PALYNOZONATION, CHRONOSTRATIGRAPHY AND PALEOENVIRONMENT OF DEPOSITION OF THE ALBIAN TO PLIOCENE SEDIMENTS OF NZAM-1 WELL, ANAMBRA BASIN, SOUTHEASTERN NIGERIA
Lithostratigraphy of the analyzed well contains various lithoafacies such as shale, sandstone, siltstone, their heterolith and intercalated gypsum. Ten palynological zones were established including Forma PO 304 Lawal zone 1, dated Albian-Lower Cenomanian; Cretacaeiporites spp. acme zone 2, dated Upper Cenomanian-Turonian; Zlivisporites blanensis zone 3, dated Coniacian-?Santonian; Milfordia spp. Acme zone 4, dated Campanian; Foveotriletes margaritae zone 5, dated Lower Maastrichtian; Longapertites margaritae zone 6, dated Middle Maastrichtian; Spinizonocolpites bacculatus zone 7, dated Upper Maastrichtian; Mauritiidites crassibaculatus zone 8, dated Lower Paleocene; Monoporites annulatus zone 9, dated Middle Eocene; Echitirolporites spinosus zone 10, dated Upper Miocene-Pliocene age. In the Nzam-1, Ajali Sandstone was not encountered.. Sequnce stratigraphy analysis indicated six sequences of events characterized by 5 sequence boundaries (SB) and 8 maximum flooding surfaces (MFS). Paleoenvironment of deposition vary tremendously from fluviatile through marginal marine to open marine systems. The established palynological zones would assist in solving stratigraphic problems; optimize hydrocarbon exploration in Anambra Basin and other Cretaceous sedimentary basins in Nigeria.