International Journal of Agriculture and Earth Science (IJAES )
E- ISSN 2489-0081
P- ISSN 2695-1894
VOL. 10 NO. 1 2024
DOI: https://doi.org/10.56201/ijaes.v10.no1.2024.pg50.72
Didei, Innocent Sunday and Ajaegwu Norbert E
An outcropping unit of the Mamu Formation in Awgu section was studied on the basis of its palynological assemblages and infer a biostratigraphic interpretation. Sediment samples obtained from the outcropping units of the Mamu Formation in the Anabra Basin, Awgu section was analysed for their palynological assemblages using the conventional maceration techniques for recovering of acid insoluble organic-walled microfossils from sediments. Lithological studies and physical description of the Formation was done in the field. The diagnostic palynomorphs recovered permitted the dating and biostratigraphic interpretation of the studied outcrop and this includes: Foveotriletes margaritae, Longapertites marginatus, Monocolpites marginatus, Mauritiidites lehmanii, Foveotriletes margaritae, Syncolporites marginatus, Proxapertites operculatus Echitriporites trianguliformis, Echitriporites trianguliformis, Proteacidites sigalii and Monocolpopollenites sphaeroidites. The results show that Mamu Formation was deposited during Late Campanian to Late Maastrichtian and the recovered palynomorphs was dominated by brackish to marine waters suggesting depositions within the shoreface to open marine thus giving rise to a lagoon-shallow marine environment.
Palynological, Age, Playnomorphs, Lithology, Anambra Basin
Akaegbobi, IM, Amaechi, GC, Boboye, OA. (2009). Source rock potential and depositional
environment of the Campanian- Maastrichtian shales outcropping along the Enugu-
Leru axis, Anambra Basin, Nigeria. NAPE Bull., 21/01, pp. 25-37.
Benkhelil, MJ. (1989). The origin and evolution of the Cretaceous Benue Trough, Nigeria.
Journal of African Earth Sciences, 9, pp. 251- 282.