Langental Formation
The Langental Formation, also spelled as Langetal Formation, is a Late Eocene (Bartonian to Priabonian) geologic formation cropping out in the Sperrgebiet, ǁKaras Region of southwestern Namibia. The siltstones and sandstones of the formation were deposited in a shallow marine environment.[1] The Langental Formation was deposited under hot and humid conditions. The formation overlies the Silica Beds unit and is overlain by the Blaubok Conglomerate.[2] The Langental Formation provides many fossil invertebrates and fish.
| Langental Formation Stratigraphic range: Bartonian-Priabonian | |
|---|---|
| Type | Geological formation |
| Underlies | Blaubok Conglomerate |
| Overlies | Silica Beds |
| Lithology | |
| Primary | Sandstone, siltstone |
| Location | |
| Coordinates | 27.4°S 15.4°E |
| Approximate paleocoordinates | 31.4°S 8.6°E |
| Region | ǁKaras Region |
| Country |  |
| Extent | Sperrgebiet |
  Langental Formation (Namibia) | |
Fossil content
Among others, the following fossils are reported from the formation:[3]
- Fish
- Alopecias smithwoodwardi
- Carcharias (Aprionodon) frequens
- Carcharias (Physodon) quartus
- Carcharodon hastalis
- Cestracion vincenti
- Chrysophrys blankenhorni
- Cylindracanthus cf. rectus
- Galeocerdo latidens
- Galeus porrectus, G. robustus
- Isurus desorii
- Labrodon stromeri
- Lamna barnitzkei, L. vincenti
- Myliobatis cf. dixoni
- Notidanus serratissimus
- Odontaspis contortidens, O. macrota, O. winkleri
- Odontorhytis pappenheimi
- Oxypristis ferinus
- Paranarrhichas damesi
- Pimelodus cf. gaudryi
- Rhinoptera rasilis
- Sphyraenodus hastatus
- Squatina prima
See also
References
- Langetal Formation at Fossilworks.org
- Dauteuil et al., 2018, p.6
- Bogenfels at Fossilworks.org
Bibliography
- Dauteuil, Olivier; Carole Picart; François Guillocheau; Martin Pickford, and Brigitte Senut. 2018. Cenozoic deformation and geomorphic evolution of the Sperrgebiet (Southern Namibia). Communications of the Geological Survey of Namibia 18. 1–18. Accessed 2018-08-26.
Further reading
- J. Bohm. 1926. Über Tertiäre versteinerungen von den Bogenfelser diamantfeldern. Beiträge zur geologischen Erforschung der deutschen Schutzgebiete 2:55-87
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