graduation at Geografia from Faculdade de Filosofia Letras e Ciências Humanas (1988) and doctorate at Geology from Universidade de São Paulo (1992). He is currently full professor at Universidade Estadual Paulista Júlio de Mesquita Filho. Has experience in Geosciences, acting on the following subjects: tafonomia, taphonomy, paleontologia, bacia do paraná and permiano. (Source: Lattes Curriculum)
| Articles published in Pesquisa FAPESP Magazine about the researcher: |
| Por qué Crato preserva fósiles |
| Why Crato uniquely preserves fossils |
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| News published in Agência FAPESP Newsletter about the researcher |
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| TITULO |
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| VEICULO: TITULO (DATA) |
| VEICULO: TITULO (DATA) |
The main goal of this research Project is to seek funds to allow Dr. ARTURO CÉSAR TABOADA, CONICET, Argentina, to come to Brazil to interact with members of our research group in the study of Late Paleozoic brachiopods of the Parana Basin. Dr. ARTURO is a leading scientist in Late Paleozoic brachiopods of Gondwana, and is interested in coeval Brazilian material. If approved the project wi…
(Only some records are available in English at this moment)
Mollusk bivalves of the Brazilian Cretaceous were, generally, widely studied since the second half of the 19th century. However, even if this assertion is true for the bivalves of the Sergipe and Paraná sedimentary basins, the same cannot be said about the Araripe Basin, Northeastern Brazil. Likewise, when compared with other South American localities, such as Argentina, there are remarka…
The geological events related to the final stages of the Gondwana breakup and the subsequent opening of the South Atlantic Ocean caused fault reactivation of the Proterozoic Borborema Province and originated the Cretaceous deposits of the Araripe Basin. During Aptian times a widespread transgression took place in the Northeastern Brazil, culminating with the deposition of the marine strat…
The Cretaceous (i.e., Crato and Romualdo formations) of the Araripe Basin, records some of the most spectacular fossil-rich deposits (Konservat-Largestätten) of the Mesozoic, which were generated during the Gondwana break-up and consequently South Atlantic Ocean opening. Because of that, upper units of the Santana Group (i.e., Romualdo Formation) record a main Aptian marine transgression.…
(Only some records are available in English at this moment)
| 11 / 6 | Completed research grants |
| 30 / 13 | Completed scholarships in Brazil |
| 41 / 19 | All research grants and scholarships |
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CV Lattes
ORCID