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Biostratigraphy And Paleoenvironmental Studies Of Onigbedu Sediments, Ewekoro Local Government, Ogun State

Umoh Ekaete Enamekere Olaniyan Olamide Rilwan

Subject area: Science,Engineering and Technology  ·  Area of research: Earth Sciences

Abstract

Eleven (11) outcrops samples in vertical succession at the blast surface of the purechem cement mine, Onigbedu, Ewekoro from the Akinbo and Ewekoro Formationsat an interval of one meter depth were reconnoiter in order to establish the lithofacies, age and paleoenvironment. The biostratigraphic results indicated that the study area was deficient of calcareous nannofossils as well as planktonic foraminifera but benthic foraminifera were moderate to abundant in sample S2 of the Akinbo formation and samples L2,L3,L4,L5,L6, L7 of the Ewekoro formation. Microfacies analysis carried out on three selected samples of the Ewekoro formation harmonized with already existing lithofacies classification of the Ewekoro formation as Sample L2 and Sample L4 -Biomicite, Sample L6- Biosparite. The presence of foraminifera species consisting of rare calcareous benthic, absence of Planktics and Calcareous nannofossils indicate deposition in a shallow water. Foraminiferal assemblage is characterized by Valvulineria sp, Quinqueloculina sp, Hanzawaia concentrica, Calcareous indeterminate and Ostracod suggesting sediments deposition in a marginal marine setting (Coastal Deltaic). The results of the analyses also indicate that these outcrop samples were deposited during the late Paleocene epoch, estimated numerical age of 56.8Ma to 57.3Ma and straddling the Valvulineria martinezensis Niger Delta Benthic Foraminiferal zone.

Keywords

Biomicrite, Foraminfera, Onigbedu and Palaeoenvironment

References

[1] Parker, D. H. (1964). Paleocene fossils from Sokoto Province, North- western Nigeria. Geol. Sur. Nigeria, Records, (7), 23-36

[2] Hockey, R. D. Jones, H. A. and Hockey, R.D (1964). Geology of part of south-western Nigeria. Geol. Sur. Nigeria, Bull. (31), 1-8.

[3] Reyment, R. A. (1964). Quantitative paleoecologic analysis of ewekoro and oshosun formations of Western Nigeria. Geologiska Foreningen Stockholm Forhandlingar, (86)3, 248- 256.

[4] Adegoke, O. S., Dessauvagie, T. F. J., Kogbe, C. A. and Ogbe, F. A. G. (1971). The type section, Ewekoro Formation (Paleocene) of southeastern Nigeria: Biostratigraphy and microfacies. Proceeding 4th African Micropaleontological Colloquium, Abidjan, 1970. 27-39.

[5] Parkinson, J. (1967). The Post – Cretaceous Stratigraphy of Southern Nigeria. Quarterly Journal of Geological Society, London, 63, 311 - 320

[6] Reyment, R. A. (1960a). Notes on the Cretaceous- Tertiary transition in Nigeria. International Geological Congress, 1960, Copenhagen. Report of the 21 st Session, Norden. 5(5), 131-135.

[7] Antolini, P. (1968). Eocene phosphate in the Dahomey Basin. Jour. Mining Geology, 3(1), 17- 23.

[8] Fayose, E. A., and Asseez, L. O. (1972). Micropaleontological investigation of Ewekoro area, southeastern Nigeria. Micropaleont. 18(3), 369-385.

[9] Adegoke. O. S. (1967). Ivyattclla, lufj turritellid genus from the Eocene of Colombia, South America. Jour. Paleont., 41(5), 1095-1100.

[10] Adegoke.O.S. (1970). Macrofauna of the Ewekoro Formation (Paleocene) of south -western Nigeria. African Geology University Press, 269- 276.

[11] Muza, J.P. (2000). Calcareous nannofossil biostratigraphy from 15km transect (cocoa plate to Caribbean plate) across the Middle America. Proc. Ocean drilling prog., sci. results. (70), 1-62

[12] Bolli, H. M., & Saunders, J. B. (1985). Oligocene to Holocene low latitude planktic foraminifera. In Bolli, H. M., Saunders, J. B., & Perch-Nielsen, K. (eds), Plankton Stratigraphy, Cambridge Earth Sciences Series, Cambridge University Press, 165-262

[13] Loeblich, A.R. Jr. and Tappan, H. (1978). The coccolithophorid genus calcidiscus kamptner and its synonyms. J. Paleontol. 52 (6), 1390- 2

[14] Stanley, S. M. And Hardie, L.A. (1999). Hypercalcification: Paleontology links Plate tectonics and Geochemistry to Sedimentology. Geological Society of America, 9(2), 1-7

[15] Rezak R. And Lavoie, D.L., (1993). Carbonate Microfabric, Springer-verlag, New York, 313.

[16] Blow, W. H. (1969). Late Middle Eocene to Recent planktonic foraminifera biostratigraphy. In Bronnimann, P. and Renz, H. H. (eds.), Proceedings of the First International Conference on Planktonic Microfossils, Geneva, E. J. Brill, Leiden, (1), 199-422

[17] Blow, W. H. (1979). The Cenozoic Globigerinida, E. J. Brill, Leiden, (3), 1413

[18] Vail, P.R. and Wornardt, W.W. (1991). Integrated approach to exploration and development in the 90s: well logs seismic A sequence stratigraphy analysis: GCAGS Transactions, 41, 630-650.

[19] Berggren, W. A., Kent D.V; Smisher, C.C. and Aubry M. (1995). A revised Cenozoic Geochronology and Chronostratigraphy. In: Geochronology Time scales and Global Stratigraphic correlation, Society of Economics Paleontologists and mineralogist special publication, (54), 129-211

[20] Haq, B.U., Hardenbol, J. and Vail, P.R. (1988): Mesozoic and Cenozoic chronostratigraphy and cycles of sea level changes, In: Wilgus, C. K. An integrated approach:Journal Society of Economic Paleontologists and Mineralogists. Special Publication (42), 71-108.

[21] Tipsword, H. L., Setzer, F. M., Fred L. Smith, Jr. (1966). Interpretation of Depositional Environment in Gulf Coast Petroleum Exploration from Paleoecolgy and Related Stratigraphy. Gulf Coast Association of Geological Societies Transactions. (16), 119-130.

[22] Oladosu Y. C, and Ogundipe, O. Y (2017). Micropaleontological studies of Ewekoro sediments southwestern Nigeria Journal of Geology & Geophysics 6 (2), 280

How to cite this paper

Umoh Ekaete Enamekere, Olaniyan Olamide Rilwan "Biostratigraphy And Paleoenvironmental Studies Of Onigbedu Sediments, Ewekoro Local Government, Ogun State" Iconic Research And Engineering Journals Volume 3 Issue 6 2019 Page 183-191
Umoh Ekaete Enamekere, Olaniyan Olamide Rilwan "Biostratigraphy And Paleoenvironmental Studies Of Onigbedu Sediments, Ewekoro Local Government, Ogun State" Iconic Research And Engineering Journals, vol. 3, no. 6, Dec. 2019
Umoh Ekaete Enamekere, Olaniyan Olamide Rilwan (2019). Biostratigraphy And Paleoenvironmental Studies Of Onigbedu Sediments, Ewekoro Local Government, Ogun State. Iconic Research And Engineering Journals, 3(6).
Umoh Ekaete Enamekere, Olaniyan Olamide Rilwan "Biostratigraphy And Paleoenvironmental Studies Of Onigbedu Sediments, Ewekoro Local Government, Ogun State" Iconic Research And Engineering Journals, vol. 3, no. 6, Dec. 2019.
@article{1701842,
      author = {Umoh Ekaete Enamekere, Olaniyan Olamide Rilwan},
      title = {Biostratigraphy And Paleoenvironmental Studies Of Onigbedu Sediments, Ewekoro Local Government, Ogun State},
      journal = {Iconic Research And Engineering Journals},
      year = {2019},
      volume = {3},
      number = {6},
      pages = {183-191},
      issn = {2456-8880},
      url = {https://www.irejournals.com/formatedpaper/1701842.pdf},
      abstract = {Eleven (11) outcrops samples in vertical succession at the blast surface of the purechem cement mine, Onigbedu, Ewekoro from  the Akinbo and Ewekoro Formationsat an interval of one meter depth were reconnoiter in order to establish the lithofacies, age and paleoenvironment. The biostratigraphic results indicated that the study area was deficient of calcareous nannofossils as well as planktonic foraminifera but benthic foraminifera were moderate to abundant in  sample S2 of the Akinbo formation and   samples L2,L3,L4,L5,L6, L7 of the Ewekoro formation. Microfacies analysis carried out on three selected samples of the Ewekoro formation harmonized with already existing lithofacies classification of the Ewekoro formation as Sample L2 and Sample L4 -Biomicite, Sample L6- Biosparite. The presence of foraminifera species  consisting of rare  calcareous  benthic, absence of  Planktics and  Calcareous nannofossils indicate deposition in a shallow water. Foraminiferal assemblage is characterized by Valvulineria sp, Quinqueloculina sp, Hanzawaia concentrica, Calcareous indeterminate and Ostracod suggesting sediments deposition in a marginal marine setting (Coastal Deltaic). The results of the analyses also indicate that these outcrop samples were deposited during the late Paleocene epoch, estimated numerical age of 56.8Ma to 57.3Ma and straddling the Valvulineria martinezensis Niger Delta Benthic Foraminiferal zone.},
      keywords = {Biomicrite, Foraminfera,  Onigbedu and Palaeoenvironment},
      month = {December},
  }