Trossingen Formation
Trossingen Formation Stratigraphic range: Upper Triassic | |
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Type | Geological formation |
The Trossingen Formation is a geological formation in Germany. It dates back to the late Norian.[1]
Vertebrate fauna
Dinosaurs of the Trossingen Formation | ||||
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Taxa | Presence | Notes | Images | |
Infraorder:
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Genus:
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Pterospondylus trielbae - "Vertebra."[7]
See also
References
- 1 2 3 4 5 6 7 8 9 10 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.
- ↑ Huene, F. von (1928). "Lebensbild des Saurischier-Vorkommens im obersten Keuper von Trossingen in Württemberg" ["Pictures of the life of the Saurischia present in the upper-most Keuper of Trossingen in Württemberg"]. Palaeobiologica 1:103–116 [German]
- ↑ Huene, F. von (1932). "Die fossile Reptil-Ordnung Saurischia, ihre Entwicklung und Geschichte" ["The fossil order of reptiles Saurischia, their development and history"]. Monographien zur Geologie und Paläontologie 4:1–361 [German]
- ↑ Galton, P.M. (1984). "Cranial anatomy of the prosauropod dinosaur Plateosaurus from the Knollenmergel (Middle Keuper, Upper Triassic) of Germany. I. Two complete skulls from Trossingen/Württ. With comments on the diet". Geologica et Palaeontologica 18:139–171
- ↑ Moser, M. (2003). "Plateosaurus engelhardti Meyer, 1837 (Dinosauria, Sauropodomorpha) aus dem Feuerletten (Mittelkeuper; Obertrias) von Bayern" ["Plateosaurus engelhardti Meyer, 1837 (Dinosauria, Sauropodomorpha) from the Feuerletten (Mittelkeuper; Obertrias) of Bavaria"]. Zitteliana Reihe B, Abhandlungen der Bayerischen Staatssammlung für Paläontologie und Geologie 24:1–186 [German with extended English summary]
- ↑ 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 50.
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