77
Views
37
CrossRef citations to date
0
Altmetric
Original Articles

A marine ichthyofauna from the Miocene of Panama, and the Tertiary Caribbean faunal province

Pages 172-186 | Published online: 24 Aug 2010
 

ABSTRACT

The marine vertebrate fauna collected from the Gatún Formation, middle Miocene of Panama, includes the following genera in the non-otolith assemblage: Carcharodon, Procarcharodon, Ginglymostoma, Hemipristis, Galeocerdo cf. Carcharhinus, Sphyrna cf. Isistius, Dasyatis, Myliobatis, Rhinoptera, Aetobatus, Acipenser, Sphyraena, Trichiurus, Lepisosteus and unidentified crocodilian, chelonian, and mammalian taxa. The otolith assemblage consists of 20 taxa of bony fishes. The fauna contains a mixture of marine forms representing coastal to open-water habitats. The Gatún ichthyofauna compares favorably to the Miocene selachian fauna from Ecuador, the Miocene ichthyofaunas from the Caribbean, and the large ichthyofauna from the Pungo River Formation in North Carolina, U.S.A. These tropical occurrences collectively represent the vertebrate fauna of the Tertiary Caribbean Faunal Province that reached its greatest interoceanic connection between the Pacific and the Caribbean in the Miocene. The provincial limit of the Miocene vertebrates extended beyond the central Gulf of Mexico to include the southeast coast of the United States.

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.