Department of Biology, University of Crete, Vassilika Vouton, GR-71409 Irakleio, Crete, Greece.
Mol Phylogenet Evol. 2010 Feb;54(2):445-56. doi: 10.1016/j.ympev.2009.09.015. Epub 2009 Sep 16.
We analyze geographic genetic variation in C. ocellatus to evaluate the influences of major climatic, paleogeographic and anthropogenic factors in its biogeographic history. Ninety four specimens from 61 populations were collected across all of its geographical range and analyzed based on partial mitochondrial sequences (cyt b, 12S, and ND1). Our results demonstrate that an ancestral form of C. ocellatus, which expanded in northwestern Africa at the end of Miocene, diverged in at least three separate evolutionary lineages approximately 4.57Ma: C. humilis spread south of the Sahara, while the other two (C. ocellatus sensu stricto) were restricted in the coastal North African region. The complicated history of the ocellated skink is a result of multiple vicariant phenomena followed by multiple active or passive dispersals. The Messinian salinity crisis and the re-flooding of the Mediterranean basin, the climatic transition from Middle to Upper Pliocene, and the hyperarid phase of the Sahara, affected the distribution and diversification of C. ocellatus, while in historical times it was introduced in the central Mediterranean islands and eastern Mediterranean region from Tunisia and Cyrenaica, respectively.
我们分析了 C. ocellatus 的地理遗传变异,以评估主要气候、古地理和人为因素对其生物地理历史的影响。从其地理分布范围内采集了 61 个种群的 94 个标本,并基于部分线粒体序列(细胞色素 b、12S 和 ND1)进行了分析。研究结果表明,一种祖先形式的 C. ocellatus 在中新世末期在非洲西北部扩张,在大约 457 万年前分化为至少三个独立的进化谱系:C. humilis 向南扩散到撒哈拉以南地区,而其他两个(C. ocellatus sensu stricto)则局限于北非沿海地区。这种有眼斑的石龙子的复杂历史是多次隔离现象以及多次主动或被动扩散的结果。墨西拿盐度危机和地中海盆地的重新洪水泛滥、从中新世到上新世的气候过渡以及撒哈拉的极度干旱阶段,影响了 C. ocellatus 的分布和多样化,而在历史时期,它分别从突尼斯和昔兰尼加被引入地中海中部岛屿和东地中海地区。