qi, Xiao Heng, Rao Ding-Qi
College of Life Sciences Yunnan University Kunming China.
State Key Laboratory of Genetic Resources and Evolution Kunming Institute of Zoology Chinese Academy of Sciences Kunming China.
Ecol Evol. 2020 Jan 18;10(3):1567-1580. doi: 10.1002/ece3.6011. eCollection 2020 Feb.
With the late Cenozoic uplift of the Qinghai-Tibetan Plateau (QTP), drainage of the southeastern edge of the QTP changed significantly. However, the impact of this dramatic change on the geographical distribution and genetic diversity of endemic organisms is still poorly understood. Here, we examined the geographical patterns of genetic variation in the Yunnan small narrow-mouthed frog, (Microhylidae), and two alternative hypotheses were tested: That is, the geographical distribution of genetic variation was determined by either the contemporary drainage basin or historical drainage basins.
The Mountains of southwest China.
Analyses were based on 417 specimens collected from across the distribution of the species. We reconstructed the genealogy (Bayesian and maximum parsimony methods) and assessed demographic history based on DNA sequencing data from mitochondrial and nuclear markers. We also mapped the genetic diversity and estimated the divergence times by a relaxed clock model.
The species has maintained a relatively stable population size without recent population expansion. Four major maternal lineages were identified with good support, one representing a possible cryptic species and the other three showing further subdivision. The distribution of these deeply differentiated lineages/sublineages corresponded well to geographical regions. The secondary contact zones and phylogeographic breaks in distinct lineages of were almost concordant with those of .
Lineage division conformed to the hypothesis of drainage system evolution, that is, the phylogeographic pattern of was shaped by historical drainage patterns. Concordance in phylogeographic patterns may suggest a shared response to common hydrogeological history and also might indicate that there was more contribution of the drainage history than ecological or life-history traits in structuring genetic variation between these two disparate codistributed taxa and .
随着青藏高原在新生代晚期隆升,青藏高原东南边缘的水系发生了显著变化。然而,这种剧烈变化对特有生物地理分布和遗传多样性的影响仍知之甚少。在此,我们研究了云南小狭口蛙(姬蛙科)遗传变异的地理格局,并检验了两种假说:即遗传变异的地理分布是由当代流域还是历史流域决定的。
中国西南部山区。
分析基于从该物种分布区域收集的417个标本。我们重建了谱系(贝叶斯法和最大简约法),并基于线粒体和核标记的DNA测序数据评估了种群历史。我们还绘制了遗传多样性图谱,并通过宽松分子钟模型估计了分歧时间。
该物种保持了相对稳定的种群规模,近期没有种群扩张。确定了四个主要母系谱系,其中一个可能代表一个隐存物种,另外三个显示出进一步的细分。这些深度分化的谱系/亚谱系的分布与地理区域高度吻合。云南小狭口蛙不同谱系中的次级接触区和系统发育间断与[另一物种名称未给出]的几乎一致。
谱系划分符合水系演化假说,即云南小狭口蛙的系统发育地理格局是由历史水系格局塑造的。系统发育地理格局的一致性可能表明对共同水文地质历史的共同响应,也可能表明在构建这两个不同但分布重叠的分类群[物种名称未给出]和[物种名称未给出]之间的遗传变异方面,水系历史比生态或生活史特征的贡献更大。