Sedimentary records curves94 the Djibouti Ville Drift: Sedimentation and record of bottom current fluctuations during the Pleistocene and Holocene. Glacial stages, stadials 5b and 5dinterglacial stages Holocene and interstadials 5a, 5c and 5e can be recognized Fig. Curves94 stages clearly correlate with the isotope curve for the Alboran Sea Martrat et al. College dorm webcam the two cores therefore allows a correlation of the lithological units in the drift-moat system Fig.
Sediment core analysis MS, Ti, Si, Sr, Ca curves  provides evidence of an along slope trend of six main correlatable sedimentary units a to f Fig. These units are composed of three main types of contourite facies: The values of these peaks vary between the moat and drift environments. The development of the Djibouti Ville Drift is conditioned by the efficiency of deep water circulation in the area in reworking, winnowing, transporting and accumulating terrigenous and biogenous particles.
The spatial distribution of the sedimentary facies reveals that muddy and silty contourites characterize both environments moat and drift Fig. The sharp vertical variations in paleocurrent proxies suggest fluctuations in the intensity of bottom currents in both environments.
Curves94 maximum and minimum values are interpreted as acceleration followed by deceleration of bottom currents, respectively.
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