Departamento de Biología Vegetal y Ecología, Facultad de Biología, Universidad de Sevilla, Apdo. 1095, 41080 Sevilla, Spain.
Departamento de Biología Vegetal y Ecología, Facultad de Biología, Universidad de Sevilla, Apdo. 1095, 41080 Sevilla, Spain; Department of Systematic and Evolutionary Botany, Faculty Centre of Biodiversity, University of Vienna, Rennweg 14, A-1030 Vienna, Austria.
Mol Phylogenet Evol. 2014 Oct;79:42-53. doi: 10.1016/j.ympev.2014.06.005. Epub 2014 Jun 24.
The current distribution of Western Mediterranean Abies species is a result of complex geodynamic processes and climatic oscillations that occurred in the past. Abies sect. Piceaster offers a good study model to explore how geo-climatic oscillations might have influenced its expansion and diversification on both sides of the W Mediterranean basin. We investigated the genetic variation within and among nine populations from five Abies species by molecular markers with high and low mutation rates and contrasting inheritance (AFLP and cpSSR). Analyses revealed the opening of the Strait of Gibraltar as an effective barrier against gene flow between the Southern Iberian (A. pinsapo) and North African (A. marocana and A. tazaotana) firs. The A. pinsapo populations in Spain and likewise those of the A. marocana - A. tazaotana population complex were not differentiated, and no evidence was found to distinguish A. tazaotana at the species level. Diversification of Abies across North Africa could occur by way of at least two vicariant events from Europe, in the west, giving rise to the A. marocana - A. tazaotana complex, and in the east, giving A. numidica. Secondary contacts among species from Abies sect. Piceaster (A. pinsapo and A. numidica), and with A. alba (Abies sect. Abies) are also indicated. However, there is a closer relationship between the Algerian fir (A. numidica) and the North Mediterranean widespread A. alba, than with the Moroccan firs (A. marocana and A. tazaotana) or the Southern Iberian (A. pinsapo). We also discuss the distribution range of these taxa in its paleogeological and paleoclimatic context, and propose that part of the modern geography of the South-Western Mediterranean firs might be traced back to the Tertiary.
当前的西方地中海冷杉物种分布是过去复杂的地球动力学过程和气候振荡的结果。松科云杉属提供了一个很好的研究模型,用于探索地理气候振荡如何影响其在西地中海盆地两侧的扩张和多样化。我们通过具有高和低突变率和不同遗传方式的分子标记(AFLP 和 cpSSR)研究了来自五个冷杉物种的九个种群内和种群间的遗传变异。分析表明,直布罗陀海峡的开放是阻止南伊比利亚(A. pinsapo)和北非(A. marocana 和 A. tazaotana)冷杉之间基因流动的有效屏障。西班牙的 A. pinsapo 种群以及 A. marocana - A. tazaotana 种群复合体的种群没有分化,也没有发现任何证据可以将 A. tazaotana 区分到种的水平。北非冷杉的多样化可能是通过至少两次来自欧洲的地理隔离事件发生的,在西部形成了 A. marocana - A. tazaotana 复合体,在东部形成了 A. numidica。松科云杉属物种(A. pinsapo 和 A. numidica)之间以及与 A. alba(松科冷杉属)之间的二次接触也表明。然而,阿尔及利亚冷杉(A. numidica)与北地中海广泛分布的 A. alba 的关系比与摩洛哥冷杉(A. marocana 和 A. tazaotana)或南伊比利亚(A. pinsapo)的关系更为密切。我们还讨论了这些类群在古地质和古气候背景下的分布范围,并提出了西南地中海冷杉的现代地理分布的一部分可能可以追溯到第三纪。