Loma Candela Formation
From Wikipedia the free encyclopedia
Loma Candela Formation | |
---|---|
Stratigraphic range: Lutetian | |
Type | Formation |
Lithology | |
Primary | Limestone, marl |
Other | Conglomerate, sandstone |
Location | |
Coordinates | 22°06′N 80°30′W / 22.1°N 80.5°W |
Approximate paleocoordinates | 22°18′N 71°24′W / 22.3°N 71.4°W |
Country | Cuba |
The Loma Candela Formation is a geologic formation in Cuba. It preserves fossils dating back to the Paleogene period.[1]
Description
[edit]The formation consists of limestones, yellowish calcareous marls and coastal conglomerates and fine calcareous sandstones. The Loma Candela Formation was deposited in a marine environment. It overlies the Universidad Formation and is correlated with the Tallahassee and Lake City Formations of Florida.[1]
Fossil content
[edit]See also
[edit]References
[edit]- ^ a b Loma Candela Formation at Fossilworks.org
Further reading
[edit]- Bermúdez, Pedro J (1961), "Las formaciones geológicas de Cuba" (PDF), Geología Cubana, 1: 1–180, retrieved 2019-02-06
- B. M. Cutress. 1980. Cretaceous and Tertiary Cidaroida (Echinodermata: Echinoidea) of the Caribbean Area. Bulletins of American Paleontology 77(309):1-221