F1. Location of Sites 1077, 1075, and GeoB1008 and main surface and subsurface currents in the eastern Angola Basin.
F2. Comparison of Sites 1077 and 1075 with core GeoB1008.
F3. Age model used at Site 1077 based on the planktonic foraminifer Globigerinoides ruber pink.
F4. Abundances of the most abundant siliceous microfossils counted.
F5. Marine signal based on accumulation rates of marine organisms.
F6. Continental signal based on relative contributions of continental organisms.
F7. Accumulation rates and relative abundances of the marine diatom groups present at Site 1077.
F8. Diatom accumulation rates and contribution of cold-temperate water taxa compared to sea-surface temperature estimates from GeoB 1008, and the reconstruction of the position of the Angola-Benguela Front.
T1. Age model used at Site 1077.
T2. Depth, density, sedimentation rate, and concentration of siliceous organisms, Site 1077.
T3. Species composition and environmental conditions of diatom groups, Site 1077.
T4. Concentrations of marine diatom groups, Site 1077.