| Laborcita Formation | |
|---|---|
| Stratigraphic range: Gzhelian–Asselian PreꞒ Ꞓ O S D C P T J K Pg N | |
| Type | Formation |
| Underlies | Abo Formation |
| Overlies | Holder Formation |
| Thickness | 400 feet (120 m) |
| Lithology | |
| Primary | Limestone, conglomerate, sandstone. shale |
| Location | |
| Coordinates | 33°00′40″N 105°56′28″W / 33.011°N 105.941°W / 33.011; -105.941 |
| Region | New Mexico |
| Country | United States |
| Type section | |
| Named for | Laborcita Canyon |
| Named by | Otté |
| Year defined | 1959 |
  Laborcita Formation (the United States)Show map of the United States Laborcita Formation (New Mexico)Show map of New Mexico | |
The Laborcita Formation is a geologic formation in the Sacramento Mountains of New Mexico. It preserves fossils dating back to the late Pennsylvanian to early Permian.
Description
The formation is composed mostly of marine beds consisting of alternating cycles of limestone and siliciclastic sedimentary beds with a thickness of about 400 feet (120 m) at the type section. It is exposed only in a small area of the northernmost Sacramento Mountains, and transitions to mostly continental red mudstones some 1,000 feet (300 m) thick before abruptly pinching out to the southeast. The formation lies on the Holder Formation and is overlain by the Abo Formation.
The formation is interpreted as cyclic sequences of terrestrial and shallow marine carbonate rocks deposited on a narrow shelf lying between the Pedernal Uplift to the east and the Orogrande Basin to the west. Cycles are generally transgressive (recording the advance of the sea), with basal conglomerate giving way to increasingly fine sandstone, siltstone, and shale and finally limestone. Corresponding regressive sequences (recording the retreat of the sea) are very poorly developed.
Fossils
The limestone beds of the formation are highly fossiliferous, containing bioclastic remains from all the main late Paleozoic shallow marine biotic groups. Fusulinids are present that are characteristic of the latest Pennsylvanian and earliest Permian. The uppermost beds contain algal bioherms 35–60 feet (11–18 m) thick. Microfossils of the formation include the cyanobacteria such as Girvanella, calcivertellid foraminiferans, and phylloid (leaflike) algae such as Eugonophyllum.
History of investigation
The formation was first named by Otté in 1959 as part of his dissertation at the University of New Mexico.
See also
Footnotes
References
- Bowsher, Arthur L. (1987). "Paleozoic reef complexes of the Sacramento Mountains, New Mexico". Rocky Mountain Section of the Geological Society of America: 447–450. doi:10.1130/0-8137-5402-X.447.
- Cross, T. A.; Klosterman, M. J. (1981). "Autecology and Development of a Stromatolitic-Bound Phylloid Algal Bioherm, Laborcita Formation (Lower Permian), Sacramento Mountains, New Mexico, U.S.A.". Phanerozoic Stromatolites: 45–59. doi:10.1007/978-3-642-67913-1_6.
- Krainer, Karl; Vachard, Daniel; Lucas, Spencer G. (March 2003). "Microfacies and microfossil assemblages (smaller foraminifera, algae, pseudoalgae) of the Hueco Group and Laborcita Formation (upper Pennsylvanian-lower Permian), south-central New Mexico, USA". Rivista Italiana di Paleontologia e Stratigrafia. 109 (1): 3–36. Retrieved 5 August 2020.
- Otté, C. Jr. (1959). "Late Pennsylvanian and Early Permian stratigraphy of the northern Sacramento Mountains, Otero County. New Mexico". New Mexico Bureau of Mines and Mineral Resources Bulletin. 5Q (1).