Biostratigraphy of the nzam-1 well in the nkporo formation, anambra basin, southeastern Nigeria

This study presents a thorough biostratigraphic analysis of the Nkporo Formation in the Nzam-1 well, aiming to evaluate the age, paleoenvironment, and biozonation of the source rock penetrated by the well using palynological analysis.A total of 17 samples from the Nzam-1 well were subjected to palynological studies.The occurrence of diverse palynomorphs provides a framework for evaluating the age, paleoenvironment, and biozonation of the formation.The assemblage of forms (pollen, spores, and dinoflagellate cysts) indicates that the shales deposited in the Nzam-1 well range between Late Cretaceous, possibly Albian to Maastrichtian age.The presence of these fossils also suggests that the Nzam-1 well represents a marine depositional environment, which can support hydrocarbon generation.Palynomorph distribution analysis (Figure 1) reveals varying abundances across depth intervals, with peak occurrences in the 2411-2438 m zone.Age zonation (Figure 2) demonstrates clear biostratigraphic subdivision from Campanian to Maastrichtian intervals.Paleoenvironmental reconstruction (Figure 3) indicates a marginal marine setting with significant terrestrial input, favorable for organic matter preservation and hydrocarbon source rock development.

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Publication Details

Journal
Journal of Interdisciplinary Postgraduate Research
Published
2026-03-22
DOI
https://doi.org/10.61955/dllyrv
Primary Topic
Geological formations and processes
Type
article
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article

Biostratigraphy of the nzam-1 well in the nkporo formation, anambra basin, southeastern Nigeria

Ayinla, Ayinla,
Journal of Interdisciplinary Postgraduate Research
Geological formations and processes
article

Biostratigraphy of the nzam-1 well in the nkporo formation, anambra basin, southeastern Nigeria

Ayinla, Ayinla,
article en

Abstract

This study presents a thorough biostratigraphic analysis of the Nkporo Formation in the Nzam-1 well, aiming to evaluate the age, paleoenvironment, and biozonation of the source rock penetrated by the well using palynological analysis.A total of 17 samples from the Nzam-1 well were subjected to palynological studies.The occurrence of diverse palynomorphs provides a framework for evaluating the age, paleoenvironment, and biozonation of the formation.The assemblage of forms (pollen, spores, and dinoflagellate cysts) indicates that the shales deposited in the Nzam-1 well range between Late Cretaceous, possibly Albian to Maastrichtian age.The presence of these fossils also suggests that the Nzam-1 well represents a marine depositional environment, which can support hydrocarbon generation.Palynomorph distribution analysis (Figure 1) reveals varying abundances across depth intervals, with peak occurrences in the 2411-2438 m zone.Age zonation (Figure 2) demonstrates clear biostratigraphic subdivision from Campanian to Maastrichtian intervals.Paleoenvironmental reconstruction (Figure 3) indicates a marginal marine setting with significant terrestrial input, favorable for organic matter preservation and hydrocarbon source rock development.

Journal of Interdisciplinary Postgraduate Research
Federal University Lokoja (NG)
Life below water
Openalex Percentile: Top 12%
Geological formations and processes
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