Bathymetric and regional benthic foraminiferal distribution on the Espirito Santo Basin slope, Brazil (SW Atlantic)

To understand the main environmental factors controlling the benthic foraminiferal distribution along continental slopes, and corroborate paleoenvironmental interpretations, we investigated benthic foraminiferal assemblages (total fauna > 63 mu m) and sedimentological data along six transects on the continental slope of the Espirito Santo Basin (ESB) between 18?degrees 20' and 21 degrees 20'& nbsp;S. Surface sediment samples (0-2 cm) were collected perpendicularly to the coast, from the upper (400 m) to the lower slope (3000 m). The density, taxonomic diversity and assemblage composition change with depth. The genus Globocassidulina dominates the upper and lower slope, whereas Bolivina is the most abundant taxon in the deepest lower slope. The differences in ecological preferences among the most abundant taxa allowed us to recognize five benthic foraminiferal groups, distributed in three main bathymetric sectors: upper, middle - lower, and lower slope. Group I (upper slope, 400 m) is characterized by the highest mean relative abundances of Globocassidulina rossensis, Trifarina spp. and Trifarina angulosa. Group II (middle - lower slope, 1000-1300 m) shows the highest mean relative abundances of Globocassidulina subglobosa, Bolivina albatrossi, Bulimina aculeata and Uvigerina peregrina. Group III (middle - lower slope, 1000-1300 m) is characterized by the highest mean relative abundances of Globocassidulina crassa, Gavelinopsis versiformis, Epistominella exigua and the unilocular group. Group IV (lower slope, 1900 m) shows the highest mean relative abundances of Alabaminella weddellensis, Bolivina inflata and E. exigua. Group V (lower slope, 2500-3000 m) is dominated by the genus Bolivina (B. lowmani, B. pseudoplicata and Bolivina spp). The most abundant taxa along the ESB slope are ecologically associated to the organic matter flux, bottom water oxygen concentration, and hydrodynamics conditions. The quantity and quality of food supply is the primary factor controlling the distribution of benthic foraminiferal assemblages along depth. Secondary factors include the properties of water masses, and intermediate and deep boundary currents. The increased fragmentation of benthic and planktic foraminifera tests (> 125 mu m) on the upper and middle - lower slope is related to abrasion during transport from shallower regions to the slope.