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Dulankara - Otar, Kazakhstan
| Formation | Dulankara |
|---|---|
| Member | Otar |
| Age: | 461 - 450 Ma Ordovician |
| Interval | Caradocian |
| Lithology | sandstone/siltstone, rudstone |
| Number of Collections | 20 |
| Number of Occurrences | 104 |
Recorded Sample Locations
| Location | Region | Stratigraphic Name |
|---|---|---|
| 112 - West side of Kopalysai Valley | Korday District, Jambyl Region, Kazakhstan | Dulankara - Otar |
| 138 - Dulankara section | Zhambyl District, Almaty Region, Kazakhstan | Dulankara - Otar |
| 543 - Dulankara section | Zhambyl District, Almaty Region, Kazakhstan | Dulankara - Otar |
Associated Units
| Stratigraphic Name | Age | Lithology | Occurrence Records |
|---|---|---|---|
| Dulankara - Akkol | 453 - 445 Ma Late/Upper Ordovician | limestone, siltstone | 6 |
Recorded Fossils
References
| Popov L. E., Nitikin I. F., et al (2000) Late Ordovician brachiopods from the Otar Member of the Chu-Ili Range, south Kazakhstan, Palaeontology 43 5, 833-870 |
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!
