The Lissauer Breccia, sometimes referred to as the Kocury Locality, is a Norian geologic formation that is part of the larger Keuper limestone, which dominates across most of west and central Europe. Dinosaur remains diagnostic to the genus level are among the fossils that have been recovered from the formation.Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607. The site was studied in 1932Huene, F. von. (1932). Die fossile Reptil-Ordnung Saurischia, ihre Entwicklung und Geschichte. Monogr. Geol. Pal. 4 (1) pts. 1 and 2, viii + 361 pp. and was later forgotten and not explored until excavations began in 2012, and the Lissauer Breccia was re-described in 2021.
Fossil content Kocurypelta silvestris cf. Metaceratodus sp. Proterochersis cf. porebensis Velocipes guerichi
See also
List of dinosaur-bearing rock formations List of stratigraphic units with few dinosaur genera
References
Bibliography Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. .