Lissauer Breccia

Last updated
Lissauer Breccia
Stratigraphic range: Norian, 221.5–205.6  Ma
Type Geological formation
Lithology
Primary Breccia
Location
Coordinates 50°46′40″N18°25′37″E / 50.77778°N 18.42694°E / 50.77778; 18.42694
Regionsouthern Poland, near Kocury
Country Poland
Relief Map of Poland.svg
Blue pog.svg
Lissauer Breccia (Poland)

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. [1] The site was studied in 1932 [2] and was later forgotten and not explored until excavations began in 2012, and the Lissauer Breccia was re-described in 2021. [3]

Contents

Fossil content

See also

References

  1. Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  2. Huene, F. von. (1932). Die fossile Reptil-Ordnung Saurischia, ihre Entwicklung und Geschichte. Monogr. Geol. Pal. 4 (1) pts. 1 and 2, viii + 361 pp.
  3. Czepiński, Ł.; Dróżdż, D.; Szczygielski, T.; Tałanda, M.; Pawlak, W.; Lewczuk, A.; Rytel, A.; Sulej, T. (2021). "An Upper Triassic Terrestrial Vertebrate Assemblage from the Forgotten Kocury Locality (Poland) with a New Aetosaur Taxon". Journal of Vertebrate Paleontology. 41: e1898977. doi:10.1080/02724634.2021.1898977. S2CID   233522981.

Bibliography