Regnana Formation | |
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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 | ||||||
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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] | ![]() |