Identification of proboscidean tusk from the Plio-Pleistocene transition of the Pekecik Section, Eastern Turkey
| dc.contributor.author | Ranjan, Pranav B. | |
| dc.contributor.author | V. Titov, Vadim | |
| dc.contributor.author | Tesakov, Alexey S. | |
| dc.contributor.author | Trikhunkov, Yaroslav I. | |
| dc.contributor.author | celik, Hasan | |
| dc.date.accessioned | 2026-08-12T17:06:54Z | |
| dc.date.issued | 2022 | |
| dc.department | Fırat Üniversitesi | |
| dc.description.abstract | A 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.sponsorship | Southern Scientific Centre RAS, [122011900166-9]; Russian Science Foundation [18-74-10081]; Geological Institute of the Russian Academy of Sciences [122011900166-9] | |
| dc.description.sponsorship | The 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.doi | 10.15298/rusjtheriol.21.1.11 | |
| dc.identifier.endpage | 101 | |
| dc.identifier.issn | 1682-3559 | |
| dc.identifier.issue | 1 | |
| dc.identifier.orcid | 0000-0002-9717-2305 | |
| dc.identifier.orcid | 0000-0003-2750-0964 | |
| dc.identifier.scopus | 2-s2.0-85131736874 | |
| dc.identifier.scopusquality | Q4 | |
| dc.identifier.startpage | 94 | |
| dc.identifier.uri | https://doi.org/10.15298/rusjtheriol.21.1.11 | |
| dc.identifier.uri | https://hdl.handle.net/11508/49444 | |
| dc.identifier.volume | 21 | |
| dc.identifier.wos | WOS:000876552800011 | |
| dc.identifier.wosquality | Q4 | |
| dc.indekslendigikaynak | Web of Science | |
| dc.indekslendigikaynak | Scopus | |
| dc.language.iso | en | |
| dc.publisher | Kmk Scientific Press Ltd, Moscow State Univ | |
| dc.relation.ispartof | Russian Journal of Theriology | |
| dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | |
| dc.rights | info:eu-repo/semantics/openAccess | |
| dc.snmz | KA_WoS_20260511 | |
| dc.subject | Quaternary | |
| dc.subject | Pliocene | |
| dc.subject | Proboscidea | |
| dc.subject | tusk | |
| dc.subject | Schreger patterns | |
| dc.subject | Mammuthus | |
| dc.subject | Archidiskodon | |
| dc.subject | CDJ | |
| dc.title | Identification of proboscidean tusk from the Plio-Pleistocene transition of the Pekecik Section, Eastern Turkey | |
| dc.type | Article |







