BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
Tapsa River basin, Pi-Khem District, Tuva, Russia
| Lat/Long (Decimal) | 51.8833,94.4167 |
|---|---|
| Co-ordinates Derivation | based on nearby landmark |
| Given Location | Tuva, Russia |
| Mindat.org Region (for given coordinates) | Pi-Khem District, Tuva, Russia |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Tapsa River basin, Bolshoy Il'chir creek, Kameshki horizon | Osadchaya D. V., Kotelnikov D. V. (1998) | Il'chir | Kameshki stage | "limestone" | 520 - 516 Ma Cambrian |
| Tapsa River basin, Bolshoy Il'chir creek, Sections 207, 208, G. howelli zone | Osadchaya D. V., Kotelnikov D. V. (1998) | Il'chir | Gordonicyathus howelli, Bazaikha stage | "limestone" | 520 - 516 Ma Cambrian |
| Tapsa River basin, Vadi-Bala creek, Section 226, Band 4 | Kotel'nikov D. V. (1995) | Band 4 (~150m thick) has a tectonic contact to the underlying Band 3 which is confined to Vadi-Bala organogenic massif (Il'chir Fm.). Kameshkian age. | tuff | 520 - 516 Ma Cambrian | |
| Tapsa River basin, Vadi-Bala creek, Section 226, Il'chir Formation, Band 3 | Kotel'nikov D. V. (1995) | Il'chir | Band 3 (about 150m thick) is confined to the thick organogenic massif (Il'chir Fm.) Atdabanian. Possible correlation with Nochoroicyathus mariinski zone in the Batenevskiy Kryazh area. | "limestone" | 520 - 516 Ma Cambrian |
| Tapsa River basin, Vadi-Bala creek, Section 9075, N. mariinskii zone | Osadchaya D. V., Kotelnikov D. V. (1998) | Il'chir | Nochoroicyathus mariinskii zone, Bazaikha stage | "limestone" | 520 - 516 Ma Cambrian |
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!
