Capitan Formation

Capitan Formation
Stratigraphic range: Guadalupian
The Capitan Formation underlies El Capitan in Guadalupe Mountains National Park.
Type	Formation
Underlies	Artesia Group, Castile Formation
Overlies	Goat Seep Dolomite, Delaware Mountain Group
Thickness	1,800 ft (550 m)
Lithology
Primary	Limestone
Other	Dolomite
Location
Coordinates	31.8773°N 104.8668°W / 31.8773; -104.8668
Region	Texas New Mexico
Country	United States
Type section
Named for	El Capitan Peak
Named by	G.B. Richardson
Year defined	1904
Capitan Formation (the United States) Capitan Formation (Texas)

The Capitan Formation is a geologic formation found in western Texas and southeastern New Mexico. It is a fossilized reef dating to the Guadalupian Age of the Permian period.

The formation underlies El Capitan in Guadalupe Mountains National Park, and the formation and its associated basin, shelf margin, and backreef formations have been described as "the largest, best-preserved, most accessible, and most intensively studied Paleozoic reef complex in the world."

History of investigation

The Guadalupe Mountains were first described in the reports of 1849 and 1850 United States military expeditions to the area. George Shumard was the first geologist to study the area, in 1855, and described an "upper white limestone" containing fossils. These included fusilinids and brachiopods, that were identified correctly by his brother, B.F. Shumard, as Permian in age. However, debate on whether the beds were Carboniferous or Permian in age continued until at least 1920. The work of Darton and Reeside in 1926 established the accepted framework for the stratigraphy of the area, and identified the Capitan Formation as late Permian in age.

The Capitan Formation itself was first named by G.B. Richardson in 1904 for exposures in the Guadalupe Mountains. Richardson was impressed by the great mass of seemingly uniform limestone, forming vertical cliffs over 1,000 feet (300 m) tall, and noted that much of the limestone was dolomitized. He was also impressed with the abundant fossils found in the middle beds of the formation, forming a fossil assemblage unlike anything else known at that time. Richardson interpreted the Guadalupe Mountains as an east-dipping monocline with a fault on the steep western boundary, and believed El Capitan itself was a product of erosion.

Interest in the formation was rekindled by the discovery in May 1923 of the Big Lake oil field in Texas and the drilling of the first commercial oil well in southeastern New Mexico in 1924. This culminated in the publication by E. Russell Lloyd in 1929 of his interpretation of the Capitan Limestone and associated formations as a gigantic fossil coral reef. Lloyd traced the reef nearly to Carlsbad and noted that the dissimilarity of the formations on the two sides of the reef, now known as the basin and backreef shelf facies. Two months later, a “Symposium on Pennsylvanian and Permian stratigraphy of southwestern United States” appeared in the August, 1929 issue of the Bulletin of the American Association of Petroleum Geologists, which provided a flood of new details on the Capitan reef.

As part of that symposium, Philip B. King and R.E. King presented their conclusion that the Tessey, Gilliam, and Vidrio Limestones of the Glass Mountains of west Texas were correlative with the Capitan Formation, and redesigned them as members of the formation. However, by 1937, King had concluded that the Tessey Limestone was not part of the Capital Formation and removed it as a member. By 1942 he had restricted the definition of the Capitan Formation to reef limestone, consistent with the stratigraphic conventions in the Guadalupe Mountains, and removed the Gilliam and most of the Vidrio Limestone from the formation.

Description

The Capital Formation consists of compact, massive, light grey to white limestone with minor dolomite. Its total thickness is 1,000–2,000 feet (300–610 m). On the backreef side of the formation, the Capitan rests on the Goat Seep Dolomite and is overlain by the Artesia Group, while on the basin side, the Capitan rests on the Delaware Mountain Group and is overlain by the Castile Formation.

Fossils

Richardson (1904) found that the upper and lower beds of the formation were relatively unfossiliferous, but the middle section contained an abundant fossil assemblage unlike any other known at that time.

Fusulinida

• Fusilina elongata

Porifera

• Numerous species

Anthozoa

• A few species

Bryozoa

• Acanthocladia
• Goniocladia

Brachiopoda

• Streptorhynchus
• Orthotetes
• Geyerella
• Orthothetina
• Chonetes
• Productus occidentalis
• P. subhotridus
• P. popei
• P. mexicanus
• Marginifera pileolus
• Spirifer mexicanus
• Spirifer sev sp.
• Martinia
• Squamularia guadalupensis
• Ambocoelia
• Spiriferina billingsi
• Hustedia meekana
• Pugnax swallowiana
• Rhynchonella indentata
• Terebratuloids
• Leptodus
• Richthofenia permiana

Mollusca

• Schizodus securas
• Aviculopecten]
• Lima
• Camptonectes
• Streblopteria
• Myalina squamosa
• Myoconcha
• Indeterminate gastropods

See also

• List of fossiliferous stratigraphic units in Texas
• Paleontology in Texas

References

• Darton, N. H.; Reeside, J. B. (30 September 1926). "Guadalupe Group". Geological Society of America Bulletin. 37 (3): 413–428. doi:10.1130/GSAB-37-413.
• King, P.B. (1930). "The geology of the Glass Mountains, Texas; Part 1, Descriptive geology". University of Texas Bulletin. 3038.
• King, P.B. (1937). "Geology of the southern Guadalupe Mountains, Texas". U.S. Geological Survey Professional Paper. 187. doi:10.3133/pp187.
• King, Philip B. (1948). "Geology of the Southern Guadalupe Mountains, Texas". U.S. Geological Survey Professional Paper. 215. doi:10.3133/pp215.
• King, P.B., (1942). "Permian of West Texas and Southeastern New Mexico: PART 1". AAPG Bulletin. 26. doi:10.1306/3D933466-16B1-11D7-8645000102C1865D.{{cite journal}}: CS1 maint: extra punctuation (link) CS1 maint: multiple names: authors list (link)
• King, Philip B.; King, Robert E. (1929). "Stratigraphy of Outcropping Carboniferous and Permian Rocks of Trans-Pecos Texas". AAPG Bulletin. 13. doi:10.1306/3D93286B-16B1-11D7-8645000102C1865D.
• Kues, Barry S. (2006). "Geological studies of the Guadalupe Mountains area, New Mexico and West Texas, to 1928" (PDF). New Mexico Geological Society Field Conference Series. 57: 127–144. Retrieved 20 September 2020.
• 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. ISBN 9781585460106.
• Lahee, Frederic H. (August 1929). "Foreword: SYMPOSIUM ON PENNSYLVANIAN AND PERMIAN STRATIGRAPHY OF SOUTHWESTERN UNITED STATES". Bulletin of the American Association of Petroleum Geologists. 13 (8). Retrieved 20 September 2020.
• Lloyd, E. Russell (1929). "Capitan Limestone and Associated Formations of New Mexico and Texas". AAPG Bulletin. 13. doi:10.1306/3D932855-16B1-11D7-8645000102C1865D.
• "Geologic Formations". Guadalupe Mountains National Park, Texas. National Park Service. Retrieved 19 September 2020.
• Richardson, G.B. (1904). "Report of a reconnaissance in Trans-Pecos Texas north of the Texas and Pacific Railway". University of Texas Mineral Survey Bulletin. 9. Retrieved 19 September 2020.
• Richardson, G B. (Jun 1908). "Paleozoic Formations in Trans-Pecos Texas". American Journal of Science (1880-1910). 25 (150): 474. Retrieved 20 September 2020.