Jump to content

Kalaza Formation

From Wikipedia, the free encyclopedia

This is an old revision of this page, as edited by FrescoBot (talk | contribs) at 23:37, 7 February 2020 (Bot: link syntax and minor changes). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.

Kalaza Formation
Stratigraphic range: Late Jurassic
TypeGeological formation
UnderliesTugulu Group
OverliesQigu Formation, Shishugou Formation
Location
Country China
ExtentJunggar Basin, Turpan Basin (equivalent unit)

The Kalaza Formation is a geological formation in Xinjiang, China whose strata date back to the Late Jurassic. There is some confusion with the stratigraphy of this unit, as the term is used for sediments of equivalent age in both the Junggar Basin and the Turpan Basin.[1] Dinosaur remains are among the fossils that have been recovered from formation[2]

Vertebrate paleofauna

Dinosaurs of the Kalazha Formation
Genus Species Presence Notes Images

Chiayusaurus[2]

C. lacustris[2]

Turpan Basin

Later found to be indeterminate sauropod remains.[2]

Hudiesaurus[2]

H. sinojapanorum[2]

Turpan Basin

"Dorsal vertebra, complete forelimb, [and four] teeth."[3]

cf. Szechuanosaurus[2]

cf. S. campi[2]

Geographically located in Xinjiang Uygur Zizhiqu, China.[2]

Later found to be indeterminate theropod remains.[2]

See also

References

  1. ^ Maisch, Michael W.; Matzke, Andreas T. (2019-01-01). "First record of a eusauropod (Dinosauria: Sauropoda) from the Upper Jurassic Qigu-Formation (southern Junggar Basin, China), and a reconsideration of Late Jurassic sauropod diversity in Xinjiang". Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 291 (1): 109–117. doi:10.1127/njgpa/2019/0792. ISSN 0077-7749.
  2. ^ a b c d e f g h i j Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Jurassic, Asia)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 550–552. ISBN 0-520-24209-2.
  3. ^ "Table 13.1," in Weishampel, et al. (2004). Page 263.