| Revista: | Anais da Academia Brasileira de Ciencias |
| Base de datos: | PERIÓDICA |
| Número de sistema: | 000412244 |
| ISSN: | 0001-3765 |
| Autores: | Piovesan, Enelise K1 Melo, Robbyson M1 Lopes, Fernando M2 Fauth, Gerson3 Costa, Denize S3 |
| Instituciones: | 1Universidade Federal de Pernambuco, Centro de Tecnologia e Geociencias, Recife, Pernambuco. Brasil 2Universidade do Vale do Rio dos Sinos, Instituto Tecnologico de Micropaleontologia, Sao Leopoldo, Rio Grande do Sul. Brasil 3Petroleo Brasileiro S.A., Centro de Pesquisa, Rio de Janeiro. Brasil |
| Año: | 2017 |
| Periodo: | Sep |
| Volumen: | 89 |
| Número: | 3 |
| Paginación: | 1443-1464 |
| País: | Brasil |
| Idioma: | Inglés |
| Tipo de documento: | Artículo |
| Enfoque: | Analítico, descriptivo |
| Resumen en inglés | Paleocene ostracods and planktonic foraminifera from the Maria Farinha Formation, Paraíba Basin, are herein presented. Eleven ostracod species were identified in the genera Cytherella Jones, Cytherelloidea Alexander, Eocytheropteron Alexander, Semicytherura Wagner, Paracosta Siddiqui, Buntonia Howe, Soudanella Apostolescu, Leguminocythereis Howe and, probably, Pataviella Liebau. The planktonic foraminifera are represented by the genera Guembelitria Cushman, Parvularugoglobigerina Hofker, Woodringina Loeblich and Tappan, Heterohelix Ehrenberg, Zeauvigerina Finlay, Muricohedbergella Huber and Leckie, and Praemurica Olsson, Hemleben, Berggren and Liu. The ostracods and foraminifera analyzed indicate an inner shelf paleoenvironment for the studied section. Blooms of Guembelitria spp., which indicate either shallow environments or upwelling zones, were also recorded reinforcing previous paleoenvironmental interpretations based on other fossil groups for this basin |
| Disciplinas: | Biología |
| Palabras clave: | Crustáceos, Paleontología, Protozoarios, Registro fósil, Ostracoda, Foraminifera, Paleoceno, Brasil |
| Keyword: | Biology, Crustaceans, Paleontology, Protozoa, Fossil record, Ostracoda, Foraminifera, Paleocene, Brazil |
| Texto completo: | Texto completo (Ver HTML) |
