Department of Ecosystem Biology, Faculty of Science, University of South Bohemia in České Budějovice, České Budějovice, Czech Republic.
Biology Centre, Institute of Soil Biology, Czech Academy of Sciences, České Budějovice, Czech Republic.
Exp Appl Acarol. 2021 Apr;83(4):493-511. doi: 10.1007/s10493-021-00605-7. Epub 2021 Apr 3.
Oribatid mites are important decomposers of dead organic matter in soils across the world. Their origin dates back at least 380 Mya. Multiple severe climatic changes during Late Pliocene and Pleistocene shaped the migration patterns of these organisms and should be reflected in the genetic variability of their current populations. In this study, we examined the genetic diversity and phylogeographic structure as well as the evolutionary history of populations of two ecologically different oribatid mite species. Pantelozetes cavaticus is a troglophile oribatid mite known mainly from Central European caves, whereas Pantelozetes paolii is a common surface eurytopic species with Holarctic distribution. We used two molecular markers-mitochondrial cytochrome c oxidase subunit I (COI) and the nuclear D3 region of the 28S rDNA gene-to reveal phylogenetic relationships between contemporary populations. Whereas the D3 region showed minimal or no variability within populations, COI appeared to be a relevant marker for population studies. Phylogeographic analysis based on COI detected two lineages of P. cavaticus ('Czech' and 'Slovak'), which separated during the Late Pliocene (2.9 Mya) and revealed the existence of one new species. In contrast, three identified genetic lineages of P. paolii (radiation time 2.9 and 1.2 Mya, respectively) uncovered in this study were found to coexist in the distant sampling localities, suggesting a connection between populations even over long distances.
食真菌甲螨是世界范围内分解死有机物质的重要分解者。它们的起源可以追溯到至少 3.8 亿年前。上新世晚期和更新世期间发生的多次剧烈气候变化塑造了这些生物的迁移模式,这些变化应该反映在它们当前种群的遗传变异性中。在这项研究中,我们研究了两种生态差异显著的食真菌甲螨物种的遗传多样性、系统地理学结构以及种群进化历史。洞穴食真菌甲螨是一种主要分布于中欧洞穴中的穴居食真菌甲螨,而帕氏食真菌甲螨是一种常见的广布性表栖物种,分布于全北极地区。我们使用了两个分子标记——线粒体细胞色素 c 氧化酶亚基 I(COI)和 28S rDNA 基因的 D3 区——来揭示当代种群之间的系统发育关系。虽然 D3 区在种群内显示出最小或没有变异性,但 COI 似乎是种群研究的一个相关标记。基于 COI 的系统地理学分析检测到洞穴食真菌甲螨的两个谱系(“捷克”和“斯洛伐克”),它们在上新世晚期(290 万年前)分离,并揭示了一个新物种的存在。相比之下,在这项研究中发现的三个帕氏食真菌甲螨的遗传谱系(辐射时间分别为 290 万年前和 120 万年前)共存于遥远的采样地点,这表明即使在长距离上,种群之间也存在联系。