Where: Santa Catarina , Brazil (26.9° S, 50.4° W)
• Paleocoordinates: 37.5° S, 18.9° W (Wright 2013)
• coordinate stated in text
• small collection-level geographic resolution
When: Morro Pelado Member (Rio do Rasto Formation), Roadian to Roadian (272.3 - 254.2 Ma)
• "The studied outcrop belongs to the Middle—Upper Permian sequence of the Rio do Rasto Formation, Paraná Basin (Holz et al. 2010)." Formation correlated with the Roadian to Wuchiapingian.
Environment/lithology: delta plain; sandstone and siltstone
Size class: macrofossils
Collected by M. C. Barberena
• " Fragments of bone elements were found in five different levels of the outcrop, mainly in the siltstone strata and fine- to medium-grained massive or bedding-parallel stratified sandstone."
Primary reference: A. Strapasson, F. L. Pinheiro, and M. B. Soares. 2015. On a New Stereospondylomorph Temnospondyl from the Middle—Late Permian of Southern Brazil. Acta Palaeontologica Polonica 60(4):843-855 [R. Butler/E. Dunne]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 184288: authorized by Richard Butler, entered by Emma Dunne on 14.02.2017
Creative Commons license: CC0 (CC0)
Taxonomic list
Amphibia | |
Parapytanga catarinensis Strapasson et al. 2015 tetrapod UFRGS-PV-0355-P (Holotype): an incomplete skeleton composed of the orbital region of the skull roof, the basicranium, some endocranial elements, a left stapes, and a right hemimandible, in addition to vertebrae and ribs, bones from the pectoral girdle, a right femur and a cluster of scales
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