Abstract
Modern and Holocene muddy strata were studied along the shoreline adjacent to the Amazon river mouth using sedimentological, radiochemical, physical, and seismic methods. The present paper is a synthesis of the results, collected during the AmasSeds project, that is used to outline a regional shoreline sediment budget. Erosion of relict Amazon muds in southern Amapa supplies 106 tons yr−1 to the Amazon advective mud stream. Local rivers are sediment-poor (total suspended discharge ~ 1 × 106 tons yr−1), but form depositional sandflats on the shoreface downdrift of the river mouths. Mudflat accumulation in northern Amapa sequesters 106–107 tons yr−1 by tidal-flat aggradation, alongshore mudcape accretion, and sediment trapping by mangroves. The processes temporarily store 1.5 × 108 tons of Amazon mud in January–June.
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Allison, M.A., Nittrouer, C.A., Faria, L.E.C. et al. Sources and sinks of sediment to the Amazon margin: The Amapa coast. Geo-Marine Letters 16, 36–40 (1996). https://doi.org/10.1007/BF01218836
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DOI: https://doi.org/10.1007/BF01218836