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Mule Spring Limestone

American geologic formation From Wikipedia, the free encyclopedia

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The Mule Spring Limestone is a geologic formation in the Saline Range of eastern California and Split Mountain and Goldfield Hills of Nevada.

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It is also to be found in the Inyo Mountains and White Mountains.

It preserves fossils, such as trilobites, and algal structures like Girvanella, dating back to the Cambrian period.[2][1]

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Geology

The Mule Spring Limestone, as its name suggests, is mainly composed of limestone rocks. These rocks are medium-gray to light-medium-gray, as well as very fine to fine crystalline, and is thin to very thin-bedded in most areas. In the lower sections of the formation, there are also occasional layers, up to 500 ft (150 m) thick, of pale-yellowish-brown or greenish-gray shale, limy siltstone and silty limestone.[1] In the Split Mountain, the formation overlies the Harkless Formation and underlies the Emigrant Formation,[1][3] whilst in other areas it overlies the Saline Valley Formation and underlies the Monola Formation.[1]

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Paleobiota

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The Mule Spring Limestone contains examples of Archaeocyatha, a clade of sponges that went extinct during this time,[4] as well as a collection of trilobites.[2][1]

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Arthropoda

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Porifera (Sponges)

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Flora

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See also

References

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