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: Itália
PhD in Geological Sciences and Geotechnologies and Associate Professor at the Institute of Geosciences and Exact Sciences of São Paulo State University (UNESP). His research interests include paleomagnetism, rock magnetism, and their applications to geological problems. Currently, his work focuses on the stratigraphy of the Plio-Pleistocene, the dating of paleontological and archaeological sites, the PermianTriassic magnetostratigraphy of the Paraná Basin, and the Cretaceous magnetostratigraphy of Northeastern Brazil.Field experience in South America (Brazil, Argentina), Europe (Italy, France, Germany, Greece, Serbia, Romania), Asia (Jordan, Israel, Turkey, Kazakhstan, Tajikistan), and the Indian Ocean (IODP Expedition 355). He is manager of the UNESP Laboratory of Paleomagnetism (UNESPmag), Associate Editor of Alpine and Mediterranean Quaternary journal, and serves as a reviewer for funding agencies (CNPq, FAPESP, Alexander von Humboldt Foundation) and international journals in the fields of geophysics and geology. (Source: Lattes Curriculum)
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The period from 2.5 to 1 million years ago (Ma) is critical, as it corresponds to a major shift in hominin evolution in East Africa, when Australopithecus was replaced by the taxa Paranthropus and Homo and when, since the beginning of the Pleistocene, the Earth's average surface temperature has become colder and the global climate more unstable, resulting in more open ecosystems and the f…
Recent Rb-Sr datings of sedimentary rocks from the Recôncavo and Sergipe-Alagoas basins and referred to the Dom João Brazilian local stage provided absolute ages around 230-220 Ma, i.e. Late Triassic. Based on 40Ar/39Ar geochronology, mafic volcanic rocks of the Lavras de Mangabeira basin are associated at the same time interval and correlated with the magmatism of the Central Atlantic Oc…
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 definition of the age of the stratigraphic units of the Araripe Basin is the subject of great debates regarding its formalization, is currently divided into 4 stratigraphic sequences limited by unconformities and correlated to the rifting phase of the Gondwana Supercontinent. The Cariri Formation, which outcrops predominantly in the eastern portion of the basin, is traditionally descr…
Mesozoic non-marine sedimentary sequences occur in several basins of Northeastern Brazil, among which are the Rio do Peixe, Araripe, and Lavras da Mangabeira. These successions mostly consist of lacustrine terrigenous deposits with ostracod fauna, which has been used to build a local zonation for the Late Jurassic?-Early Cretaceous (Dom João, Rio da Serra Aratu, Buracica, Juquiá, and Alag…
The Dom João stage is a local chronostratigraphic unit of the Brazilian Mesozoic defined in the Northeast of Brazil. It is considered to precede the rift that broke Gondwana by driving away the South American plate from the African plate. Biostratigraphic studies on ostracods and palynomorphs in several basins from the Brazilian Northeast referred the Dom João stage to the Late Jurassic, …
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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…
| 1 / 1 | Ongoing grants |
| 4 / 3 | Completed research grants |
| 1 / 1 | Ongoing scholarships in Brazil |
| 9 / 9 | Completed scholarships in Brazil |
| 2 / 2 | Completed scholarships abroad |
| 17 / 16 | All research grants and scholarships |
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