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

Description: Mj - The anteroconid is narrow and undivided. The cones are slightly alternately positioned. There is no mesolophid. The closing cingulum is well-developed and connects the mesoconid and the hypoconid. Cricetinus ZDANSKY, 1928 Cricetinus europaeus KRETZOI, 1959 Fig. 1:10, Fig. 5:6, Fig. 6: 6 1959. Cricetinus europaeus n. sp. - KRETZOI, p. 240-241. 1962. Cricetinus europaeus - KRETZOI, p. 308-309. Taf. IV, Fig. 1-3. Material

: Csarnóta 2/1 locality 1 Mj (Holotype, V. 12769, Vt. 110.) Csarnóta 2/1 locality 1 M

2 Csarnóta 2/2 locality 1 M

1 Description : M^ - Holotype. The anteroconid is narrow. The anterolophulid is bifid, underdeveloped, and joins the inner margin of the protoconid in the axis of the tooth. There is no mesolophid or island among the cones. M* - The anterocone is bifid. The two anterolophules are connected in the front part of the protocone. The two cone couples are positioned parallel while the islands are also enclosed. There is no mesoloph. 2 M - There is an island among the cones. The closing cingulum is extremely reduced. Measurement: 1.9x1.1; M

1 2.1x1.4; M

2 2.0x1.5 Allocricetus SCHAUB, 1930 Allocricetus cf. bursae SCHAUB, 1930 From the Ivanovce locality described by FEJFAR (1970). See at Kowalskia intermedia FEJFAR. Baranomys KORMOS, 1933 Baranomys sp. - Baranomys loczyi KORMOS From the Ivanovce locality described by FEJFAR (1970). See at Kowalskia intermedia FEJFAR. From Osztramos 1 also known as Baranomys loczyi (JÁNOSSY 1972). SYSTEMATIC AND STRATIGRAPHIC EVALUATION In the course of the revision of the cricetids found in the Carpathian Basin, the finds originating from two localities proved to be of extreme importance: - the extremely rich and morphologically uniform Karstocricetus skofleki gen. n., sp. n. from Tardosbánya (MN 12) - and the Cricetus kormosi SCHAUB finds discovered recently at the Polgárdi 4 locality (MN 13) These two discoveries and the analyses of the material made it possible for us to distinguish the following evolutionary stages: 1. Taxa surviving from the Sarmatian characterized by Democricetodon gaillardi and Eumya rion bifidus (Rudabánya, MN 9).