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

ua 1 I 1 1 1 1 1 1 1 "fí»»1.4 1.6 1.8 2.0 2,2 I Fig. 10 Scatter diagramm of different Neogene Cricetidae from the Carpathian Basin a= Karstocricetus skofleki gen.n., sp. n. from Tardosbánya, b= Karstocricetus sp. from Széchenyi Hill in Budapest, c= Neocricetodon schaubi from Csákvár, d= Neocricetodon fahlbuschi from Sümeg, e = Neocricetodon fahlbuschi (= Kowalskia fahlbuschi) from Kohfidisch (after BACHMAYER and WILSON 1970) Cricetus LESKE, 1779 Cricetus kormosi SCHAUB, 1930 Fig. 1:5, Fig. 2:7-8, Fig. 3:3-4, Fig. 5:3-4, Fig. 6:7-8, Fig. 7:5-6 Material

: While working the limestone luarry at Polgárdi bone remains were reported by geologists I. DUNKL, S. JÓZ SA and K. SCHLEMMER. The remains were found in a newly opened fissure. Together with the discoverers the author collected some 0. 6 m

3 bone-bearing sediment in 1984-1985. The material is deposited in the Hungarian Geological Institute. The location, that has proved to be the richest in the region so far, was given the name Polgárdi 4 (Loc. 1 the first sporadic find; Loc. 2 the cave sediments, found by KORMOS in 1910 and published in 1911; Loc. 3 cemented bone-breccia explored and collected by G. SCHOLTZ and S. MIHÁLY in 1974 (MIHÁLY 1975) ).