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Capoeta damascina (Teleostei: Cyprinidae) is one of the most common freshwater fish species, found throughout the Levant, Mesopotamia, Turkey and Iran. According to the state of knowledge prior to this study, C. damascina, which is distributed over a wide range of isolated water bodies, was not a well-defined species. It was questionable whether it represents a single species or a complex of closely related species with high intraspecific and comparatively low interspecific variability. The goal of this study was to investigate the taxonomy, systematic position of the C. damascina species complex and the phylogenetic relationships among its members, based on morphological features as well as molecular phylogeny. Samples obtained from throughout the geographic range of this species complex were subjected to comparative morphological analyses in order to define, properly diagnose and separate species within the C. damascina complex. To elucidate phylogenetic relationships among members of the C. damascina species complex, samples were subjected to genetic analyses, using two molecular markers targeting the mitochondrial cytochrome oxidase I (COI, n = 103) and the two adjacent divergence regions (D1-D2) of the nuclear 28S rRNA genes (LSU, n = 65). Based on morphological and molecular genetic data, six closely related species were recognized within the C. damascina complex: C. buhsei, C. caelestis, C. damascina, C. saadii, C. umbla and an undescribed species, Capoeta sp.1. Analyses of the morphometric and meristic data obtained in this study revealed phenotypic variability among the various populations within a species and among the different species. Such differences in morphological characters reflect genetic differences, environmentally induced phenotypic variation or both, as the meristic phenotype of fish is sometimes a consequence of environmental parameters acting on the genotype. Based on phylogenetic analyses, two main lineages were identified within the C. damascina species complex: a western lineage represented by C. caelestis, C. damascina and C. umbla and an eastern lineage represented by C. buhsei, C. saadii and Capoeta sp.1. The close phylogenetic relationships between C. damascina and C. umbla and the sharing of same haplotypes between one specimen of C. damascina from Euphrates and another of C. umbla from Tigris reflect one of three possibilites: recent speciation, mitochondrial introgression or a combination of both. The results obtained in this study indicate that speciation of the above-mentioned six taxa is quite recent and that their dispersal and present-day distribution can be related to Pleistocene events. The drying out of the Persian Gulf, probably during one of the first glacials of the Pleistocene, led the ancestor of the C. damascina species complex in Mesopotamia to reach the rivers of the Gulf and of Hormuz basins and differentiate there, giving rise to the eastern lineage (ancestor of C. buhsei, C. saadii and Capoeta sp.1). As connections presumably existed among the different river drainages and basins in Iran during the wet periods of the Pleistocene, the ancestor of C. buhsei, C. saadii and Capoeta sp.1 was subsequently able to colonize the various Iranian drainages and differentiate there, giving rise to C. buhsei, C. saadii and Capoeta sp.1. After the separation from the eastern lineage, the western lineage, represented by the ancestor of C. damascina, C. umbla and C. caelestis, most likely reached the Levant from the Tigris-Euphrates system during the Pleistocene glacials, when river connections existed in the regions of the upper courses of Ceyhan Nehri (southern Turkey) and some western affluents to the Euphrates. From Ceyhan Nehri, it dispersed into other rivers in southern Turkey during Pleistocene periods of low sea levels until it reached Göksu Nehri and evolved into C. caelestis. The sister population differentiated into C. damascina and C. umbla. Based on the results obtained in this study, it is likely that C. damascina colonized the Levant and southern Turkey during the Pleistocene glacials. This is well supported by the low genetic variability among the C. damascina populations. Direct connections existed among the river drainages in the Levant during the Pleistocene periods of low sea level, thus serving as a pathway for the dispersal of C. damascina. The results of this study provide a coherent picture of the taxonomic position, phylogenetic relationships and evolutionary history of the C. damascina species complex and explain present patterns of distribution considering paleogeographic events.