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              <p>The objective of this work is to establish the sediment routing systems of the West African and Guyana Shieldsto the rift and passive margin basins of the Equatorial Atlantic at geological time scales (since 200 Ma). Thesemargins, alternating transform and divergent segments, show a strong structural variability in the margin width,continental geology and relief, drainage networks and subsidence/accumulation patterns. We analyze thesesystems combining onshore geology and geomorphology as well as offshore sub-surface data. We quantifyaccumulation histories in the passive margin basins histories taking into account the whole depositional system(from the shoreline to the most distal deposits onto the oceanic crust). We correct these from remaining porosityand in-situ production (mainly carbonates) and compute uncertainties related to depth conversion, absolute ageattribution from biostratigraphy as well as porosity and in-situ production corrections. We verify that the observedtrends in accumulation rates are robust despite the saddler effect related to the increase in temporal resolution withtime. We compare accumulation histories to paleo-geographic maps of sources and sinks established at continentscale. These maps, spanning the continental domain of West African and Guyana Shields and their offshore basinssince 200 Ma, give the framework of the evolution of the sediment routing system through time.Along the African margin, we defined the stratigraphic architectures of the 3 sub-basins (Sierra Leone/Liberia,Ivory Coast, and Ghana/Togo/Benin) to establish their post break-up accumulation (since ca.100 Ma). Accumulationsrates are significantly higher during (i) the Cenomanian that may be related to the erosion of EquatorialAtlantic rift-shoulders, (ii) the Maastrichtian that may be related to either the tectonic inversion of western Africaat the time or a change in the erosion capacity in the continental drainage area driven by climate change and (iii)the Oligocene that marks a major drainage reorganization in West Africa following the rise of the Hoggar and amajor sea-level fall in Rupelian (ca.30 Ma).Along the conjugate South American margin, we are currently defining the stratigraphic architectures of 2sub-basins (Guyana/Suriname to the West and Foz d’Amazonas to the East) that will allow for establishingtheir accumulation histories. The long term stratigraphic trends of those basins shows : (i) the Central Atlanticrifting in the Guyana/Suriname basin (165 – 156 Ma) and the Equatorial Atlantic rifting ([U+F07E]100 Ma)in the Foz d’Amazonas basin; (ii) massive syn-rift deposits in the western Guyana/Suriname; (iii) a progressivedecrease of the clastic input during most of the Paleogene allowing for carbonate platform deposits followedby (iv) a major clastic accumulation in the Foz d’Amazonas basin since the Upper Miocene resulting froma major drainage reorganization on the Guyana Shield during the Neogene (drainage inversion toward the Atlantic).</p>
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