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

1. Szentgál, Tüzköves Hill (Fig. 1) and Gombáspuszta, 2. Hárskút, Közöskút Ravine (Fig. 2), 3. Kericser Hill (Fig. 3) 4. Hamuháza (Fig. 4) Fig. 1. Lithological profile of the Szentgál, Tüzköves-Hill section (after GÖRÖG, 1995) 1. The investigated sample of Szentgál, Tüzköves-Hill (T/l, layer N° II) is the same from which GÖRÖG (1995) has published the foraminifera fauna. This bed is Carixian in age, and consists of thin-bedded, brownish-red "ammonitico rosso" limestones with rich macrofauna (ammonites, brachiopoda, bivalves) often bearing feromanganese encrusting. The Gombás-puszta material is obtained also from Carixian limestone. Fig. 2. Lithological profile of the Hárskút, Közöskút-Ravine section (after GÉCZY, 1976) 1,2 = samples Fig. 3. Lithological profile of the Kericser-section (after VÖRÖS, 1983). 1,2 = samples