Botucatu
Description
Source: Wikipédia
The Botucatu Formation is an Aptian geologic formation of the Paraná and Pelotas Basins in southern Brazil and northern Uruguay. The formation is composed of quartzitic sandstones, deposited in an eolian environment. Fossil theropod tracks have been reported from the formation.
Découvertes
Source: The Paleobiology Database
Site(s) correspondant(s) à cette formation: 8
Brodósqui tracksite, Visconde Farm quarries : São Paulo - ? 14677 38312 59104 62875 69655 Brodósqui, on road between Brodósqui and Jurecê (= Jurucê), entrance at highway police station of Highway SP 334, Visconde Farm. Four quarries: Leitão, Nordestina, Ecládio, and Visconde. Most tracks in flagstones in town of Franca, but presumed to come primarily from Visconde quarry.- Califórnia quarry, Araraquara (ARCA) : São Paulo - ? 14677 15225 38312 62875 3-5 km E of the old Ouro railway station, 8 km ESE of Araraquara, on the São Carlos-Araraquara railway line
- Cerrito Velho quarry, Araraquara (ARCE) : São Paulo - ? 14677 15225 38312 59104 62875 69655 3-5 km E of the old Ouro railway station, 8 km ESE of Araraquara, on the São Carlos-Araraquara railway line. Near a "ghost village", 700 m WSW of the São Bento (Corpedras) quarry
- São Bento quarry, Araraquara (ARSB) : São Paulo - ? 14677 15225 17329 38312 59104 62875 69655 flagstone quarry, 3-5 km E of the old Ouro railway station, 8 km ESE of Araraquara, on the São Carlos-Araraquara railway line
- Cerrito Novo quarry, Araraquara (ARCN) : São Paulo - ? 14677 38312 59104 62875 3-5 km E of the old Ouro railway station, 8 km ESE of Araraquara, on the São Carlos-Araraquara railway line
- Chave do Calixto quarry, Rifaina : São Paulo - ? 14677 38312 59104 62875 69655 Chave do Calixto quarry (abandoned), 3 km SE of city of Rifaina. Tracks found in city sidewalks of Rifaina (on edge of Rio Grande)
- SP 300, Serra de Botucatu : São Paulo - ? 14677 38312 59104 roadcuts along highway SP 300, Serra de Botucatu, 10 km E of Botucatu
- Adolf Kessler Quarry, Sete Curvas : Rio Grande do Sul - ? 14677 59104 Adolf Kessler Quarry, "Sete Curvas" locality, a few km E of Santa Cruz do Sul; tracks found in flagstones of city sidewalks
Publication(s)
La base comprend 7 publication(s).
Source: The Paleobiology Database
- ↑1 2 3 4 5 6 G. Leonardi and L. C. Godoy. 1980. Novas pistas de tetrápodes da Formação Botucatu no Estado de São Paulo [New tetrapod trackways from the Botucatu Formation in Sao Paulo state]. Anais do XXXI Congresso Brasileiro de Geologia 5:3080-3089
- ↑1 2 3 4 5 6 7 8 G. Leonardi. 1994. Annotated Atlas of South America Tetrapod Footprints (Devonian to Holocene) with an Appendix on Mexico and Central America. . República Federativa do Brasil, Ministério de Minas e Energia, Secretaria de Minas e Metalurgia, Companhia de Pesquisa de Recursos Minerais, Brasília
- ↑1 2 3 4 5 6 7 G. Leonardi and I. d. S. Carvalho. 2002. Jazigo icnofossilífero do Ouro – Araraquara (SP) [Ichnofossiliferous grave of Ouro – Araraquara (SP)]. Sítios Geológicos e Paleontológicos do Brasil. SIGEP, Brasilia
- ↑1 2 3 4 5 6 7 8 9 G. Leonardi. 1989. Inventory and statistics of the South American dinosaurian ichnofauna and its paleobiological interpretation. Dinosaur Tracks and Traces
- ↑1 2 3 4 5 6 7 G. Leonardi. 1981. As localidades com rastros fósseis de tetrápodes na América Latina [Localities with fossil tetrapod tracks in Latin America]. Anais II Congresso Latino-Americano de Paleontologia 2:929-940
- ↑1 2 3 4 5 6 G. Leonardi. 1980. On the discovery of an abundant ichno-fauna (vertebrates and invertebrates) in the Botucatu Formation s.s. in Araraquara, São Paulo, Brazil. Anais da Academia Brasileira de Ciências 52(3):559-567
- ↑1 M. A. Fernandes and I. S. Carvalho. 2005. As pistas do paleodeserto Botucatu: aspectos preservacionais [The tracks of the Botucatu paleodesert: preservational aspects]. Resumos do XIX Congresso Brasileiro de Paleontologia e VI Congresso Latino-Americano de Paleontologia
Galerie d'image
Pas d'image.