CV Lattes
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Universidade Estadual Paulista (UNESP). Campus de Bauru. Faculdade de Ciências (FC) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Associate Professor (Full Professor) at the Paulista State University Júlio de Mesquita Filho (UNESP - Bauru, SP) where he teaches the disciplines of Geology, Paleontology and Fundamentals of Human Sciences. Head of the Laboratory at LAPALMA since 2007 where he carries out his research in Macroinvertebrates Paleontology. He holds a degree in Biological Sciences, Bachelor's degree from the Universidade Estadual Paulista Júlio de Mesquita Filho (UNESP/Botucatu 1995), a Master's degree in Geosciences (Sedimentary Geology) from the University of São Paulo (USP 1999) and a PhD in Geosciences (Sedimentary Geology) from the University of São Paulo. São Paulo (USP 2004). Graduated in Philosophy from Unifran in 2016. He has a lato sensu postgraduate degree in Thanatology. He is a professor of the graduate course in Biodiversity at Unesp Assis / Bauru where he teaches Taphonomy and Geomorphology as a tool in paleoenvironmental interpretations. He participates as coordinator of the CNPq research group "Palaios" and as a collaborator of the CNPq research groups "Conservation Paleobiology Research Group", "Center for Studies on Public Domain Natural Assets", "Phanerozoic Paleoinvertebrates of South America and Antarctica" and "Paleontology of Mato Grosso". President of the Brazilian Society of Paleontology between 2017 and 2021. Current vice-president of the Brazilian Society of Paleontology. (Source: Lattes Curriculum)
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The project "Marine Incursions and Faunistic Exchanges in the Interior of South America During the Devonian and the Paleobiogeographical Impacts in the Paraná Basin" has as its main objective to investigate the paleobiogeographical changes resulting from marine incursions in South America during the Devonian, focusing on the Paraná. The project involves collaborations with several univers…
Eolian deposits are generated when there is a combination of intense winds, sediment availability and impossibility of substrate stabilization. There are emblematic examples in modern deserts, but also in rainy areas with high sediment availability and intense winds. The Octopodichnus-Entradichnus ichnofacies is common to all types of eolian deposits, and it is not clear how the ichnologi…
The macro and micro fauna of invertebrates present in the intracratonic basins of Paraná and Parnaíba are relatively well studied and documented in the literature in general, on the other hand, in the Parecis and Alto Tapajós basins, paleofaunistic studies are extremely poor. Recent work shows that during the end of the Eifelian to the Frasnian (Middle-Upper Devonian), from global climati…
The macro and micro invertebrate fauna present in intracratonic basins of Paraná, Amazonas and Parnaíba are relatively well studied and documented in the literature in general. However, the northwest, north and south borders of the Paraná Basin, which covers the states of Mato Grosso, Goiás and Uruguay, are extremely poor in paleofauna studies. Recent papers show that during the late Eife…
(Only some records are available in English at this moment)
The paleoenvironment of sedimentary deposits, the depositional environment influenced byphysical, chemical, and biological processes until rock formation, is one of the main issuesinvolving paleontology since its inception. Taphonomy combined with ecological analyses,through guilds, can be useful tools for defining a depositional environment. The Parecis Basinis an intracratonic basin loc…
Researchers' interest in highlighting the cultural and scientific value of the environment's geodiversity grew at the end of the 20th century. They sought to popularize the science of natural heritage among the community in order to expand the discussion about geological potential. To this end, urban geotourism is projected as a new sector of tourism that allows residents or visitors to d…
Conservation Paleobiology is characterized by the application of theories and analytical tools from paleontology, especially Atualistic Taphonomy, to solve problems involving the conservation of biodiversity. In this context, the analysis of the compositional fidelity of living and dead assemblages of molluscs, when associated with factors intrinsic and extrinsic to the bioclastic materia…
(Only some records are available in English at this moment)
Eurypterids are extinct aquatic arthropods that present a basic body organization in accordance with the morphology of Chelicerata. They have a ventral plate on the prosoma (metastoma), a median genital appendage and twelve abdominal segments. These animals had different eating habits and were able to occupy benthic, nektonic and nektobenthic regions. They are typical organisms of salt, b…
The mollusk shell consists of an organic-mineral biocomposite consisting of calcium carbonate and an organic polymer matrix. The material combines the properties of both components, so that the valva has the hardness of the carbonate ceramics and some flexibility from the organic matrix. Understanding this structure, from a paleontological point of view, provides subsidies to identify whi…
Conulariids are extinct invertebrate scyphozoans, sessile of epifauna, benthic, with generally phosphatic and elongated theca and, most often, with four faces. Most of the species in this group are from shallow marine and platform waters. In contrast to the quantity and frequency of publications focused on conulariids from the Paraná Basin, research in the Parnaíba Basin is sparse and pre…
(Only some records are available in English at this moment)
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| 39 / 26 | All research grants and scholarships |
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