Karamazar Fm
Type Locality and Naming
By the village of Karamazar, right bank of the Aksakata River, Prishashkent district. M.V. Mikulin, T.M. Kremlyakova, M.P. Safarov, 1999 (Safarov et al., 1999f.).
Synonym: Karamazar Formation, Карамазарская т.
Lithology and Thickness
Dark brown, light brown subaerial loess with pedo-complexes with a clearly expressed alluvial layer and two horizons of dirty white travertine-like marls at the base. Paleosol is dark gray with a large cloddy structure with mole burrows. Thickness up to 14m.
Relationships and Distribution
Lower contact
It lies without visible unconformity on the Turasay Fm, or on various horizons of the Kandyrsay Fm.
Upper contact
It is overlain by subaerial deposits of the Zarkent Fm
Regional extent
Prishashkent district, along the Aksakata River, Zarkent village, Samsarekskaya anticline, Angren (Aparatak) and Kashkadarya (Mingkuchar village) valleys.
GeoJSON
Fossils
At the base, containing bone remains of the maral deer - Carvus elaphus and Casella sp.
Loess above the marls contains rodent fauna - Ellobius (Ellobius) ex gr. talpinus Pal., Cricetulus (Cricetulus) nigratorius Pal., Microtus (Plaiomys) ex gr. juldaschi sewertsov Thomas., M. (Branfordimys) afghanus Th., M. (Microtus) arvalic Pal., M. (Microtus) transcaspicus Sat., etc.
Age
Depositional setting
Additional Information