Bell Ranch Formation

Last updated
Bell Ranch Formation
Stratigraphic range: Kimmeridgian
~155–151  Ma
O
S
D
C
P
T
J
K
Pg
N
Type Geological formation
Unit of San Rafael Group
Underlies Morrison Formation
Overlies Exeter Sandstone
Thickness66 feet (20 m)
Lithology
Primary Sandstone
Other Siltstone
Location
Coordinates 35°18′14″N103°53′12″W / 35.3040°N 103.8867°W / 35.3040; -103.8867
Approximate paleocoordinates 31°30′N49°42′W / 31.5°N 49.7°W / 31.5; -49.7
Region New Mexico
Oklahoma
CountryFlag of the United States (23px).png  United States
Type section
Named forBell Ranch
Named byGriggs and Read
Year defined1959
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Cyan pog.svg
Bell Ranch Formation (the United States)
USA New Mexico relief location map.svg
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Bell Ranch Formation (New Mexico)

The Bell Ranch Formation is a Late Jurassic (Kimmeridgian) geologic formation in eastern and northeastern New Mexico and the western Oklahoma panhandle. Fossil theropod tracks have been reported from the formation. [1] [2]

Contents

Description

At the type section near Tucumcari, the formation consists of alternating beds of light gray sandstone and brownish red siltstone. Bed thicknesses vary from 2–10 feet (0.61–3.05 m), distinguishing the unit from the massive sandstone of the underlying Exeter Sandstone and poorly bedded sediments of the overlying Morrison Formation. Small gypsum nodules are present in the upper beds. Thickness is up to 66 feet (20 m). [3] Further north, in the valley of the Dry Cimarron, the facies changes to dark mudstone with no cycles and more abundant gypsum. Here the thickness is no more than 8 meters (26 ft). [4]

Fossil content

The formation contains sandy track beds which are "mud-cracked" with finer brownish silty interbeds and an overlying conglomeratic sandstone which fills the mudcracks of the upper bed. [5] Three trackways of large dinosaurs are present. [2]

Ichnofossils

History of investigation

The beds making up the unit were originally assigned to the Wanakah Formation, but were renamed by Griggs and Read in 1959 for exposures at Carpenter's Point, 13 miles (21 km) northwest of Tucumcari. [3] The correlation with the Wanakah is uncertain. [6] In 1987, Conrad et al. correlated the "brown-silt member" assigned by Baldwin and Muehlberger to the Morrison Formation in the valley of the Dry Cimarron [7] to the Bell Ranch Formation. [2]

In 1992, Anderson and Lucas advocated abandoning the Bell Ranch Formation in favor of the Summerville Formation. [8] However, this has not be universally accepted. [4]

See also

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References

  1. Weishampel, Dodson & Osmólska 2004, pp. 517–607.
  2. 1 2 3 Conrad, Lockley & Prince 1987.
  3. 1 2 Griggs & Read 1959.
  4. 1 2 Ziegler, Ramos & Zimmerer 2019.
  5. Fossilworks 2021.
  6. Scott 1986.
  7. Baldwin & Muehlberger 1959.
  8. Anderson & Lucas 1992.

Bibliography

Further reading