Hostname: page-component-8448b6f56d-c4f8m Total loading time: 0 Render date: 2024-04-19T14:33:03.011Z Has data issue: false hasContentIssue false

Palynostratigraphy, biochronology and palaeobathymetry of a section of Awaizombe-1 well, eastern Niger Delta, Nigeria

Published online by Cambridge University Press:  06 September 2022

Jacinta N. CHUKWUMA-ORJI*
Affiliation:
Department of Geology, Federal University of Technology, Minna, Nigeria.
*
Corresponding author. E-mail: jacinta@futminna.edu.ng

Abstract

Ditch cuttings (69 samples) from a section of Awaizombe-1well located in the Northern Depobelt of the eastern Niger Delta Basin were used for this study. The lithology of the studied interval 1373–1812 m (439 m thick) consists of fissile grey shale and mudstone units. The scid method of sample preparation for palynormorphs’ recovery was adopted. Analysis recorded a well-preserved and diverse assemblage of palynomorphs, rich in pollen, spores and dinoflagellate cysts (dinocysts). First and last occurrences of marker and age diagnostic species were used for palynostratigraphic interpretation. Four palynostratigraphic interval range zones were established: Psilatriporites sp.–Racemonocolpites hians Zone; early Oligocene (Rupelian age), Praedapollis africanus–Doualaidites laevigatus Zone; late Eocene (Priabonian age), middle Eocene (Lutetian and Bartonian ages), Doualaidites laevigatusPraedapollis flexibilies Zone; and early Eocene (Ypresian age), Verrucatosporites usmensisRetitricolpites ituensis Zone. The first downhole occurrence of D. laevigatus at the 1482 m marks the late Eocene/early Oligocene boundary. Established zones are useful for inter and intra basins correlation. Lithology and age of the studied section are suggestive of the lower Agbada Formation. Palaeoenvironmental interpretations using diagnostic species revealed two environments: brackish and inner neritic to upper bathyal (0–600 m) under relatively warm-water marine condition indicated by thermophilic dinocyst taxa, such as Lingulodinium machaerophorum, Polysphaeridium zoharyi and Homotryblium spp. The lithology and these types of environments are good sites for hydrocarbon generation.

Type
Spontaneous Article
Copyright
Copyright © The Author(s), 2022. Published by Cambridge University Press on behalf of The Royal Society of Edinburgh

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

7. References

Bankole, S. I. 2010. Palynology and stratigraphy of three deep wells in the Neogene Agbada Formation, Niger Delta, Nigeria. Implications for petroleum exploration and paleoecology. PhD thesis, der Technischen Universität Berlin, 1190.Google Scholar
Chekar, M., Slimani, H., Jbari, H., Guédé, K. E., Mahboub, I., Asebriy, L. & Habiba Aassoumi, H. 2018. Eocene to Oligocene dinoflagellate cysts from the Tattofte section, western External Rif, northwestern Morocco: paleoenvironments and paleoclimate. Palaeogeography, Palaeoclimatology, Palaeoecology 507, 97114.CrossRefGoogle Scholar
Chukwuma-Orji, J. N., Okosun, E. A., Goro, I. A. & Waziri, S. H. 2017. Palynofacies, sedimentology and palaeoenvironment evidenced by studies on IDA-6 well, Niger Delta, Nigeria. Paleoecology of Africa 34, 87105.Google Scholar
Chukwuma-Orji, J. N., Okosun, E. A. & Onoruoiza, A. L. 2021. Palynostratigraphy and paleobathymetric studies of XAD-1 well Niger Delta Basin, Nigeria. Journal of Mining and Geology 57, 193202.Google Scholar
Doust, H. & Omatsola, E. 1990. Niger Delta biostratigraphy divergent/passive margin basins. American Association of Petroleum Geologists Memoir 48, 201–38.Google Scholar
Durugbo, E. U. & Uzodimma, E. 2013. Effects of lithology on palynomorph abundance in wells X1 and X2 from the Western Niger Delta, Nigeria. International Journal of Geology, Earth and Environmental Sciences 3, 170–9.Google Scholar
Ejedawe, J. E. 1981. Patterns of incidence of oil reserves in Niger Delta basin. American Association of Petroleum Geologists Bulletin 65, 1574–85.Google Scholar
Evamy, B. D., Haremboure, J., Karmerling, P., Knaap, W. A., Molloy, F. A. & Rowlands, P. H. 1978. Hydrocarbon habitat of the Tertiary Niger Delta. American Association of Petroleum Geologists Bulletin 62, 139.Google Scholar
Legoux, O. 1978. Quelques espéeces de pollen caractéristique du Néogène du Nigéria [Some characteristic pollen species of the Neogene of Nigeria]. Bulletin des Centres de Recherche Exploration-Production d'Elf-Aquitaine 2, 265317. [In French.]Google Scholar
Murphy, M. A. & Salvador, A. 1999. International Stratigraphic Guide – An abridged version, International Subcommission on Stratigraphic Classification of IUGS, International Commission on Stratigraphy. Special Episodes 22, 255–72.CrossRefGoogle Scholar
Okosun, E. A. & Osterloff, P. 2014. Ostracod, Diatom and Radiolarian Biostratigraphy of the Niger Delta. Earth Science Research 3, 7293.Google Scholar
Reijers, T. J. A., Petters, S. W. & Nwajide, C. S. 1996. The Niger Delta basin, sedimentary geology and sequence stratigraphy. In Reijers, T. J. A. (ed.) Selected chapters on geology, 100–17. Warri: SPDC Corporate Reprographic Services.Google Scholar
Short, K. C. & Stauble, A. J. 1967. Outline of the geology of Niger Delta. American Association of Petroleum Geologists Bulletin 51, 761–79.Google Scholar
Stover, L. E., Brinkhuis, H., Damassa, S. P., De Verteuil, L., Herby, R. J., Monteil, E., Partridge, A. D., Powell, A. J., Riding, J. B., Smelror, M. & Williams, G. L. 1996. Mesozoic–Tertiary dinoflagellates, acritarchs and prasinophytes. In Jannsonius, J. & McGregor, D. C. (eds) Palynology: principles and applications Vol. 2, 641750. College Station, Texas: American Association Stratigraphic Palynologists Foundation.Google Scholar
Stover, L. E. & Williams, G. L. (1982). Dinoflagellates, Third North American Paleontological Convection, Proceedings 2, 525–33.CrossRefGoogle Scholar