Balumtun Sandstone

Balumtun Sandstone
Stratigraphic range: Aquitanian
~23–22.5 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeFormation
Unit ofRío Concepción Group
UnderliesTulijá Formation
OverliesMazantic Shale
Thickness760 metres
Lithology
PrimarySandstone
OtherConglomerate
Location
Coordinates17°06′N 92°42′W / 17.1°N 92.7°W / 17.1; -92.7
Approximate paleocoordinates17°42′N 89°00′W / 17.7°N 89.0°W / 17.7; -89.0
RegionChiapas
Country Mexico
Type section
Named forBalumtun

The Balumtun Sandstone is a geologic formation in Chiapas, Mexico. The formation is up to 760 metres thick, and consists of gray sandstone, that were deposited during the Upper Aquitanian stage of the Early Miocene.[1]

See also

References

  1. ^ Carbot-Chanona, Gerardo; Rivera-Velázquez, Gustavo; Jiménez-Hidalgo, Eduardo; Reynoso, Víctor Hugo (December 2020). "The first Pan-Carettochelys turtle in the Neogene of the American continent and its paleobiogeographical relevance". Journal of South American Earth Sciences. 104: 102925. Bibcode:2020JSAES.10402925C. doi:10.1016/j.jsames.2020.102925. S2CID 224976641.
  • Various Contributors to the Paleobiology Database. "Fossilworks: Gateway to the Paleobiology Database". Retrieved 17 December 2021.

Further reading

  • M. d. C. Perrilliat, F. J. Vega, and M. A. Coutiño. 2010. Miocene mollusks from the Simojovel area in Chiapas, southwestern Mexico. Journal of South American Earth Sciences 30:111-119
  • S. D. Webb, B. L. Beatty, and G. Poinar, Jr. 2003. New evidence of Miocene Protoceratidae including a new species from Chiapas, Mexico. Bulletin of the American Museum of Natural History 279:348-367


  • v
  • t
  • e

This article related to the Neogene period is a stub. You can help Wikipedia by expanding it.

  • v
  • t
  • e