- Research Grants
Graduate at Chemistry with emphasis in Geochemistry from Universidade Federal do Rio Grande do Sul (1979), master's at Chemistry from Universidade Estadual de Campinas (1986) and PhD at Chemistry from Universidade Estadual de Campinas (1991). Has experience in Geosciences, focusing on Environmental and Analytical Geochemistry. (Source: Lattes Curriculum)
Superficial and ground waters constitute the main sources for water supply. Hydrogeochemistry relates the chemical composition of natural waters to their environment and depends on complex processes that include the interaction of water with minerals/rocks, atmosphere and biosphere. Mostly, the chemical characterization of waters is restricted to the main dissolved constituents and some...
(Only some records are available in English at this moment)
The Araguaia Orogen represents part of the amalgamation history of the Gondwana Supercontinent during the late Neoproterozoic. The metasedimentary sequences record the tectonic history of the development and formation of this geotectonic unit. However, tectono-metamorphic studies performed in these sequences are rare and the existing works have a regional character. This scientific init...
The appearance of the first complex organisms during the Ediacaran period (635 to 541 Ma) is one of the most notable episodes in Earth's history. Nevertheless, the causes that led to such life evolution remain still unclear. One of the hypotheses is the enhanced influx of nutrients into the ocean via chemical weathering of newly formed large continental masses. Such high nutrient availa...
Natural waters contain trace elements as part of their dissolved constituents. Among them are the lanthanides (Ln) that with scandium and yttrium form the rare earth elements (REE). These elements find a wide range of technological uses and as a result they are being introduced in the environment, at levels never registered before. This research intends to characterize the occurrence of...
he rise of the first complex organisms at the end of the Ediacaran period (635 to 541 Ma) is one of the most intriguing episodes in the history of the Planet. The causes for such move of life to its complex forms remain unclear. An enhanced influx of nutrients into the ocean via chemical weathering of large continental masses is one of the leading hypotheses to explain it. This high nut...
(References retrieved automatically from Web of Science and SciELO through information on FAPESP grants and their corresponding numbers as mentioned in the publications by the authors)
|Data from Web of Science|
(References retrieved automatically from State of São Paulo Research Institutions)
FIORENTINO, Janaina Correa. Geoquimica do mercurio e outros elementos em perfil de solo desenvolvido sobre diabasio, Paulinia-SP. 2007. Dissertação (Mestrado) - Instituto de Geociências. Universidade Estadual de Campinas (UNICAMP). (05/53599-0)
JORGE, Alexandre Paulo de Souza. Determinação dos elementos do grupo da platina após fusão coletora com sulfeto de nível. 1999. Dissertação (Mestrado) - Instituto de Geociencias. Universidade Estadual de Campinas (UNICAMP). (97/06848-7)
CAMPOS, Francisco Ferreira de. Anomalias antrópicas de gadolínio e distribuição dos elementos terras raras nas águas do Rio Atibaia e Ribeirão Anhumas (SP). 2014. Dissertação (Mestrado) - Instituto de Geociências. Universidade Estadual de Campinas. (12/02486-5)