Manda Beds Fm
Type Locality and Naming
Ruhuhu Basin (Tanzania). Named for the Manda region near Lake Nyasa (Lake Malawi) in the Ruhuhu Basin of southwestern Tanzania. It was initially described and named by Stockley (1932) as part of the classic Songea Series (now recognized as the Karoo Supergroup succession in Tanzania).
Synonym: Manda Formation, Manda beds
Lithology and Thickness
Composed of a cyclical fluviatile sequence characterized by thick, coarse-grained, pink to grey cross-bedded feldspathic sandstones alternating with massive, purplish-red, maroon, and green mudstones and siltstones. It is often subdivided into a massive basal sandstone unit (the Kingori Sandstone, which is sometimes elevated to formation status) and an upper, mudstone-rich fossiliferous unit (the Lifua Member).
Relationships and Distribution
Lower contact
Unconformably or disconformably overlies the Late Permian Usili Fm (formerly the Kawinga Fm/Lower Bone Bed).
Upper contact
Represents the top of the preserved Karoo sequence in much of the Ruhuhu Basin, though in some areas it is unconformably overlain by younger post-Karoo sediments.
Regional extent
Correlates directly with the Ntawere Fm in Zambia and the Lipirichi Fm in Mozambique. In the Main Karoo Basin of South Africa, it correlates with the upper Beaufort Gr (specifically the Cynognathus Assemblage Zone) and the basal Stormberg Gr.
GeoJSON
Fossils
Age
Depositional setting
Terrestrial, semi-arid environments.
Additional Information