Castilletes Formation
| Castilletes Formation Stratigraphic range: Burdigalian-Langhian (Colloncuran-Friasian) ~ | |
|---|---|
| Type | Geological formation |
| Unit of | Cocinetas Basin |
| Underlies | Ware Formation |
| Overlies | Jimol Formation |
| Thickness | up to 440 m (1,440 ft) |
| Lithology | |
| Primary | Mudstone, siltstone |
| Other | Sandstone |
| Location | |
| Coordinates | 11°56′48.48″N 71°19′56″W / 11.9468000°N 71.33222°WCoordinates: 11°56′48.48″N 71°19′56″W / 11.9468000°N 71.33222°W |
| Approximate paleocoordinates | 11°12′N 68°36′W / 11.2°N 68.6°W |
| Region | La Guajira Caribbean region |
| Country |  Colombia |
| Type section | |
| Named for | Castilletes |
| Named by | Rollins |
| Location | Uribia |
| Year defined | 1965 |
| Coordinates | 11°56′48.48″N 71°19′56″W / 11.9468000°N 71.33222°W |
| Region | La Guajira |
| Country | Colombia |
  Type locality of the formation in La Guajira | |
The Castilletes Formation (Spanish: Formación Castilletes, N1c) is a fossiliferous geological formation of the Cocinetas Basin in the northernmost department of La Guajira, Colombia. The formation consists of fossiliferous mudstones, siltstones and medium-grained to conglomeratic fossiliferous lithic to quartzitic sandstones. The Castilletes Formation dates to the Neogene period; Burdigalian to Langhian stages, Colloncuran and Friasian in the SALMA classification, and has a maximum thickness of 440 metres (1,440 ft).
Etymology[]
The formation was defined by Rollins in 1965 and named after the village of Castilletes.[1]
Description[]
Lithologies[]
The Castilletes Formation consists of fossiliferous mudstones, siltstones and medium-grained to conglomeratic fossiliferous lithic to quartzitic sandstones.[2]
Stratigraphy and depositional environment[]
The Castilletes Formation overlies the Jimol Formation and is overlain by the Ware Formation. The age has been estimated to be Middle Miocene (16.7 to 14.2 Ma), Colloncuran and Friasian in the SALMA classification. The invertebrate fauna of the Castilletes Formation is highly similar not only to that of the underlying Jimol Formation, but also to the Cantaure Formation of Venezuela.[3] The Castilletes Formation was deposited in a shallow marine (estuarine, lagoonal, and shallow subtidal) to fluvio-deltaic environment with strong fluvial influence.[4] The Castilletes Formation correlates with the upper and of the Venezuelan . This unit is also correlative with the of the Paraguaná Peninsula in Venezuela.[5]
Fossil content[]
See also[]
Geology of the Eastern Hills
Cesar-Ranchería Basin- Honda Group
Abanico, Pebas, Pisco Formations
References[]
- ^ Moreno et al., 2015, p.27
- ^ Moreno et al., 2015, pp.27-32
- ^ Moreno et al., 2015, p.31
- ^ Rodríguez & Londoño, 2002, p.138
- ^ Moreno et al., 2015, p.32
- ^ Carillo, 2018, p.142
- ^ Suárez et al., 2015, p.4
- ^ Amson et al., 2016, p.7
- ^ a b c d Moreno et al., 2015, p.35
- ^ Moreno Bernal, 2014, p.7
- ^ Moreno Bernal, 2014, p.11
- ^ Moreno Bernal, 2014, p.13
- ^ Moreno Bernal, 2014, p.15
- ^ Moreno Bernal, 2014, p.19
- ^ Moreno Bernal, 2014, p.26
- ^ Moreno Bernal, 2014, p.29
- ^ Moreno Bernal, 2014, p.30
- ^ Cadena & Jaramillo, 2015, p.190
- ^ a b Cadena & Jaramillo, 2015, p.194
- ^ Cadena & Jaramillo, 2015, p.196
- ^ Kaitamana at Fossilworks.org
- ^ Moreno et al., 2015, p.29
- ^ Hendy et al., 2015, p.52
- ^ Hendy et al., 2015, p.53
- ^ Hendy et al., 2015, p.54
Bibliography[]
Local geology[]
- . 2010. Guajira Basin - Colombia Open Round 2010, 1. . Accessed 2017-08-30.
- ; ; ; ; ; ; ; , and . 2015. Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia. Swiss Journal of Palaeontology 134. 5–43. Accessed 2017-08-08.
- , and . 2002. Mapa geológico del Departamento de La Guajira - 1:250,000, 1–259. INGEOMINAS. Accessed 2017-08-08.
Paleontology[]
- ; , and . 2016. Neogene sloth assemblages (Mammalia, Pilosa) of the Cocinetas Basin (La Guajira, Colombia): Implications for the Great American Biotic Interchange. Palaeontology _. 1–20. Accessed 2017-08-31.
- , and . 2015. Early to middle Miocene turtles from the northernmost tip of South America: giant testudinids, chelids, and podocnemidids from the Castilletes Formation, Colombia. Ameghiniana 52. 188–203. Accessed 2017-08-08.
- . 2018. Systematics of the South American Native Ungulates and the Neogene Evolution of Mammals from Northern South America (PhD thesis), 1–285. University of Zurich. Accessed 2018-05-15.
- ; ; ; , and . 2015. Neogene molluscs, shallow marine paleoenvironments, and chronostratigraphy of the Guajira Peninsula, Colombia. Swiss Journal of Palaeontology 134. 45–75. Accessed 2017-08-08.
- . 2014. Fossil Crocodilians from the High Guajira Peninsula of Colombia, and the History of Neogene Crocodilian Diversity in Tropical South America, 1–66. University of Nebraska. Accessed 2017-08-08.
- ; ; , and . 2015. Insights into the Neotropics prior to the Great American Biotic Interchange: new evidence of mammalian predators from the Miocene of Northern Colombia. Journal of Vertebrate Paleontology e1029581. 1–10. Accessed 2017-08-31.
Maps[]
- ; ; ; ; ; ; ; , and . 2008. Plancha 3 - Puerto Estrella - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- ; ; ; ; ; ; ; , and . 2008. Plancha 5 - Bahía Portete - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- ; ; ; ; ; ; ; , and . 2008. Plancha 10 - Rancho Grande - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- ; ; ; ; ; ; ; , and . 2008. Plancha 10bis - Rancho Grande - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
- Geologic formations of Colombia
- Neogene Colombia
- Burdigalian
- Langhian
- Miocene Series of South America
- Colloncuran
- Friasian
- Mudstone formations
- Siltstone formations
- Sandstone formations
- Deltaic deposits
- Fluvial deposits
- Shallow marine deposits
- Fossiliferous stratigraphic units of South America
- Paleontology in Colombia
- Geography of La Guajira Department