Authors:
Attila VörösResearch Group for Paleontology Hungarian Academy of Sciences, Hungarian Natural History Museum, Budapest, Hungary
H-1083, Budapest, Ludovika tér 2, Hungary

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Tamás BudaiGeological Institute of Hungary, Budapest, Hungary, budai@mafi.hu
H-1143, Budapest, Stefánia u. 14, Hungary

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Imre SzabóH-1113, Budapest, Villányi u. 56, Hungary

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Abstract

Recent excavation and sampling in the upper part of the Felsőörs section (Balaton Highland, Hungary) yielded important ammonoid findings, identified as belonging to the genera Nevadites, Chieseiceras, Eoprotrachyceras and Falsanolcites. Several specimens of Chieseiceras chiesense were found in a dm-thick clay layer with limestone nodules, regarded as the equivalent of the “Chiesense Groove“ of the Bagolino and other sections in the Giudicarie area (North Italy). The immediately overlying limestone bed yielded Eoprotrachyceras cf. curionii and Falsanolcites cf. rieberi. Together these reliably prove the base of the Curionii Zone, corresponding to the base of the Ladinian Stage, the GSSP of which was recently established at Bagolino. The new data further improved the excellent correlation between the ammonoid records of the Felsőörs section and the Global Stratotype Section at Bagolino. Felsőörs may be considered the most important reference section for the Anisian to Ladinian boundary interval.

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  • Vörös, A. 1998: A Balaton-felvidék triász ammonoideái és biosztratigráfiája (Triassic ammonoids and biostratigraphy of the Balaton Highland). — Studia Naturalia, 12, pp. 105 p. (In Hungarian.).

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  • A. Vörös T. Budai J. Haas S. Kovács H. Kozur J. Pálfy 2003 GSSP (Global Boundary Stratotype Section and Point) proposal for the base of Ladinian (Triassic). A proposal for the GSSP at the base of the Reitzi Zone (sensu stricto) at Bed 105 in the Felsöörs section, Balaton Higland, Hungary Albertiana 28 35 47.

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Editor(s)-in-Chief: Attila DEMÉNY

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  • Zsolt BENKÓ (Geochemistry, Ar dating; Institute for Nuclear Research, Debrecen)
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Due to the changes in editorial functions, the Advisory Board has been terminated. The participation of former Advisory Board members is highly appreciated and gratefully thanked.

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Central European Geology
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Vol 64- : A4
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