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Negligible isotopic fractionation of nitrogen within temperate Zostera spp meadows

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Figure

Figure 1. Western Port and Port Phillip Bay, Australia, showing the field sites. The sites marked with circles were sampled during Augustand December 2016, and the sites marked with squares were sampled approximately bimonthly over the period February–November 2016.
Figure 2. Porewater NHPort andfor the isotopic signature of porewater NH+4 concentrations for (a) Western Port and (b) Port Phillip Bay, seagrass root isotopic signature (δ15N) for (c) Western (d) Port Phillip Bay, and porewater NH+4 isotopic signature for
Table 1. Summary of possible nitrogen isotopic endmembers in Western Port and Port Phillip Bay.
Figure 5. Plot of porewater NH+4 concentration against (a) the dif-ference between the porewater δ15N-NH+4 and the seagrass δ15N(b) the difference between the porewater δ15N-NH+4 and the bulksediment δ15N.

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