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Carrara Formation
Geologic formation in Nevada, United States From Wikipedia, the free encyclopedia
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The Carrara Formation is a geologic formation in California and Nevada. It preserves fossils dating back to the Cambrian period.[2][3][1]
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Geology
The Carrara Formation is primarily composed of olive-gray and greenish-gray siltstones and shales, as well as medium-gray limestone in the lower half of the formation, with medium-gray to yellowish-brown silty limestone and limy limestone in the upper half of the formation.[1] The lower half also contains quartzite rocks, similar to that seen in the underlying Zabriskie Quartzite. In other areas of the lower half, there are olive-gray, greenish-gray or dusky-yellow siltstones and sandy siltstones, along with small amounts of sandstone and limestone. The upper half also contains fine to medium-grained quartzites, white in colour, forming a distinctive band.[1] In other areas of the formation, it instead consists of inter-stratified siltstones, shales and very fine to medium-grained quartzite.[1]
Members
The Carrara Formation contains in total nice Members, which are as follows, in ascending age:[4]
- Eagle Mountain Shale Member
- Thimble Limestone Member
- Echo Shale Member
- Gold Ace Limestone Member
- Pyramid Shale Member
- Red Pass Limestone Member
- Pahrump Hills Shale Member
- Jangle Limestone Member
- Desert Range Limestone Member
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Paleobiota
Summarize
Perspective
The Carrara Formation contains an abundance of arthropods, like the spiny Bristolia, as well as ichnotaxon like Skolithos, a type of burrow trace fossil.[1] It also contains some examples of Archaeocyatha, a clade of sponges that went extinct during this time.[5]
Color key
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Notes Uncertain or tentative taxa are in small text; |
Arthropoda
Lophotrochozoa
Chancelloriidae
Porifera (Sponges)
Ichnogenera
Undescribed
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See also
References
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