Rincão dos Weiss: Induan - Olenekian, Brazil
collected by Fundação Zoobotânica do Rio Grande do Sul 1997

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Reptilia - Procolophonidae
Procolophon sp. Owen 1876
Dias-da-Silva et al. 2006 4 specimens
UFRGS PV 9252 T, 0494 T, 0498 T; MCT/PUCRS 3790; one partial skull and 3 vertebrae of large individuals, not found associated
Procolophon brasiliensis n. sp. Cisneros and Schultz 2002
1 individual
synonym of Procolophon trigoniceps
MCN PV 1905 (type)
see common names

Geography
Country:Brazil State/province:Rio Grande do Sul County:Mata
Coordinates: 29.6° South, 54.4° West (view map)
Paleocoordinates:49.1° South, 23.7° West
Basis of coordinate:estimated from map
Geographic resolution:small collection
Time
Period:Triassic Epoch:Early/Lower Triassic
10 m.y. bin:Triassic 1
Key time interval:Induan - Olenekian
Age range of interval:251.90200 - 247.20000 m.y. ago
Stratigraphy
Geological group:Rosário do Sul Formation:Sanga do Cabral
Stratigraphic resolution:group of beds
Stratigraphy comments: The Sanga do Cabral Fm. is correlated with the "impoverished zone" (Procolophon subzone) of the Lystrosaurus Assemblage Zone of the Main Karoo Basin of South Africa by some authors on the basis of the abundant records of Procolophon, i.e., it is Upper Induan to Lower Olenekian in age (see Dias-da-Silva et al., 2006, Can. J. Earth Sci. and references therein). However, Langer et al. (2007; New Mexico Mus. Nat. Hist. Sci. Bull. 41) pointed out that the prevalence of Procolophon in the Brazilian sequence might represent a taphonomic bias, and that only an undifferentiated Lower Triassic age is currently possible.

The Sanga do Cabral Fm. belongs to the Rosario do Sul Group according to various authors (e.g., Langer et al. 2007, New Mexico Mus. Nat. Hist. Sci. Bull. 41).
Lithology and environment
Primary lithology:massive,"cross stratification" conglomerate
Secondary lithology:tabular sandstone
Includes fossils?Y
Lithology description: "It [the Sanga do Cabral Fm.] consists of massive to trough cross-bedded intraformational conglomerates and horizontally bedded sandstones, which are interpreted as being deposited by braided river systems which poorly confined channels that developed on a low-gradient alluvial plain. [...] The intraformational conglomerates are the bone-bearing beds, [...]." (Dias-da-Silva et al., 2006).
Environment:fluvial indet. Tectonic setting:cratonic basin
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils
Fragmentation:frequent
Temporal resolution:snapshot
Spatial resolution:parautochthonous
Collection methods and comments
Collection methods:mechanical,survey of museum collection
Reason for describing collection:taxonomic analysis
Collectors:Fundação Zoobotânica do Rio Grande do Sul Collection dates:1997
Collection method comments: MCN PV = vertebrate paleontology collections of the Museu de Ciências Naturais, Fundação Zoobotânica do Rio Grande do Sul, Porto Alegre
UFRGS PV = vertebrate paleontology collections of the Universidade Federal do Rio Grande do Sul, Porto Alegre
MCT/PUCRS = Museu de Ciência e Technologia da Pontifícia Universidade Católica do Rio Grande do Sul, Porto Alegre
Metadata
Also known as:Rincao dos Weiss; holotype site of Procolophon brasiliensis
Database number:93720
Authorizer:J. Mueller Enterer:T. Liebrecht
Modifier:M. Carrano Research group:vertebrate
Created:2010-01-29 04:08:53 Last modified:2021-03-26 13:26:28
Access level:the public Released:2010-01-29 04:08:53
Creative Commons license:CC BY
Reference information

Primary reference:

31834. J. C. Cisneros and C. L. Schultz. 2002. Procolophon brasiliensis n. sp., a new procolophonid reptile from the Lower Triassic of southern Brazil. Neues Jahrbuch für Geologie und Paläontologie Monatshefte 2002(11):641-648 [J. Mueller/T. Liebrecht]

Secondary references:

31842 S. Dias-da-Silva, S. Modesto, and C. L. Schultz. 2006. New Material of Procolophon (Parareptilia: Procolophonoidea) from the Lower Triassic of Brazil, with remarks on the ages of the Sanga do Cabral and Buena Vista formations of South America. Canadian Journal of Earth Sciences 43(11):1685-1693 [J. Mueller/T. Liebrecht]