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Neogene
Paleogene
Cretaceous


Compiled by: Jacques LeBlanc (2021), Stratigraphic Lexicon: The Onshore Cenozoic Sedimentary Formations of The Republic of Panama. Biosis: Biological Systems, vol. 2/1, 1-173. https://doi.org/10.37819/biosis.002.01.0095(or via https://sites.google.com/site/leblancjacques).

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Galique Formation

Galique Fm


Period: 
Neogene

Age Interval: 
Early Miocene (Burdigalian?) - Ministerio de Comercio e Industrias (1991)


Province: 
Tonosí & Azuero basin

Type Locality and Naming

Unknown

Synonym:


Lithology and Thickness

No formal description of the formation could be found.


Lithology Pattern: 
No Data


Relationships and Distribution

Lower contact

Since Ministerio de Comercio e Industrias (1991) places the formation in the Upper Eocene to Oligocene and that more recent studies by Florida Museum (2011) and Perez-Consuegra et al. (2018) confirm it as Early Miocene, and that no formal description of the formation has been found so far, it is unclear what formation underlies it.

Upper contact

Since Ministerio de Comercio e Industrias (1991) places the formation in the Upper Eocene to Oligocene and that more recent studies by Florida Museum (2011) and Perez-Consuegra et al. (2018) confirm it as Early Miocene, and that no formal description of the formation has been found so far, it is unclear what formation overlies it.

Regional extent

(Geo-JSON is left empty on purpose)


GeoJSON

null

Fossils


Age 


Age Span: 

    Beginning stage: 
Burdigalian

    Fraction up in beginning stage: 
0

    Beginning date (Ma): 
20.45

    Ending stage: 
Burdigalian

    Fraction up in the ending stage: 
1

    Ending date (Ma):  
15.99

Depositional setting


Depositional pattern:  


Additional Information

References:

  • Ministerio de Comercio e Industrias (1991). The legend of the map places the formation in the Upper Eocene to Oligocene.
  • Florida Museum (2011) states “Roger and Austin continued westward to the city of David, in Panama’s Chiriqui Province, where the PCP-PIRE team has recently begun paleontological reconnaissance. The rocks exposed to the east and north of David are of the Galique Fm, which appears to be intermediate in age between the Culebra Fm and Gatún Fm we have been studying in the Panama Canal. Courtesy of AES Panama we were able to access outcrops at Presa Baragon, north of Gualaca, and make large collections of rich mollusk and crab assemblages. The Galique Fm appears to have a diverse Early-Middle Miocene fauna, which has never been described, and therefore is a critical new element to Panama’s Neogene fossil record”.
  • Making reference to a section of the western Azuero Peninsula, Perez-Consuegra et al. (2018) state “Mollusks associated with this section — Leopecten sp., Crassostrea sp., Ampullinopsis spenceri, Galeodea sp. and Ficus cf. F. carbasea and gastropod fossils of Naticidae, Muricidae, Antillophos aff. A. gatunensis, Conus sp., and Turridae — are similar to other faunas in Miocene strata from Panamá (e.g., Culebra Fm, Galique Fm, Gatún Fm and Chucunaque Fm; Hendy (2013)). The presence of Ampullinopsis spenceri in the lower part of the succession indicates an Early Miocene (Aquitanian – Burdigalian) age. Based on the data, we assign an Early Miocene age (Burdigalian?) to the sedimentary sequence in the Torio Beach”. See also Góngora-Blanco (2016) for a study on Torio Beach and Palo Seco Beach


Compiler:  

Jacques LeBlanc (2021), Stratigraphic Lexicon: The Onshore Cenozoic Sedimentary Formations of The Republic of Panama. Biosis: Biological Systems, 2(1), 173 pp. https://doi.org/10.37819/biosis.002.01.0095 (or via https://sites.google.com/site/leblancjacques)