Earth:Langental Formation

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Langental Formation
Stratigraphic range: Bartonian-Priabonian
~41–34 Ma
TypeGeological formation
UnderliesBlaubok Conglomerate
OverliesSilica Beds
Lithology
PrimarySandstone, siltstone
Location
Coordinates [ ⚑ ] : 27°24′S 15°24′E / 27.4°S 15.4°E / -27.4; 15.4
Paleocoordinates [ ⚑ ] 31°24′S 8°36′E / 31.4°S 8.6°E / -31.4; 8.6
RegionǁKaras Region
Country Namibia
ExtentSperrgebiet
Langental Formation is located in Namibia
Langental Formation
Langental Formation (Namibia)

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.

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

  • List of fossiliferous stratigraphic units in Namibia
  • Geology of Namibia
  • Elisabeth Bay Formation

References

  1. Langetal Formation at Fossilworks.org
  2. Dauteuil et al., 2018, p.6
  3. Bogenfels at Fossilworks.org

Bibliography


Further reading

  • J. Bohm. 1926. Über Tertiäre versteinerungen von den Bogenfelser diamantfeldern. Beiträge zur geologischen Erforschung der deutschen Schutzgebiete 2:55-87