Please use this identifier to cite or link to this item: http://earsiv.odu.edu.tr:8080/xmlui/handle/11489/1919
Full metadata record
DC FieldValueLanguage
dc.contributor.authorAksu, Ismail-
dc.contributor.authorBektas, Yusuf-
dc.contributor.authorBeldz, Osman-
dc.contributor.authorCiftci, Yilmaz-
dc.contributor.authorEroglu, Oguzhan-
dc.contributor.authorKalayci, Gokhan-
dc.contributor.authorTuran, Davut-
dc.date.accessioned2022-08-16T11:23:45Z-
dc.date.available2022-08-16T11:23:45Z-
dc.date.issued2017-
dc.identifier.urihttp://doi.org/10.1016/j.bse.2016.11.005-
dc.identifier.urihttps://www.sciencedirect.com/science/article/pii/S0305197816302617?via%3Dihub-
dc.identifier.urihttp://earsiv.odu.edu.tr:8080/xmlui/handle/11489/1919-
dc.description.abstractPhylogeny of Capoeta genus distributed in Anatolia were carried out by analysing mitochondria cytochrome b gene (1140 bp) sequences from 332 samples representing 59 populations of 15 species across their geographical distribution. Haplotype network and phylogenetic analysis (neighbor-joining, maximum-likelihood, maximum parsimony, and bayesian inference) of the 103 cytochrome b haplotypes detected in Capoeta species resulted in similar tree topologies including four distinct clades, in congruent with taxonomic classification of Capoeta based on morphological characteristics such as scale size, mouth shape, and body spotting. Based on cyt b nucleotide sequences, the present study suggests that four undescribed Capoeta species may exist in Anatolia freshwater; one species in the Kizilirmak River, the second species in the Dirgine River, the third species B. Menderes River, and the fourth species in the some Yesilirmak tributaries that run into the Black Sea Basin. Capoeta taxa distributed in the rivers of Anatolian freshwater basins are isolated from each other during middle Miocene (Serravallian)-late Pleistocene (Ionian) (about 13.75-0.41 million years). This suggests that distribution and presence of Capoeta species were shaped under paleogeographic conditions such as Pleistocene climate changes in Quarternary period as well as tectonic uplift and faulting, which probably has not changed up to now. (C) 2016 Elsevier Ltd. All rights reserved.en_US
dc.language.isoengen_US
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD, THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLANDen_US
dc.relation.isversionof10.1016/j.bse.2016.11.005en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectCapoeta; Mitochondrial DNA; Cytochrome b; Genetic identification; Phlogeny; Anatoliaen_US
dc.subjectCYTOCHROME-B DNA; SPECIES COMPLEX; BIOGEOGRAPHICAL PATTERNS; EVOLUTIONARY; SEA; RIVER; CYPRINODONTIFORMES; CYPRINIFORMES; POPULATIONS; SYSTEMATICSen_US
dc.titleMolecular phylogeny of the genus Capoeta (Teleostei: Cyprinidae) in Anatolia, Turkeyen_US
dc.typearticleen_US
dc.relation.journalBIOCHEMICAL SYSTEMATICS AND ECOLOGYen_US
dc.contributor.departmentOrdu Üniversitesien_US
dc.contributor.authorID0000-0002-2104-9888en_US
dc.contributor.authorID0000-0002-8367-9746en_US
dc.contributor.authorID0000-0003-1255-496Xen_US
dc.contributor.authorID0000-0003-4553-990Xen_US
dc.identifier.volume70en_US
dc.identifier.startpage80en_US
dc.identifier.endpage94en_US
Appears in Collections:Balıkçılık Teknolojisi Mühendisliği

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.