Camelids do not occur in the late Miocene mammal locality of Cobanpinar, Turkey
Sen S.
P. 87-91
The provenance and age of camelid remains referred to Paracamelus cf. aguirrei by van der Made et al. (2002, 2003) are here questioned. These authors stated that the fossil material was collected from Cobanpinar, a Late Miocene locality in Central Anatolia (Turkey). Here, we demonstrate that these fossils probably came from an archeological site near Yozgat that was investigated at the same time as Cobanpinar. This paper provides detailed information concerning the origin of the material, and discusses differences in fossilization characters and colouration between the camel specimens and the mammalian fossils from Cobanpinar.References- Becker-Platen J.D. & Sickenberg O. 1968. Die unterpleistozÐ?nan Kiese von Eskisehir (Anatolien) und ihre Saugertierfauna // Mitteilungen aus dem Geologischen Institut der Technischen UniversitÐ?t Hannover. Vol.8. P.7-20.
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