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Campito Formation
Geologic formation in Nevada, United States From Wikipedia, the free encyclopedia
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The Campito Formation is a geologic formation in the Last Chance Range, California, and Esmeralda County, Nevada. It preserves fossils dating back to the Cambrian period.
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Geology
The Campito Formation is mainly composed of very fine to fine-grained quartzite, with small amounts of siltstone, getting up to 3,500 ft (1,100 m) thick.[3]
Members
The formation is split into two distinct members, which are as follows, in ascending age:
- Andrews Mountain Member: It is the thickest of the two members, getting up to 2,800 ft (850 m) thick. It is composed of olive-gray or greenish-gray very fine to fine grained silty quartzitic sandstone or quartzite and interbedded layers of dark-greenish-gray siltstones, which weather to a greenish-black or just black. The quartzite layers are composed of sub-angular very fine to fine grains of quartz, feldspar and other metallic minerals, all set within a muscovite, chlorite, and biotite.[3]
- Montenegro Member: It is the thinnest of the two members, only getting up to 1,000 ft (300 m) thick. It is composed of dark-greenish-gray and greenish-gray siltstone composed of a mixture of quartz, muscovite, and chlorite. The siltstone is evenly laminated to thin-bedded. There are also commonly occurring archeocyathid-bearing limestone beds in the upper sections of the member.[3]
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Paleobiota
Summarize
Perspective
The Campito Formation contains a number of fossils, most of which are found within the Montenegro Member. They range from archeocyathid sponges like Ethmophyllum, to arthropod trilobites like Nevadia,[3] and a wealth of ichnogenera, from burrows like Skolithos, to resting traces like Rusophycus.[4]
Color key
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Notes Uncertain or tentative taxa are in small text; |
Arthropoda
Lobopodia
Lophotrochozoa
Chancelloriidae
Cnidaria
Porifera (Sponges)
Echniodermata
Foraminifera
incertae sedis
Ichnogenera
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See also
References
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