Aspects of holocene vegetation reconstruction of south eastern nigeria pollen record from ozzi lake, opi, nsukka, enugu state

 

Table Of Contents


Chapter ONE

INTRODUCTION

  • 1.1Introduction
  • 1.2Background of Study
  • 1.3Problem Statement
  • 1.4Objective of Study
  • 1.5Limitation of Study
  • 1.6Scope of Study
  • 1.7Significance of Study
  • 1.8Structure of the Research
  • 1.9Definition of Terms

Chapter TWO

LITERATURE REVIEW

  • 2.1Overview of Holocene Vegetation
  • 2.2Importance of Vegetation Reconstruction
  • 2.3Pollen Analysis in Paleoecology
  • 2.4Previous Studies on Holocene Vegetation
  • 2.5Techniques for Pollen Record Analysis
  • 2.6Vegetation Changes in South Eastern Nigeria
  • 2.7Factors Influencing Vegetation Dynamics
  • 2.8Challenges in Vegetation Reconstruction
  • 2.9Application of Pollen Records
  • 2.10Holocene Vegetation Trends in Enugu State

Chapter THREE

RESEARCH METHODOLOGY

  • 3.1Research Methodology Overview
  • 3.2Study Area Description
  • 3.3Sampling Design and Collection
  • 3.4Pollen Extraction and Analysis
  • 3.5Data Interpretation Methods
  • 3.6Statistical Analysis Techniques
  • 3.7Chronology Establishment
  • 3.8Data Validation and Quality Control

Chapter FOUR

DATA PRESENTATION AND ANALYSIS

  • 4.1Overview of Research Findings
  • 4.2Holocene Vegetation Patterns
  • 4.3Vegetation Succession Dynamics
  • 4.4Climate-vegetation Relationships
  • 4.5Human Impact on Vegetation
  • 4.6Comparison with Previous Studies
  • 4.7Implications of Findings
  • 4.8Recommendations for Further Research

Chapter FIVE

SUMMARY, CONCLUSION AND RECOMMENDATIONS

  • 5.1Summary of Research
  • 5.2Conclusions Drawn
  • 5.3Contributions to Knowledge
  • 5.4Areas for Future Research
  • 5.5Final Thoughts and Reflections

Project Abstract

<p> A palynological study of the Palaeo-vegetation of Opi Nsukka, north eastern Enugu State was investigation through a palyno-analysis of 1.5 m lake sediment core collected from Ozzi Lake, Ugwu Ozioko Opi- Agu Nsukka Enugu State. The pollen flora showed that a total of 52 pollen types belonging to 30 families were recorded. Fungal and fern spores in addition to charred plant particles were also recorded from the sediment profile. The pollen diagram was divided into four zones based on the pollen curves which suggest possible changes in vegetation. The pollen profile provided evidence of a southern guinea savannah in the late Holocene. Prior to about 3800 ± 30 BP and mid part of zone iv, there was paucity of both the lowland rainforest and savannah elements in the vegetation, but with a relative increase in grass. Also the decrgease in the members of aquatic species and hydrophytic plants indicate that the period must have been drier than humid. This can also be substantiated by the rise in the peaks of Poaceae curve. Prior to 1910 ± 25 BP to about 340 ± 25 BP, there were subtle floristic changes in the vegetation from that of closed forest-savannah vegetation to an open vegetation. This is attributed to successional changes between the lowland rainforest and the savannah species due to alternating fluctuations between the dry and humid conditions. The paucity of pollen of both the savannah and the lowland rainforest species at the later part of 340 ± 25 BP is attributed highly to increase in anthropogenic activities. <br></p>

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