Paul Yves Jean Antonio in research grants and scholarships supported by FAPESP.
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The Neoproterozoic is a period marked by extreme climatic variations with the possibility of events of snowball earth but also by the Ediacaran biotic revolution. This period (1000 - 541 Ma) corresponds to the transition between the supercontinent Rodinia and the amalgamation of Gondwana. Due to a poor paleomagnetic database for the different cratons, the paleogeography during this period…
During Paleoproterozoic (1.98 to 1.78 Ga) anorogenic plutonism AMGC type designated by the event Uatuma covers a vast area of northern Amazonian craton. Locally, the event has received other names, such as Surumu, Iriri, Sobreiro and Colider, exposed in the states of Roraima (Group Surumu), Para (Group Iriri, Sobreiro) and Mato Grosso (Group Iriri and Intrusive Suite Colider). Surumu Grou…
The Neoproterozoic era (1000 - 541 Ma) was a turning point in Earth's history. It is a period of great biological changes between the microbial Precambrian life and the Ediacaran biotic revolution with the earliest multicellular organisms. In parallel, this period is marked by a large continental reorganization (Rodinia-Gondwana transition) and by major climatic changes (snowball earth ev…
The Amazonian Craton is one of the largest pieces of the Columbia "puzzle". It covers almost half the surface of Brazil and some parts of Bolivia, Colombia, Venezuela, Guyana, Suriname and French Guiana in South America. Its geological evolution is unique compared to that of other cratons in the continent, bearing more similarities with the evolution of Laurentia, Baltica, and West Africa…
| 2 / 2 | Completed scholarships in Brazil |
| 2 / 2 | Completed scholarships abroad |
| 4 / 4 | All Scholarships |
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