Obernkirchen Sandstein Explained

Obernkirchen Sandstein
Type:Geological formation
Age:Late
Period:Berriasian
Prilithology:Sandstone
Otherlithology:Coal, mudstone
Region:Niedersachsen
Coordinates:52.3°N 9.1°W
Paleocoordinates:43.5°N 17.6°W
Unitof:Bückeberg Formation (Obernkirchen Member)
Thickness:Up to 20m (70feet)
Extent:Lower Saxony Basin

The Obernkirchen Sandstein or Obernkirchen Sandstone is a geological unit in Lower Saxony, Germany whose strata date back to the Early Cretaceous. The remains of the dinosaur Stenopelix and numerous dinosaur tracks are known from the unit.[1] [2] The unit is a thin interval within the Bückeberg Formation As its name would suggest the lithology primarily consists of sandstone with thin intercalations of coal. This was deposited in a sandy barrier to lagoonal complex setting. The unit has historically been extensively quarried for its high quality building stone, which has been used as far away as Jakarta.

Vertebrate paleofauna

Ornithischians of the Obernkirchen Sandstein
Taxa Presence Notes Images
Infraorder:
  1. Tracks
Niedersachsen
Genus:
  1. Tracks
Niedersachsen
Genus:
  1. Iguanodon sp.
Niedersachsen
Order:
  1. Possible ornithischian tracks.
Niedersachsen
Genus:
  1. S. valdensis.
Niedersachsen"Partial skeleton, no skull."[3]
Suborder:
  1. Indeterminate remains.
  2. Tracks
Niedersachsen"(= Megalosaurus dunkeri)"

See also

Notes and References

  1. Hornung. Jahn J.. Böhme. Annina. van der Lubbe. Torsten. Reich. Mike. Richter. Annette. September 2012. Vertebrate tracksites in the Obernkirchen Sandstone (late Berriasian, Early Cretaceous) of northwest Germany— their stratigraphical, palaeogeographical, palaeoecological, and historical context. Paläontologische Zeitschrift. 86. 3. 231–267. 10.1007/s12542-012-0131-7. 0031-0220. free. 2012PalZ...86..231H .
  2. Weishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 562. .
  3. "Table 21.1," in Weishampel, et al. (2004). Page 465.