Löwenstein Formation
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]
Löwenstein Formation Stratigraphic range: Mid Norian (Alaunian) 215.6–212 Ma | |
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Type | Geological formation |
Unit of | Keuper |
Underlies | Trossingen Formation |
Overlies | Mainhardt Formation |
Thickness | At least 80 m |
Lithology | |
Primary | Sandstone |
Other | Marl |
Location | |
Region | Europe |
Country | |
Extent | Bavaria, Baden-Württemberg |
Vertebrate fauna
- Ceratodus elegans Vollrath, 1923, a lungfish from the Stubensandstein[2]
- Lisowicia, an elephant-sized dicynodont.
Archosaurs
Theropod tracks and an unnamed herrerasaur genus are known from the Lower Stubensandstein.[3]
Color key
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Notes Uncertain or tentative taxa are in small text; |
Archosaurs of the Stubensandstein | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
D. cristatus[4] |
|
"Tibia."[5] |
Actually indeterminate ceratosaur remains.[4] |
| ||
H. longotarsus[4] |
|
"Mandibular fragment, vertebrae, humerus, illium, femur, metatarsal."[5] |
Actually indeterminate ceratosaur remains.[4] | |||
P. giganteus |
"Broad Lizard."[6] |
|||||
P. diagnosticus [4] |
|
Actually Sellosaurus gracilis remains. Yates assigned the type material of Sellosaurus gracilis to Plateosaurus gracilis [7] | ||||
P. triassicus[4] |
|
"Partial postcranial skeleton."[8] |
||||
S. fraasi[4] |
|
Yates assigned the type material of Sellosaurus gracilis to Plateosaurus gracilis [7] | ||||
S. gracilis[9] |
"[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] | ||||
T. minor[4] |
|
Galton and Benton showed that Teratosaurus is actually a rauisuchian.[10][11] | ||||
T. trossingensis[4] |
|
Galton and Benton showed that Teratosaurus is actually a rauisuchian.[10][11] | ||||
T. hermannianus[4] |
|
Thecodontosaurus hermannianus was named by Huene (1905), and then recombined as Sellosaurus hermannianus by Huene (1914). Smith and Pol (2007) recombined it as Plateosaurus gracilis[12] | ||||
See also
- List of dinosaur-bearing rock formations
Footnotes
- Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Triassic, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 521–525. ISBN 0-520-24209-2.
- Ceratodus elegans n. sp. aus dem Stubensandstein. P Vollrath, Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins, 1923
- "17.2 Baden-Württemberg, Germany; 1. Lower Stubensandstein," in Weishampel, et al. (2004). Page 524.
- "17.2 Baden-Württemberg, Germany; 2. Middle Stubensandstein," in Weishampel, et al. (2004). Page 524.
- "Table 3.1," in Weishampel, et al. (2004). Page 50.
- "Table 12.1," in Weishampel, et al. (2004). Page 236.
- Yates, A.M. (2003). "Species taxonomy of the sauropodomorph dinosaurs from the Löwenstein Formation (Norian, Late Triassic) of Germany". Palaeontology 46 (2): 317–337
- "Table 3.1," in Weishampel, et al. (2004). Page 48.
- "17.2 Baden-Württemberg, Germany; '1. Lower Stubensandstein' and '2. Middle Stubensandstein,'" in Weishampel, et al. (2004). Page 524.
- Galton, P. M. (1985). "The poposaurid thecodontian Teratosaurus suevicus von Meyer, plus referred specimens mostly based on prosauropod dinosaurs". Stuttgarter Beiträge zur Naturkunde, B, 116: 1-29.
- Benton, M.J. (1986). "The late Triassic reptile Teratosaurus - a rauisuchian, not a dinosaur". Palaeontology 29: 293-301.
- N. D. Smith and D. Pol. 2007. Anatomy of a basal sauropodomorph dinosaur from the Early Jurassic Hanson Formation of Antarctica. Acta Palaeontologica Polonica 52(4):657-674
References
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.