Sediment from four cores of the north part of the continental upper slope, Bahia State, consist predominantly of siliciclastic mud in its bottom and carbonatic mud in the top of the majority of the studied cores. The sediment color varies from light olive gray to brownish black. The sediments are mainly composed of foraminifera, mollusk fragments, coralline algae debris, plant fragments and quartz grains. The following major foraminifera benthonic species were recorded in the studied cores: Cibicides pseudoungerianus, Bulimina marginata, Amphistegina lessonii, Cassidulina laevigata, Bolivina subaenariensis, Uvigerina peregrina. The following major foraminifera planctonic species are frequent in the cores: Globigerinoides ruber, Globigerina bulloides, Orbulina universa, Globigerinoides trilobus, G. elongatus, Globigerina quinqueloba, Globigerinoides ruber f. pyramidalis. The siliciclastic sediment (higher quartz percentage) in the core bottom, suggests that sedimentation occurred with strong continental influence, indicating proximity to the coast line. The benthonic foraminifera predominance in the bottom cores and the higher planctonic frequency toward the top cores is an indicative of the sea-level oscilation events during Quaternary time.

The foraminiferal fauna present in 1.90 m long cores from the north coast of the State of Bahia, were analyzed for developing a biostratigraphic zonation and interpretating paleoclimatic and paleobathymetric events that occurred during the Quaternary in this part of the Brazilian Continental Margin. Four sample stations were piston cored from the upper continental slope: cores 132 (730 m deep), 141 (790 m deep), 147 (640 m deep) and 160 (480 m deep). From forty samples selected from the cores, 10,544 foraminifer specimens were picked up and 312 taxa were identified representing 96 genera and 302 species. The frequency and distribution patterns of the planktonic foraminifera suggest the presence of assemblage indicators that may be correlated with international Quaternary biozones. The frequency variations of planktonics indicate warm water as Globigerinoides ruber and Globorotalia menardii s.l. show an increasing frequency from the top to 40 cm of cores 132, 141 and 160, and to 60 cm depth of core 147. The presence of Globorotalia menardii f. fimbriata and Globorotalia menardii f. ungulata, which occur only in the Holocene, suggests warm water conditions for this core interval, as well as absence of Globorotalia inflata, which is a bioindicator of cold water. This is a suggestion that this core interval might be correlated with the international biozone Z of Quaternary time (Holocene -Interglacial). Likewise, the variations observed in the frequency of the cold water planktonic bioindicators, Globigerina bulloides and Globorotalia truncatulinoides, show an increasing frequency from 40 cm depth in the cores 132, 141 and 160 to their bottoms and from 60 cm deep until the bottom of core 147. This observation suggests that this core interval might be correlated with international Y zone (Pleistocene -Glacial) of the Quaternary. Variations observed in the relative frequency of benthonic versus planktonic speces show predominance of benthonics at the bottom of cores 141, 147 and 160. Moreover, changes in the high proportion of Anuário do Instituto de Geociências -UFRJ