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)