| Berino Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Formation |
| Underlies | Bishop Cap Formation |
| Overlies | La Tuna Formation |
| Thickness | 555 ft (169 m) |
| Lithology | |
| Primary | Limestone |
| Other | Shale |
| Location | |
| Coordinates | 31°58′0″N 106°31′30″W / 31.96667°N 106.52500°W |
| Region | New Mexico |
| Country | United States |
| Type section | |
| Named for | Berino, New Mexico |
| Named by | L.A. Nelson |
| Year defined | 1940 |
  Berino Formation (the United States)  Berino Formation (New Mexico) | |
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 20 feet (6.1 meters) thick, with a prominent massive limestone bed 70 feet (21 meters) thick capping the formation. [1] The total thickness is 555 feet (169 meters). 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]
- ^ a b c d Harbour, R.L. (1972). "Geology of the northern Franklin Mountains, Texas and New Mexico". U.S. Geological Survey Bulletin. 1298. doi: 10.3133/b1298.
- ^ a b Nelson, L.A. (1940). "Paleozoic stratigraphy of the Franklin Mountains, West Texas". American Association of Petroleum Geologists Bulletin. 24 (1): 157–172. doi: 10.1306/3D93319A-16B1-11D7-8645000102C1865D.
- ^ Nelson, L.A. (1937). "Gastropoda from the Pennsylvanian (Magdalena) of the Franklin Mountains of west Texas [abstract of thesis]". Colorado University Studies. 25 (1): 89–91.
- ^ Kues, B.S.; Giles, K.A. (2004). "The late Paleozoic Ancestral Rocky Mountain system in New Mexico". In Mack, G.H.; Giles, K.A. (eds.). The geology of New Mexico. A geologic history (Special Volume 11). New Mexico Geological Society. p. 98.
| Berino Formation | |
|---|---|
| Stratigraphic range: | |
| Type | Formation |
| Underlies | Bishop Cap Formation |
| Overlies | La Tuna Formation |
| Thickness | 555 ft (169 m) |
| Lithology | |
| Primary | Limestone |
| Other | Shale |
| Location | |
| Coordinates | 31°58′0″N 106°31′30″W / 31.96667°N 106.52500°W |
| Region | New Mexico |
| Country | United States |
| Type section | |
| Named for | Berino, New Mexico |
| Named by | L.A. Nelson |
| Year defined | 1940 |
Berino Formation (the United States) Berino Formation (New Mexico) | |
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 20 feet (6.1 meters) thick, with a prominent massive limestone bed 70 feet (21 meters) thick capping the formation. [1] The total thickness is 555 feet (169 meters). 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]
- ^ a b c d Harbour, R.L. (1972). "Geology of the northern Franklin Mountains, Texas and New Mexico". U.S. Geological Survey Bulletin. 1298. doi: 10.3133/b1298.
- ^ a b Nelson, L.A. (1940). "Paleozoic stratigraphy of the Franklin Mountains, West Texas". American Association of Petroleum Geologists Bulletin. 24 (1): 157–172. doi: 10.1306/3D93319A-16B1-11D7-8645000102C1865D.
- ^ Nelson, L.A. (1937). "Gastropoda from the Pennsylvanian (Magdalena) of the Franklin Mountains of west Texas [abstract of thesis]". Colorado University Studies. 25 (1): 89–91.
- ^ Kues, B.S.; Giles, K.A. (2004). "The late Paleozoic Ancestral Rocky Mountain system in New Mexico". In Mack, G.H.; Giles, K.A. (eds.). The geology of New Mexico. A geologic history (Special Volume 11). New Mexico Geological Society. p. 98.