New insectivores (Lipotyphla, Mammalia) from the Late Miocene of the Sivas Basin, Central Anatolia

Marc Furió*, Jan Van Dam, Ferhat Kaya

*Corresponding author for this work

    Research output: Contribution to journalArticleResearchpeer-review

    13 Citations (Scopus)

    Abstract

    The ages of the rich Central Anatolian Late Miocene mammal sites Hayranlý 1 and Düzyayla are only approximately known. One of the main reasons for the age uncertainties is the substantial faunal difference between Anatolia and Europe during this time slice, hampering correlations to the European MN system. Previously, a MN 10 or MN 11 age has been assigned to Hayranli 1 (Anatolian Zone J) and a MN 12 age to Düzyayla (Zone K) based on rodents. Here we studied the fossil insectivores from these two Turkish Miocene localities. We found an almost identical faunal content of the two localities, including one erinaceid (Schizogalerix sinapensis), five soricids (Paenelimnoecus sp., Amblycoptus oligodon, Petenyia dubia, Soricinae indet. and Crocidurinae/Crocidosoricinae indet.), and two talpids (Desmanella aff. cingulata and Desmanodon larsi sp. nov.). With the only difference being the absence of Paenelimnoecus in Düzyayla, the insectivore fauna suggests that the sites are not significantly different in age. The presence of A. oligodon is indicative of MN 12 in Europe. The rest of the assemblage is in complete agreement with a Turolian (MN 11-13) age. Our results also imply that D. larsi sp. nov. represents the youngest record of Desmanodon, extending the biostratigraphical range of this genus significantly.

    Original languageEnglish
    Pages (from-to)163-181
    Number of pages19
    JournalBulletin of Geosciences
    Volume89
    Issue number1
    DOIs
    Publication statusPublished - 2014

    Keywords

    • Biostratigraphy
    • Desmanodon
    • Düzyayla
    • Hayranlý
    • Insectivora
    • Neogene
    • Turkey

    Fingerprint

    Dive into the research topics of 'New insectivores (Lipotyphla, Mammalia) from the Late Miocene of the Sivas Basin, Central Anatolia'. Together they form a unique fingerprint.

    Cite this