East Aristanau Reef Fm
Type Locality and Naming
Along the Aristatau Mountains, Central Kyzylkum. N.V. Cherkashenko, N.M. Larin et al., 1989 (495, p.42)
Synonym: East Aristantau Topsya, Восточноаристантауская т.
Lithology and Thickness
A mighty reefogenic layer of limestones. Thickness 1000m.
Relationships and Distribution
Lower contact
Relationships with underlying and overlying deposits are not established (165; 495).
Upper contact
Relationships with underlying and overlying deposits are not established (165; 495).
Regional extent
Kyzylkumy, eastern part of Aryanstantau.
GeoJSON
Fossils
The lower part contains brachiopods - Ivdelinia pseudoivdelensis Khod., Sieberella sieberi Buch., Cymostrophia stephani Barr., characteristic of the Pragian level of the Lower Devonian. In the middle part, corals - Favosites sp. (ex gr. macrospinosus Dubat.); brachiopods - Megastrophia cf. uralensis Vern., Productella sp., Carinatina cf. arimaspa Eichw.; Tentaculites - Dicriconus sp., Striatostiliolina sp., conodonts Polygnathus inversus Klapp. et John., P. serotinus Telf. of Emsian age. In the upper part, stromatoporoids - Columnostroma ex gr. fenestratum Nich., Trupetostroma">Trupetostroma ex gr. tschernyschevi Yavor., brachiopods - Gypidula sp., Eospirifer ex gr. nobilis Barr., Atrypa ex gr. vulgaris Alekx., A. devoniana Webst.; conodonts - Polygnathus linguiformis Hinde., P. linguiformis betta Bult., determining the age interval from Eifelian to the lower part of the varcus zone of the Givetian.
Age
Depositional setting
Additional Information