The formation is interpreted as a shallow-shelf marine formation of Virgilian (latest Pennsylvanian) age[3] during a global ice age.[4]
Fossils
Bioherms are present at the base of the formation.[1] These are up to 50–75 feet (15–23 meters) thick.[3] They are composed of uncalcified cup-shaped phylloid (leaf-like[5]) algae surrounded by masses of beresellid algae.[4]
History of investigation
The unit was first named by Lloyd C. Pray in 1954[1] and a type section was designated in 1959.[6] Pray originally assigned the formation to the Magdalena Group, but the Magdalena Group has subsequently been abandoned.[3][2]
Baars, D. L.; Torres, Andrew M. (October 1991). "Late Paleozoic Phylloid Algae: A Pragmatic Review". PALAIOS. 6 (5): 513. doi:10.2307/3514989.
Choh, Suk-Joo; Kirkland, Brenda L. (1 September 2008). "Sedimentologic role ofin situ Beresellid algal colonies, Holder Formation (Upper Pennsylvanian), New Mexico, U.S.A.". Carbonates and Evaporites. 23 (2): 79–88. doi:10.1007/BF03176154.
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: New Mexico Geological Society Special Volume 11. pp. 95–136. ISBN9781585460106.
Pray, L.C. (1959). "Stratigraphic and structural features of the Sacramento Mountain Escarpment, New Mexico". In Pray, L.C. (ed.). Guidebook for joint field conference in the Sacramento Mountains of Otero County, New Mexico. Alamogordo, NM: Society of Economic Paleontologists and Mineralogists, Permian Basin Section, Field Trip Guidebook, Joint field conference of Society of Economic Paleontologists and Mineralogists, Permian Basin Section, and Roswell Geological Society. pp. 86–130.