Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 16. 1993. (Budapest, 1993)

Text-fig. 1. Location map of the Eucladoceros remains at Sárbogárd 4., grey fat clay with calcareous lumps (remains), 5., greyish yellow lean clay, 6., yellowish grey silt. SKELETAL REMAINS OF EUCLADOCEROS The teeth and bones are fragmentary but they are not worn. - P sup. et inf. fr., - M sup. fr., - vert, thoracalis fr. (the epiphysis lamellae are fused, ossified), - vert, thoracalis arcus fr., - humerus sin. dist. (the medial side of hum. is damaged), - humerus dext. dist. (the lateral side of hum. is damaged. Pl. I. Fig.L), - radius dext. prox. (the breadth of the articular surface is 52 mm, Pl. I. Fig. 2.), - radius dext. dist. (damaged, Pl. I. Fig. 3.), - magnum (C 2+3) sin. fr. the lateral side had broken off), - metacarpus sin. prox. (strong, wide and large prox. epiphysis; diaphysis is flattened, Pl. I. Fig. 4.), - metacarpus dext. dist. fr. (Pl. I. Fig. 7.), - metacarpus sin. dist. fr. (Pl. I. Fig. 8.), - tibia dext. dist. (Pl. I. Fig. 6.), - astragalus dext. fr. (Pl. I. Fig. 9.), - metatarsus dext. prox. fr. (damaged, Pl. I. Fig. 5.), - os phalangis I. ant. (Pl. I. Fig. 10.), - os phalangis II. ant. (Pl. I. Fig. 11.), - os phalangis III. ant. (Pl. I. Fig. 12.). Comparing the Osteometrie data of the Sárbogárd Eucladoceros remains (Table 1.) with those of similar cervidae found at the French localities St. Vallier, Senéze and Peyrolles (Heintz 1970. Tab. 92-120.) we can say that the dimensions of the Sárbogárd find correspond with those of the smallest Eucladoceros, that is