Coyote Butte Limestone facts for kids

Quick facts for kids Coyote Butte Limestone Stratigraphic range: Sakmarian (Wolfcampian)-Kungurian ~296–273Ma PreЄ Є O S D C P T J K Pg N
Type	Formation
Lithology
Primary	Limestone
Other	Sandstone
Location
Coordinates	43°58′N 119°44′W / 43.96°N 119.74°W / 43.96; -119.74
Approximate paleocoordinates	17°54′N 38°48′W / 17.9°N 38.8°W / 17.9; -38.8
Region	Crook County, Oregon
Country	United States
Extent	Isolated buttes (Coyote & Tuckers) south and north (Triangulation Hill) of Grindstone & Twelvemile Creeks, Crook County, Oregon
Type section
Named for	Coyote Butte
Named by	Merriam & Berthiaume
Year defined	1943

The Coyote Butte Limestone (OR085) is a geologic formation in Oregon. It preserves fossils dating back to the Sakmarian to Kungurian stages of the Permian period, spanning an estimated 23 million years. The formation occurs in isolated buttes to the north; Triangulation Hill, and south; type locality and name giver Coyote Butte and Tuckers Butte, on either side of the Grindstone and Twelvemile Creeks in Crook County, Oregon.

Description

The Coyote Butte Formation was first defined by Merriam and Berthiaume in 1943. The formation crops out in isolated buttes (Coyote & Tuckers) south and north (Triangulation Hill) of the Grindstone and Twelvemile Creeks in Crook County, central Oregon. The formation comprises an uncommonly unaltered and well-exposed set of Permian shallow marine and reefal limestones in the tectonically complex Permian present-day Pacific margin of western North America.

The Coyote Butte Formation is represented by isolated limestone hills (0.1 to 2.0 square kilometres (0.039 to 0.772 sq mi) in area), of which most appear to have the same stratigraphic and biostratigraphic sequence and appear to be right-side-up. The resistant limestone blocks stand above the surrounding rocks of the "melange." The Coyote Butte Formation represents shallow-water carbonate-platform deposition and contains a varied faunal assemblage of corals, bryozoans, algae, fusulinids, brachiopods, crinoids, and conodonts.

"The Permian Coyote Butte Formation is dated by conodonts, fusulinids, and brachiopods as Aktastinian, Leonardian, and Roadian (stages of Furnish, 1973). The formation shows remarkable similarity in age, fauna, and sedimentation to the limestones near Quinn River Crossing, Nevada. The Paleozoic limestone blocks rest among oceanic-derived blocks that are probably early Mesozoic in age. To imply that the limestone belonged to the same tectonic-sedimentary package as the oceanic sediments (Dickinson and Thayer, 1978) seems precluded. The limestones contain volcaniclastic sand (Dickinson and Thayer, 1978, p. 152), indicating probable local presence of volcanics during deposition. Because the outcrops of the Coyote Butte Formation appear to all be stratigraphically right-side-up, the "melange" is not as chaotic as proposed by Dickinson and Thayer (1978); it has some order.

Also, it would be hard to imagine the Coyote Butte Formation as deposited as local limestone in a volcanic island chain and then admixed to the deformed oceanic sediments while maintaining its stratigraphic integrity.

It is easier to imagine the Coyote Butte Formation as being introduced as a late-stage structural event to deforming oceanic sediments in Mesozoic time. This implies that the other Paleozoic rocks would be similar late-stage introductions to the "melange." Whether the Coyote Butte Formation represents the remnants of a large olistostrome (gravity slide block) or thrust block or blocks that maintained stratigraphic integrity is difficult to resolve, given the poor exposures in the Coyote Butte area.

Because the Coyote Butte Formation is so similar to rocks found near Quinn River Crossing, it is suggestive that the rocks belong to a larger mass of shelfal limestones, parts of which are now found at several scattered localities."

Paleogeographic situation

The formation is dated to the Sakmarian to Kungurian stages of the Early to Middle Permian period, spanning an estimated 23 million years from 296 to 273 Ma. During these times, what is now central Oregon, was located at the edge of Pangea in the northern paleotemperate zone, at paleolatitudes of 16-18° North.

Climate

Tectonics

The hinterland of the carbonate platform where the Coyote Butte Limestone was deposited, was formed by the Arizonan and Utahan arid landscapes of a Pangea starting to break up. This occurred before the Sonoma orogeny was active in western North America and during the Alleghanian orogeny in eastern Laurentia and western Europe.

The 23 million year deposition coincided with impact of the Clearwater West crater, dated at 286.2 ± 2.6 million years ago.

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  Paleogeography of the Early Permian, 280 Ma

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  Location of the Alleghanian mountain chains in the Carboniferous period, just before the Permian

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  Clearwater Lakes in Quebec, the larger West crater dated to 286.2 ± 2.6 Ma

Paleontological significance

The formation is the only discovered Paleozoic fossiliferous formation in the state of Oregon, and comprises an uncommonly unaltered and well-exposed set of Early to Mid Permian shallow marine and reefal limestones in the tectonically complex Permian present-day Pacific margin of western North America. The formation just predates Olson's Extinction; a mass extinction that occurred 273 million years ago in the early Guadalupian of the Permian period and which predated the Permian–Triassic extinction event.

Fossil content

Among others, the following fossils have been reported from the formation:

Brachiopods

Trilobites

Cummingella belisama

• Proetida
  • Phillipsiidae
    • Cummingella (Cummingella) sp.

Rostroconchia

• Conocardiida
  • Conocardiidae
    • Arceodomus sphairikos

Gastropods

• Prosobranchia
  • Acteoninidae
    • Acteonina permiana

Polyplacophora

• Neoloricata
  • Acutichitonidae
    • Arcochiton soccus
  • Homeochiton triangularis
  • Gryphochitonidae
    • Gryphochiton planoplata
  • Lepidopleuridae
    • ?Chauliochiton sp.
    • Pterochiton sp.
  • Strobilepidae
    • Diadeloplax apiculatus

Corals

Correlations

Geologic correlations

Faunal correlations

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  Restoration of Captorhinus from Oklahoma and Texas

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  Restoration of Cisuralian, 295–272 Ma, Dimetrodon and the temnospondyl Eryops, both found in the Red Beds of Texas

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  Platyhystrix (small, foreground) and Edaphosaurus from Early Permian Texas

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  A fossil of Seymouria baylorensis displayed at the National Museum of Natural History

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  Ophiacodon widespread in Early Permian North America

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  Callibrachion from Black Shales of Autun, near Margenne (Artinskian France)