Emigrant Formation
The Emigrant Formation is a Cambrian to Ordovician geologic formation in Nevada. It preserves fossils dating back to the Cambrian period, as well as the Ordovician period.
Geology
The Emigrant Formation is dominated by shales, with limestone common at the base and top of the formation.Members
The formation contains three members, which are as follows, in ascending age:- Limestone & Siltstone Member: This member is the thinnest of the three, only getting up to thick in some areas, and is dominated by lime mudstone. At the base of the member, it is entirely composed of shale, which gives way to calcareous sandstone, and then the common lime mudstones above that. Within these lime mudstones, there are occasional layers of more shale and chert.
- Shale Member: This member can get up to thick in some areas, and is, as the name suggests, entirely dominated by shale, which may be faulted and repeated in many places.
- Limestone & Chert Member: This member is the thickest of the three, getting up to thick in some areas, and contains a mixture of ribbon limestone, inter-bedded shales, as well as mega-breccia.
Paleobiota
The biota of the Emigrant Formation is mainly composed of trilobites like Olenellus and Bathyuriscus, as well as some small shelly fauna in the form of Pelagiella and Microcornus. It also contains a sparse collection of fossils from a lower Ordovician unitright at the top of the formation, containing the chelicerate Esmeraldacaris, as well as some graptolite fauna.
Cambrian
This section details all the fossils from the Cambrian sections of the Emigrant formation.Lophotrochozoa
| Genus | Species | Notes | Images |
| Microcornus | Microcornus sp. | Lophotrochozoan hyolith. | |
| Parkula | P. esmeraldina | Lophotrochozoan hyolith. | |
| Haplophrentis | H. carinatus | Lophotrochozoan hyolith. | |
| Hyolithellus | Hyolithellus sp. | Lophotrochozoan hyolith. May possibly be an annelid. | |
| Hyolithides |
| Undetermined lophotrochozoan hyoliths, are either preserved as molds, or are too poorly preserved for identification. | |
| Anabarella | A. chelata | Helcionellid mollusc. | |
| Pelagiella | P. subangulata | Pelagiellid mollusc. | |
| Costipelagiella | C. nevadense | Pelagiellid mollusc. |
Chancelloriidae
| Genus | Species | Notes | Images |
| Allonia | Allonia sp. | Chancelloriid. | |
| Chancelloria | Chancelloria sp. | Chancelloriid. |
Echinodermata
| Genus | Species | Notes | Images |
| Echinoderm Ossicles |
| Calcareous element that makes up the endoskeleton of echinoderms. |
Porifera (Sponges)
| Genus | Species | Notes | Images |
| Hexactinellid spicules |
| Sponge skeleton, with six rays. |
Flora
| Genus | Species | Notes | Images |
| Archaeooides | A. granulatus | Microalgae. | |
| Girvanella | Girvanella sp. | Cyanobacteria structures. |
Ordovician
This section details all the fossils from the Ordovician unit at the top of the Emigrant Formation.Lophotrochozoa
| Genus | Species | Notes | Images |
| Inarticulate brachiopods |
| Lophotrochozoan brachiopods, poor preservation hinders full identification. |
Hemichordata
| Genus | Species | Notes | Images |
| Dictyonema | Dictyonema sp. | Dendroid graptolite. | |
| Clonograptus | Clonograptus sp. | Graptolites. |
Porifera (Sponges)
| Genus | Species | Notes | Images |
| Hexactinellid spicules |
| Sponge skeleton. | |
| Tetractinellid spicules | Sponge skeleton. |
Ichnogenera
| Genus | Species | Notes | Images |
| Branching Trace Fossils |
| Branching traces. |