Klettgau Formation: Difference between revisions
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Klettgau Formation | |
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Stratigraphic range: | |
Type | Geological formation |
Sub-units | Ergolz Member, Gansingen Member, Berlingen Member, Seebi Member,Gruhalde Member, Belchen Member |
Underlies | Staffelegg Formation |
Overlies | Bänkerjoch Formation |
Thickness | 30–60 metres (100–200 ft), locally up to 75 metres (250 ft) |
Lithology | |
Primary | Mudstone, Marl |
Other | Dolomite, Sand |
Location | |
Location | Switzerland |
Type section | |
Named for | Klettgau |
Named by | Jordan, et al |
Location | Seebi quarry |
Year defined | 2016 |
The Klettgau Formation is a geological formation in Switzerland, It is Late Triassic in age, covering most of the mid to late Norian, the Carnian, and into the Rhaetian, spanning a period of 26-30 million years. The primary enviroment of deposits was that of a playa, with marine and fluvial intercalations. The lithology is quite variable consisting primarily of fine grained rocks typically claystones and dolocretes, often with sandstone or carbonaic fluvial channel fills.[1] Dinosaur fossils are known from the formation, including those of Plateosaurus and Notatesseraeraptor.[2]
References
- ^ Jordan, Peter; Pietsch, Johannes S.; Bläsi, Hansruedi; Furrer, Heinz; Kündig, Nicole; Looser, Nathan; Wetzel, Andreas; Deplazes, Gaudenz (2016-9). "The middle to late Triassic Bänkerjoch and Klettgau formations of northern Switzerland". Swiss Journal of Geosciences. 109 (2): 257–284. doi:10.1007/s00015-016-0218-3. ISSN 1661-8726.
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(help) - ^ Zahner, Marion; Brinkmann, Winand (2019-8). "A Triassic averostran-line theropod from Switzerland and the early evolution of dinosaurs". Nature Ecology & Evolution. 3 (8): 1146–1152. doi:10.1038/s41559-019-0941-z. ISSN 2397-334X.
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