Nutrient limitations in an extant and drained poor fen: implications for restoration

In a species-rich poor fen (Caricetum nigrae) and a species-poor drained fen, the difference in nutrient limitation of the vegetation was assessed in a full-factorial fertilization experiment with N, P and K. The results were compared to the nutrient ratios of plant material and to chemical analysis of the topsoil. A rewetting experiment with intact sods was carried out in the glasshouse and the results are discussed in view of restoration prospects of drained and degraded peatlands. In the undrained poor fen the above-ground biomass yield was N-limited while the vegetation of the drained fen was K-limited. Experimental rewetting of intact turf samples, taken in the drained site, did not change the biomass yield or the type of nutrient limitation. It was concluded that mire systems which have been subjected to prolonged drainage are inclined to pronounced K-deficiency, probably due to washing out of potassium and harvesting the standing crop. This may hamper restoration projects in degraded peat areas where nature conservation tries to restore species-rich vegetation types with a high nature value.     

The relation between vegetation and soil chemistry gradients in a ground water discharge fen

Abstract. The soil chemistry of a headwater valley fen is influenced by local ground water discharge that supplies base cations and alkalinity to the fen. An irrigation canal just upward of the fen is the source of this alkalinity. The ecological consequences of this artificial system are studied both on the soil and vegetation level. Rich-fen species of the alliance Caricion davallianae are connected to soil water alkalinity and soil base status. They depend directly on the alkaline ground water discharge. In addition, the local input of this water causes a gradient-rich pattern from poor to rich fen, and it is therefore concluded that it is responsible for the presence of intermediate fen vegetation too. High nutrient levels in the irrigation water have not influenced the fen until now. This case study illustrates the possibility for rich fen restoration after acidification. Irrigation with alkaline water is efficient if excess nutrients can be removed.     

Relationship between synthesis and cleavage of poliovirus-specific proteins.

Poliovirus proteinase was studied in vitro in lysates from poliovirus-infected HeLa cells. Preincubation of these lysates caused (i) a reduction in poliovirus proteinase activity and (ii) a partial dependence on exogenous mRNA for optimal translation. Proteins translated from endogenous poliovirus RNA in preincubated extracts from virus-infected HeLa cells are poorly cleaved. This cleavage deficiency is alleviated by adding fresh poliovirus RNA to the translation system, thus, allowing re-initiation to occur. This suggests that the poliovirus proteinase is highly unstable.     

Nutrient limitation in species-rich lowland fens

Abstract. Nitrogen, phosphorus and potassium were supplied to some Belgian fens of varying nutrient status and productivity. Plant growth in the lowest productive fen with a species-rich Caricion davallianae vegetation was strongly P-limited. N was ineffective when applied alone, but increased the effect of P-addition when applied together. Summer biomass and plant nutrient concentrations were monitored for four years, and showed partial recovery of nutrient limitation. In a more productive fen dominated by Carex lasiocarpa and in a fen meadow, nutrient limitation was less strong. N limited growth in the productive fen, and N and K were co-limiting in the fen meadow. The P-concentration in the productive fen vegetation showed a marked increase after P-fertilization, but it did not result in higher standing crop. The significance of P-limitation for the conservation of species rich low productive fens is discussed. P-limitation may be an essential feature in the conservation of low productive rich fens: because it is less mobile in the landscape than N and/or because it is an intrinsic property of this vegetation type. Plant nutrient concentrations and N:P-ratios may be used as an indication for the presence and type of nutrient limitation in the vegetation. We found N:P-ratios of 23 to 31 for a P-limited site and 8 to 15 in N-limited sites. This was in agreement with critical values from the literature: N:P > ca. 20 for P-limitation and N:P < 14 for N-limitation. Thus, this technique appears valid in the vegetation types that were studied here.     

Differential recovery of above‐ and below‐ground rich fen vegetation following fertilization

Abstract. For seven years we studied the recovery of vegetation in a Belgian P limited rich fen (Caricion davallianae), which had been fertilized with nitrogen (200 g.m^?2) and phosphorus (50 g.m^?2) in 1992. The vegetation in this fen has low above‐ground biomass production (< 100 g m^?2) due to the strong P limitation. Above‐ground biomass was harvested from 1992 to 1998 and P and N concentrations measured. In 1998, below‐ground biomass was also harvested. The response to fertilization differed markedly between below‐ and above‐ground compartments. Above‐ground, P was the single most important factor that continued to stimulate growth 7 yr after fertilization. Below‐ground, N tended to decrease live root biomass and increase dead root biomass and seemed to have a toxic effect on the roots. In the combined NP treatment the stimulating effect of P (an increase of live root biomass) was countered by N. The 1998 soil analysis showed no difference in soil P in the plots. Thus, Fe hydroxides are not capable of retaining P in competition with fen vegetation uptake. However, higher capture of P in root Fe coatings from N plots may partially explain this negative N effect. The results suggest that N root toxicity will be amplified in strongly P limited habitats but that its persistence will be less influenced by P availability. This mechanism may be a competitive advantage for N₂ fixing species that grow in strongly P limited wetlands.     

A local rich fen fed by calcareous seepage from an artificial river water infiltration system

The habitat of low growing, herbaceous rich-fen vegetation (Caricion davallianae) is now threatened throughout Western Europe. Its conservation, restoration and even recreation receives increasing attention. In the Campine area of Belgium a rich fen, that depends entirely on an artificial river water infiltration system for its alkaline discharge, is present. The rich fen vegetation cannot be older then a century, i.e. the age of the infiltration system. This illustrates that poor-fen precursors can be transformed into rich fen by alkaline ground-water discharge. The possibilities for restoration and the difficulties with use of allochtonous water for nature conservation are discussed. Finally, the hydrochemical consequences of the alkaline discharge in the fen soil are considered: in dry summers periodical acidification of the peat soils occurs.     

Intertypic cross-reactions of nonneutralizing, monoclonal poliovirus antibodies.

Quantitative data are presented on (i) the intertypic cross-reactions of polyclonal, guinea pig antibodies directed against the N or H antigen of type 1 poliovirus and (ii) a set of five nonneutralizing, mouse hybridoma antibodies raised against N antigen or a mixture of capsid polypeptides VP1, VP2, and VP3. Three of these antibodies recognize H antigen and VP1, the fourth H antigen only, and the fifth VP3 only. The antibodies recognize either only homotypic antigens or the antigens of the three serotypes.     

Phosphorus fertilization in a phosphorus-limited fen: effects of timing

Abstract. Phosphorus availability in low P-soils is primarily controlled by soil processes that are subject to seasonal fluctuation. There is evidence that summer drought causing low fen-water levels induces temporal high P-availability. We investigate here whether and how fen vegetation responds to P-pulses at different times in the season. Plots were fertilized with equal P-doses at three different times in the season. Four conclusions can be drawn from the experiment: 1. The vegetation is able to increase P-uptake independent of the timing of fertilizer application; 2. Early-season fertilization stimulates growth and increases P-concentration in above-ground tissue while late-season fertilization does not stimulate growth but strongly increases above-ground tissue concentration; 3. Timing effects cause differential species responses: the response of Carex demissa, a stress-tolerant species, is truly independent of timing, while Juncus articulatus, a CSR-type species (sensu Grime) profits more from early-season fertilization; 4. Timing effects persist over several years. The differences between the experimental treatment and the events it aimed to simulate are discussed. We expect that higher frequencies of drought events, that may be induced by climate change, will cause a shift from nutrient-stress tolerant towards stress-tolerant-competitor fen species.