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A sediment core from the Cabo Frio coastal shelf (−23.19S, −41.8W; 117m depth), was analyzed for TOC, C/N ratio, organic petrography and planktonic foraminiferal content to evaluate variations in local productivity caused by changes in upwelling intensity and its relation to regional and global climatic variations during the last millennium. The Cabo Frio core recorded the last 1200years of sedimentation,...
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