The Glencairn Formation consists of dark gray shale and buff sandstone and siltstone. It disconformably overlies the Lytle Formation, underlies the Dakota Group, and varies in thickness from 10–145 feet (3.0–44.2 m).[1][3] The formation is present from central Colorado[1] to the valley of the Dry Cimarron in northeastern New Mexico.[3] The formation locally contains gypsum veins and gypsum-filled desiccation cracks.[1]
The exposures at the valley of the Dry Cimarron include a basal sandstone bed, the Long Canyon Sandstone Bed, that is up to 3 meters (9.8 ft) thick, is heavily bioturbated, and contains an abundant late Albian invertebrate fossil fauna.[3] This is interpreted as infilling of a drainage system preceding the Kiowa-Skull Creek transgression.[4] It is likely the lateral equivalent of the Tucumcari Shale.[5]
Fossils
The lower beds of the formation are heavily bioturbated and contain abundant fossils of the gryphaeid oyster Texigryphea.[6] The upper beds locally contain petrified plant material.[3] The formation also contains ammonoids, including Goodhallites, Idiohamites, and Engonoceras uddeni, and associated solitary corals, bivalves, and gastropods[7]
History of investigation
The formation was first named as the Glencairn shale member of the now abandoned Purgatoire Formation by G.I. Finlay in 1916, for exposures near Lytle, Colorado.[1] Waage subsequently traced the unit into northeastern New Mexico,[2] where it has been raised to formation rank.[8][3]
^Holbrook, John M.; Dunbar, Robyn Wright (1 July 1992). "Depositional history of Lower Cretaceous strata in northeastern New Mexico: Implications for regional tectonics and depositional sequences". GSA Bulletin. 104 (7): 802–813. Bibcode:1992GSAB..104..802H. doi:10.1130/0016-7606(1992)104<0802:DHOLCS>2.3.CO;2.
