Possible species-flock scenario for the evolution of the cyprinid genus Capoeta (Cypriniformes: Cyprinidae) within late Neogene lake systems of the Armenian Highland
We studied 4 Ma old isolated pharyngeal teeth from lake sediments of Çevirme (Tekman Palaeolake, Erzurum Province). Based on shape characters defined for 3D models of modern species, we found that the Pliocene lake constitutes sympatric occurrence of four Capoeta species (C. cf. umbla, C. cf. baliki...
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| description | We studied 4 Ma old isolated pharyngeal teeth from lake sediments of Çevirme (Tekman Palaeolake, Erzurum Province). Based on shape characters defined for 3D models of modern species, we found that the Pliocene lake constitutes sympatric occurrence of four Capoeta species (C. cf. umbla, C. cf. baliki, C. cf. sieboldi and C. sp. sevangi/capoeta), whose modern relatives belong to a monophyletic clade inhabiting today three different drainage systems of this region (Euphrates River, Kura River and Black Sea). We interpreted this high local diversity of closely related species in terms of the species-flock model. The Tekman palaeolake was a part of an unrecognized extended late Miocene to Pliocene palaeolake system in the present-day Armenian Highland, which has been disrupted by Pliocene tectonic activities. Surface uplift of the Armenian Highland contributed to the very characteristic biogeographic distribution and endemism of Capoeta in West Asian drainage systems. Thus, we proposed a species-flock scenario for the evolution and dispersal of the cyprinid genus Capoeta in a huge unrecognized palaeolake system in the present-day Armenian Highland. |
| doi_str_mv | 10.1371/journal.pone.0215543 |
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Based on shape characters defined for 3D models of modern species, we found that the Pliocene lake constitutes sympatric occurrence of four Capoeta species (C. cf. umbla, C. cf. baliki, C. cf. sieboldi and C. sp. sevangi/capoeta), whose modern relatives belong to a monophyletic clade inhabiting today three different drainage systems of this region (Euphrates River, Kura River and Black Sea). We interpreted this high local diversity of closely related species in terms of the species-flock model. The Tekman palaeolake was a part of an unrecognized extended late Miocene to Pliocene palaeolake system in the present-day Armenian Highland, which has been disrupted by Pliocene tectonic activities. Surface uplift of the Armenian Highland contributed to the very characteristic biogeographic distribution and endemism of Capoeta in West Asian drainage systems. Thus, we proposed a species-flock scenario for the evolution and dispersal of the cyprinid genus Capoeta in a huge unrecognized palaeolake system in the present-day Armenian Highland.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0215543</identifier><identifier>PMID: 31067236</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Animals ; Armenia ; Basins ; Biodiversity ; Biogeography ; Biological Evolution ; Biology and Life Sciences ; Capoeta ; Cyprinidae ; Cyprinidae - anatomy & histology ; Cyprinidae - classification ; Dispersal ; Drainage systems ; Earth Sciences ; Ecology and Environmental Sciences ; Endemism ; Evolution ; Fish ; Fishes ; Fishing ; Fossils ; Fossils - anatomy & histology ; Lake sediments ; Lakes ; Medicine and Health Sciences ; Miocene ; Natural history ; Neogene ; Neogene period ; Pharynx ; Pliocene ; Rivers ; Sediments ; Sediments (Geology) ; Species ; Species diversity ; Sympatric populations ; Tectonics ; Teeth ; Three dimensional models ; Tooth - anatomy & histology ; Uplift ; Zoology</subject><ispartof>PloS one, 2019-05, Vol.14 (5), p.e0215543-e0215543</ispartof><rights>COPYRIGHT 2019 Public Library of Science</rights><rights>2019 Ayvazyan et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 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Based on shape characters defined for 3D models of modern species, we found that the Pliocene lake constitutes sympatric occurrence of four Capoeta species (C. cf. umbla, C. cf. baliki, C. cf. sieboldi and C. sp. sevangi/capoeta), whose modern relatives belong to a monophyletic clade inhabiting today three different drainage systems of this region (Euphrates River, Kura River and Black Sea). We interpreted this high local diversity of closely related species in terms of the species-flock model. The Tekman palaeolake was a part of an unrecognized extended late Miocene to Pliocene palaeolake system in the present-day Armenian Highland, which has been disrupted by Pliocene tectonic activities. Surface uplift of the Armenian Highland contributed to the very characteristic biogeographic distribution and endemism of Capoeta in West Asian drainage systems. Thus, we proposed a species-flock scenario for the evolution and dispersal of the cyprinid genus Capoeta in a huge unrecognized palaeolake system in the present-day Armenian Highland.</description><subject>Animals</subject><subject>Armenia</subject><subject>Basins</subject><subject>Biodiversity</subject><subject>Biogeography</subject><subject>Biological Evolution</subject><subject>Biology and Life Sciences</subject><subject>Capoeta</subject><subject>Cyprinidae</subject><subject>Cyprinidae - anatomy & histology</subject><subject>Cyprinidae - classification</subject><subject>Dispersal</subject><subject>Drainage systems</subject><subject>Earth Sciences</subject><subject>Ecology and Environmental Sciences</subject><subject>Endemism</subject><subject>Evolution</subject><subject>Fish</subject><subject>Fishes</subject><subject>Fishing</subject><subject>Fossils</subject><subject>Fossils - anatomy & histology</subject><subject>Lake sediments</subject><subject>Lakes</subject><subject>Medicine and Health Sciences</subject><subject>Miocene</subject><subject>Natural history</subject><subject>Neogene</subject><subject>Neogene period</subject><subject>Pharynx</subject><subject>Pliocene</subject><subject>Rivers</subject><subject>Sediments</subject><subject>Sediments (Geology)</subject><subject>Species</subject><subject>Species diversity</subject><subject>Sympatric populations</subject><subject>Tectonics</subject><subject>Teeth</subject><subject>Three dimensional models</subject><subject>Tooth - 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Academic</collection><collection>PubMed Central (Full Participant titles)</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>PloS one</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Ayvazyan, Anna</au><au>Vasilyan, Davit</au><au>Böhme, Madelaine</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Possible species-flock scenario for the evolution of the cyprinid genus Capoeta (Cypriniformes: Cyprinidae) within late Neogene lake systems of the Armenian Highland</atitle><jtitle>PloS one</jtitle><addtitle>PLoS One</addtitle><date>2019-05-08</date><risdate>2019</risdate><volume>14</volume><issue>5</issue><spage>e0215543</spage><epage>e0215543</epage><pages>e0215543-e0215543</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract>We studied 4 Ma old isolated pharyngeal teeth from lake sediments of Çevirme (Tekman Palaeolake, Erzurum Province). Based on shape characters defined for 3D models of modern species, we found that the Pliocene lake constitutes sympatric occurrence of four Capoeta species (C. cf. umbla, C. cf. baliki, C. cf. sieboldi and C. sp. sevangi/capoeta), whose modern relatives belong to a monophyletic clade inhabiting today three different drainage systems of this region (Euphrates River, Kura River and Black Sea). We interpreted this high local diversity of closely related species in terms of the species-flock model. The Tekman palaeolake was a part of an unrecognized extended late Miocene to Pliocene palaeolake system in the present-day Armenian Highland, which has been disrupted by Pliocene tectonic activities. Surface uplift of the Armenian Highland contributed to the very characteristic biogeographic distribution and endemism of Capoeta in West Asian drainage systems. Thus, we proposed a species-flock scenario for the evolution and dispersal of the cyprinid genus Capoeta in a huge unrecognized palaeolake system in the present-day Armenian Highland.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>31067236</pmid><doi>10.1371/journal.pone.0215543</doi><orcidid>https://orcid.org/0000-0003-3484-9398</orcidid><orcidid>https://orcid.org/0000-0001-8712-0678</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | Animals Armenia Basins Biodiversity Biogeography Biological Evolution Biology and Life Sciences Capoeta Cyprinidae Cyprinidae - anatomy & histology Cyprinidae - classification Dispersal Drainage systems Earth Sciences Ecology and Environmental Sciences Endemism Evolution Fish Fishes Fishing Fossils Fossils - anatomy & histology Lake sediments Lakes Medicine and Health Sciences Miocene Natural history Neogene Neogene period Pharynx Pliocene Rivers Sediments Sediments (Geology) Species Species diversity Sympatric populations Tectonics Teeth Three dimensional models Tooth - anatomy & histology Uplift Zoology |
| title | Possible species-flock scenario for the evolution of the cyprinid genus Capoeta (Cypriniformes: Cyprinidae) within late Neogene lake systems of the Armenian Highland |
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