Fig. 2 | Nature Communications

Fig. 2

From: Transient hydrodynamic effects influence organic carbon signatures in marine sediments

Fig. 2

Down-core age relationships among grain-size sediment fractions. Down-core relationships in conventional 14C (R) age of organic carbon in bulk sediment and among grain-size classes as a function of calendar age derived from 14C measurements on coincident planktonic foraminifera (c.f., Supplementary Data 1). Between sediment-fraction differences are magnified in Fig. 3 and furthermore available in Supplementary Data 1

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