Ware Formation
Stratigraphic range: Late Miocene-Early Pleistocene, typically Pliocene
~3.5–2.8 Ma

PreЄ

Type| Geological formation
Unit of| Cocinetas Basin
Underlies| Alluvium
Overlies| Castilletes Formation
Thickness| up to 25 m (82 ft)
Lithology
Primary| Sandstone, mudstone
Other| Conglomerate
Location
Coordinates|  [ ⚑ ] : 11°51′4.32″N 71°19′26.4″W﻿ / ﻿11.8512°N 71.324°W﻿ / 11.8512; -71.324
Paleocoordinates|  [ ⚑ ] 11°42′N 70°48′W﻿ / ﻿11.7°N 70.8°W﻿ / 11.7; -70.8
Region| La Guajira
Caribbean region
Country|  Colombia
Type section
Named for| Wayuunaiki: "friend"
Named by| Moreno et al.
Location| Uribia
Year defined| 2015
Coordinates|  [ ⚑ ] 11°51′4.32″N 71°19′26.4″W﻿ / ﻿11.8512°N 71.324°W﻿ / 11.8512; -71.324
Region| La Guajira
Country|  Colombia

Type locality of the formation in La Guajira

The Ware Formation (Spanish: Formación Ware) is a fossiliferous geological formation of the Cocinetas Basin in the northernmost department of La Guajira. The formation consists of fine lithic to quartzitic sandstones, mudstones, pebbly conglomerates with sedimentary and metamorphic rock fragments, fossiliferous packstones and sandy to conglomeratic beds with high fossil content. The Ware Formation dates to the Neogene and Quaternary periods; Late Miocene to Early Pleistocene epochs, typically Pliocene (3.5 to 2.8 Ma), Uquian, Chapadmalalan and Montehermosan in the SALMA classification, and has a maximum thickness of 25 metres (82 ft).

## Contents

* 1 Etymology
* 2 Description
* 2.1 Lithologies
* 2.2 Stratigraphy and depositional environment
* 2.3 Fossil content
* 3 See also
* 4 References
* 4.1 Bibliography
* 4.1.1 Local geology
* 4.1.2 Paleontology
* 4.1.3 Maps

## Etymology

The formation was defined in 2015 by Moreno et al., and given the name Ware, meaning "friend" in Wayuunaiki, the language of the local indigenous Wayuu, meaning "friend". The name has been given to pay tribute to the friendship between Colombia and Venezuela.[1]

## Description

### Lithologies

The Ware Formation consists of fine lithic to quartzitic sandstones, mudstones, pebbly conglomerates with sedimentary and metamorphic rock fragments, fossiliferous packstones and sandy to conglomeratic beds with high fossil content.[2]

### Stratigraphy and depositional environment

The Ware Formation overlies the Castilletes Formation and is overlain by Quaternary alluvium. The age has been estimated to be Late Miocene to Early Pleistocene (5.2 to 1.22 Ma), Uquian, Chapadmalalan and Montehermosan in the SALMA classification, with a narrow definition in the Pliocene (3.5 to 2.8 Ma). The marine invertebrate fauna of the Ware Formation shows a greater similarity with modern assemblages offshore of the Guajira Peninsula than with those of the underlying units.[3] The base of the Ware Formation was deposited in a fluvio-deltaic environment, whereas the marine invertebrate assemblage at the top of the unit contains taxa typical of exposed open-ocean shoreface and nearshore settings, but with proximity to coral reef habitats. The Ware Formation correlates with the San Gregorio Formation in the Venezuelan Falcón Basin.[4]

### Fossil content

Group  | Fossils  | Notes

|
|

Mammals | Camelidae, Glyptodontidae, Pampatheriidae, Proterotheriidae, Toxodontidae, Caviidae, Erethizontidae |

[5]

Tardigrada gen. et sp. indet. |

[6]

Mylodontidae gen. et sp. indet. |

[6]

Lestodontini gen. et sp. nov. |

[7]

Scelidotheriinae gen. et sp. indet., ?Hyperleptus sp. |

[8]

Megalonychidae gen. et sp. nov. |

[9]

Pliomegatherium lelongi |

[10]

Nothrotherium sp. |

[11]

Chapalmalania sp. |

[12]

Hydrochoeropsis wayuu |

[13]

Reptiles | Crocodylus sp., Crocodylidae indet., Alligatoridae, Podocnemididae |

[5][14]

Fish | Characidae, Cynodontidae, Serrasalmidae, Cichlidae, Sciaenidae, Doradidae, Pimelodidae, Carcharhinidae, Sphyrnidae, Myliobatidae, Pristidae |

[5]

Invertebrates | Argopecten sp., Euvola sp., Nodipecten sp., Crassostrea sp., Plicatula sp., Spondylus sp., Anodontia sp., Codakia sp., Bulla sp., Laevicardium sp., Trachycardium sp., Macrocallista sp. |

[3]

## See also

Geology of the Eastern Hills
Cesar-Ranchería Basin
Honda Group
Chorrera, Pisco, Tilatá, Tunjuelo Formations
Urumaco

## References

1. ↑ Moreno et al., 2015, p.32
2. ↑ Moreno et al., 2015, pp.32-34
3. ↑ 3.0 3.1 Moreno et al., 2015, p.33
4. ↑ Moreno et al., 2015, p.34
5. ↑ 5.0 5.1 5.2 Moreno et al., 2015, p.35
6. ↑ 6.0 6.1 Amson et al., 2016, p.3
7. ↑ Amson et al., 2016, p.4
8. ↑ Amson et al., 2016, p.7
9. ↑ Amson et al., 2016, p.8
10. ↑ Amson et al., 2016, p.9
11. ↑ Amson et al., 2016, p.12
12. ↑ Amson et al., 2016, p.15
13. ↑ Pérez et al., 2017
14. ↑ Police Station 470062 at Fossilworks.org

### Bibliography

#### Local geology

* Moreno, F.; A.J.W. Hendy; L. Quiroz; N. Hoyos; D.S. Jones; V. Zapata; S. Zapata; G.A. Ballen, and Edwin Cadena, A.L. Cárdenas, J.D. Carrillo Briceño, J.D. Carrillo, D. Delgado Sierra, J. Escobar, J.I. Martínez, C. Martínez, C. Montes, J. Moreno, N. Pérez, R. Sánchez, C. Suárez, M.C. Vallejo Pareja, C. Jaramillo. 2015. Revised stratigraphy of Neogene strata in the Cocinetas Basin, La Guajira, Colombia. Swiss Journal of Palaeontology 134\. 5–43. Accessed 2017-08-08.
* Rodríguez, Gabriel, and Ana Cristina Londoño. 2002. Mapa geológico del Departamento de La Guajira - 1:250,000, 1–259. INGEOMINAS. Accessed 2017-08-08.

#### Paleontology

* Amson, Eli; Juan D. Carrillo, and Carlos Jaramillo. 2016. Neogene sloth assemblages (Mammalia, Pilosa) of the Cocinetas Basin (La Guajira, Colombia): Implications for the Great American Biotic Interchange. Palaeontology _. 1–20. Accessed 2017-03-31.
* Hendy, Austin J.W.; Douglas S. Jones; Federico Moreno; Vladimir Zapata, and Carlos Jaramillo. 2015. Neogene molluscs, shallow marine paleoenvironments, and chronostratigraphy of the Guajira Peninsula, Colombia. Swiss Journal of Palaeontology 134\. 45–75. Accessed 2017-08-08.
* Pérez, María E.; María C. Vallejo Pareja; Juan D. Carrillo, and Carlos Jaramillo. 2017. A New Pliocene Capybara (Rodentia, Caviidae) from Northern South America (Guajira, Colombia), and its Implications for the Great American Biotic Interchange. Journal of Mammalian Evolution 24\. 111–125. Accessed 2017-04-04.

#### Maps

* Zuluaga, Carlos A.; Alberto Ochoa; Carlos A. Muñoz; Camilo E. Dorado; Nathalia M. Guerrero; Ana M. Martínez; Paula A. Medina; Edgar F. Ocampo, and Alejandro Pinilla and Paula A. Ríos, Bibiana P. Rodríguez, Edward A. Salazar, Vladimir L. Zapata. 2008. Plancha 3 - Puerto Estrella - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
* Zuluaga, Carlos A.; Alberto Ochoa; Carlos A. Muñoz; Camilo E. Dorado; Nathalia M. Guerrero; Ana M. Martínez; Paula A. Medina; Edgar F. Ocampo, and Alejandro Pinilla and Paula A. Ríos, Bibiana P. Rodríguez, Edward A. Salazar, Vladimir L. Zapata. 2008. Plancha 5 - Bahía Portete - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
* Zuluaga, Carlos A.; Alberto Ochoa; Carlos A. Muñoz; Camilo E. Dorado; Nathalia M. Guerrero; Ana M. Martínez; Paula A. Medina; Edgar F. Ocampo, and Alejandro Pinilla and Paula A. Ríos, Bibiana P. Rodríguez, Edward A. Salazar, Vladimir L. Zapata. 2008. Plancha 10 - Rancho Grande - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.
* Zuluaga, Carlos A.; Alberto Ochoa; Carlos A. Muñoz; Camilo E. Dorado; Nathalia M. Guerrero; Ana M. Martínez; Paula A. Medina; Edgar F. Ocampo, and Alejandro Pinilla and Paula A. Ríos, Bibiana P. Rodríguez, Edward A. Salazar, Vladimir L. Zapata. 2008. Plancha 10bis - Rancho Grande - 1:100,000, 1. INGEOMINAS. Accessed 2017-06-06.

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