Abstract

Capoeta damascina was earlier considered by many authors as one of the most common freshwater fish species found throughout the Levant, Mesopotamia, Turkey, and Iran. However, owing to a high variation in morphological characters among and within its various populations, 17 nominal species were described, several of which were regarded as valid by subsequent revising authors. Capoeta damascina proved to be a complex of closely related species, which had been poorly studied. The current study aims at defining C. damascina and the C. damascina species complex. It investigates phylogenetic relationships among the various members of the C. damascina complex, based on mitochondrial and nuclear DNA sequences. Phylogenetic relationships were projected against paleogeographical events to interpret the geographic distribution of the taxa under consideration in relation to the area’s geological history. Samples were obtained from throughout the geographic range and were subjected to genetic analyses, using two molecular markers targeting the mitochondrial cytochrome oxidase I (n = 103) and the two adjacent divergence regions (D1-D2) of the nuclear 28S rRNA genes (n = 65). Six closely related species were recognized within the C. damascina complex, constituting two main lineages: A western lineage represented by C. caelestis, C. damascina, and C. umbla and an eastern lineage represented by C. buhsei, C. coadi, and C. saadii. The results indicate that speciation of these taxa is rather a recent event. Dispersal occurred during the Pleistocene, resulting in present-day distribution patterns. A coherent picture of the phylogenetic relationships and evolutionary history of the C. damascina species complex is drawn, explaining the current patterns of distribution as a result of paleogeographic events and ecological adaptations.

Highlights

  • The tectonic events, which started in the Middle East during the Upper Miocene, played a major role in shaping its geomorphological features and had a considerable influence on its PLOS ONE | DOI:10.1371/journal.pone.0156434 June 16, 2016Molecular Phylogeny and Zoogeography of the Capoeta damascina Species Complex doi:10.1371/journal.pone.0156434.g001 fluviatile catchments basins [1–3; Fig 1]

  • The condensed cladogram (Fig 2) showed that a monophyletic group (A-E) consisting of six closely related species can be recognized within the C. damascina complex: C. buhsei, C. caelestis, C. damascina, C. saadii, C. umbla, and a recently described new species C. coadi Alwan et al, 2016 [59]

  • The most important result of the present study is that what was earlier considered C. damascina represents a complex of six closely related species: C. buhsei from Daryacheh-ye Namak basin (Iran); C. caelestis from Göksu Nehri (Turkey); C. coadi from Rud-e Karun and possibly Rudkhaneh-ye Karkheh; C. damascina from rivers in the Levant, Mesopotamia and parts of southern Turkey; C. saadii from rivers draining into the Persian Gulf and the Strait of Hormuz, and from watercourses in the Rud-e Kor, Daryacheh-ye Maharlu, and Kerman basins in Iran; and C. umbla from the Tigris-Euphrates River system

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Summary

Introduction

The tectonic events, which started in the Middle East during the Upper Miocene, played a major role in shaping its geomorphological features and had a considerable influence on its PLOS ONE | DOI:10.1371/journal.pone.0156434 June 16, 2016Molecular Phylogeny and Zoogeography of the Capoeta damascina Species Complex doi:10.1371/journal.pone.0156434.g001 fluviatile catchments basins [1–3; Fig 1]. During the Miocene and for much of the Pliocene, the major Levantine river systems (Orontes, Litani, and Jordan) drained to the Euphrates [4,5,6]. Nahr Quwayq, which was connected to the central course of the Orontes, drained into the Euphrates [4]. Connections between the western affluents of the Euphrates River and upper courses of the Ceyhan Nehri existed during the Pliocene and probably continued during the Pleistocene [8].

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