Nice Chris C, Bell Katherine L, Gompert Zachariah, Lucas Lauren K, Ott James R, Tovar Ruben U, Crump Paul, Diaz Peter H
Department of Biology, Population and Conservation Biology Program Texas State University San Marcos Texas USA.
Department of Biology University of Nevada Reno Nevada USA.
Ecol Evol. 2025 Jan 9;15(1):e70785. doi: 10.1002/ece3.70785. eCollection 2025 Jan.
Karst ecosystems often contain extraordinary biodiversity, but the complex underground aquifers of karst regions present challenges for assessing and conserving stygobiont diversity and investigating their evolutionary history. We examined the karst-obligate salamanders of the species complex in the Edwards Plateau region of central Texas using population genomics data to address questions about population connectivity and the potential for gene exchange within the underlying aquifer system. The species complex has historically been divided into three nominal species, but their status, and spatial extent of species ranges, have remained uncertain. We discovered evidence of extensive admixture among species within the complex and with adjacent lineages. We observed relatively low levels of differentiation among all sampling localities which supports the hypothesis of recent divergence. Nominal taxonomy, aquifer region and geography each accounted for a modest amount of the overall population genomic variation; however, these predictors were largely confounded and difficult to disentangle. Importantly, current taxonomy of the three nominal species does not reflect the admixture apparent in clustering analyses. Inference of migration events revealed a complex pattern of gene exchange, suggesting that salamanders have a dynamic history of dispersal through the aquifer system. These results highlight the need for greater understanding of how stygobiont populations are connected via dispersal and gene exchange through karst aquifers. These results also highlight the applicability of population genomics data as a powerful lever for investigating connectivity among populations in systems where direct detection of dispersal paths is difficult, as in underground, aquatic systems.
喀斯特生态系统通常拥有非凡的生物多样性,但喀斯特地区复杂的地下含水层给评估和保护穴居生物多样性以及研究它们的进化历史带来了挑战。我们利用种群基因组学数据,对德克萨斯州中部爱德华兹高原地区该物种复合体中 obligate 的喀斯特蝾螈进行了研究,以解决有关种群连通性以及潜在含水层系统内基因交流可能性的问题。该物种复合体在历史上被划分为三个名义种,但其分类地位以及物种分布范围的空间范围仍不明确。我们发现了该复合体中各物种之间以及与相邻谱系之间广泛混合的证据。我们观察到所有采样地点之间的分化水平相对较低,这支持了近期分化的假说。名义分类、含水层区域和地理因素各自在总体种群基因组变异中占了一定比例;然而,这些预测因素在很大程度上相互混淆且难以区分。重要的是,目前这三个名义种的分类法并未反映出聚类分析中明显的混合情况。对迁移事件的推断揭示了一个复杂的基因交流模式,表明蝾螈在含水层系统中有动态的扩散历史。这些结果凸显了更深入了解穴居生物种群如何通过喀斯特含水层的扩散和基因交流相互连接的必要性。这些结果还凸显了种群基因组学数据作为一种强大手段在研究地下、水生等难以直接检测扩散路径的系统中种群连通性方面的适用性。