Carlile Shale

Geologic formation in the western US From Wikipedia, the free encyclopedia

Carlile Shale

The Carlile Shale is a Turonian age Upper/Late Cretaceous series shale geologic formation in the central-western United States, including in the Great Plains region of Colorado, Kansas, Nebraska, New Mexico, North Dakota, South Dakota, and Wyoming.[2]

Quick Facts Type, Unit of ...
Carlile Shale
Stratigraphic range: Turonian
~93.9–89.8 Ma
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Rare exposure of the Fairport Chalk member of the Carlile Shale in southern Ellis County, Kansas
TypeGeological formation
Unit ofColorado Group (lower); or
Benton Formation
Mancos Group (NM)
Sub-unitsJuana Lopez (CO, NM)
Codell Sandstone
Blue Hill Shale
Fairport Chalk
UnderliesNiobrara Formation
OverliesGreenhorn Limestone
Thickness170–230 feet (52–70 m)
Lithology
PrimaryShale, chalky to carbonaceous
OtherLimestone
Sandstone
Siltstone
Septarians
Bentonite
Location
Coordinates38.376°N 104.979°W / 38.376; -104.979
RegionMid-continental
Country United States
Type section
Named forCarlile Spring and Carlile Station, 21 mi west of Pueblo, Colorado[1]
Named byGilbert
Year defined1896
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Carlile Shale (the United States)
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Carlile Shale (Colorado)
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History of investigation

The Carlile Shale was first named by Grove Karl Gilbert for exposures at Carlile Spring, located about 21 miles (34 km) west of Pueblo, Colorado. He described it as a medium gray shale, capped with limestone or sandstone, and assigned it to the Benton Group.[3] By 1931, William Walden Rubey and his coinvestigators had mapped it into Kansas[4] and the Black Hills. Rubey also first assigned it to the Colorado Group.[5] C.H. Dane assigned it to the Mancos Shale in New Mexico in 1948.[6]

Description

The formation is composed of marine deposits of the generally retreating phase (hemi-cycle) of the Greenhorn cycle of the Western Interior Seaway, which followed the advancing phase of the same cycle that formed the underlying Graneros Shale and Greenhorn Formation.[7] As such, the lithology progresses from open ocean chalky shale (with thin limestones) to increasing carbonaceous shale to near-shore sandstone.[8] Near the center of the seaway, currents in the remnant shallows sorted skeletal remains into a mass of calcareous sand. The contact between the Carlile Shale and the overlying Niobrara Formation is marked by an unconformity in much of the outcrop area, but where an unconformity is not discernible, the boundary is typically placed at the first resistant, fine-grained limestone bed at the base of the Niobrara Formation.[9]

Fossil content

Summarize
Perspective

Upper Turonian series plesiosaur remains are among the fossils that have been recovered from the strata of its Blue Hill Shale Member in Kansas.[10] The Carlile in eastern South Dakota contains shark teeth, fossil wood and leaves, and ammonites.[11]

Reptiles

Crocodyliforms

More information Crocodyliforms, Genus ...
Crocodyliforms
GenusSpeciesLocation Stratigraphic position MaterialNotesImages
Terminonaris T. cf. T. browni Russell County, Kansas.[12] Fairport Chalk Member.[12] A partial rostrum.[12] A pholidosaur.
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Plesiosaurs

More information Plesiosaurs, Genus ...
Plesiosaurs
GenusSpeciesLocation Stratigraphic position MaterialNotesImages
Megacephalosaurus M. eulerti Near Fairport, Kansas.[13] Fairport Chalk Member.[13] A skull & anterior cervical material (FHSM VP-321).[13] A pliosaurid.
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Plesiosauria Mitchell County, Kansas.[10] Blue Hill Member.[10] Portions of a rib (FHSM VP-17299).[10] May represent a large elasmosaur or pliosaur.
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Squamates

More information Squamates, Genus ...
Squamates
GenusSpeciesLocation Stratigraphic position MaterialNotesImages
Coniasaurus C. cf. C. crassidens Russell County, Kansas.[14] Fairport Chalk Member.[14] 2 incomplete vertebrae (FHSM VP-4418).[14] A dolichosaurid.
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Russellosaurina Ellis County, Kansas.[15] Middle of the Fairport Chalk Member.[15] 7 successive proximal caudal vertebrae (FHSM VP-17564).[15] A russellosaurine mosasaur.
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Fish

Cartilaginous fish

More information Cartilaginous fish, Genus ...
Cartilaginous fish
GenusSpeciesLocation Stratigraphic position MaterialNotesImages
Cretodus C. houghtonorum North-central Kansas.[16] Blue Hill Shale.[16] A partial skeleton consisting of 134 disarticulated teeth, 61 vertebrae, 23 placoid scales, and fragments of calcified cartilage.[16] A mackerel shark.
Cretoxyrhina C. mantelli Dixon County, Nebraska.[17] Fairport Chalky Shale Member.[17] A tooth (UNSM 129549).[17] A large mackerel shark.
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Ptychodus P. latissimus Kansas.[18] Codell Sandstone Member.[18] 3 teeth.[18] A ptychodontid.
P. mammillaris North of Schoenchen, Ellis County, Kansas.[19] Fairport Chalk Member.[19] A medial tooth (FHSM VP-15284).[19] A ptychodontid.
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P. sp. Ellis County, Kansas.[20] Blue Hill Shale Member.[20] A tooth contained in a coprolite (FHSM VP-13325).[20] A ptychodontid.
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See also

  • Volcanic mineralization of the Greenhorn cycle:
    • Bentonite, sedimentary volcanic ash (named for the original Graneros/Greenhorn/Carlile classification), generally showing some weathered iron stain in the Colorado Group
    • Pyrite, precipitation of volcanic sulfuric acid with oceanic iron as FeS2
    • Limonite, pyrite in limestone weathered to HFeO2 (rust stain or yellow ochre)
    • Selenite, CaSO4 associated with Bentonite seams and ochre[21]

References

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