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| Candelaria Formation Stratigraphic range: Induan | |
|---|---|
| Type | Formation |
| Lithology | |
| Primary | Shale |
| Other | Limestone |
| Location | |
| Coordinates | [ ⚑ ] : 38°06′N 118°06′W / 38.1°N 118.1°W |
| Paleocoordinates | [ ⚑ ] 12°06′N 41°36′W / 12.1°N 41.6°W |
| Region | Nevada |
| Country | |
| Type section | |
| Named for | Candelaria Hills |
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The Candelaria Formation is a geologic formation in Nevada, United States . The formation comprises shales and limestones deposited in an open marine environment and preserves fossils dating back to the Induan (Griesbachian to Dienerian) age of the Early Triassic epoch.[1][2][3] Outcrops of the Candelaria Formation are present in the Candelaria Hills southeast of the now abandoned mining town of Candelaria (Mineral and Esmeralda counties), and near Willow Springs (Nye County).[2]
Among the invertebrates, fossils of the following species of ammonoids, nautiloids, and bivalves have been recovered from the formation:[2][3]
Among the vertebrates, fossils of the following species of ray-finned fishes[2][4] have been collected from the formation: