Where: Hungary (47.0° N, 17.0° E: paleocoordinates 28.9° N, 25.8° E)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Kardosret Formation, Hettangian to Hettangian (201.3 - 161.5 Ma)
• The Kardosret Formation overlies the Dachstein Formation of the Upper Triassic (Rhaetian) age, formed by loferitic cycles, megalodonts and foraminifers Triasina.
• group of beds-level stratigraphic resolution
Environment/lithology: lithified carbonate
Primary reference: A. Dulai. 1993. Hettangian (Early Jurassic) megafauna and paleogeography of the Bakony Mts. (Hungary). In J. Palfy, A. Voros (eds.), Mesozoic Brachiopods of Alpine Europe 31-37 [F. Fursich/A. Tomasovych/P. Wagner]more details
Purpose of describing collection: paleoecologic analysis
PaleoDB collection 28955: authorized by Franz Fursich, entered by Adam Tomasovych on 06.03.2003
Creative Commons license: CC BY (attribution)
Taxonomic list
Rhynchonellata | |
Lobothyris ? sospirolensis, Lobothyris andleri, Lobothyris ? complanata, Lobothyris ovatissimaeformis
Lobothyris ? sospirolensis Uhlig 1879
Lobothyris andleri Oppel 1861
Lobothyris ? complanata Bockh 1874
Lobothyris ovatissimaeformis Bockh 1874 | |
Zeilleria sp. Bayle 1878 | |
Gastropoda | |
Coelostylina sp. Kittl 1894 snail | |
Procerithium ? sp. Cossmann 1902 snail | |
Neridomus ? sp. Morris and Lycett 1915 snail | |
"Proconulinae sp." = Proconulidae
"Proconulinae sp." = Proconulidae Cox 1960 snail | |
"Promathilda ? sp." = Promathildia
"Promathilda ? sp." = Promathildia Andreae 1887 snail | |
Echinoidea | |
Diademopsis ? sp. sea urchin |