Aytym-Cret Fm
Type Locality and Naming
Named after the village of Aytym, Central Kyzylkum I. M. Abdurazimova, 1998 (165, p. 144). The name proposed by A.I. Pak (1959) for the Aitym horizon was used. The stratotype is located 700 m northeast of the Tamdy-truba well, on the southwestern plunge of the Bukantau Mountains.
Synonym: Aytym Suite, Айтымская св.
Lithology and Thickness
Nearshore-marine sandstones, sands, and clays—yellow, gray, greenish-gray, and dark brown—with lenses of sandy coquina. Thickness: 22–56 m.
Relationships and Distribution
Lower contact
It lies with an erosional unconformity on the Bissektin Fm
Upper contact
It is overlain, also with an erosional unconformity, by the Karakatin Fm and Upper Paleocene deposits.
Regional extent
In the central Kyzylkum, the foothills of Bukantau, and on the adjacent plains, it is penetrated by boreholes.
GeoJSON
Fossils
Contains ammonites Stantonoceras sp.; marine bivalve mollusks Ostrea itemiriensis Vinok., Fatina akkaptschigensis Bobk., Exogyra dzharanensis Vinok., Korobkovitrigonia akkaptschigensis Beliak., Linotrigonia syrdariensis (Arkh.); foraminifera Gaudryinella pseudoasiatica N. Byk.; a spore and pollen assemblage (%): Stenozonotriletes radiatus Chl. (1), Gnetaceapollenites evidens (Bolch.) Verb. (11), Kuprianipollis santaloides (Stelm.) Kom. (7), K. elegans (Zak.) Kom. (1), Proteacidites sp. (1.5); numerous bones of armored and predatory dinosaurs, fragments of turtle shells, and crocodile teeth.
Age
Depositional setting
Additional Information