| Regnana Formation | |
|---|---|
| Stratigraphic range: Early Permian, | |
| Type | Geological formation |
| Unit of | Athesian Volcanic Complex |
| Sub-units |
|
| Underlies | Ora Formation |
| Lithology | |
| Primary | Andesite |
| Other | Pyroclastic rock |
| Location | |
| Region | Pinè Valley, Italian Alps |
| Country | Italy |
The Regnana Formation is an Early Permian (Kungurian) geologic formation located in the Italian Alps that is part of the Athesian Volcanic Complex. [1] Reptile and plant remains are among the fossils that have been recovered from the formation. [2] [3] The formation is mainly made up of andesite and pyroclastic rock. [4]
| Fossils reported from the Regnana Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Plantae [3] | Indeterminate [3] | Stramaiolo' (Redebus) [3] | Large, possibly coalified, shoot and leaf fragments [2] | Discovered in the same fossil layer as the holotype of Tridentinosaurus [3] | ||
| Tridentinosaurus [2] | T. antiquus [2] | Stramaiolo' (Redebus) [2] [3] | Poorly preserved femora, tibiae, and fibulae, possible osteoderm skin impressions near the shoulder and pelvis [3] | The body outline of the specimen is a forgery and only the scales and hindlimbs are real [3] | | |