| Sierra Perenchiza Formation | |
|---|---|
| Stratigraphic range: Late Campanian-early Maastrichtian ~ | |
| Type | Geological formation |
| Lithology | |
| Primary | Limestone |
| Other | Marl |
| Location | |
| Coordinates | 39°36′N1°00′W / 39.6°N 1.0°W |
| Approximate paleocoordinates | 30°18′N0°12′E / 30.3°N 0.2°E |
| Region | Valencia |
| Country | Spain |
| Type section | |
| Named for | Sierra Perenchiza |
The Sierra Perenchiza Formation is a geologic formation in Spain. A late Campanian to early Maastrichtian age is supported by paleomagnetic data and fossil pollen analysis. [1] The Sierra Perenchiza Formation "consists mainly of interbedded carbonate marls and lacustrine limestones, interpreted as deposits of small ephemeral lakes and ponds of a coastal environment". [2] Vertebrate fossils are common in the formation: these include dinosaurs, pterosaurs, crocodylomorphs, turtles, squamates, frogs, albanerpetontids, and ray-finned fish, as well as dinosaur eggshell fragments. Also known are freshwater invertebrates (ostracods, gastropods, and bivalves) and plant remains. [2]
Color key
| Notes Uncertain or tentative taxa are in small text; |
| Paleofauna of the Tremp Formation | |||||||
|---|---|---|---|---|---|---|---|
| Genus | Species | Locality | Stratigraphic unit | Material | Description | Images | Notes |
| Doratodon | D. ibericus | Incomplete left mandible with teeth [3] | A crocodylomorph, closely related to or within Sebecosuchia | | |||
| Megaloolithus | M. aff. siruguei | Unusually thick (up to 4.9 mm) eggshell fragments [4] | Possible titanosaur eggs | ||||
| Rhabdodon | R. sp. | A maxillary tooth (MGUV CH-162) [5] | A rhabdodontid | ||||