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Chemistry of Late Quaternary sediments and their interstitial waters of sediment cores from the Nort-West African continental margin
In the sediments of the NW African continental margin the mainly biogenic carbonate constituents become increasingly diluted with terrigenous material as one approaches the coast, as indicated by the carbonate-CO2 content, the Al2O3/SiO2-ratios, and the presence of ammonia fixed to alumino-silicates
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