SciELO - Scientific Electronic Library Online

 
vol.74 número2Gondwana biogeography: a phylogenetic approachMorphological variation among the appendicular bones of the Titanosauridae (Dinosauria: Sauropoda) from the Bauru Basin (upper Cretaceous) of Peirópolis (MG), Brazil índice de autoresíndice de assuntospesquisa de artigos
Home Pagelista alfabética de periódicos  

Serviços Personalizados

Journal

Artigo

  • Inglês (pdf)
  • Artigo em XML
  • Como citar este artigo
  • SciELO Analytics
  • Curriculum ScienTI
  • Tradução automática

Indicadores

Links relacionados

Compartilhar


Anais da Academia Brasileira de Ciências

versão impressa ISSN 0001-3765versão On-line ISSN 1678-2690

An. Acad. Bras. Ciênc. v.74 n.2 Rio de Janeiro jun. 2002

http://dx.doi.org/10.1590/S0001-37652002000200019 

A BRIEF NOTE ON THE PALEOFAUNA OF "TARTARUGUITO SITE", ADAMANTINA FORMATION, BAURU GROUP, BRAZIL

DEISE D.R. HENRIQUES 1, JOSÉ M. SUÁRES 2, SERGIO A.K. AZEVEDO 1, RAMSES CAPILLA 1 AND LUCIANA B. CARVALHO 1

1 Setor de Paleovertebrados, Departamento de Geologia e Paleontologia, Museu Nacional / UFRJ - 20940-040, Rio de Janeiro, RJ.
2 Universidade Estadual Paulista, Presidente Prudente, SP.

Presented by ALEXANDER W.A. KELLNER

 

The Bauru Group is mainly composed of fluvial sandstones, siltstones and mudstones, representing the most extensive continental Cretaceous deposits from Brazil. In the years 2000 and 2001, fieldwork was carried out by the researchers of the Paleovertebrate Sector of the Museu Nacional/UFRJ, in conjunction with researchers from UNESP, to the outcrops of the Adamantina Formation near Pirapozinho, Presidente Prudente and Álvares Machado localities, all situated in the State of São Paulo. Emphasis was placed at the site know informally as "Tartaruguito'', located in the municipality of Pirapozinho, which is mainly known for the numerous turtle skeletons and carapace fragments found there. A great excavation was made at this Lagerstätte and several turtle remains were collected, some fairly complete with cranial and postcranial elements. Other reptilian taxa previously unknown from that site were found associated with them and are still being prepared. Preliminary taphonomic studies of this site indicate that this accumulation was due to a drought that resulted in an accumulation of fossil vertebrates. — ( December 20, 2001 ).

Creative Commons License Todo o conteúdo deste periódico, exceto onde está identificado, está licenciado sob uma Licença Creative Commons