Helocrenic Springs As Sources Of Nutrient Rich Fine Particulate Organic Matter In Small Foothill Watershed

Despite the large number of studies devoted to organic matter dynamics in fluvial ecosystems, the detrital pathways of spring headwater systems remain neglected. In particular, spring wetlands (helocrenes or seepages) might have considerable influence on downstream headwater stream systems due to the alteration of the nutrient and organic matter content of the water. In this study, we examined fine particulate organic matter (FPOM) drained from helocrenic springs to describe its downstream transport. We studied the quantity, nutrient content and physical components of FPOM gathered from the outflowing water using continuous sediment samplers. The nutrient content of local leaf litter deposits, residence time of water in the springs and concentration of dissolved nutrients in spring sources and outflows were also measured to characterize the inputs and outputs of the studied system. The results show that headwater spring wetlands represent a significant source of high-quality FPOM for downstream river networks. The estimated concentration of FPOM (< 1000 mu m) in the 11 investigated springs was 3.1 +/- 2.5 mg.L-1. In general, the FPOM was relatively nutrient-rich ( N = 19.25 +/- 4.73 mg.L-1; P = 2.04 +/- 0.78 mg.L-1; Ca = 9.65 +/- 2.63 mg. L-1; S = 4.07 +/- 1.16 mg.L-1; C = 278.68 +/- 80.81 mg.L-1). The C:N and C:P ratios in the local leaf litter deposits were higher than in FPOM (41.04 +/- 14.32 vs. 14.70 +/- 2.46 and 591.7 +/- 168.83 vs. 154,77 +/- 64,73, respectively), indicating that suspended FPOM is more nutritious for consumers. A significant trend in terms of size fractions of FPOM was identified: with decreasing C:N and C:P ratios particle size decreases as well. Overall, the data suggest that the relatively small helocrenes can serve as an organic matter transformers, receiving primary particles and dissolved organic matter, transforming them and favouring their transport downstream. These biotopes may represent a substantial discontinuity of the river continuum at its origin, important for nutrient dynamics and food supply of associated biotic communities.