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Predebon outcrop , Rio Grande do Sul, Brazil
| Lat/Long (Decimal) | -29.6414,-53.4478 |
|---|---|
| Co-ordinates Derivation | stated in text |
| Given Location | Rio Grande do Sul, Brazil |
| Mindat.org Region (for given coordinates) | Rio Grande do Sul, Brazil |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Predebon outcrop (1 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | upper part of member | sandstone | 237 - 228 Ma Late/Upper Triassic |
| Predebon outcrop (2.8 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | Santa Maria 2 (upper half of Santa Maria Formation), from the so-called "Rhynchosaur Cenozone" or "Hyperodapedon Assemblage Zone". The Hyperodapedon Assemblage Zone has generally considered been late Carnian in age, but could extend into the early Norian. upper part of Alemoa member, close to contact with Caturrita Formation | sandstone | 237 - 208.5 Ma Late/Upper Triassic |
| Predebon outcrop (3.5 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | Santa Maria 2 (upper half of Santa Maria Formation), from the so-called "Rhynchosaur Cenozone" or "Hyperodapedon Assemblage Zone". The Hyperodapedon Assemblage Zone has generally considered been late Carnian in age, but could extend into the early Norian. upper part of Alemoa member, close to contact with Caturrita Formation | sandstone | 237 - 208.5 Ma Late/Upper Triassic |
| Predebon outcrop (4.1 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | Santa Maria 2 (upper half of Santa Maria Formation), from the so-called "Rhynchosaur Cenozone" or "Hyperodapedon Assemblage Zone". The Hyperodapedon Assemblage Zone has generally considered been late Carnian in age, but could extend into the early Norian. upper part of Alemoa member, close to contact with Caturrita Formation | sandstone | 237 - 208.5 Ma Late/Upper Triassic |
| Predebon outcrop (4.6 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | Santa Maria 2 (upper half of Santa Maria Formation), from the so-called "Rhynchosaur Cenozone" or "Hyperodapedon Assemblage Zone". The Hyperodapedon Assemblage Zone has generally considered been late Carnian in age, but could extend into the early Norian. upper part of Alemoa member, close to contact with Caturrita Formation | sandstone | 237 - 208.5 Ma Late/Upper Triassic |
| Predebon outcrop (5.1 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | Santa Maria 2 (upper half of Santa Maria Formation), from the so-called "Rhynchosaur Cenozone" or "Hyperodapedon Assemblage Zone". The Hyperodapedon Assemblage Zone has generally considered been late Carnian in age, but could extend into the early Norian. upper part of Alemoa member, close to contact with Caturrita Formation | sandstone | 237 - 208.5 Ma Late/Upper Triassic |
| Predebon outcrop (5.5 m) | da Silva R. C., Carvalho I. d. S., et al (2008) | Rosário do Sul - Santa Maria - Alemoa | Santa Maria 2 (upper half of Santa Maria Formation), from the so-called "Rhynchosaur Cenozone" or "Hyperodapedon Assemblage Zone". The Hyperodapedon Assemblage Zone has generally considered been late Carnian in age, but could extend into the early Norian. upper part of Alemoa member, close to contact with Caturrita Formation | sandstone | 237 - 208.5 Ma Late/Upper Triassic |
Recorded Fossils
| Accepted Name | Hierarchy | Age |
|---|---|---|
| Arenicolites sp. genus | Arenicolites | 237 - 208.5 Ma Late/Upper Triassic |
| Skolithos sp. genus | Skolithos | 237 - 228 Ma Late/Upper Triassic |
 Dinosauriaorder | Animalia : Chordata : Reptilia : Dinosauria | 237 - 208.5 Ma Late/Upper Triassic |
 Rhynchosauriaorder | Animalia : Chordata : Reptilia : Rhynchosauria | 237 - 208.5 Ma Late/Upper Triassic |
 Grallator (Eubrontes) sp.subgenus | Animalia : Chordata : Saurischia : Eubrontidae : Grallator (Eubrontes) | 237 - 208.5 Ma Late/Upper Triassic |
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
