Matskási István (szerk.): A Magyar Természettudományi Múzeum évkönyve 90. (Budapest 1998)

Hír, J.: Cricetids (Rodentia, Mammalia) of the Early Pleistocene vertebrate fauna of Somssich-hegy 2 (Southern Hungary, Villány Mountains)

Table 3. Percentage of the morphotypes of the M3 molars in four investigated Cricetus materials C. cricetus C. praeglacialis C. runtonensis C. runtonensis solymarensis runtonensis A 15.7 9.7 18 13 B 12.3 24.75 6 8.4 C 11.6 12.2 12 3.8 1) 1.9 2.7 4.6 I-: 3.9 4.« 12 9.2 F 28.3 4.1 10.7 G 0.64 13 23 11.4 H 25.7 28.7 29 38.9 Remarks to the results of the morphotype-analysis Ml (Fig. 26, Table 1). The most reduced morphotype AObYObO (without any additional elements) is the dominant one in the studied materials. Only the frequency of the ramified posterolophule (AObYObl) is remarkable in the Solymár material. M2 (Fig. 27. Table 2). In the recent material and in the sample of Villany 8 the reduced type is dominant (A00), but among the molars from Solymár and Somssich-hegy 2 the dominant one is the type bearing ramified posterolophule (A01 ). Fig. 27. The morphotype classification system of the Cricetus M2 molars. Explanation: A = anterolophule is simple: B = anterolophulc is doubled; 0 = mesolophe is missing; 1 = mesolophe is found; 0 = posterolophule is simple; 1 = posterolophule is ramified. The distribution of the morphotypes is given in Table 2