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139 - Dulankara section, Zhambyl District, Almaty Region, Kazakhstan
Lat/Long (Decimal) | 44.7097,75.3489 |
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Co-ordinates Derivation | estimated from map |
Mindat.org Region (for given coordinates) | Zhambyl District, Almaty Region, Kazakhstan |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
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139 - Dulankara section | Popov L. E., Cocks L. R. M. (2006) | Dulankara - Degeres | Late Caradoc age is defined by the underlying occurrence of the graptolite Pseudoclimacograptus scharenbergi in the uppermost part of the underlying Anderken Formation (Nikitin 1972; Popov et al. 1999; Text-fig. 2), which is characteristic of the Climacograptus caudatus Biozone, the local equivalent of the Climacograptus clingani Biozone. | siltstone | 453 - 445.2 Ma Late/Upper Ordovician |
Recorded Fossils
Accepted Name | Hierarchy | Age |
---|---|---|
Christiania proclivis species | Animalia : Brachiopoda : Strophomenata : Strophomenida : Christianiidae : Christiania : Christiania proclivis | 453 - 445.2 Ma Late/Upper Ordovician |
Platymena tersa species | Animalia : Brachiopoda : Strophomenata : Strophomenida : Glyptomenidae : Platymena : Platymena tersa | 453 - 445.2 Ma Late/Upper Ordovician |
Sowerbyella (Sowerbyella) akdombakensis species | Animalia : Brachiopoda : Strophomenata : Strophomenida : Sowerbyellidae : Sowerbyella : Sowerbyella (Sowerbyella) akdombakensis | 453 - 445.2 Ma Late/Upper Ordovician |
Sowerbyella (Sowerbyella) ampla species | Animalia : Brachiopoda : Strophomenata : Strophomenida : Sowerbyellidae : Sowerbyella : Sowerbyella (Sowerbyella) ampla | 453 - 445.2 Ma Late/Upper Ordovician |
Strophomena (Strophomena) orthonurensis species | Animalia : Brachiopoda : Strophomenata : Strophomenida : Strophomenidae : Strophomena : Strophomena (Strophomena) orthonurensis | 453 - 445.2 Ma Late/Upper Ordovician |
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!