| Carrara Formation | |
|---|---|
| Stratigraphic range: [1] | |
| Fossils from the Pyramid Shale member, Carrara Formation | |
| Type | Formation |
| Sub-units | See: Members |
| Overlies | Zabriskie Quartzite |
| Thickness | 0–2,000 feet (0–610 m) [1] |
| Lithology | |
| Primary | Siltstone |
| Other | Shale, Limestone, Quartzite, Sandstone |
| Location | |
| Region | California and Nevada |
| Country | United States |
The Carrara Formation is a geologic formation in California and Nevada. It preserves fossils dating back to the Cambrian period. [2] [3] [1]
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]
The Carrara Formation contains in total nice Members, which are as follows, in ascending age: [4]
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
| Notes Uncertain or tentative taxa are in small text; |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Houcaris (?) |
| Radiodont arthropod. Previously described as Anomalocaris magnabasis in 2019, but was reassigned to Houcaris in 2021, [6] although this assignment is now up in the air with subsequent analysis suggesting H. magnabasis may not form a monophyletic clade with other species of Houcaris. [7] | |
| Ursulinacaris [8] |
| A Hurdiid radiodont. | |
| Bristolia [1] |
| An olenellid trilobite. | |
| Olenellus |
| An olenellid trilobite. Fossil specimens from the Pyramid Shale Member have been found preserving the first evidence of chitin in trilobites. [9] | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Microcornus [4] |
| Lophotrochozoan hyolith. | |
| Parkula [4] |
| Lophotrochozoan hyolith. | |
| Hyolithellus (?) [4] |
| Lophotrochozoan hyolith. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Allonia [4] |
| Chancelloriid. | |
| Chancelloria [4] |
| Chancelloriid. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Archaeocyathus [5] |
| Archaeocyathide sponge. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Skolithos [1] [10] |
| Burrows. | |
| Genus | Species | Notes | Images |
|---|---|---|---|
| Disc-shaped fossils [11] |
| Disc-shaped organisms, resemble either porpitids or eldonids, especially to Discophyllum . | |