CV Lattes
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Universidade de São Paulo (USP). Instituto de Geociências (IGC) (Institutional affiliation from the last research proposal) Birthplace: Brazil
Henrique Albuquerque Fernandes is a Brazilian geologist (2020) and a PhD student in Geology at the University of São Paulo, Brazil. Between 2018 and 2020, he developed undergraduate research in the field of sedimentology, with a grant from the Foundation for Research Support of the State of São Paulo (FAPESP). Since 2016, he develops works related to the practice and teaching of speleology. Between 2018 and 2021, he worked as a volunteer mathematics teacher in the Preparatory Course at the Faculty of Philosophy, Letters and Human Sciences at the University of São Paulo (FFLCH - USP). In 2020, he was an online internship student at the University of Tsukuba - Japan. In 2021, he iniciated his Ph.D. in the Geochemistry and Geotectonics program at the Geosciences Institute - USP, with a project in the area of isotopic chemostratigraphy (C, Sr, Cr and Cd) funded by FAPESP, and linked to the GRIND (Geological Research through Integrated Neoproterozoic Drilling) project from ICDP (International Continental scientific Drilling Program). In 2023-2024, he did an internship at the University of Copenhagen, Denmark, where he performed Sr, Cr and Cd isotope analysis funded by FAPESP (BEPE). (Source: Lattes Curriculum)
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The rise of atmospheric oxygen levels to near present values is still a controversial question. Some geochemical proxies indicate a gradual increase during the Neoproterozoic, while others suggest fluctuations in the levels of atmospheric and marine O2 after 800My, with the main rise only in the Paleozoic. In this context, investigating events of atmospheric oxygenation during the Neoprot…
The Tamengo Formation, a unit of the upper portion of the Corumbá Group (Ediacarano), has been of great interest for geochemical investigations, in addition to its already known paleontological potential. These geochemical investigations have been carried out in order to understand the global changes that preceded the diversification of Cambrian life. For this, the study of its deposition…
The Late Ediacaran is a period of major perturbations in the Earth System that ultimately paved the way to a Phanerozoic World. Among these upheavals, there is the rise of oxygen levels in the atmosphere-ocean system, which may be linked to the emergence of complex life on Earth. In order to investigate these oxygen fluctuations, geochemical proxies based on stable isotopes have been succ…
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