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The Baltic Sea is an epicontinental sea surrounded by a catchment in boreal and sub-boreal vegetation zones. The isotopic composition (δ 13 C) of organic carbon was in the range of −30‰ to −20‰, but, contrary to our expectations, had no statistically significant relation to lignin oxidation product yields (0.4 to 10 mg g −1 TOC) in a large set of Baltic Sea surface sediments. The isotopic...
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