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Langston - Lead Bell Shale, Bear Lake County, Idaho, USA
Formation | Langston |
---|---|
Member | Lead Bell Shale |
Age: | 513 - 505 Ma Cambrian |
Interval | Delamaran |
Tectonic Setting | Passive margin |
Lithology | shale |
Number of Collections | 1 |
Number of Occurrences | 2 |
Recorded Sample Locations
Location | Region | Stratigraphic Name |
---|---|---|
EC-1 | Bear Lake County, Idaho, USA | Langston - Lead Bell Shale |
Recorded Fossils
Accepted Name | Hierarchy | Age |
---|---|---|
Ctenocystoidea class | Animalia : Echinodermata : Ctenocystoidea | 513 - 505 Ma Cambrian |
Gogia palmeri species | Animalia : Echinodermata : Eocrinoidea : Gogiida : Eocrinidae : Gogia : Gogia palmeri | 513 - 505 Ma Cambrian |
References
Sprinkle J. (1973) Morphology and evolution of blastozoan echinoderms, Harvard University Museum of Comparative Zoology, Special Publication, 1-283 |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!