Figures
Abstract
Background
Floodplain meadows along rivers are semi-natural habitats and depend on regular land use. When used non-intensively, they offer suitable habitats for many plant species including rare ones. Floodplains are hydrologically dynamic ecosystems with both periods of flooding and of dry conditions. In German floodplains, dry periods may increase due to reduced summer precipitation as projected by climate change scenarios. Against this background, the question arises, how the forage quantity and quality of these meadows might change in future.
Methods
We report results of two field trials that investigated effects of experimentally reduced summer precipitation on hay quantity and quality of floodplain meadows at the Rhine River (2011-2012) and at two Elbe tributaries (2009-2011). We measured annual yield, the amount of hay biomass, and contents of crude protein, crude fibre, energy, fructan, nitrogen, phosphorus, and potassium.
Results
The annual yield decreased under precipitation reduction at the Rhine River. This was due to reduced productivity in the second cut hay at the Rhine River in which, interestingly, the contents of nitrogen and crude protein increased. The first cut at the Rhine River was unaffected by the treatments. At the Elbe tributaries, the annual yield and the hay quantity and quality of both cuts were only marginally affected by the treatments.
Conclusion
We conclude that the yield of floodplain meadows may become less reliable in future since the annual yield decreased under precipitation reduction at the Rhine River. However, the first and agriculturally more important cut was almost unaffected by the precipitation reduction, which is probably due to sufficient soil moisture from winter/spring. As long as future water levels of the rivers will not decrease during spring, at least the use of the hay from the first cut of floodplain meadows appears reliable under climate change.
Citation: Ludewig K, Donath TW, Zelle B, Eckstein RL, Mosner E, Otte A, et al. (2015) Effects of Reduced Summer Precipitation on Productivity and Forage Quality of Floodplain Meadows at the Elbe and the Rhine River. PLoS ONE 10(5): e0124140. https://doi.org/10.1371/journal.pone.0124140
Academic Editor: Bo Li, Fudan University, CHINA
Received: September 7, 2014; Accepted: March 10, 2015; Published: May 7, 2015
Copyright: © 2015 Ludewig et al. This is an open access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited
Data Availability: All relevant data are within the paper and its Supporting Information files
Funding: The Elbe study was funded by the Federal Ministry of Education and Research within the research project KLIMZUG-NORD (grant number 01LR0805D) and the Rhine study was financed by the Federal Ministry of Transport, Building and Urban Development within the research project KLIWAS. The Landwirtschaftskammer Niedersachsen gave financial support for analysing samples from the Elbe tributaries. KL was further supported by the Estuary and Wetland Research Graduate School Hamburg (ESTRADE), which was funded by the Hamburg Science and Research Foundation as member of the State Excellence Initiative (LExI). The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.
Competing interests: The authors have declared that no competing interests exist.
Introduction
European semi-natural habitats such as agriculturally unimproved grasslands make a large contribution to the species diversity of landscapes [1, 2]. This is not only due to the high plant species richness, which is characteristic for semi-natural grasslands, but also due to large numbers of animal species (e.g. insects and birds) for which grasslands offer suitable habitats (e.g. [3]). Floodplain grasslands along large lowland rivers are hotspots of biodiversity and the outcome of typical flooding regimes and long lasting land use practices with moderate intensity [4]. They harbour many rare [5, 6], typical river corridor plants such as Cnidium dubium, Thalictrum flavum or Viola elatior [7]. Due to the impact of flooding events in combination with dry conditions over the summer, floodplains are highly dynamic and variable environments [8]. Floodplains are mainly used as grasslands for grazing (pastures) and mowing (meadows) to gain fodder for domestic livestock. Mowing once or twice annually without fertilizer application is recommended for facilitating a high species richness [4].
As other semi-natural grasslands in Europe, floodplain meadows strongly declined over the last centuries. The main causes for loss of species-rich floodplain meadows are the reduction of the dynamic hydrologic conditions due to river regulations [9] or river training [10], and land use changes as intensification (e.g. [11]) or abandonment (e.g. [12]). Consequently, these meadows are of high conservation value and certain types of meadows found in European floodplains are protected by the Habitats Directive (92/43/EEC, habitat type 6440: Alluvial meadows of river valleys of the Cnidion dubii; 6510: Lowland hay meadows) and subject to various restoration measures [13–15].
It is an ongoing nature conservation concern how the biomass of species-rich non-intensively managed meadows can be incorporated into agricultural land use systems [16–18] and animal nutrition. Undoubtedly, it is preferable to integrate these meadows into farming systems instead of just managing them in the framework of nature conservation schemes. In future, however, the productivity of semi-natural grasslands may be affected by increased rainfall variability due to climate change.
Precipitation is one of the most influential abiotic factors for plant productivity [19]. Changes in precipitation patterns are projected to occur in the course of climate change [20]. For Germany, regional climate change projections indicate higher temperatures and an increasing risk for summer droughts for the late 21st century due to less summer precipitation in relation to the reference period 1961–1990 [21, 22]. Accordingly, river discharges during summers are projected to decrease, e.g. at the large rivers Rhine [22] and Elbe [23]. This, in turn, could lower the water table in the adjacent floodplains with negative effects on the soil water potential. In combination with increased transpiration at higher temperatures, these changes could induce drought stress in plants of floodplain meadows [24]. Plant responses to drought stress are manifold, including decreased cell elongation and reduced photosynthesis; the responses generally lead to reduced plant growth and delayed plant development [25].
Nitrogen fertilization generally affects the vegetation of semi-natural grasslands: besides increased productivity, shifts in species compositions were observed [26, 27]. With respect to forage quality, mostly increases [28, 27] but also decreases in nitrogen contents [26] were recorded after nitrogen addition. How nitrogen addition affects the vegetation of floodplain meadows is less known.
In recent years, some climate change experiments were conducted in grassland ecosystems, e.g. in a semi-arid steppe [29], in mesic tallgrass prairies [30], and in temperate grasslands [31–34]. Only one of these studies focused on how forage quality—the ecosystem service relevant to farmers—might change in the future using the example of nitrogen and protein content of the biomass [34]. Still, additional variables relevant for farmers such as crude fibre, crude protein, energy content or fructan have not been analysed in this context. Generally, data on the forage quality of non-intensively used semi-natural grasslands are scarce in the international literature (but see [17, 18, 35]). Also in the UK, data for biomass from species-rich semi-natural grasslands are lacking [36] and it seems that there is still a current need to examine this topic. Generally, high values of crude protein, digestible energy and contents of nitrogen (N), phosphorus (P), and potassium (K) indicate high forage quality of hay while high amounts of crude fibre and fructan impair forage quality [37].
To clarify the effects of changes in summer precipitation on the quantity and quality of the biomass of European floodplain grasslands, we conducted field experiments in which we reduced the amount of precipitation with rainout shelters. We harvested biomass, analysed its amount and the above mentioned parameters. Further, we calculated the annual yield as the product of biomass amount and energy content. The data we present here originate from two independent precipitation experiments, conducted at the rivers Rhine and at two Elbe tributaries.
We aimed at answering the following research questions: Does reduced summer precipitation affect the quantity of hay, its quality in the first and second cut, and the overall annual energy yield of floodplain meadows?
Materials and Methods
Experiments at the Elbe and the Rhine River
We summarise results of two precipitation reduction experiments in floodplain meadows at the Rhine River and at two Elbe River tributaries originating from two independent studies. Because the two studies were planned and conducted independently from each other, different experimental designs were employed. However, as the overall aims and the used rainout shelters were identical, we present the results in this integrating paper.
Permissions
The permits for the field experiments were provided by the Biosphere Reserves Elbe River of Lower Saxony for the experiment at the Sude, from the Biosphere Reserves Elbe River of Saxony-Anhalt as well as from the Nature Conservation Authority from Saxony-Anhalt for the Havel. Permits for the experiment at the Rhine were provided from the city of Riedstadt, the regional council Darmstadt and the forestry administration of Hesse.
Study areas and study sites
The studies were conducted on floodplain meadows belonging to the functional floodplain (not disconnected from the river and thus inundated in times of high water) at the Rhine River and at two Elbe River tributaries, the Havel and the Sude River. All studied floodplains have in common that the climatic and hydrological conditions result in highly variable soil water potentials: while winter, spring and early summer may bring floods, the summer periods are notably dry (especially the continental Havel site in the Elbe region and the Rhine site). Along with the strong seasonal and inter-annual fluctuations of the water level of the rivers, the groundwater tables also strongly fluctuate [38, 39].
The study area at the Rhine River is situated in the Hessian part of the Holocene floodplain of the northern Upper River Rhine near Riedstadt, about 30 km southwest of Frankfurt, Germany (N 49°49′, E 8°26′). The climate in this area is relatively dry and warm with a mean annual precipitation of 602 mm (1961–1990 Riedstadt-Erfelden, DWD 2013) and a mean annual temperature of 9.7°C (1961–1990 Frankfurt Main airport, DWD 2013). The soils can be classified as calcic Fluvisols [40]. The vegetation of the study site itself is relatively species poor because it was an arable field until 1983 (for details on the history of the site see [41, 42]). Since 1983, the meadows are mown up to two times annually. Two sites differing in elevation were chosen as study sites (a higher/dryer site and a lower/wetter site). The species composition of the study meadow is dominated by Festuca arundinacea. Further frequently occurring species are Dactylis glomerata and Leucanthemum vulgare on the higher site and Potentilla reptans and Symphytum officinale on the lower site. The nomenclature of plant species follows Wisskirchen and Haeupler [43].
The meadows at Elbe tributaries are located at the Sude River (near Sückau in Lower Saxony, N53°19′ E010°57′) and the Havel River (near Kuhlhausen in Saxony-Anhalt, N52°47′ E012°11′). The site at the Sude River experiences rather oceanic climatic conditions with a mean annual precipitation of 663 mm and a mean annual temperature of 8.3°C (1961–1990; data from the nearest weather station in Boizenburg; DWD 2013). The site at the Havel River has on the contrary relatively continental climatic conditions with a mean annual precipitation of 503 mm (1961–1990; data from the nearest weather station in Havelberg; DWD 2013) and a mean annual temperature of 9.1°C (1976–2009; data from the nearest weather station measuring temperature in Seehausen; DWD 2013). Both sites are regularly flooded by either the Sude or the Havel River, which are first order tributaries of the Elbe River. The soils of both sites are gleyic Fluvisols, which consist mainly of loamy material over sandy sediments. The active floodplains along the Sude and Havel are typically used as grasslands and the two meadows are mown twice annually. Both study sites contain Cnidium-floodplain meadow vegetation with characteristic river corridor plants (according to [7]), such as Cnidium dubium, Stellaria palustris and Carex vulpina, and more frequently occurring species, such as Alopecurus pratensis, Deschampsia cespitosa, Potentilla anserina, Potentilla reptans, and Ranunculus repens.
The experiment at the Rhine River
The experiment at two sites at the Rhine River was conducted in the vegetation periods 2011 and 2012. The rainout shelters measured 3 m x 3 m and were built according to Yahdjian & Sala [44] using acrylic glass pipes as flumes. To minimize edge effects, the investigated plots beneath the rainout shelters were adjusted to 4 m2. The two studied experimental factors were elevation above base flow (high: 320 cm above base flow; low: 240 cm above base flow) and precipitation reduction (-50%, -25%, no reduction). Two types of controls were used: 1) control plots with rainout-shelters where the acrylic glass pipes were turned upside down (to test the rainout-shelter effect without rain reduction) and 2) control plots without rainout shelters (see Table 1). Precipitation reduction was conducted from March to October. The experiment was run with three replicates. The weather conditions of the study years are shown in Fig 1c.
The black line with grey shade represents daily average, minimal and maximal monthly temperatures. The grey bars are monthly sums of precipitation. Arrows indicate the dates of biomass sampling.
The experiment at the Elbe River tributaries
In the vegetation periods 2009 to 2011, we conducted a field experiment at the two Elbe River sites. In a two-factorial design, we manipulated summer precipitation, which was reduced by approx. 25% with rainout shelters, and N deposition, which was imitated by fertilization with ammonium-nitrate (35 kg N ha-1 a-1). Precipitation reduction and fertilization treatments were conducted from May to October (in 2009 from July to October). Fertilizer was applied at seven dates evenly distributed over this period. As in the Rhine experiments, the rainout shelters measured 3 m x 3 m and were built according to Yahdjian & Sala [44], but using UV permeable greenhouse plastic as flumes. To minimize edge effects, study plots covered only the inner approx. 4 m2 of the rainout shelter. Four treatments were implemented (see Table 1): 1.) precipitation reduction and fertilization (-25%/+N), 2.) only fertilization (+N), 3.) only precipitation reduction (-25%), and 4.) controls without treatments (controls). The experiment was run with seven replicates. The weather conditions of the study years are shown in Fig 1a and 1b.
Response variables
As response variables we measured the amount of biomass (g m-2), its contents of crude fibre (XF, % dry weight; dw), crude protein (XP, % dw), the elements N (mg g-1 dw), P (mg g-1 dw), and K (mg g-1 dw) and fructan (% dw). Fructans are storage carbohydrates of many grass species [45]. High contents of fructan in the forage can be unhealthy for horses and ponies [46]. Energy content of the biomass was assessed as digestible energy (DE), net energy for lactation (NEL) and metabolisable energy (ME; all in MJ kg-1 dw). While the latter two are applicable in case of ruminants, DE is an estimate relevant for horse fodder. As these energy values are interrelated and the hay of semi-natural meadows is per se preferably used for horses in the study regions, we focus on DE in this study, but as an overview, we present the ME- and NEL-values in Tables 2 and 3.
On the Elbe sites, biomass samples were taken from 0.25 m2 subplots (three samples of biomass of which one was taken for the forage quality measurements and two were used for the element content measurements) in June 2010 and 2011 (first cuts) and September 2009, 2010 and 2011 (second cuts). At the Rhine sites, biomass samples were taken from 0.1 m2 subplots (12 samples which were ground together and then separated for the forage quality and element content measurements) in June 2011 and 2012 (first cuts) and September 2011 and 2012 (second cuts). In autumn 2011, not enough biomass could be sampled for the fructan analysis on the plots at the Rhine. Biomass samples of all sites were dried at 60°C for three days.
Crude protein, crude fibre, energy variables, and fructan were estimated using a NIRSystem 5000 (Foss GmbH Rellingen, Germany) and scanned between 1100 and 2500 nm. Annual yield (GJ ha-1) was calculated as the product of digestible energy (DE, GJ kg-1 dw) and dry biomass (kg dw ha-1). N contents of the Elbe samples were measured using a CN-Analyzer (vario MAX, elementar, Hanau, Germany) and of the Rhine samples using an Auto-Analyzer (AA 3, Bran & Lübbe, Norderstedt, Germany). K and P contents of the Elbe samples were measured with the ICP-OES technique (samples of 2009: Perkin Elmer ICP/OES, Perkin Elmer, Hamburg, Germany; samples of 2010/2011: iCAPTM 6300 ICP-OES Analyzer, Thermo Scientific, Germany) after digestion of the samples in a Lab microwave (MLS Start 1500, Leutkirch, Germany). The Rhine samples were dry ash combusted and afterwards P contents were measured photometrically (Spectrophotometer, Zeiss, Jena, Germany) and K contents were measured using an Atomic Absorption Spectrometer (AAS-Varian 220 FS, Varian, Darmstadt, Germany).
Data handling and statistical analyses
Due to the differences in study design at the Elbe and Rhine River, both data sets were analysed individually. The effects of the predictor variables on the response variables (annual yield, amount of biomass, crude protein, crude fibre, digestible energy, fructan, N-, P-, and K-content) were tested with repeated measures ANOVAs (with study year as the within subject factor). Except for annual yield, these analyses were done separately for the data from the first and the second cut. The fructan results of the Rhine samples (second cut) were analysed with a two-way ANOVA for the year 2012. In the analysis of the Elbe data set, the experimental predictor variables were precipitation reduction, N-addition, and site. In the analysis of the Rhine data set, the experimental predictor variables were the precipitation treatments (50% and 25% precipitation reduction, control with rainout-shelters, and control) and elevation above base flow (high, low). ANOVAs with significant results were followed by Tukey HSD-tests for comparisons between treatment groups. Basic requirements to conduct a parametric ANOVA such as normality and homoscedasticity were visually checked using diagnostic plots. All statistical tests were conducted using STATISTICA 10 (StatSoft Inc.).
Results
Rhine experiment
The total annual yield significantly decreased by app. 30% under 50% precipitation reduction (21.5 ± 2.6 GJ ha-1) compared to the controls with rainout-shelters (31.7 ± 3.0 GJ ha-1; repeated measures ANOVA: F3,16 = 4.3, p = 0.0215; Tukey: p = 0.0248; Fig 2) and was higher on the lower (35.2 ± 1.8 GJ ha-1) compared to the higher site (19.0 ± 0.6 GJ ha-1; repeated measures ANOVA: F1,16 = 52.3, p < 0.0001; Tukey: p = 0.0002).
The study sites were pooled. Different letters indicate significant differences at p<0.05 across the study years.
In the first cut, no main effects of experimental treatments on the amount of biomass (overall mean ± SE: 222.3 ± 13.1 g m-2) or on the forage quality variables crude fibre (35.5 ± 0.4% dw), crude protein (8.5 ± 0.3% dw), digestible energy (7.3 ± 0.1 MJ kg-1 dw), net energy for lactation (4.2 ± 0.1 MJ kg-1 dw), metabolisable energy (7.5 ± 0.1 MJ kg-1 dw), and the N- and K-contents (N: 12.7 ± 0.4 mg g-1 dw; K: 15.9 ± 0.2 mg g-1 dw) were detected. Only the fructan content significantly increased with 50% reduced precipitation (3.0 ± 0.4% dw) compared to the controls with rainout shelters (1.8 ± 0.4% dw; repeated measures ANOVA: F3,16 = 7.9, p = 0.0019; Tukey: p = 0.0023) and without rainout shelters (2.0 ± 0.4% dw; Tukey: p = 0.0110). Further, the P-content was significantly affected by precipitation reduction (repeated measures ANOVA: F3,16 = 4.2, p = 0.0221) and by an interaction between ‘precipitation reduction’ and ‘site’ (repeated measures ANOVA: F3, 16 = 4.7, p = 0.0151). The P-content of the biomass decreased at 50% precipitation reduction (2.9 ± 0.1 mg g-1 dw) compared to the controls without rainout-shelters (3.3 ± 0.2 mg g-1 dw; Tukey: p = 0.0195) and the P-content differed between differently treated groups at the higher site in 2012 (see Table 2).
In the second cut, all response variables (except for K-content and fructan) were affected by the precipitation treatments (Fig 3 and S1 Fig). The two differently elevated sites mainly reacted in the same way—an interaction between precipitation reduction and elevation was only detected for the response variable P-content (repeated measures ANOVA: F3,16 = 3.6, p = 0.0365). At both elevations, crude fibre and biomass decreased under precipitation reduction treatments while crude protein and digestible energy increased in 2011. Concerning the element contents, N-contents increased on the higher site by 32% between controls with rainout shelters and plots with 50% precipitation reduction, and P-contents increased by 30% between the same treatments on the lower site in 2011 (see S1 Fig). In 2012, the effects of precipitation treatments were generally less pronounced (see Fig 3 and S1 Fig).
Results refer to second cuts of Rhine sites of the years 2011 and 2012. Different letters indicate significant differences at p<0.05; (mean ± SE; n = 3).
Elbe experiment
The total annual yield did not respond significantly to the precipitation reduction of 25% (repeated measures ANOVA, F1,48 = 0.4, p = 0.51, Fig 2).
In the first cut of the experimental grasslands in the Elbe region, no main effects of the experimental treatments were detected on any of the response variables (for mean values of the variables see Table 3). Significant differences occurred only between the two sites characterised by different climatic conditions (for p-values between sites within years see Table 3). and between the study years 2010 and 2011 (all p < 0.0001; except for fructan: F1,48 = 0.7, p = 0.3938).
In the second cut, the quantity and quality of the biomass did not respond to main effects of the experimental treatments. As in the first cut, significant differences were only detected between the two sites with differing climatic conditions (for p-values between sites within years see Table 3). Further, the differences between years (2009–2011) were significant for all response variables (repeated measures ANOVAs, all p < 0.0001) except for fructan (F2,96 = 2.5, p = 0.0878). Though not significant, the percentage of crude fibre tended to decrease under precipitation reduction at the oceanic site, and tended to increase under these conditions at the more continental site (repeated measures ANOVA, F1,48 = 2.9, p = 0.0941). Vice versa, the amount of digestible energy tended to increase under precipitation reduction at the oceanic site, while it tended to decrease under these conditions at the more continental site (repeated measures ANOVA, F1,48 = 3.2, p = 0.0797).
Discussion
The productivity of the meadows in this study is in the same range as that of other flood meadows [47], but lower than that of non-flooded meadows [34] or fertilized semi-natural grasslands [36]. Generally, data on crude fibre, crude protein, energy content and fructan of European semi-natural grasslands are scarce in the literature. The few existing studies report values of these variables in the range of our study [17, 18, 47] or slightly higher NEL values in a calcareous grassland [48]. Our contents of N, P and K were very variable, but roughly in the same range [48, 49] or lower [36] compared to other studies on semi-natural grasslands. The hay quality of semi-natural floodplain meadows is low compared to agriculturally improved and intensively used sown hay meadows [36]. This is in accordance with Franke [47] who concluded that the hay originating from semi-natural meadows is especially suitable for leisure horses and young cattle or not lactating cows. For lactating cows, the energy content is too low [47] but can be incorporated into basic ration [50].
As our most important result, the annual yield decreased under precipitation reduction by 50% in the experiment at the Rhine River. However, the precipitation reduction of 25% did not affect the quantity and quality of hay from the meadows at all sites. Therefore, our findings indicate that climate change could affect the quantity and quality of hay in the future, when the reduction of precipitation is severe.
At the Rhine River, the responses of the meadow vegetation to the experimental treatments were more pronounced in the second than in the first cut. Most importantly, the amount of biomass and its content of crude fibre decreased under reduced precipitation in the second cut, while interestingly, the digestible energy and the contents of crude protein, N, and P increased in the biomass. Generally, an increase in hay quality in dry years was already reported by Opitz von Boberfeld [37], but the underlying processes still remain unclear. A possible explanation for the higher N-contents in the biomass from plots with reduced productivity could be the dilution effect, i.e. a decrease in N-concentrations through a proportionally higher accumulation of C than of N during growth of the aboveground biomass [26]. Secondly, the N-contents in the biomass might have been higher at the precipitation reduction treatment because of slower re-growth of the meadow plants after the first cut. Under dryer conditions, plant development is decelerated [25] and the aboveground biomass remains longer in an earlier phenological state, i.e. it consists mainly of leaves at harvest compared to plots with full precipitation, where plants already developed stems. The N concentration in leaves is greater than in stems and the N concentration of the whole herbage depends largely on the leaf/stem ratio [51]. A third explanation for the higher N- and protein contents under reduced precipitation might be a larger variability in soil moisture. Fluctuations in moisture content stimulate nutrient mineralisation [52]. Especially the extractable P pool was reported to increase upon soil re-wetting [53]. These fluctuations may be the reason why we detected higher P-contents in the biomass of the control plots in spring 2012 on the dry site while on the contrary we measured higher P-values under experimentally reduced precipitation in the plant foliage in autumn 2011 on the lower site. Drought stress also increased foliar N and P concentration of eastern cottonwood Populus deltoides [54] and in Salix spp. [55]. The observation that plants absorb nutrients at a higher rate than is required for their actual plant growth when another resource is limiting, is interpreted as advantageous as these absorbed nutrients can be readily incorporated in assimilates when the limiting resource is available again [56]. Further, higher concentrations of osmotic compounds (e.g. N containing amino-acids) decrease the water potential of tissues and thus helps the plants to take up water from the soil [57].
The N input of 35 kg ha-1 a-1 at the Elbe tributaries had no effect on the quantity and quality of the hay. Probably the experimental N input was negligible compared to inputs by flooding events, which are the main source of nutrients in floodplain ecosystems [58].
Besides of the weak treatment effects, our data demonstrate a high variability of the response variables between the study years at both rivers. This is probably due to the different weather conditions in the study years. Shortly before the second cuts, for example, the weather conditions were very dry in 2009, very wet in 2010, and intermediate in 2011 at the Elbe tributaries (see Fig 1a and 1b).
High variability of the response variables was also found between the experimental sites at both rivers. At the Elbe tributaries, it is striking that the responses of crude fibre and energy content were completely different between the two sites. A possible explanation for this pattern could be that the percentage of dicots differed between the sites. The oceanic site (with the tendency of reduced crude fibre and higher energy at reduced precipitation in the second cut) showed higher abundances of grasses compared to the more continental site, which tended to develop reduced energy and higher crude fibre in the second cut hay at reduced precipitation (see S2 Fig). The grasses mostly reproduce (i.e. set seeds) before the first cut in floodplain grasslands and grow leaves until the second cut. Since the N concentration (and energy content) is larger in leaves than in stems [51], leaves contain less crude fibre. In the more continental site, the dicots might have been in the process of reproduction at the second cut, in which the reduced precipitation might have had a ‘slow down’ effect on the reproduction process.
Overall, the meadows at the Rhine were more responsive to the experimental treatments than the Elbe meadows. This may, on the one hand, be due the lack of a 50% reduction treatment in the Elbe experiment. Therefore, the measured responses were limited and the effects at the Elbe River may be underestimated. On the other hand, the ‘new’ meadows of the Rhine floodplain were less species rich compared to the ‘old’ meadows at the Elbe tributaries. Species richness might have buffered possible effects of reduced precipitation on the response variables: in species-rich stands, some species may be facilitated through the treatments, compensating reduced growth of other species and thus increasing the reliability of grassland productivity under variable conditions [59, 60, 61]. Thus, the role of meadow age and species richness in the drought resilience of grasslands requires further research.
Conclusions
The annual yield decreased under precipitation reduction of 50% in the experiment at the Rhine River. Therefore, we conclude that the yield of floodplain meadows may become less reliable in future. Nevertheless, the effects of the two precipitation reduction experiments on forage quality and the amount of biomass were, overall, rather small. This finding fits with other studies reporting weak or no effects of drought events on grassland productivity [32, 34, 62, 63]. The first cut was not affected by precipitation reduction (except for fructan at the Rhine sites) in the floodplain meadows at both rivers. As the first cut is usually of higher quantity and quality than the second cut and, therefore, economically more important for agricultural purposes, at least the use of the first cut hay may be still possible under climate change. In case of our studied floodplain meadows, soil moisture was probably sufficient for plant growth from winter/spring until the first cut in June. It has to be considered that the groundwater levels of floodplains correspond to the water level of the associated river. Consequently, whether the productivity of the floodplain meadows will be affected in future will largely depend on whether the river discharges will decrease during winter and spring in future. Finally, as multiple factors may simultaneously change in the course of climate change, additive effects of reduced summer precipitation, higher temperatures and increased CO2 concentrations, and possibly lowered groundwater tables are likely to influence productivity of floodplain meadows.
Supporting Information
S1 Fig. Responses of the content of fructan, N, P, and K to experimental treatments.
Results refer to second cuts of Rhine-sites of the years 2011 and 2012. Different letters indicate significant differences at p<0.05; (Mean ± SE; n = 3).
https://doi.org/10.1371/journal.pone.0124140.s001
(TIF)
S2 Fig. The abundance of the functional groups ‘grasses’ and ‘herbs’ at the time of cutting in June and September 2011 at the experimental sites at the Elbe tributaries Sude and Havel.
https://doi.org/10.1371/journal.pone.0124140.s002
(TIF)
Acknowledgments
We thank the landowners and tenants for allowing us to work on their property. We thank Josef Scholz-vom Hofe, Jacqueline Abels, Harry Stöckmann, Cynthia Erb, Lotte Korell and Jana M. Hanke for field assistance, and the AG FUKO (Hannover) for analysing our samples. We thank Peter Horchler (Bundesanstalt für Gewässerkunde), Johannes Prüter, Tobias Keienburg and Christiane Schreck (Biosphere Reserves Elbe River of Lower Saxony), Andreas Berbig (Biosphere Reserves Elbe River of Saxony-Anhalt), Wilko Trapp (Nature Conservation Authority from Saxony-Anhalt) Matthias Harnisch (city of Riedstadt), Matthias Ernst (regional council Darmstadt) and Ralph Baumgärtel (forestry administration of Hesse) for kind cooperation. We thank Gerd Lange and Sandra Dullau for valuable comments on the interpretation of our forage quality values and the manuscript.
Author Contributions
Conceived and designed the experiments: KL TWD BZ RLE EM AO KJ. Performed the experiments: KL TWD BZ RLE. Analyzed the data: KL TWD RLE. Contributed reagents/materials/analysis tools: KL TWD BZ RLE AO KJ. Wrote the paper: KL TWD RLE EM AO KJ.
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