Abstract

Suspended particulate organic matter was sampled monthly between June 1999 and April 2000 in the Scheldt river and estuary to investigate the seasonal and spatial patterns of δ 13C and δ 15N signatures. δ 15N of suspended matter showed large seasonal variation. Minimum values ranged from −0.5‰ in the freshwater zone (spring situation) to +2.3‰ in the mesohaline zone (winter situation). Maximum values (summer situation) ranged from +8.8‰ in the freshwater zone to +12.9‰ in the mesohaline zone. δ 13C showed less seasonal variation and ranged overall from −31.1‰ in the freshwater zone to −23.7‰ in the mesohaline zone. During the growth season, decrease of δ 13C and increase of δ 15N of suspended matter were due to local phytoplanktonic and bacterial biomass. There is strong evidence that the 15N enrichment of suspended matter during the growth season reflects the 15N enrichment of the ambient NH 4 + pool induced by nitrification and NH 4 + uptake. Zooplankton in the mesohaline section of the river was consistently enriched in 15N relative to suspended matter but followed its seasonal trend. During summer and autumn the isotopic offset between zooplankton and the suspended particulate organic matter was consistent with a pattern of selective feeding on phytoplankton. During summer, δ 15N of zooplankton reached a value as high as +25.5‰, the highest value observed during this study. During spring, present-day δ 15N of suspended matter in the oligohaline and mesohaline section increased compared to the 1970s, probably because today nitrification, which enriches the NH 4 + pool in 15N, starts earlier in the season. For summer, the discrepancy between present-day suspended matter δ 15N values and those observed in the 1970s was even larger, especially in the oligohaline and freshwater reaches, probably as a result of improved O 2 conditions now favouring nitrification. Likewise, the present decreased input of 15N-depleted sewage will enhance 15N enrichment of suspended matter during the growth season.

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