Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 13. 1987. (Budapest, 1987)

ridge-like (like in case of Eumyarion)

, and the hypolophulid is perpendicular to the axis. The hypoconid-posterolophid ridge is uniform, and this latter has no labial appendix (cingulum). Mg - Its structure is the same as M-p and is characterized by the fact that the mesolophid is missing in 50% of the cases. M3 - Beside the basic structure it is characterized by short or medium-length mesolophid. M - The anterocone is bifid. The lingual anteroloph is stronger than the labial one. The labial epiphysis is present on three teeth among the six, and it is long. Between the proto- and paracone there is a tendency for island formation (in the six cases examined islands Fig. 3 Lower third molars from the Hungarian Neogene localities: 1 = Eumyarion bifidus from Rudabánya, 2 = Democricetodon gaillardi from Rudabánya, 3 = Cricetus kormosi from Polgárdi 3, 4= Cricetus kormosi from Polgárdi 4, 5= Karstocricetus sp. from Széchenyi Hill in Budapest, 6 = Kowalskia polonica from Osztramos 1 appeared in two cases, "péninsule" were found also in two cases, and in two cases no islands developed). The mesoloph is long and cone-shaped at the labial margin (mesostyl). The metacone is joined, through the mesolophule, to the hypocone-posteroloph arch from the hinder part.