CV Lattes
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Universidade Estadual Paulista (UNESP). Campus de Rio Claro. Instituto de Geociências e Ciências Exatas (IGCE) (Institutional affiliation from the last research proposal) Birthplace: Brazil
graduation at Geologia from Universidade Estadual Paulista Júlio de Mesquita Filho (1979), master's at Geology from Universidade Estadual Paulista Júlio de Mesquita Filho (1990) and doctorate at Geology from Universidade de São Paulo (1996). Has experience in Geosciences, focusing on Stratigraphic, acting on the following subjects: pantanal mato-grossense, bacia do paraná, geomorfologia fluvial, estratigrafia and bacia do araripe. (Source: Lattes Curriculum)
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Late Pleistocene to Holocene paleo-hydrologic changes are recorded in the landscape and sedimentary record of the Pantanal wetlands, central-west Brazil. Environmental changes are mainly controlled by climatic events that took place since the aridity during the Last Glacial Maximum to more humid conditions prevailing during the Holocene and by structural factors related to the tectonic r…
The Cretaceous (145.5 - 65.5 Ma) was a period characterized by several environmental changes triggered by intense volcanic and tectonic activity. The occurrence of large igneous provinces (LIPs) had a significant impact on the concentrations of greenhouse gases, including carbon dioxide (CO2), raising the temperature of the planet. Despite the dominance of arid and semi-arid conditions, m…
The Cretaceous deposits from the Araripe Basin record the opening of the Atlantic Ocean and the earliest marine incursions in the northeastern Brazil following the Gondwana fragmentation. Although recording important chapter of the Earth's history, the Araripe Basin has been studied more often paleontologically - mainly taxonomically - due to the high quality of fossil preservation. The e…
This project aims to develop depositional models for different preserved fluvial fan systems on the rock record through highly-detailed studies of the preserved sedimentary facies and architectural elements on recent and modern-day fluvial fan systems from the Pantanal wetlands in western Brazil. The motivation of this project is to understand the relationship between the reserved deposit…
The Taquari alluvial megafan is a multi-fan depositional system. The system covers 37% of the total Pantanal area and displays a circular geometry and a length of 250km from the apex to the toe. Three subsystems characterize the natural landscape: a meander belt in the upper fan; an active depositional lobe in the middle and lower fan, and several abandoned lobes with intricate network of…
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