Palynology, palynofacies and palaeoenvironments of sedimentary organic matter from Bonyere - 1 Well, Tano basin, western Ghana

Palynofacies analyses from Bonyere Well No. 1 in the Tano basin, western Ghana has revealed five palynofacies associations (I - V) based on the percentage relative abundances of the sedimentary organic matter (SOM). The palynofacies associations reflect deposition in a fluvio-deltaic (oxic) environment, a distal dysoxic-anoxic shelf environment, a proximal dysoxic-suboxic environment, nearshore (oxic) and a fluvio-deltaic/nearshore environment with high oxygen levels and low preservation rates respectively. Based on marker palynomorphs, Campanian - Maastrichtian age has been assigned to sediments within the interval (1800-10 ft) - (90-100 ft), Turonian - Lower Senonian (Santonian) age between (3160-70 ft) - (1980-90 ft) and Aptian age between the interval (8140-50 ft) - (3340-50 ft). The absence of the elater-bearing pollen which are typical Africa-South America (ASA) elements for the Albian - Cenomanian age is indicative of an unconformity between the Aptian and Turonian sediments.