Coordinates: 52°18′N 9°06′E / 52.3°N 9.1°E / 52.3; 9.1

Obernkirchen Sandstein

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Obernkirchen Sandstein
Stratigraphic range: Late Berriasian
TypeGeological formation
Unit ofBückeberg Formation (Obernkirchen Member)
ThicknessUp to 20 m (66 ft)
Lithology
PrimarySandstone
OtherCoal, mudstone
Location
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Approximate paleocoordinatesLua error: callParserFunction: function "#coordinates" was not found.
RegionNiedersachsen
CountryGermany
ExtentLower 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

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

See also

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References

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  1. ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
  2. ^ a b c d e f g h i j k l m n o p q r s t u 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. Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value)..
  3. ^ "Table 21.1," in Weishampel, et al. (2004). Page 465.