Anducho-Reyes Miguel A, Cognato Anthony I, Hayes Jane L, Zúñiga Gerardo
Lab. de Variación Biológica y Evolución, Escuela Nacional de Ciencias Biológicas-IPN, Prol. de Carpio y Plan de Ayala s/n, Col. Santo Tomas, C.P. 11340 México, DF, Mexico.
Mol Phylogenet Evol. 2008 Dec;49(3):930-40. doi: 10.1016/j.ympev.2008.09.005. Epub 2008 Sep 17.
Dendroctonus mexicanus is polyphagous within the Pinus genus and has a wide geographical distribution in Mexico and Guatemala. We examined the pattern of genetic variation across the range of this species to explore its demographic history and its phylogeographic pattern. Analysis of the mtDNA sequences of 173 individuals from 25 Mexican populations allowed to us identify 53 geographically structured haplotypes. High haplotype and low nucleotide diversities and Tajima's D indicate that D. mexicanus experienced rapid population expansion during its dispersal across mountain systems within its current range. The nested clade phylogeographic analysis indicates that the phylogeographic pattern of D. mexicanus is explained by continuous dispersion among lineages from the Sierra Madre Occidental, the Sierra Madre Oriental and the Trans-Mexican Volcanic Belt. However, we also observed isolation events among haplotypes from the Cofre de Perote/Trans-Mexican Volcanic Belt/Sierra Madre Oriental and the Trans-Mexican Volcanic Belt/Sierra Madre del Sur, which is consistent with the present conformation of mountain systems in Mexico and the emergence of geographical barriers during the Pleistocene.
墨西哥齿小蠹在松属内具有多食性,在墨西哥和危地马拉有着广泛的地理分布。我们研究了该物种分布范围内的遗传变异模式,以探究其种群历史和系统发育地理模式。对来自墨西哥25个种群的173个个体的线粒体DNA序列进行分析,使我们能够识别出53个具有地理结构的单倍型。高单倍型多样性、低核苷酸多样性以及 Tajima's D 值表明,墨西哥齿小蠹在其当前分布范围内跨山脉系统扩散期间经历了快速的种群扩张。嵌套分支系统发育地理分析表明,墨西哥齿小蠹的系统发育地理模式可以通过来自西马德雷山脉、东马德雷山脉和跨墨西哥火山带的谱系之间的连续扩散来解释。然而,我们也观察到来自佩罗特火山/跨墨西哥火山带/东马德雷山脉以及跨墨西哥火山带/南马德雷山脉的单倍型之间存在隔离事件,这与墨西哥当前山脉系统的构造以及更新世期间地理屏障的出现是一致的。