The Red Beds of Texas and Oklahoma are a group of Early Permian-age geologic strata in the southwestern United States cropping out in north-central Texas and south-central Oklahoma. They comprise several stratigraphic groups, including the Clear Fork Group, the Wichita Group, and the Pease River Group.Nelson, John W., Robert W. Hook, and Dan S. Chaney (2013). Lithostratigraphy of the Lower Permian (Leonardian) Clear Fork Formation of North-Central Texas from The Carboniferous-Permian Transition: Bulletin 60, ed. Spencer G. Lucas et al. New Mexico Museum of Natural History and Science, pg. 286-311. Retrieved December 28, 2017. The Red Beds were first explored by American paleontologist Edward Drinker Cope starting in 1877.Cope, E.D. (1878). Descriptions of Batrachia and Reptilia from the Permian Formation of Texas. Proceedings of the American Philosophical Society, vol. 17, no. 101, pg. 505-30. Retrieved December 28, 2017. Fossil remains of many Permian tetrapods (four-limbed vertebrates) have been found in the Red Beds, including those of Dimetrodon, Edaphosaurus, Seymouria, Platyhystrix, and Eryops. A recurring feature in many of these animals is the sail structure on their backs.

Location Deposits dating from the Permian are present contiguously stretching from central Texas all the way into southern Nebraska.King, Philip B., and Helen M. Beikman (1976). The Paleozoic and Mesozoic Rocks; A Discussion to Accompany the Geologic Map of the United States. United States Geological Survey, Professional Paper 903, pg. 29-32. Retrieved December 29, 2017. In Nebraska and Kansas, deposits of light-colored limestone are frequent, while red-colored rocks are rare. In Oklahoma, the light-colored limestone transitions gradually into red-colored sandstone and shale until the limestone is virtually nonexistent in north-central Texas.Case, E.C. (1915). Chapter 1: Description of the Southern Portion of the Plains Province in The Permo-Carboniferous Red Beds of North America and Their Vertebrate Fauna. Carnegie Institute of Washington, pg. 5-61. Retrieved December 29, 2017. The portion of the red beds with abundant fossil deposits is in Texas between the Red River and the Salt Fork Brazos River.Benton, Michael (2001). Chapter Three: Four Feet on the Ground from The Book Of Life: An Illustrated History of the Evolution of Life on Earth, ed. Stephen Jay Gould. W.W. Norton: pg. 93-5. Retrieved December 28, 2017. The area includes the city of Wichita Falls, and rural communities such as Seymour and Archer City.Barnes, V.E., et al. (1987). Geologic atlas of Texas, Wichita Falls-Lawton sheet. University of Texas at Austin Bureau of Economic Geology. Retrieved December 28, 2017.

Properties

The Texas and Oklahoma red beds are sedimentary rocks, mostly consisting of sandstone and red mudstone.Sander, P. Martin (1989). Early Permian depositional environments and pond bonebeds in central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology, vol. 69, pg. 1-21. Retrieved December 28, 2017. The red color of the rocks is due to the presence of ferric oxide.Van Houten, Franklin (1973). Origin of Red Beds: A review - 1961-1972. Annual Review of Earth and Planetary Sciences, Vol. 1, pg. 39-61. Retrieved December 28, 2017. The rocks were deposited during the early Permian in a warm, moist climate,Baker, Charles Laurence (1916). Origin of Texas Red Beds. Bulletin of the University of Texas, No. 26. Retrieved December 28, 2017. with seasonal periods of dry conditions.Chaney, D.S., and W.A. DiMichele (2007). Paleobotany of the classic redbeds of north central Texas. Proceedings of the XVth International Congress on Carboniferous and Permian Stratigraphy, pg. 357-66. The Netherlands: Utrecht. Retrieved December 29, 2017.

Stratigraphy The Texas and Oklahoma red beds can be split into three primary stratigraphic groups: the Wichita Group, the Clear Fork Group, and the Pease River Group. The Wichita Group is the oldest of the three groups, having been deposited in the Sakmarian age.Johnson, Garyd (2013). Xenacanth Sharks and other Vertebrates from the Geraldine Bonebed, Lower Permian of Texas from The Carboniferous-Permian Transition: Bulletin 60, ed. Spencer G. Lucas et al. New Mexico Museum of Natural History and Science, pg. 161-7. Retrieved December 28, 2017. The Wichita Group contains some of the richest fossil deposits in the red beds, including the Geraldine Bonebed in Archer County. The Pease River Group is the most recent deposition, occurring during the Guadalupian epoch. The Clear Fork Group is in between the other two, being deposited during the Kungurian age. The stratigraphic groups are layered such that the Pease River Group overlies the Clear Fork Group, which overlies the Wichita group.

From youngest to oldest:

Pease River Group Blaine Formation San Angelo Formation Clear Fork Group Upper Clear Fork (Choza Formation) Middle Clear Fork (Vale Formation) Lower Clear Fork (Arroyo Formation) Wichita Group Waggoner Ranch Formation (equivalent to the Lueders Formation, Clyde Formation, Belle Plains Formation) Petrolia Formation (equivalent to the Belle Plains Formation) Nocona Formation (equivalent to the Admiral Formation) Bowie Group Archer City Formation (equivalent to the Moran Formation, Putnam Formation)

Fossil record In 1877, Edward Drinker Cope was the first paleontologist to study the red beds in search of fossils. Cope employed collectors to aid him in his search for bones, including Swiss botanist Jacob Boll. After Boll's death in 1880 while collecting, Cope employed preacher W.F. Cummins to continue the search. After Cope, paleontologists such as Ermine Cowles CaseCase, E.C. (1914). The Red Beds between Wichita Falls, Texas, and Las Vegas, New Mexico, in Relation to their Vertebrate Fauna. The Journal of Geology, vol. 22, no. 3, pg. 243-59. Retrieved December 28, 2017. and Alfred RomerRomer, Alfred, and Llewellyn Price (1940). Review of the Pelycosauria. Geological Society of America, Vol. 28, Special Paper. Retrieved December 28, 2017. found rich deposits of Permian-era tetrapods.

Geraldine Bonebed

The most prolific fossil site in the red beds is the Geraldine Bonebed within the Nocona Formation of the Wichita Group. During the Permian, the bonebed was the site of a freshwater pond. After a catastrophic event this became the burial site for a variety of terrestrial and marine animals.Sander, P. Martin (1987). Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology, Volume 61, pg. 221-36. Retrieved December 28, 2017. As a result, the bonebed contains a cross-section of life during the early Permian. Plant remains found in the bonebed include Calamites, ferns, and conifers. Marine life present in the bonebed include Xenacanthus, ostracods, and lungfish. The Geraldine Bonebed is most famous as a prolific source of temnospondyls, synapsids, basal reptiliomorphs and reptiles, including partial and complete skeletons of Archeria, Eryops, Edaphosaurus, Dimetrodon, Bolosaurus, Trimerorhachis, Zatrachys, and Ophiacodon.

Clear Fork deposits

The Clear Fork Group also contains multiple fossil sites. Like the Geraldine Bonebed and other Wichita Group sites, the Clear Fork Group is most famous for its early Permian amphibian deposits, especially Seymouria baylorensis. The species and genus were first discovered in 1904 by German paleontologist Ferdinand Broili.Williston, S.W. (1911). Restoration of Seymouria baylorensis Broili, an American Cotylosaur. The Journal of Geology, vol. 19, no. 3, pg. 232–7. Retrieved December 29, 2017. Seymouria baylorensis is named for the location of its discovery in Baylor County near the city of Seymour. As one of the few Seymouria bone sites in the world, paleontologists have studied the Clear Fork deposit for evidence of Seymouria as a transitional fossil between aquatic and terrestrial animals, as well as Seymouria's close relationship to amniotes.Laurin, Michel (1996) A redescription of the cranial anatomy of Seymouria baylorensis, the best known seymouriamorph. PaleoBios, Vol. 17, no. 1, pg. 1-16. Retrieved December 29, 2017.Carrol, Robert L., and Robert B. Holmes (2008). Evolution of the Appendicular Skeleton of Amphibians from Fins into Limbs: Evolution, Development, and Transformation, ed. Brian K. Hall. University of Chicago Press, pg. 206-9.

The Clear Fork Group also contains deposits of plant species throughout its different sections. The increasing prevalence of seed plants with pockets of water-based plants can be used to infer a wet, but drying climate.

See also Geology of Wichita Falls, Texas Geology of Texas Paleontology in Texas

References