Cuha-volgy,Kardosret (Jurassic of Hungary)

Where: Hungary (47.0° N, 17.0° E)

• Paleocoordinates: 26.6° N, 32.1° E (Wright 2013)

• coordinate based on nearby landmark

• small collection-level geographic resolution

When: Kardosret Formation, Hettangian (201.4 - 199.5 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

• Zone of unstable sand shoals and their protected backbround in the shallow, warm sea of normal salinity. A deeper, calm, more protected environment, between seamounts
• yellowish-grey or pinkish-reddish micritic limestones, strongly oncoidal (3-4, rarely 5-6 in diameter, irregular shape)

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 28962: authorized by Franz Fursich, entered by Adam Tomasovych on 06.03.2003

Creative Commons license: CC0 (CC0)

Taxonomic list

Show authors, comments, and common names
Echinoidea
  -
Echinoidea indet.
Echinoidea indet. Leske 1778 sea urchin
Bivalvia
 Pectinida - Pectinoidae
Pseudopecten sp.
Pseudopecten sp. Bayle 1878 scallop
Rhynchonellata
 Rhynchonellida - Wellerellidae
Calcirhynchia ? plicatissima
 Terebratulida - Lobothyrididae
Lobothyris ovatissimaeformis, Lobothyris andleri
Lobothyris andleri Oppel 1861