Abstract
In Hungary, Senonian sediments are known in the Bakony Mountains of western Hungary, in North Hungary, in the southern part of the Great Hungarian Plain and in the Trans-Tisza region east from the Tisza River. The deposits from these four areas represent different Senonian facies types; these are known as the Central Range type, the Gosau type, the Bácsalmás type and the Flysch type, respectively. A palynozonation for Late Santonian-Late Maastrichtian sequences of the Central Range type consists of eight zones (dominance zones and assemblage zones); in addition six subzones can be recognized. The recognition of the zones and subzones is largely related to the fast evolutionary trend within the Normapolles group.
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