La Pedrera de Rúbies Formation
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The La Pedrera de Rúbies Formation, also called as La Pedrera de Meià[1][2] is an Early Cretaceous (late Berriasian to early Barremian geologic formation in Catalonia, Spain. The formation crops out in the area of the Montsec in the Organyà Basin. At the La Pedrera de Meià locality, the formation consists of rhythmically laminated, lithographic limestones that formed in the distal areas of a large, shallow coastal lake.[3] It is noted for the exceptional preservation of articulated small vertebrates and insects, similar to that of the Solnhofen Limestone.
Quick Facts Type, Unit of ...
La Pedrera de Rúbies Formation | |
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Stratigraphic range: Late Berriasian-early Barremian ~140–125 Ma | |
Type | Geological formation |
Unit of | Montsec Group |
Underlies | Prada Formation |
Area | Montsec |
Lithology | |
Primary | Limestone |
Location | |
Coordinates | 42.0°N 0.9°E / 42.0; 0.9 |
Approximate paleocoordinates | 31.3°N 11.3°E / 31.3; 11.3 |
Region | Lérida Province, Catalonia |
Country | Spain |
Extent | Pre-Pyrenees |
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