Identification of proboscidean tusk from the Plio-Pleistocene transition of the Pekecik Section, Eastern Turkey

dc.contributor.authorRanjan, Pranav B.
dc.contributor.authorV. Titov, Vadim
dc.contributor.authorTesakov, Alexey S.
dc.contributor.authorTrikhunkov, Yaroslav I.
dc.contributor.authorcelik, Hasan
dc.date.accessioned2026-08-12T17:06:54Z
dc.date.issued2022
dc.departmentFırat Üniversitesi
dc.description.abstractA fragment of proboscidean tusk from Pekecik (Plio-Pleistocene transition), Turkey, was studied to ascertain its taxonomic identification and biostratigraphic signal. Characteristic properties of the dentine (Schreger structures) were measured along the transversal and longitudinal sections. Schreger angles showed an increasing range from the tusk axis to the cement-dentine junction (CDJ) with values ranging from 61-109 degrees. The variability of the qualitative Schreger pattern from the X type near the tusk axis to the V type at the cement-dentine junction (CDJ), were recorded. The wavelength of dentinal tubules showed a decreasing trend from 1.67 mm near the axis to 1.0 mm near the CDJ. Based on these properties, the specimen was compared with already published data and is tentatively assigned to a meridionaloid elephant cf. Archidiskodon sp. In our research, we conclude that the tusk microstructure features are a practical means of taxonomic study.
dc.description.sponsorshipSouthern Scientific Centre RAS, [122011900166-9]; Russian Science Foundation [18-74-10081]; Geological Institute of the Russian Academy of Sciences [122011900166-9]
dc.description.sponsorshipThe authors thank Pavel Nikolskiy, Nikolai Sysoev, and members of the Laboratory of Technical Processing of Rocks (Geological Institute, RAS) for preparing the material and cutting the sections for microscopic study. We are grateful to Kirill Yushin (Geological Institute, RAS) for his help in produc-ing the microphotographs and assisting in measurements and calculations. We would also like to thank Martina Abelova (Bratislava, Slovak Republic) for her valuable recommendations. Lastly, we thank all the editors and reviewers for their suggestions and insights, which ultimately helped us to improve the article. This work was performed in the framework of the state assignments of the Geological Institute of the Russian Academy of Sciences, and the Southern Scientific Centre RAS, project No. 122011900166-9 (Titov V.V.). The work of Alexey Tesakov (correlations and biostratigraphic control) was supported by the Russian Science Foundation, project No. 18-74-10081.
dc.identifier.doi10.15298/rusjtheriol.21.1.11
dc.identifier.endpage101
dc.identifier.issn1682-3559
dc.identifier.issue1
dc.identifier.orcid0000-0002-9717-2305
dc.identifier.orcid0000-0003-2750-0964
dc.identifier.scopus2-s2.0-85131736874
dc.identifier.scopusqualityQ4
dc.identifier.startpage94
dc.identifier.urihttps://doi.org/10.15298/rusjtheriol.21.1.11
dc.identifier.urihttps://hdl.handle.net/11508/49444
dc.identifier.volume21
dc.identifier.wosWOS:000876552800011
dc.identifier.wosqualityQ4
dc.indekslendigikaynakWeb of Science
dc.indekslendigikaynakScopus
dc.language.isoen
dc.publisherKmk Scientific Press Ltd, Moscow State Univ
dc.relation.ispartofRussian Journal of Theriology
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
dc.rightsinfo:eu-repo/semantics/openAccess
dc.snmzKA_WoS_20260511
dc.subjectQuaternary
dc.subjectPliocene
dc.subjectProboscidea
dc.subjecttusk
dc.subjectSchreger patterns
dc.subjectMammuthus
dc.subjectArchidiskodon
dc.subjectCDJ
dc.titleIdentification of proboscidean tusk from the Plio-Pleistocene transition of the Pekecik Section, Eastern Turkey
dc.typeArticle

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