A revision of the ammonites from the Bakony Mountains (Hungaty) based on collections of the Geological Institute
of Hungary (MAFI) in Budapest, revealed the following sequence of faunas. The youngest Campanian ammonites
from the South Bakony are three specimens ofPachydiscus (P.)praecolligatus COLLIGNON, 1955 from the Siimeg area;
this is a typical Campanian species. Two specimens of former "Lower Maastrichtian Pachydiscus neubergicus
(HAUER)" from Haraszt quany have been re-determined as Early Campanian Eupachydiscus levyi (GROSS OUVRE,
1894). The fragmentary specimen of Mortoniceras sp. has been determined as Texanites (Texanites) sp. from the
Upper Santonian. Two ammonite zones can be recognised for these sequences: Texanites sp. (Santonian) and
Eupachydiscus levyi (Lower Campanian)
