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1 Nederlands Instituut voor Onderzoek der Zee (NIOZ), Landsdiep 4, t Horntje, Texel NL-1797 SZ, Netherlands
2 Fachbereich 5-Geowissenschaften, Universität Bremen, Bremen D-28334, Germany
The assessment of diagenetic influences on the sedimentary record is problematic despite its crucial importance for accurate environmental reconstruction and understanding of biochemical cycles. We propose a general applicable method that uses differences in degradation rates of organic components to separate degradation and productivity. We demonstrate this method on a southeastern Atlantic sediment core covering the past 145 k.y. The new method solves discrepancies between existing organic matter, silica- and carbonate-based productivity reconstructions, and emphasizes the importance of bottom- and pore-water characteristics for transformation of the sedimentary record.
Key Words: dinoflagellates lipids organic carbon pollen preservation productivity
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