Canoa Formation
In today's article we are going to talk about Canoa Formation, a topic that has captured the attention of many people in recent times. Canoa Formation is a topic that arouses curiosity and interest in a large number of people due to its relevance in today's society. Throughout this article we will explore different aspects related to Canoa Formation, from its origin and evolution to its impact on everyday life. In addition, we will analyze the opinions of experts in the field and present relevant data that will help to better understand Canoa Formation and its importance today. Without a doubt, Canoa Formation is a topic that deserves to be explored in depth to understand its influence in different areas of modern life.
| Canoa Formation | |
|---|---|
| Stratigraphic range: Piacenzian-Calabrian (Chapadmalalan-Uquian) ~ | |
| Type | Geological formation |
| Lithology | |
| Primary | Sandstone |
| Location | |
| Coordinates | 1°06′S 80°54′W / 1.1°S 80.9°W |
| Approximate paleocoordinates | 1°12′S 80°30′W / 1.2°S 80.5°W |
| Region | Manabí & Santa Elena Provinces |
| Country |  Ecuador |
| Type section | |
| Named for | Canoa |
  Canoa Formation (Ecuador) | |
The Canoa Formation is a Piacenzian to Calabrian (Chapadmalalan to Uquian in the SALMA classification) geologic formation in Ecuador. The sandstones were deposited in a coastal environment.[1] The formation is correlated to the Charco Azul Formation of western Panama and southeastern Costa Rica.[2]
Fossil content
The formation has provided bivalve, gastropod, crustacean, echinoid and scaphopod fossils and vertebrates of:
See also
References
- ^ Canoa Formation at Fossilworks.org
- ^ Charco Azul Formation at Fossilworks.org
Further reading
- G. Bianucci, C. Di Celma, W. Landini and J. Buckeridge. 2006. Palaeoecology and taphonomy of an extraordinary whale barnacle accumulation from the Plio-Pleistocene of Ecuador. Palaeogeography, Palaeoclimatology, Palaeoecology 242:326-342
- H. A. Pilsbry and A.A. Olsson. 1941. A Pliocene fauna from Western Ecuador. Proceedings of the Natural Sciences of Philadelphia 93:1-79