ASYMMETRY IN UPPER CRETACEOUS DEPOSITIONAL SEQUENCES OF THE NORTHEASTERN GULF COASTAL PLAIN, ALABAMA, MISSISSIPPI AND TENNESSEE
Two major marine tongues interpreted as transgressive peaks (maximum flooding surfaces) extend into the nearshore regions. In eastern Alabama, the Mooreville Chalk occurs as a marly tongue in the middle of the Blufftown Formation. This tongue occurs near the top of the planktonic foraminiferal Dicarinella asymetrica Taxon Range Zone. Another tongue occurs in the ostracode Ascetoleberis plummeri Interval Zone (IZ), which correlates to the lower portion of the planktonic foraminiferal Globotruncana ventricosa IZ of early Campanian age. In northern Mississippi, a tongue also occurs in the Mooreville Chalk, which extends between the relatively nearshore Tombigbee Sand Member of the Eutaw Formation and the Tupelo Tongue of the Coffee Sand. This northern Mississippi tongue occurs, however, in the Ascetoleberis plummeri IZ, correlable with the younger tongue in eastern Alabama. Thus, the older tongue observed in eastern Alabama is not observed in northern Mississippi. The effects of sediment supply, associated with the ancestral Tombigbee River, are believed to have masked the eustatic signal of this earlier sequence.