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Lower Karoo Formation

Lower Karoo Fm


Period: 
Carboniferous, Permian

Age Interval: 
Late Carboniferous-Early Permian (Moscovian- Sakmarian)


Province: 
Zimbabwe-Mozambique

Type Locality and Naming

Metangula Basin (Mozambique). Noted as a foundational lithostratigraphic division within the Karoo-aged Metangula Basin, located near the border of Mozambique and Tanzania. Like the "Middle Karoo," it is often utilized as a broad formational or sequence descriptor for the lowermost, oldest sediments filling this specific rift graben. Included in Dwyka Gr in Metangula Basin (Mozambique)

Synonym:


Lithology and Thickness

Composed of a basal terrestrial sequence that typically includes glacial or proglacial deposits. In regional stratigraphy, these basal Karoo units consist of diamictites (tillites), poorly sorted conglomerates, and interbedded sandstones and mudstones that represent the initial fill of the rift valleys.


Lithology Pattern: 
Glacial till


Relationships and Distribution

Lower contact

Rests unconformably upon the ancient Precambrian crystalline basement, marking a massive temporal hiatus prior to the initiation of Karoo sedimentation.

Upper contact

Conformably to semi-conformably overlain by the coal-bearing Middle Karoo Fm.

Regional extent

Geographically restricted to the deepest portions of the Metangula Basin in northern Mozambique. Correlates broadly with the Dwyka Gr and basal Ecca Gr equivalents of the main and eastern African Karoo rift basins.


GeoJSON

null

Fossils


Age 

Late Carboniferous-Early Permian (Moscovian- Sakmarian)

Age Span: 

    Beginning stage: 
Moscovian

    Fraction up in beginning stage: 
0.5

    Beginning date (Ma): 
311.09

    Ending stage: 
Sakmarian

    Fraction up in the ending stage: 
0.5

    Ending date (Ma):  
292.02

Depositional setting

Intracratonic rift basin environments.


Depositional pattern:  


Additional Information


Compiler:  

From the O. Catuneanu et al. The Karoo basins of south-central Africa, Journal of African Earth Sciences 43 (2005) 211–253