Corral de Enmedio Formation

The Corral de Enmedio Formation is a Mesozoic geologic formation in Mexico.[1] The formation may be from the Kirtlandian land vertebrate age.[2] It has a similar fauna to the Packard Formation.[2]

Corral de Enmedio Formation
Stratigraphic range: Mesozoic
TypeGeological formation
Unit ofCabollona Group
Location
Country Mexico

Paleofauna

The fragmentary remains of indeterminate lepisosteids, trionychids, eusuchians, hadrosaurids, and ceratopsids are known from the Corral de Enmedio Formation.

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
Vertebrates of the Corral de Enmedio Formation
Genus Species Location Stratigraphic position Abundance Notes

Albertosaurus[3]

Indeterminate[3]

Chamops[2]

C. segnis[2]

Melvius[2]

Indeterminate[2]

Trachodon[1]

T. mirabilis[1]

Later found to be indeterminate hadrosaurid remains.[1]

See also

Footnotes

  1. Weishampel, et al. (2004). "Dinosaur distribution." Pp. 517-607.
  2. "Corral De Enmedio and Packard Formations, Cabollona Group, Sonora, Mexico," in Sullivan and Lucas (2006). Page 16.
  3. Listed as "cf. Albertosaurus sp." "Corral De Enmedio and Packard Formations, Cabollona Group, Sonora, Mexico," in Sullivan and Lucas (2006). Page 16.

References

  • Sullivan, R.M., and Lucas, S.G. 2006. "The Kirtlandian land-vertebrate "age" – faunal composition, temporal position and biostratigraphic correlation in the nonmarine Upper Cretaceous of western North America." New Mexico Museum of Natural History and Science, Bulletin 35:7-29.
  • Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.


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