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
Ph.D. student in geosciences at Universidade Estadual Paulista "Júlio de Mesquita Filho" (UNESP), with emphasis on stratigraphic analysis, paleomagnetism, and lithostratigraphic evolution. Awarded for best performance in graduation. Awarded with a Fapesp Direct Doctorate grant "EVOLUTION OF THE ZARQA VALLEY, JORDAN, DURING THE PLEISTOCENE IN THE CONTEXT OF THE FIRST HOMININ MIGRATIONS OUTSIDE AFRICA" (2022-2025), in addition to two scientific initiation studies, the first (2018-2019) entitled "TECHNOLOGICAL CHARACTERIZATION OF THE RIO CLARO FORMATION FOR USE AS CIVIL CONSTRUCTION SAND", on Monday (2019-2020) "PALEOMAGNETIC ANALYSIS OF ROCKS IN THE MANGABEIRA LAVRAS BASIN (CE)". (Source: Lattes Curriculum)
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The Zarqa Valley is a geomorphological feature a few kilometers from Amman (Jordan) that hosts tributary rivers with perennial water from the Jordan River. Its geological and archaeological importance is due to the fact that it has three floors of terraces, high, medium and low, all with hominin tools and distinct stratigraphic characteristics. The recent dating of archaeological levels i…
The Lavras da Mangabeira Basin is a basin traditionally included in the set of the of the Brazilian Northeast's interior basins, linked to the Cretaceous rift of the South Atlantic. It is originated upon pre-Cambrian rocks, it's filling is composed of two sedimentary units, the formations Iborepi and Serrote do Limoeiro, and a basaltic flow between them. From the radiometric dating method…
The project aims to characterize technologically the lithologies and to locate the best sites of the Rio Claro Formation, for the exploration of sand in the context of the civil construction. By means of a study on the formation, aerial images of the outcrops, fieldwork and technological analyzes of the sandstone, soil and its products, it will be possible to show its qualities that will …
Carbonate materials can reveal vegetation and climate changes in the past through the analysis of its stable isotope content of carbon (´13C) and oxygen (´18O). The isotopic signature of pedogenic carbonates, like nodules, rhizoliths, and caliche, has been commonly used in eastern Africa to unravel the paleoenvironment of early hominins. Recently, the oldest paleolithic artifacts outside …
Carbonate rock can record specific isotopic signatures that can be used to identify its deposition and diagenetic age, in addition to geomorphological and paleoclimatic conditions. Recent studies have been developing a new method for dating carbonate materials, known as solid-state in-situ U-Pb geochronology by Laser Ablation. This method has an important advantage over the traditional li…
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