Klettgau Formation: Difference between revisions

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Klettgau Formation
Stratigraphic range: Carnian–Rhaetian
TypeGeological formation
Sub-unitsErgolz Member, Gansingen Member, Berlingen Member, Seebi Member,Gruhalde Member, Belchen Member
UnderliesStaffelegg Formation
OverliesBänkerjoch Formation
Thickness30–60 metres (100–200 ft), locally up to 75 metres (250 ft)
Lithology
PrimaryMudstone, Marl
OtherDolomite, Sand
Location
Location  Switzerland
Type section
Named forKlettgau
Named byJordan, et al
LocationSeebi quarry
Year defined2016

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

  1. ^ 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. {{cite journal}}: Check date values in: |date= (help)
  2. ^ 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. {{cite journal}}: Check date values in: |date= (help)