FORAMINIFERA FROM THE MAASTRICHTIAN LOWER MAMU FORMATION NEAR LERU (SOUTHERN NIGERIA) - PALEOECOLOGY AND PALEOGEOGRAPHIC SIGNIFICANCE

Authors
Citation
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
Citations number
56
Categorie Soggetti
Paleontology
ISSN journal
00961191
Volume
28
Issue
1
Year of publication
1998
Pages
76 - 89
Database
ISI
SICI code
0096-1191(1998)28:1<76:FFTMLM>2.0.ZU;2-2
Abstract
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.