| Zaza Formation | |
|---|---|
| Stratigraphic range: Early Cretaceous | |
| Type | Geological formation |
| Overlies | Paleozoic granite basement |
| Thickness | Around 80 metres at Baissa |
| Lithology | |
| Primary | Sandstone, siltstone, marl, and bituminous shale |
| Other | Conglomerate, limestone |
| Location | |
| Region | Buryatia |
| Country |  Russia |
The Zaza Formation is a geological formation located in Buryatia (Russia). It dates to the Lower Cretaceous. The age of the formation is disputed, and is considered likely to be Valanginian-Hauterivian, or Aptian in age.[1] It comprises sandstones, siltstones, marls and bituminous shales, deposited in a stratified lake. It is situated on a large granite plateau in the NE of Buryatia.[2] The formation is known for its numerous compression fossils of many varieties of insect found predominantly at the Baissa locality, located on the banks of the Vitim River.[3] Insects are found in multiple beds throughout the succession, predominantly in the finer grained facies, the preservation of insect fossils is variable between beds, with good preservation in marl and poor preservation in shale beds.[2]
- ^ Zhang, Xin; Zheng, Daran; Zhang, Qianqi; Zhang, Haichun (April 2023). "Discovery of the snakefly Siboptera Ponomarenko, 1993 (Insecta: Raphidioptera: Mesoraphidiidae) from the Lower Cretaceous of southwestern Henan (China) and its biostratigraphic significance". Cretaceous Research. 144: 105428. doi:10.1016/j.cretres.2022.105428.
- ^ a b Zherikhin, V.V., Mostovski, M.B., Vrsansky, P., Blagoderov, V.A. and Lukashevich, E.D. 1999. The unique Lower Cretaceous locality of Baissa and other contemporaneous insect-bearing sites in North and West Transbaikalia. Proceedings of the First Palaeoentomological Conference, Moscow, 1998. Bratislava: Amba Projects, pp. 185-192.
- ^ "Baissa (PIN collection 3064, bed 31) (Cretaceous of Russian Federation)". fossilworks.org. Retrieved 17 December 2021.