BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
Babii Kamen' ,
| Lat/Long (Decimal) | 54.405,87.535 |
|---|---|
| Co-ordinates Derivation | based on nearby landmark |
| Given Location | Kemerovo, Russia |
| Mindat.org Region (for given coordinates) |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Babii Kamen' (Javorsky collection) | Zalessky G. (1935) | Mal'tseva | Immediately above the basalts, 0.8-1.2 m above the top. "When the locality was described, it was dated to the Early Triassic; some specialists still believe that it is Early Triassic (Durante and Luvsantseven, 2002; Shcherbakov et al., 2002); Losovsky (1998) believed that the lower beds of the Mal’tsevo Formation, to which this locality belongs, are Permian, and the upper beds are Triassic; Gomankov and Meyen (1986) considered the entire formation Permian, corresponding to the Vyatkian–Vetlugian | "shale" | 254.17 - 252.17 Ma Permian |
| Babii Kamen' (PIN collection 1062) | Martynov A. V. (1936) | Mal'tseva | "When the locality was described, it was dated to the Early Triassic; some specialists still believe that it is Early Triassic (Durante and Luvsantseven, 2002; Shcherbakov et al., 2002); Losovsky (1998) believed that the lower beds of the Mal’tsevo Formation, to which this locality belongs, are Permian, and the upper beds are Triassic; Gomankov and Meyen (1986) considered the entire formation Permian, corresponding to the Vyatkian–Vetlugian gap; this is also what it was considered later by Goman | "siliciclastic" | 254.17 - 252.17 Ma Permian |
| Babii Kamen' (PIN collection 4887) | Aristov D. S. (2004) | Mal'tseva | "When the locality was described, it was dated to the Early Triassic; some specialists still believe that it is Early Triassic (Durante and Luvsantseven, 2002; Shcherbakov et al., 2002); Losovsky (1998) believed that the lower beds of the Mal’tsevo Formation, to which this locality belongs, are Permian, and the upper beds are Triassic; Gomankov and Meyen (1986) considered the entire formation Permian, corresponding to the Vyatkian–Vetlugian gap; this is also what it was considered later by Goman | "siliciclastic" | 254.17 - 252.17 Ma Permian |
Recorded Fossils
References
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!
