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Correlation of palyno- (spores, pollen, dinoflagellates) and calcareous nannofossil zones in the Late Cretaceous of the Northern Calcareous Alps (Austria) and the Transdanubian Central Range (Hungary).
Siegl-Farkes, A. and Wagreich, M.
1996b
ADVANCES in Austrian--Hungarian joint Geological Research Budapest, 1996, pp. 127-135.ADVANCES in A
Correlation of palyno- (spores, pollen, dinoflagellates) and calcareous nannofossil zones in the Late Cretaceous of the Northern Calcareous Alps (Austria) and the Transdanubian Central Range (Hungary).

Siegl-Farkes, A. and Wagreich, M., 1996. Correlation of palyno- (spores, pollen, dinoflagellates) and calcareous nannofossil zones in the Late Cretaceous of the Northern Calcareous Alps (Austria) and the Transdanubian Central Range (Hungary). ADVANCES in Austrian--Hungarian joint Geological Research Budapest, 1996, pp. 127-135. Abstract The Upper Cretaceous palynostratigraphic standard zonation of the Transdanubian Central Range of Hungary has beel1 correlated to the calcareous nannofossil zonation of the Gosau Group of Austria. In the Gams section (Northern Calcareous Alps, Austria) two new palynostratigraphic zones of the Late Turonian to Coniacian are defined: the Subtrudopo/lis-Complexiopollis Assemblage Zone, and the Complexiopollis Dominance Zone. For the marine formations of the Transdanubian Central Range two Dinoflagellate Assemblage Zones and two Subzones within each of these were established. The base of the transgression of the Jako Marl Formation in the Hungarian sections is dated as late Late Santoniar1 to early Early Campanian (nannofossil zone CC17b, Hungaropollis palynostratigraphic zone, Odontochitina oper-culata dinoflagellate zone). The uppermost part of the Hungarian sections is dated as Late Campanian (nannofossil zone CC22c, Plicapollis-Subtriporopollenites Assemblage Zone, Pyxidinopsis bakonyensis Assembla~e Zone).
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