Article · Wikipedia archive · Last revised Jul 17, 2026

Letrero Formation

The Letrero Formation is a Late Miocene geologic formation in south-central Ecuador. The formation comprises lacustrine sediments with strong fluvial clastic input and contains siltstones and fine-grained sandstones.

Last revised
Jul 17, 2026
Read time
≈ 1 min
Length
237 w
Citations
6
Source
Letrero Formation
Stratigraphic range: Late Miocene
(Mayoan-Montehermosan)
~
TypeGeological formation
Lithology
PrimarySiltstone
OtherSandstone
Location
Coordinates3°18′S 79°06′W / 3.3°S 79.1°W / -3.3; -79.1
Approximate paleocoordinates3°42′S 77°24′W / 3.7°S 77.4°W / -3.7; -77.4
RegionAzuay Province
CountryEcuador
ExtentSierra Region
Letrero Formation (Ecuador)

The Letrero Formation is a Late Miocene (Mayoan to Montehermosan in the SALMA classification) geologic formation in south-central Ecuador. The formation comprises lacustrine sediments with strong fluvial clastic input and contains siltstones and fine-grained sandstones.1

Fossil content

Mammals

Mammals of the Letrero Formation
Genus Species Location Material Notes Images
Litopterna1 Indeterminate RHM Locality 4 A litoptern.
Caviomorpha1 Indeterminate A caviomorph rodent.
Nabondasypus2 Nabondasypus maddeni Nabón basin Several osteoderms. An armadillo.
source ↗
Anadasypus3 A. aequatorianus RHM Locality 4 A member of cingulata.
Toxodontia1 Indeterminate A toxodont.
See also

See also

References

References

  1. RHM Locality 4 at Fossilworks.org
  2. Barasoain, D.; Zurita, A. E.; Carrión, J. L.; Ñauñay Michilena, D. A.; Luna, C. A.; Miño-Boilini, A. R. (2026). "New endemic Dasypodidae (Xenarthra, Cingulata) from the Late Miocene of Ecuador and the importance of the tropics in the cladogenesis of armadillos". Journal of Systematic Palaeontology. 24 2648714. doi:10.1080/14772019.2026.2648714.
  3. Carlini et al., 2014

Bibliography