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Journal of Applied Sciences and Environmental Management
World Bank assisted National Agricultural Research Project (NARP) - University of Port Harcourt
ISSN: 1119-8362
Vol. 23, No. 12, 2019, pp. 2239-2244
Bioline Code: ja19333
Full paper language: English
Document type: Research Article
Document available free of charge

Journal of Applied Sciences and Environmental Management, Vol. 23, No. 12, 2019, pp. 2239-2244

 en Recognition of Blow Foraminifera Zones in the Tertiary Sediments in F- Well, Niger Delta
LUCAS, F A & ONONEME, O E

Abstract

Foraminiferal Micropaleontology of Tertiary sediment in F-Well Niger Delta Basin were carried out using foraminiferal biostratigraphy as geologic tools. Sedimentological description was carried out on 679 ditch cutting samples which aided the erection of 103 lithozones. Fifty (50) ditch cutting samples was used with the aim of establishing the Foraminiferal Biozones and age of the well. A total of eighty (80) foraminiferal species were recorded, most of the species recorded are calcareous and arenaceous benthic foraminiferal species. They were about twenty-eight (28) diagnostic foraminifera recognized. The evaluation of these foraminifera species enabled us to recognize the zones. The foraminiferal abundances revealed two bio zones N4-N3 Planktic zone and N3 – N2 Planktic zone which were suggested based on index species among the recovered foraminiferal assemblages. N4-N3 Planktic zone has a reference interval of 8,000ft – 9,400ft. The top of this zonal interval which ought to be marked by the FDO of Ammonia becarril was absent but was estimated to be 8,000ft. The base of this zonal interval is marked by the LDO of Epistominella vitriea check for this species in other resources at 9,400ft. Planktic zone N3 – N2 has a reference interval of 9,400ft – 10,000ft. The top of this interval is marked by the FDO of Bolivina imperatrix check for this species in other resources at 9,400 ft. The base of this interval is marked by the LDO of Spirosplectamina wrightii check for this species in other resources at 10,000 ft. The studied intervals in the wells are dated Early Miocene - Oligoocene. Using the lithologic and foraminiferal studies, it is inferred that the intervals penetrated by the well correspond to Agbada Formation.

Keywords
Foraminifera; First Downhole Occurrence; Last Downhole Occurrence; Oligocene.

 
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