H. Gebhardt, FORAMINIFERA FROM THE MAASTRICHTIAN LOWER MAMU FORMATION NEAR LERU (SOUTHERN NIGERIA) - PALEOECOLOGY AND PALEOGEOGRAPHIC SIGNIFICANCE, Journal of foraminiferal research, 28(1), 1998, pp. 76-89
Qualitative and quantitative analyses of benthic foraminiferal faunas
from the lower Mamu Formation of Leru in the southern Anambra Basin of
Nigeria allow a detailed paleoecologic interpretation for the investi
gated section and the interpretation of depositional environments. The
foraminiferal faunas represent marine to brackish deltaic deposits of
prodelta to lagoon/interdistributary bay environments. Large parts of
the fauna were described formerly as endemic from the Iullemmeden Bas
in. Their occurrence in the Anambra Basin indicates that, at least, an
ephemeral marginal marine connection existed between the two basins d
uring the Maastrichtian. Three of the reported species are new and are
described here. These species are Ammotium leruensis sp, nov., Ammoba
culoides parvus sp. nov., and Haplophragmoides pettersi sp. nov.