Mamos Tomasz, Wattier Remi, Burzyński Artur, Grabowski Michał
Department of Invertebrate Zoology and Hydrobiology, University of Lodz, Banacha, 12/16, 90-237, Lodz, Poland.
Equipe Ecologie Evolutive, UMR CNRS 6282 Biogéosciences, Université de Bourgogne, 6 Boulevard Gabriel, 21000, Dijon, France.
Mol Ecol. 2016 Feb;25(3):795-810. doi: 10.1111/mec.13499. Epub 2016 Jan 19.
The formation of continental Europe in the Neogene was due to the regression of the Tethys Ocean and of the Paratethys Sea. The dynamic geology of the area and repetitious transitions between marine and freshwater conditions presented opportunities for the colonization of newly emerging hydrological networks and diversification of aquatic biota. Implementing mitochondrial and nuclear markers in conjunction with a large-scale sampling strategy, we investigated the impact of this spatiotemporal framework on the evolutionary history of a freshwater crustacean morphospecies. The Gammarus balcanicus species complex is widely distributed in the area previously occupied by the Paratethys Sea. Our results revealed its high diversification and polyphyly in relation to a number of other morphospecies. The distribution of the studied amphipod is generally characterized by very high local endemism and divergence. The Bayesian time-calibrated reconstruction of phylogeny and geographical distribution of ancestral nodes indicates that this species complex started to diversify in the Early Miocene in the central Balkans, partially in the shallow epicontinental sea. It is possible that there were several episodes of inland water colonization by local brackish water lineages. Subsequent diversification within clades and spread to new areas could have been induced by Alpine orogeny in the Miocene/Pliocene and, finally, by Pleistocene glaciations. The present distribution of clades, in many cases, still reflects Miocene palaeogeography of the area. Our results point out that investigations of the historical aspect of cryptic diversity in other taxa may help in a general understanding of the origins of freshwater invertebrate fauna of Europe.
新近纪欧洲大陆的形成是由于特提斯洋和副特提斯海的退缩。该地区的动力地质学以及海洋和淡水环境之间反复的转变为新出现的水文网络的殖民化和水生生物群的多样化提供了机会。我们结合大规模采样策略,利用线粒体和核标记,研究了这种时空框架对一种淡水甲壳动物形态物种进化历史的影响。巴尔干钩虾物种复合体广泛分布于先前被副特提斯海占据的区域。我们的结果揭示了它相对于其他一些形态物种的高度多样化和多系性。所研究的端足类动物的分布通常以非常高的地方特有性和分化为特征。贝叶斯时间校准的系统发育重建和祖先节点的地理分布表明,这个物种复合体在中新世早期于巴尔干半岛中部开始多样化,部分是在浅陆缘海。当地的微咸水谱系可能有几次内陆水域殖民事件。随后在分支内的多样化以及向新区域的扩散可能是由中新世/上新世的阿尔卑斯造山运动,最终是由更新世冰川作用引起的。在许多情况下,分支的当前分布仍然反映了该地区的中新世古地理。我们的结果指出,对其他类群隐秘多样性历史方面的研究可能有助于全面了解欧洲淡水无脊椎动物区系的起源。