Also known as Chapada Diamantina, Baixa Grande
Where: Bahia, Brazil (11.5° S, 40.1° W: paleocoordinates 11.5° S, 40.1° W)
• coordinate stated in text
• outcrop-level geographic resolution
When: Holocene (0.0 - 0.0 Ma)
• The geology of the region is characterized by crystalline rocks belonging to the complex Caraíba, New Tank-Ipirá, Health and Mairi (Vieira et al., 2005). It is the latter which occur migmatitic orthogneisses with mafic and ultramafic enclaves in which are embedded the tanks observed in the rural area. In one of these, in the town of Lagoa Towards were discovered fossils of Late Quaternary megafauna.
Environment/lithology: terrestrial; breccia and black mudstone
Size classes: macrofossils, mesofossils
Collection methods: quarrying,
• Repository: Collection macrofossils Fossils Geology Department of the Federal University of Rio de Janeiro (UFRJ-DG).
Primary reference: R. Costa Ribeiro and I. Souza Carvalho. 2009. Megafauna do Quaternário tardio de Baixa Grande , Bahia , Brasil Megafauna of the late Quaternary from Baixa Grande , Bahia , Brazil. Anuário do Instituto de Geociências - UFRJ 32:42-80 [C. Jaramillo/M. Vallejo/A. Cardenas ]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 147605: authorized by Carlos Jaramillo, entered by Maria Vallejo on 10.07.2013
Creative Commons license: CC BY (attribution)
Taxonomic list
Mammalia | |
| |
"Stegomastodon waringi" = Notiomastodon platensis
| |
| |
|