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For the Pomeranian Bight of the Baltic Sea the influence of riverine POM is clearly reflected in the isotopic (δ 15 N, δ 13 C) signature of suspended matter and surface sediments. High δ 15 N values of 10-14‰ characterize recent river borne particulates and surface sediments along the outflow routes and in the upper 10-15 cm of sediment cores from the lagoon...
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