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Sediment carbon sink in low-density temperate eelgrass meadows (Baltic Sea)

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Academic year: 2021

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Figure 2. Mean values (  SD) of δ 13 C ( ‰ ) and δ 15 N ( ‰ ) in the bulk sediment samples for three stations (vegetated indi- indi-cated by red dots, unvegetated black dots) and potential organic matter sources
Table 1. Seagrass (Density (shoot m 1 ), Total Macrophyte Biomass (g dwt 1 )) and Sediment Granulometry Characteristcs (Fine Sand Contribution (%), Mean Grain Size ( φ )) at Two Bottom Types and Three Study Locations
Table 3. Results of Three-Way PERMANOVA Tests for Differences in Sediment Characteristics (POC, δ 13 C, δ 15 N, POC/PON, Chla, Pheo, Chla%, Chla/POC, CPE) Between Two Bottom Types (BT), Among Three Locations (Loc), and Five Layers (L) for Samples Represent
Figure 5. Boxplots of the relative contributions of the most likely organic matter sources (epiphytes, Zostera, POM) to the bulk sediment suspended organic matter pool compared to the vegetated and nonvegetated bottoms at three locations.
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