| Berino Formation | |
| Type: | Formation |
| Period: | middle Pennsylvanian |
| Prilithology: | Limestone |
| Otherlithology: | Shale |
| Namedfor: | Berino, New Mexico |
| Namedby: | L.A. Nelson |
| Year Ts: | 1940 |
| Region: | New Mexico |
| Country: | United States |
| Coordinates: | 31.9667°N -106.525°W |
| Underlies: | Bishop Cap Formation |
| Overlies: | La Tuna Formation |
| Thickness: | 555feet |
The Berino Formation is a geologic formation in the Franklin Mountains of southern New Mexico and western Texas. It preserves fossils dating back to the middle Pennsylvanian.[1]
The unit consists mostly of fossiliferous limestone with some interbedded shale.[2] The shale is more abundant in the base of the formation, and the formation as a whole appears brown banded in outcrop. Beds are typically about 20feet thick, with a prominent massive limestone bed 70feet thick capping the formation.[1] The total thickness is 555feet. The unit lies on the La Tuna Formation and is overlain by the Bishop Cap Formation.[2]
The formation is interpreted as resulting from deposition of rhythmically alternating lime and clay in a shallow marine environment.[1]
The Berino Formation contains abundant fossils, including ichnofossils. These include the fusulinid Fusulinella euryteines and brachiopods, corals, and bryozoa. Fragments of petrified wood are found at the base of the formation and are interpreted as remnants of tree trunks carried out to sea.[1]
The unit was designated the Berino Member of the Magdalena Group by L.A. Nelson in 1937.[3] Kues and Giles recommended discarding the Magdalena Group and raising the unit to formation rank in 2004.[4]