Löwenstein Formation | |
Type: | Geological formation |
Age: | Mid Norian (Alaunian) |
Period: | Norian |
Prilithology: | Sandstone |
Otherlithology: | Marl |
Region: | Europe |
Country: | Germany |
Unitof: | Keuper |
Underlies: | Trossingen Formation |
Overlies: | Mainhardt Formation |
Thickness: | At least 80 m |
Extent: | Bavaria, Baden-Württemberg |
The Löwenstein Formation (Stubensandstein in Baden-Württemberg, Burgsandstein in Bavaria) is a lithostratigraphic formation of the Keuper in Germany. It is underlain by the Mainhardt Formation and overlain by the Trossingen Formation. It dates back to the middle Norian.[1]
Theropod tracks and an unnamed herrerasaur genus are known from the Lower Stubensandstein.
Archosaurs of the Stubensandstein | |||||||
---|---|---|---|---|---|---|---|
Genus | Species | Location | Stratigraphic position | Material | Notes | Images | |
Aetosaurus | A. feratus A. crassicauda | Lower | |||||
Apatosuchus | A. orbitoangulatus | Lower | "Partial skull" | ||||
Dolichosuchus[2] Dubious | D. cristatus | Middle | "Tibia"[3] | Actually indeterminate coelophysoid remains | |||
Efraasia | E. minor | Lower | |||||
Halticosaurus Dubious | H. longotarsus | Middle | "Mandibular fragment, vertebrae, humerus, illium, femur, metatarsal." | Later found to be indeterminate coelophysoid remains | |||
Liliensternus | L. liliensterni | ||||||
Mystriosuchus | M. ? | ||||||
Nicrosaurus | N. kapffiN. meyeri | Middle | |||||
Paratypothorax | P. andressi | Middle | |||||
Plateosaurus[4] | P. gracilis |
| "[Twenty one] partial skeletons, isolated elements, [three] partial skulls, juvenile to adult."[6] | Yates assigned the type material of Sellosaurus gracilis to Plateosaurus gracilis [7] | |||
Procompsognathus | P. triassicus | Middle | "Partial postcranial skeleton."[8] | ||||
Saltoposuchus | S. connectens S. longipes | ||||||
TanystrosuchusDubious | T. posthomus | Middle | " Neck vertebra" | ||||
Teratosaurus | T. suevicus | Middle | Galton and Benton showed that Teratosaurus is actually a rauisuchian.[9] [10] |