Earth:McRae Formation

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Short description: A geologic formation in New Mexico
McRae Formation
Stratigraphic range: Maastrichtian (Lancian)
~70–66 Ma
McRae Formation.jpg
McRae Formation near its type location, Elephant Butte Reservoir, New Mexico, USA. The light bands are "bathtub rings" from stands of the reservoir.
TypeGeological formation
Sub-unitsHall Lake & Jose Creek Members
UnderliesLove Ranch Formation
OverliesMesaverde Group
Thickness3,000 ft (910 m)
Lithology
PrimarySandstone, shale, conglomerate
OtherTuff
Location
Coordinates [ ⚑ ] : 33°11′49″N 107°10′01″W / 33.197°N 107.167°W / 33.197; -107.167
Paleocoordinates [ ⚑ ] 40°24′N 85°42′W / 40.4°N 85.7°W / 40.4; -85.7
RegionNew Mexico
Country United States
Type section
Named forFort McRae
Named byKelley & Silver
Year defined1952
McRae Formation is located in the United States
McRae Formation
McRae Formation (the United States)
McRae Formation is located in New Mexico
McRae Formation
McRae Formation (New Mexico)

The McRae Formation is a geological formation exposed in southern New Mexico whose strata date back to the Late Cretaceous.[1] Dinosaur remains are among the fossils that have been recovered from the formation.[2][3][4][5]

Description

The formation consists of a basal conglomerate interbedded with shale and siltstone and a sequence of alternating sandstone and shale. The lower conglomerates contain volcanic debris, while the upper beds contain sparse nonvolcanic rock fragments. The shales are reddish brown to purplish while the sandstones are light gray. The sandstones are medium bedded to massive and sometimes form hogbacks. The total thickness is in excess of 3,000 feet (910 m). The formation is present around Elephant Butte Reservoir, in the Caballo Mountains, and under much of the Jornada del Muerto. It overlies the Mesaverde Group, from which it derives much of its sediments.[1] It is overlain by the Love Ranch Formation.[6]

The formation is divided into the lower Jose Creek Member and the upper Hall Lake Member. The Jose Creek member is interpreted as mudflow or alluvial fan deposits emplaced in a humid tropical to semitropical environment. It includes distinctive breccia conglomerate beds.[7][8]

Fossil evidence firmly establishes that most of the McRae Formation is late Cretaceous in age. However, it is possible that some of the uppermost beds extend into the Paleocene.[9]

Fossil content

The formation contains a floral assemblage that includes Geinitzia cf. formosa, Canna magnifolia, Phyllites cf. ratonensis, Salix, Cinnamomum, Sabalites montana, Araucarites longifolia, Ficus planicostata, and Sequoia.[8][10][11]

Vertebrate paleofauna

W.T. Lee found a ceratopsian skeleton in the area in 1905. Additional vertebrate fossil fragments have been found at twelve locations, generally along the contact between the Jose Creek and Hall Lake members, that include ceratopsian frill and jaw fragments, ankylosaur armor fragments, a sauropod femur, and an incomplete jaw of Tyrannosaurus rex (found by a yachtsman in 1983.)[9][8] Turtle fossils have also been unearthed here.[12]

History of investigation

The formation was first named by V.C. Kelley and Caswell Silver in 1952 for Fort McRae. They designated the type location as the base of Elephant Butte and the eastern shore of Elephant Butte Reservoir.[1] H.P. Bushnell divided the formation into members in 1955.[7]

Kenneth Segerstrom and his coinvestigators argued in 1979 that the beds of the Cub Mountain Formation properly belong to the McRae Formation.[18] Spencer G. Lucas and his coinvestigators disagreed on the basis of fossil evidence, placing the former formation in the Eocene.[19]

In 2019, Lucas and his coinvestigators proposed promoting the McRae Formation to group rank and adding the Double Canyon Formation as its uppermost member. The Double Canyon Formation is over 425 meters (1,394 ft) of mudstone with some sandstone and conglomerate found between Elaphant Butte Reservoir and the Fra Cristobal Mountains to the northeast.[20]

See also

References

  1. 1.0 1.1 1.2 Kelley & Silver 1952.
  2. Weishampel, Dodson & Osmólska 2004, pp. 574-588.
  3. Lozinsky, Richard; Hunt, Adrian; Wolberg, Donald; Lucas, Spencer. "Late Cretaceous (Lancian) dinosaurs from the McRae Formation, Sierra County, New Mexico". New Mexico Geology 6: 72–77. https://www.researchgate.net/publication/267818177. 
  4. Wolberg, Donald; Lozinsky, Richard; Hunt, Adrian (1986). "Late Cretaceous (Maastrichtian-Lancian) vertebrate paleontology of the McRae Formation, Elephant Butte area, Sierra County, New Mexico". New Mexico Geological Society 37: 227–234. https://nmgs.nmt.edu/publications/guidebooks/downloads/37/37_p0227_p0234.pdf. 
  5. Buck, Brenda J.; Mack, Greg H. (October 1995). "Latest Cretaceous (Maastrichtian) aridity indicated by paleosols in the McRae Formation, south-central New Mexico". Cretaceous Research 16 (5): 559–572. doi:10.1006/cres.1995.1036. ISSN 0195-6671. Bibcode1995CrRes..16..559B. http://dx.doi.org/10.1006/cres.1995.1036. 
  6. Seager 2004, p. 192.
  7. 7.0 7.1 Bushnell 1955.
  8. 8.0 8.1 8.2 Lozinsky 1986.
  9. 9.0 9.1 Lozinsky et al. 1984.
  10. Estrada-Ruiz, Emilio; Upchurch, Garland R.; Wheeler, Elisabeth A.; Mack, Greg H. (May 2012). "Late Cretaceous Angiosperm Woods from the Crevasse Canyon and McRae Formations, South-Central New Mexico, USA: Part 1". International Journal of Plant Sciences 173 (4): 412–428. doi:10.1086/664714. ISSN 1058-5893. http://dx.doi.org/10.1086/664714. 
  11. Estrada-Ruiz, Emilio; Wheeler, Elisabeth A.; Upchurch, Garland R.; Mack, Greg H. (February 2018). "Late Cretaceous Angiosperm Woods from the McRae Formation, South-Central New Mexico, USA: Part 2". International Journal of Plant Sciences 179 (2): 136–150. doi:10.1086/695503. ISSN 1058-5893. http://dx.doi.org/10.1086/695503. 
  12. Lichtig, Asher; Lucas, Spencer (2015). "Cretaceous Turtles of New Mexico". Fossil Record 4 (67): 129–138. https://books.google.com/books?id=au2oDQAAQBAJ. 
  13. 13.0 13.1 13.2 Lozinsky et al. 1984, pp. 73-77.
  14. Gillette, David; Wolberg, David; Hunt, Adrian (1986). "Tyrannosaurus rex from the McRae Formation (Lancian, Upper Cretaceous), Elephant Butte reservoir, Sierra County, New Mexico". New Mexico Geological Society 37th Annual Fall Field Conference Guidebook: 235–238. https://nmgs.nmt.edu/publications/guidebooks/downloads/37/37_p0235_p0238.pdf. 
  15. Lucas, Mack & Estep 1998, pp. 223–227.
  16. Hunt, Rebecca K.; Lehman, Thomas M. (November 2008). "Attributes of the ceratopsian dinosaur Torosaurus, and new material from the Javelina Formation (Maastrichtian) of Texas". Journal of Paleontology 82 (6): 1127–1138. doi:10.1017/s0022336000055335. ISSN 0022-3360. http://dx.doi.org/10.1017/s0022336000055335. 
  17. Williamson, Thomas E.; Weil, Anne (2008-12-12). "Stratigraphic distribution of sauropods in the Upper Cretaceous of the San Juan Basin, New Mexico, with comments on North America's Cretaceous 'sauropod hiatus'". Journal of Vertebrate Paleontology 28 (4): 1218–1223. doi:10.1671/0272-4634-28.4.1218. ISSN 0272-4634. Bibcode2008JVPal..28.1218W. http://dx.doi.org/10.1671/0272-4634-28.4.1218. 
  18. Segerstrom, Stotelmeyer & Williams 1979.
  19. Lucas et al. 1989.
  20. Lucas et al. 2019.

Bibliography