dc.contributor.author | Made, Jan Van Der | |
dc.contributor.author | Güleç, Erksin | |
dc.contributor.author | Erkman, Ahmet Cem | |
dc.date.accessioned | 12.07.201910:49:13 | |
dc.date.accessioned | 2019-07-11T21:54:37Z | |
dc.date.available | 12.07.201910:49:13 | |
dc.date.available | 2019-07-11T21:54:37Z | |
dc.date.issued | 2013 | |
dc.identifier.issn | 1300-0179 | |
dc.identifier.uri | https://app.trdizin.gov.tr/makale/TVRRd01UTXpNdz09 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12513/445 | |
dc.description.abstract | The suid remains from localities 58-HAY-2 and 58-HAY-19 in the Late Miocene Derindere Member of the İncesu Formation in the Hayranlı-Haliminhanı area (Sivas, Turkey) are described and referred to as Microstonyx major (Gervais, 1848–1852). Microstonyx shows changes in incisor morphology, which are interpreted as a further adaptation to rooting. This occurred probably in a short period between 8.7 and 8.121 Ma ago and possibly is a reaction to environmental change. The incisor morphology in locality 58-HAY-2 suggests that it is temporally close to this change, which would imply that this locality and the lithostratigraphically lower 58-HAY-19 belong to the lower part of MN11 and not to MN12. The findings are discussed in the regional context and contribute to the knowledge of the Anatolian fossil mammals. | en_US |
dc.description.abstract | The suid remains from localities 58-HAY-2 and 58-HAY-19 in the Late Miocene Derindere Member of the İncesu Formation in the Hayranlı-Haliminhanı area (Sivas, Turkey) are described and referred to as Microstonyx major (Gervais, 1848–1852). Microstonyx shows changes in incisor morphology, which are interpreted as a further adaptation to rooting. This occurred probably in a short period between 8.7 and 8.121 Ma ago and possibly is a reaction to environmental change. The incisor morphology in locality 58-HAY-2 suggests that it is temporally close to this change, which would imply that this locality and the lithostratigraphically lower 58-HAY-19 belong to the lower part of MN11 and not to MN12. The findings are discussed in the regional context and contribute to the knowledge of the Anatolian fossil mammals. | en_US |
dc.language.iso | eng | en_US |
dc.rights | info:eu-repo/semantics/openAccess | en_US |
dc.subject | Biyoloji | en_US |
dc.title | Microstonyx (Suidae, Artiodactyla) from the Upper Miocene of Hayranlı-Haliminhanı, Turkey | en_US |
dc.type | article | en_US |
dc.relation.journal | Turkish Journal of Zoology | en_US |
dc.contributor.department | Kırşehir Ahi Evran Üniversitesi | en_US |
dc.identifier.volume | 37 | en_US |
dc.identifier.issue | 1 | en_US |
dc.identifier.startpage | 106 | en_US |
dc.identifier.endpage | 122 | en_US |
dc.relation.publicationcategory | Makale - Ulusal Hakemli Dergi - Kurum Öğretim Elemanı | en_US] |