Posgrado en Ciencias Biológicas, Universidad Nacional Autónoma de México, Ciudad de México, Mexico.
Jardín Botánico, Instituto de Biología, Universidad Nacional Autónoma de México, Ciudad de México, Mexico.
PeerJ. 2022 Jul 26;10:e13802. doi: 10.7717/peerj.13802. eCollection 2022.
The most recent glacial cycles of the Pleistocene affected the distribution, population sizes, and levels of genetic structure of temperate-forest species in the main Mexican mountain systems. Our objective was to investigate the effects these cycles had on the genetic structure and distribution of a dominant species of the "mexical" vegetation across North and Central America. We studied the genetic diversity of , a conifer distributed from the Southwestern United States to the highlands of Central America. We combined information of one plastid marker and two nuclear markers to infer phylogeographic structure, genetic diversity and demographic changes. We also characterized the climatic niche for each variety to infer the plausible area of suitability during past climatic conditions and to evaluate climatic niche discontinuities along with the species distribution. We found a marked phylogeographic structure separating the populations North and South of the Isthmus of Tehuantepec, with populations to the South of this barrier forming a distinct genetic cluster corresponding to var. . We also found signals of population expansion in the Northern genetic cluster. Ecological niche modeling results confirmed climatic niche differences and discontinuities among varieties and heterogeneous responses to climatic oscillations. Overall, 's genetic diversity has been marked by distribution shifts, population growth and secondary contact the North, and permanence in the South since the last interglacial to the present. High genetic variation suggests a wide and climatically diverse distribution during climatic oscillations. We detected the existence of two main genetic clusters, supporting previous proposals that and may be considered two separate species.
更新世最近的冰期影响了主要墨西哥山脉系统中温带森林物种的分布、种群大小和遗传结构水平。我们的目的是研究这些周期对北美和中美洲“mexical”植被的优势种遗传结构和分布的影响。我们研究了分布于美国西南部到中美洲高地的针叶树 的遗传多样性。我们结合了一个质体标记和两个核标记的信息,以推断系统地理学结构、遗传多样性和种群动态。我们还描述了每个品种的气候生态位,以推断过去气候条件下的适宜区域,并评估物种分布的同时,评估气候生态位不连续性。我们发现,伊斯特莫斯·特万特佩克地峡南北的种群存在明显的系统地理学结构,该屏障以南的种群形成了一个独特的遗传聚类,对应于 var. 。我们还发现北方遗传聚类中存在种群扩张的信号。生态位建模结果证实了不同品种之间的气候生态位差异和不连续性,以及对气候波动的异速响应。总体而言,自上一个间冰期以来,的遗传多样性一直以分布转移、北部种群增长和与南部的二次接触为特征,而南部则保持稳定。高遗传变异表明,在气候波动期间存在广泛的气候多样化分布。我们检测到存在两个主要的遗传聚类,这支持了之前的提议,即 和 可能被视为两个不同的物种。