Vörös A. szerk.: Fragmenta Mineralogica Et Palaentologica 18. 1996. (Budapest, 1996)

There is a distinct difference between the fauna of several sections. In some beds the Myodocopid genus Polycope is frequent (12-28 %). The Kericser (Carixian and Domerian) samples and the Szentgál, Gombáspuszta samples are of this kind (Figs. 810) . The first and second sample came from micritic limestones of a "Hierlatzkalk" section. This type of sediment was deposited on the slope or the foot of the seamounts (VÖRÖS, 1983, 1986). Similarly high percent of myodocopids is observable in the Bajocian "fissure-fauna" of Somhegy (Bakony Mts., Hungary) (MONOSTORI 1995b). O I r I 1—

I '—

I !—-1 S—

I L-J ' -1 I 1 2 3 4 5 5 7 8 Fig. 8. Distribution of ostracods in the Carixian (Ibex Zone) sample of Kericser. Legend: see in Fig. 5 1 2 3 4 5 6 7 8 Fig. 9. Distribution of ostracods in the Domerian (Spinatum Zone) sample of Kericser. Legend: see in Fig. 5