Jump to content

Shendi Formation

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by Tisquesusa (talk | contribs) at 15:46, 18 August 2018 (References). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Shendi Formation
Stratigraphic range: Campanian–Maastrichtian
TypeGeological formation
Lithology
PrimarySandstone, siltstone, mudstone
Location
RegionNorthern State
Country Sudan

The Shendi Formation is a Late Cretaceous geologic formation. Indeterminate Theropod remains have been recovered from it.[1] As well as those of the dyrosaurid Hyposaurus. It consists of a lower unit of fine grained meandering channel sediments, separated by an erosive contact with overlying meandering to braided river channel sandstones.[2]

See also

References

  1. ^ Weishampel, et al. (2004). "Dinosaur distribution" Pp. 517-607. in Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2. " Pp. 517-607.
  2. ^ Salih, Khalaf Allah O.; Evans, David C.; Bussert, Robert; Klein, Nicole; Nafi, Mutwakil; Müller, Johannes (2015-12-30). "First record ofHyposaurus(Dyrosauridae, Crocodyliformes) from the Upper Cretaceous Shendi Formation of Sudan". Journal of Vertebrate Paleontology. 36 (1): e1115408. doi:10.1080/02724634.2016.1115408. ISSN 0272-4634.