| La Caja Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Formation |
| Underlies | Taraises Formation |
| Overlies | Zuloaga Formation |
| Thickness | Around 60 metres |
| Lithology | |
| Primary | Marl |
| Other | Limestone, Siltstone, Sandstone, Shale |
| Location | |
| Country | Mexico |
The La Caja Formation is a geologic formation in Mexico. It preserves fossils dating from the Kimmeridgian to the lower Berriasian. [1] La Caja Formation is widespread in northeastern and central Mexico and known for their abundant and diverse well-preserved ammonites. It was deposited in hemipelagic conditions, and predominantly consists of siliclastic sediments, including marl, with limestone. [2] It is laterally equivalent to the La Casita Formation, which represent more proximal facies. [3] The ichthyosaurs Ophthalmosaurus icenicus and Parrassaurus yacahuitztli , metriorhynchid Cricosaurus saltillensis , and the giant pliosaur "Monster of Aramberri" are known from the formation. [4] [5] [6] [7]
{{cite journal}}: CS1 maint: multiple names: authors list (link){{cite journal}}: CS1 maint: multiple names: authors list (link)