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<p>Palynoflora analyses from Benin west -1, Anambra Basin has unfold three<strong> </strong>palynozones based on abundance, composition of palynoflora and cluster analysis. Palynozone-1 has been dated as Late Maastrichtian age and belong to the lowermost Imo Shale, palynozone-2; Middle Eocene and palynozone -3 is dated Lutetian to Bartonian age. Sediments between depth intervals of 2649-2560 m is marked a sequence boundary, 1650-2560 m, and 970-1190 m is delineated as high stand system tract.doi:10.3329/jsr.v8i2.25180 fatcat:ejvil2wpijbozpufpq37grrhn4