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Securing Biodiversity in Breckland - European Commission

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Nitrogen Deposition: Potential Impacts and MitigationGrass-heath communities depend on low nutrient conditionsEricoid (heather) heathland vegetation, <strong>in</strong> common with chalk grassland, dune and grass-heathvegetation, depends on the low nutrient status of the soil for the characteristic stress tolerant plantcommunities to persist. With <strong>in</strong>creased nutrients, less competitive stress-tolerant species arereplaced by more vigorously competitive species. The diversity and composition of vegetation isfundamentally altered, generally result<strong>in</strong>g <strong>in</strong> a loss of scarce species, low grow<strong>in</strong>g species, lichens andbryophytes.Experimental work conducted <strong>in</strong> the Netherlands has shown the susceptibility of heather heathlandvegetation to <strong>in</strong>creased nitrogen deposition, with dwarf shrub heather species be<strong>in</strong>g replaced byperennial grass species as nitrogen loads <strong>in</strong>crease (Berendse et al. 1993). Effects <strong>in</strong>clude thereplacement of l<strong>in</strong>g heather Calluna vulgaris by wavy-hair grass Deschampsia flexuosa on dry heaths(Heil and Diemont 1983) as well as replacement of both l<strong>in</strong>g heather Calluna vulgaris and crossleavedheather Erica tetralix by purple moor grass Mol<strong>in</strong>ia caerulea on damp or wet heaths (Heil andBrugg<strong>in</strong>k 1987; Aerts et al. 1990; Berendse 1990; Berendse et al. 1993).Experimental work shows that addition of either phosphorous or nitrogen to calcareous <strong>Breckland</strong>grass-heath vegetation results <strong>in</strong> greater dom<strong>in</strong>ance and growth of perennial grasses and loss oflichens and other low-grow<strong>in</strong>g stress-tolerant plants, together with a reduction <strong>in</strong> vascular plantdiversity <strong>in</strong> the sward (Davy and Bishop 1984). Similar effects have been demonstrated onecologically similar habitats , <strong>in</strong>clud<strong>in</strong>g sand dune vegetation, with a decl<strong>in</strong>e <strong>in</strong> annual species,mosses and lichens and <strong>in</strong>crease <strong>in</strong> red fescue Festuca rubra (Willis 1963; Boorman and Fuller 1982),and on calcareous grassland <strong>in</strong> which Festuca rubra became vigorous and dom<strong>in</strong>ant (Smith, Elstonand Bunt<strong>in</strong>g 1971).In <strong>Breckland</strong>, nitrogen appears to be the primary limit<strong>in</strong>g nutrient (Davy and Bishop 1984), as bothsand dune soils (Boorman and Fuller 1982) and chalk grasslands (Bobb<strong>in</strong>k et al. 1989). Unpublishedwork carried out by P. Dolman and S. Lake showed that diverse lichen-heath sub-communities of U1acid grassland occurred on soils that were higher <strong>in</strong> phosphorous than grass dom<strong>in</strong>ated subcommunities,as long as their nitrogen status was very low. The effects of nitrogen enrichment arepartially l<strong>in</strong>ked with those of graz<strong>in</strong>g (Berendse 1985). Work by both Davy and Bishop (work<strong>in</strong>g atDeadman's Graves, <strong>Breckland</strong>) and Boorman and Fuller (work<strong>in</strong>g on dune vegetation on the Norfolkcoast) showed that graz<strong>in</strong>g was not sufficient to offset the impacts of nitrogen addition on lichen richgrass-heath.Increased nitrogen deposition <strong>in</strong> the UK and <strong>Breckland</strong>There has been a very large reduction <strong>in</strong> the emissions of nitrogen attributable to domestic coal s<strong>in</strong>cethe peak of that source <strong>in</strong> c.1900. Despite this, overall reduced nitrogen (NH 3 and NH 4 +) emissionshave cont<strong>in</strong>ued to <strong>in</strong>crease throughout 1900-2000 due to large <strong>in</strong>creases from the agricultural sector(Fowler et al. 2004). Oxidised nitrogen emissions (NO 3 - , NO 2 and HNO 3 ) form c80% of total emissionsand have decl<strong>in</strong>e s<strong>in</strong>ce a peak <strong>in</strong> 1980. Overall emissions have thus decl<strong>in</strong>ed <strong>in</strong> recent decades(Fowler et al. 2004).98

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