Special Issue dedicated to Francisco Hervé: Global tectonic processes of the ancient southwestern Gondwana margin in South America and the Antarctic Peninsula
Edited by:
- Mauricio Calderón, PhD, Universidad del Desarrollo, Chile
- Paula Castillo, PhD, Universität Münster, Deutschland
- Robert Pankhurst, PhD ScD, United Kingdom
Submission status: Extended until September 30, 2025
Special Issue: Geoethics in Chile and Latin America - Contextual reflections for responsible geoscience
Edited by:
- Luisa Pinto, Universidad de Chile
- Hernán Bobadilla, Politecnico di Milano
- Tania Villaseñor, Pontificia Universidad Católica de Chile
- Pablo Ramírez, Universidad de Chile
- Millarca Valenzuela, Universidad Católica del Norte
Submission status: Open between August 15, 2025, and March 31, 2026
Graduada em Ciências Biológicas Licenciatura e Bacharel pela Universidade de Rio Verde (2013). Atualmente é colaboradora do Projeto de Pesquisa "Geologia e Paleobiogeografia dos Vertebrados do Neocretáceo no Sul do Estado de Goiás e Pontal do Triângulo Mineiro" do Laboratório de Paleontologia e Evolução do Curso de Geologia da Faculdade de Ciência e Tecnologia da UFG do Campus Aparecida de Goiânia.
Titanosauria of the Bauru Group: a summary of records and their importance for understanding the diversity of the clade in Brazil
Edna Gomes Nascimento, Carlos Roberto Candeiro, Luciano Vidal, Emerson Ferreira Oliveira, Tamires Carmo Dias, Stephen Brusatte
Abstract
ABSTRACT. The present study provides a synthesis of the diversity and geographical distribution of Titanosauria (Dinosauria: Sauropoda) from Upper Cretaceous rocks of the Bauru Group in Brazil. There are currently ten valid species of titanosaurs described for the Bauru Group, some of which exhibit similarities to species found in Argentina. Among these species is the well-known clade Aeolosaurini, which is considered as endemic to South America. Members belonging to the Aeolosaurini clade remains have so far been found only in Argentina and Brazil. This faunal similarity helps in the interpretation of the paleogeographic distribution of these organisms, which reflects intense faunal interchange between these regions, thereby indicating a chrono-correlated geological age.