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Neogene sharks and rays from the Brazilian 'Blue Amazon'
Orangel Aguilera1,2, Zoneibe Luz2, Jorge D Carrillo-Briceño3
1Departamento de Biologia Marinha, Instituto de Biologia, Universidade Federal Fluminense, Niterói, Rio de Janeiro, Brasil.
Plos One
|August 24, 2017
Summary
The early Miocene Pirabas Formation in Brazil reveals a diverse shark and ray fauna, similar to the proto-Caribbean but unique to the Atlantic coast. Paleotemperature data suggest a tropical marine environment with distinct inshore and offshore habitats.
Area of Science:
- Paleontology
- Marine Biology
- Geochemistry
Background:
- The lower Miocene Pirabas Formation in Northern Brazil experienced significant ecological niche changes.
- This formation was influenced by the proto-Amazon River and is characterized by marine, carbonate-rich beds.
Purpose of the Study:
- To investigate the elasmobranch fauna of the Pirabas Formation to understand early Miocene ecological changes.
- To reconstruct paleotemperatures and paleoecology using phosphate oxygen isotope analysis of elasmobranch teeth.
Main Methods:
- Systematic identification of elasmobranch taxa (sharks and rays).
- Analysis of phosphate oxygen isotope composition in elasmobranch teeth.
- Comparison of fossil fauna with modern assemblages and other Neogene fish assemblages.
Main Results:
- A diverse fauna of 24 elasmobranch taxa was identified, dominated by carcharhiniforms and myliobatiforms.
- Faunal composition resembles proto-Caribbean early Miocene assemblages but is unique for the Atlantic coast of the Americas.
- Isotope data indicate a tropical marine setting with inshore and offshore habitats, and probable depth preferences for certain taxa.
Conclusions:
- The Pirabas Formation provides a unique Neogene fossil fish assemblage from the Atlantic coast.
- Paleoecological reconstructions suggest predominantly coastal and shallow water habitats for key taxa.
- Variations in modern selachian isotope composition indicate increased Amazon River influence on coastal waters in the Holocene compared to the early Miocene.
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