Victoriano Pedro F, Muñoz-Mendoza Carla, Sáez Paola A, Salinas Hugo F, Muñoz-Ramírez Carlos, Sallaberry Michel, Fibla Pablo, Méndez Marco A
From the Depto. de Zoología, Fac. de Cs. Naturales y Oceanográficas, Universidad de Concepción, Concepción, Chile (Victoriano and Muñoz-Mendoza); Laboratorio de Genética y Evolución, Facultad de Ciencias, Universidad de Chile, Santiago, Chile (Sáez, Salinas, Sallaberry, Fibla, and Méndez); Department of Ecology and Evolutionary Biology, University of Michigan, Ann Arbor, MI 48109, USA (Muñoz-Ramírez).
J Hered. 2015;106 Suppl 1:546-59. doi: 10.1093/jhered/esv039.
The Andean Altiplano has served as a complex setting throughout its history, driving dynamic processes of diversification in several taxa. We investigated phylogeographic processes in the Telmatobius marmoratus species complex occurring in this region by studying the geographic patterns of genetic variability, genealogies, and historical migration, using the cytochrome b (cyt-b) gene as a marker. DNA sequences from Telmatobius gigas and Telmatobius culeus, Bolivian species with an uncertain taxonomic status, were also included. Additionally, we evaluated the phylogenetic diversity (PD) represented within Chilean protected areas and the complementary contribution from unprotected populations. Phylogenetic reconstructions from 148 cyt-b sequences revealed 4 main clades, one of which corresponded to T. culeus. T. gigas was part of T. marmoratus clade indicating paraphyletic relationships. Haplotypes from Chilean and Bolivian sites were not reciprocally monophyletic. Geographic distribution of lineages, spatial Bayesian analysis, and migration patterns indicated that T. marmoratus displays a weaker geographic structure than expected based on habitat distribution and physiological requirements. Demographic and statistical phylogeography analyses pointed out to a scenario of recent population expansion and high connectivity events of a more recent age than the post Last Glacial Maximum, probably associated to more humid events in Altiplano. PD of T. marmoratus populations within protected areas represents 55.6% of the total estimated PD. The unprotected populations that would contribute the most to PD are Caquena and Quebe (21%). Recent evolutionary processes and paleoclimatic changes, potentially driving shifts in habitat connectivity levels and population sizes, could explain the phylogeographic patterns recovered herein.
安第斯高原在其整个历史中一直是一个复杂的环境,推动了几个分类群多样化的动态过程。我们通过研究遗传变异、系统发育关系和历史迁移的地理模式,以细胞色素b(cyt-b)基因为标记,调查了该地区出现的大理石纹高原蛙物种复合体的系统地理学过程。还纳入了来自玻利维亚的分类地位不确定的物种——巨高原蛙和科氏高原蛙的DNA序列。此外,我们评估了智利保护区内所代表的系统发育多样性(PD)以及未受保护种群的补充贡献。对148个cyt-b序列的系统发育重建揭示了4个主要分支,其中一个对应于科氏高原蛙。巨高原蛙是大理石纹高原蛙分支的一部分,表明存在并系关系。来自智利和玻利维亚地点的单倍型并非相互单系的。谱系的地理分布、空间贝叶斯分析和迁移模式表明,大理石纹高原蛙显示出的地理结构比基于栖息地分布和生理需求预期的要弱。人口统计学和统计系统地理学分析指出,近期存在种群扩张的情况,以及比末次盛冰期之后更年轻的高连通性事件,这可能与高原更湿润的事件有关。保护区内大理石纹高原蛙种群的PD占估计总PD的55.6%。对PD贡献最大的未受保护种群是卡克纳和克韦贝(21%)。近期的进化过程和古气候变化可能推动了栖息地连通性水平和种群规模的变化,这可以解释本文所恢复的系统地理学模式。