Sediment Fe:PO4 Ratio As a Diagnostic and Prognostic Tool for the Restoration of Macrophyte Biodiversity in Fen Waters
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Freshwater Biology (2008) 53, 2101–2116 doi:10.1111/j.1365-2427.2008.02038.x APPLIED ISSUES Sediment Fe:PO4 ratio as a diagnostic and prognostic tool for the restoration of macrophyte biodiversity in fen waters JEROEN J. M. GEURTS*,†,ALFONSJ.P.SMOLDERS*,†, JOS T. A. VERHOEVEN‡,JANG.M. ROELOFS* AND LEON P. M. LAMERS* *Aquatic Ecology and Environmental Biology, Institute for Wetland and Water Research, Radboud University Nijmegen, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands †B-WARE Research Centre, Radboud University Nijmegen, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands ‡Landscape Ecology, Institute of Environmental Biology, Utrecht University, Sorbonnelaan 16, 3584 CA Utrecht, The Netherlands SUMMARY 1. Globally, freshwater wetlands, including fen waters, are suffering from biodiversity loss due to eutrophication, water shortage and toxic substances, and to mitigate these pressures numerous restoration projects have been launched. Water quality data are generally used to evaluate the chances of reestablishment of aquatic vegetation in fen waters and shallow peat lakes. Here we investigated whether sediment characteristics, which are less prone to fluctuate in time, would result in more reliable predictions. 2. To test if sediment characteristics can indeed be used not only for an easy and early diagnosis of nutrient availability and water quality changes in fen waters, but also for the prognosis of biodiversity response, we recorded the aquatic vegetation and collected surface water, sediment pore water and sediment samples in 145 fen waters in the Netherlands, Ireland and Poland. 3. Endangered macrophyte species were more closely related to surface water chemis- try than common species in terms of occurrence and abundance. Sites featuring endangered species appeared to have significantly lower turbidity and pH, and lower concentrations of SO4,PO4, total phosphorus (TP) and NH4 than other sites. 4. PO4 and TP concentrations in the water layer increased markedly at PO4 concentra- )1 tions above 5–10 lmol L in the sediment pore water. High surface water PO4 and TP concentrations appeared to be SO4-induced and only occurred below certain threshold )1 )1 values for pore water Fe:PO4 (3.5 mol mol ) and total sediment Fe:P (10 mol mol ). 5. Interestingly, the occurrence of endangered species also correlated strongly with sediment and sediment pore water ratios; the number of endangered species increased )1 markedly at pore water Fe:PO4 ratios above 1 mol mol , whereas their actual ) abundance had the greatest increase at ratios above 10 mol mol 1. Additionally, endangered species seemed to be more sensitive to accumulation of potentially toxic substances such as sulphide and ammonium than non-endangered species. 6. As an indicator of both biogeochemical processes and biodiversity, pore water Fe:PO4 ratios could be a valuable diagnostic and prognostic tool for the restoration of water Correspondence: Jeroen J. M. Geurts, Aquatic Ecology and Environmental Biology, Institute for Wetland and Water Research, Radboud University Nijmegen, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands. E-mail [email protected] Ó 2008 The Authors, Journal compilation Ó 2008 Blackwell Publishing Ltd 2101 2102 J. J. M. Geurts et al. quality and biodiversity in fen waters, e.g. for selecting the most promising sites for restoration and for optimization of restoration measures. Keywords: aquatic macrophytes, fen restoration, iron, phosphate, sediment needed for good prediction of vegetation responses, Introduction although alkalinity seems quite conservative (Ves- Worldwide, freshwater wetlands are being threatened tergaard & Sand-Jensen, 2000). By contrast, the by anthropogenic disturbance, causing huge biodi- predictive power of certain sediment characteristics versity losses (Lake et al., 2000; Dudgeon et al., 2006). may be greater than water chemistry because they are In recent decades, many fen waters in the Netherlands more stable over time and indicative of several have deteriorated, mainly due to eutrophication and important sediment processes, such as nutrient avail- pollution (Smolders & Roelofs, 1995a; Lamers et al., ability in the sediment and nutrient fluxes from the 2001, 2002a). Several characteristic aquatic macro- sediment to the overlaying water. Hence, sediment phytes, such as Stratiotes aloides L., Potamogeton com- characteristics might be more appropriate and less pressus L. and Potamogeton acutifolius Link have expensive than water quality data for estimating the declined in lakes, ditches and turf ponds (Roelofs, chances of reestablishment of aquatic vegetation. 1991; Lamers, Smolders & Roelofs, 2002b; Smolders Aquatic macrophytes are known to be capable of et al., 2003a). For rooting macrophyte species sedi- regulating both water quality and sediment charac- ment is very important with respect to nutrient teristics by reducing sediment resuspension, erosion availability and toxicity. Moreover, in these shallow, and turbidity (Madsen et al., 2001; No˜ges et al., 2003) mostly phosphorus-limited fen waters (N:P in plant and by influencing the phosphorus availability both tissue >16; Koerselman & Meuleman, 1996; Verhoe- positively and negatively (Wigand, Stevenson & ven, Koerselman & Meuleman, 1996; Wassen et al., Cornwell, 1997; Søndergaard et al., 2003). It is thus 2005), sediment plays a key role in determining water obvious that sediment properties are both a product quality, due to the small water volume per unit of and a limiter of aquatic macrophyte growth (Barko sediment surface and the lack of a thermocline. et al., 1991). Therefore, biogeochemical processes in the sediment, General mechanisms of phosphorus binding, and wind-induced resuspension and bioturbation have a more specifically phosphate (PO4) binding, by iron great impact on water quality and growth of algae and (Fe), aluminium (Al) and calcium (Ca) compounds in submerged macrophytes in these systems (Barko, sediment and pore water have been investigated to Gunnison & Carpenter, 1991; Søndergaard, Jensen & determine thresholds for PO4 mobilization to the Jeppesen, 2003). Moreover, luxuriant growth of algae surface water (e.g. Jensen et al., 1992; Golterman, 1998; and certain fast-growing aquatic macrophyte species Smolders et al., 2001; Zak, Gelbrecht & Steinberg, will outcompete rooting macrophytes for light, even if 2004; Maassen, Uhlmann & Roske, 2005). PO4 immo- the sediment is P-rich. bilization by Fe, Fe oxides or Fe hydroxides is redox- Many studies have shown that growth of aquatic dependent and especially sensitive to sulphate (SO4) macrophytes is related to water quality (Onaindia, De input via surface water or ground water. Under Bikuna & Benito, 1996; Lougheed, Crosbie & Chow- anaerobic circumstances, SO4 and Fe reduction lead Fraser, 2001; James et al., 2005). Species composition is to sulphide production, FeSx formation and mobiliza- thus indicative of water quality and, conversely, water tion of Fe-bound PO4 (Fig. 1; Smolders & Roelofs, quality data can be used to predict the restoration of 1993; Roden & Edmonds, 1997; Wetzel, 2001; Lamers aquatic vegetation in shallow lakes (Bloemendaal & et al., 2002a). In addition, there will be competition Roelofs, 1988; Grasmu¨ ck et al., 1995; Goslee, Brooks & between SO4 and PO4 for anion binding sites (Caraco, Cole, 1997; Van den Berg, Joosse & Coops, 2003). Cole & Likens, 1989; Beltman et al., 2000), and SO4 Water quality, however, is subject to large temporal could also stimulate organic matter decomposition fluctuations (e.g. due to seasonal influences or plant and alkalinization (Drever, 1997). All of these pro- and algal growth), so that frequent sampling is cesses result in PO4 being released from the sediment Ó 2008 The Authors, Journal compilation Ó 2008 Blackwell Publishing Ltd, Freshwater Biology, 53, 2101–2116 Sediment Fe:PO4 ratio and fen biodiversity 2103 Considering the importance of these biogeochemi- cal interactions for the functioning of macrophytes in fen waters, we assume that sediment and sediment pore water characteristics may be important not only for an understanding of sediment biogeochemical processes determining water quality in shallow peat lakes, but also for the prediction of the response of plant species composition to restoration measures. Therefore, we investigated the distribution of aquatic and semi-aquatic macrophytes in 145 fen waters in the Netherlands, Ireland and Poland in relation to surface water, pore water and other sediment characteristics, focusing on the occurrence of endangered species. Specifically, we evaluate the use of sediment para- meters as a diagnostic and prognostic tool for wetland management in relation to ecological rehabilitation and the development of new nature reserves. Methods Field sampling Between 2002 and 2006, surface water and pore water samples were taken from 145 different fen waters from 15 areas in the Netherlands and two reference Fig. 1 Schematic diagram showing relevant biogeochemical sites in Ireland and Poland (Table 1). Both species-rich interactions in surface water and sediment of fen waters. Arrows and species-poor study sites were included, covering indicate net fluxes of chemical variables. Input of polluted sur- shallow peat lakes, turf ponds, peat ditches and face water or ground water leads to SO4 reduction, FeSx for- terrestrializing fen waters in different geographical mation, alkalinization and mineralization in anaerobic regions (Fig. 2). At each site, vegetation releve´es were sediments. This may result in H2S