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Asencio Formation: Difference between revisions

Coordinates: 33°00′S 57°12′W / 33.0°S 57.2°W / -33.0; -57.2
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[[Category:Sandstone formations]]
[[Category:Sandstone formations]]
[[Category:Paleontology in Uruguay]]
[[Category:Paleontology in Uruguay]]
[[Category:Paraná Basin]]
[[Category:Paraná Basin|Formations]]
[[Category:Colonia Department|Formations]]
[[Category:Colonia Department|Formations]]
[[Category:Río Negro Department|Formations]]
[[Category:Río Negro Department|Formations]]

Revision as of 16:51, 7 September 2018

Asencio Formation
Stratigraphic range: Campanian-Maastrichtian
TypeGeological formation
Sub-unitsDel Palacio Member
Lithology
PrimarySandstone
Location
Coordinates33°00′S 57°12′W / 33.0°S 57.2°W / -33.0; -57.2
Approximate paleocoordinates36°36′S 41°36′W / 36.6°S 41.6°W / -36.6; -41.6
RegionColonia, Río Negro, Soriano, Tacuarembó
Country Uruguay
ExtentParaná Basin
Type section
Named forCry of Asencio

The Asencio Formation is a geological formation in the Paraná Basin of southwestern Uruguay whose strata date back to the Late Cretaceous (Campanian-Maastrichtian). Dinosaur remains are among the fossils that have been recovered from the formation.[1]

Vertebrate paleofauna

Fossil eggs

See also

References

  1. ^ Weishampel, David B; et al. (2004). "Dinosaur distribution (Late Cretaceous, South America)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 600-604. ISBN 0-520-24209-2.
  2. ^ a b c Drable-Palmitas at Fossilworks.org
  3. ^ a b Mones, A. (1980) "Nuevos elementos de la paleoherpetofauna del Uruguay (Crocodilia y Dinosauria)." Actas II Congreso Argentino de Paleontologia y Bioestratigrafia y I Congreso Latinoamericano, Buenos Aires 1:265-277 (in Spanish)

Further reading

  • F. v. Huene. 1929. Terrestrische Oberkreide in Uruguay [The terrestrial Upper Cretaceous in Uruguay]. Centralblatt für Mineralogie, Geologie und Paläontologie Abteilung B 1929:107-112