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Securing Biodiversity in Breckland - European Commission

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<strong>Biodiversity</strong> Implications of the Chang<strong>in</strong>g <strong>Breckland</strong> Climate<strong>Breckland</strong> has become wetter <strong>in</strong> autumn, spr<strong>in</strong>g and especially <strong>in</strong> w<strong>in</strong>ter with an <strong>in</strong>crease <strong>in</strong> thefrequency of extreme ra<strong>in</strong>fall events <strong>in</strong> all seasons. <strong>Breckland</strong> temperatures have become lesscont<strong>in</strong>ental, with much milder w<strong>in</strong>ters, milder nights <strong>in</strong> spr<strong>in</strong>g and summer, and fewer frosts. Thesechanges are predicted to cont<strong>in</strong>ue under current climate change scenarios. Note that the magnitudeof change <strong>in</strong> temperature may have been under-estimated <strong>in</strong> our analysis, due to the relocation ofthe Santon weather station from Grimes Graves to Santon Downham – mak<strong>in</strong>g our test conservative.These changes are likely to have profound consequences for ecological processes, for vegetation, andfor species. These can only be considered qualitatively and with a large degree of uncerta<strong>in</strong>ty.Possible effects may <strong>in</strong>clude: Wetter w<strong>in</strong>ters may favour leach<strong>in</strong>g of m<strong>in</strong>eralisable nitrogen down soil profiles, mak<strong>in</strong>g theuse of soil disturbance treatments to reduce soil fertility more effective. Greater w<strong>in</strong>ter ground-water recharge may occur, with positive benefits for fen and p<strong>in</strong>go(fluctuat<strong>in</strong>g waterbodies) systems. However, it is recommended that ground water scenariosbe explored by models that comb<strong>in</strong>e temperature and precipitation <strong>in</strong> equations for potentialevapo-transpiration. Milder and wetter w<strong>in</strong>ters are likely to result <strong>in</strong> greater growth of perennial grasses that werepreviously kept <strong>in</strong> check by low w<strong>in</strong>ter temperatures and frost. Anecdotal evidence suggeststhis is already occurr<strong>in</strong>g with<strong>in</strong> Thetford Forest. Greater grass growth would result <strong>in</strong> morerapid sward closure and encroachment onto bare ground to the detriment of speciesrequir<strong>in</strong>g bare sand or exposed m<strong>in</strong>eral soil. This may be mitigated by greater use of soildisturbance treatments, and adjustments <strong>in</strong> graz<strong>in</strong>g regimes to remove excess biomass.Current climate predictions <strong>in</strong>dicate that summers will be warmer and drier; if summerdrought<strong>in</strong>g <strong>in</strong>creases significantly, this may mitigate some of the effects of the milder, wetterw<strong>in</strong>ters. Many of the <strong>Breckland</strong> speciality and coastal species are more widely distributed <strong>in</strong>cont<strong>in</strong>ental steppe or Mediterranean ecosystems. These are often stress tolerant butvulnerable to competition, or to pathogens that can be active <strong>in</strong> damper or more temperateconditions. Thus wetter autumn, w<strong>in</strong>ter and spr<strong>in</strong>g soil conditions may be detrimental toseeds, aestivat<strong>in</strong>g plants or soil dwell<strong>in</strong>g <strong>in</strong>sect larvae. For example, beetle larvae adapted toxeric conditions may have less resistance to fungal pathogens that can be important <strong>in</strong>population dynamics (Holland 2002).In addition, frost can reduce the vigour of competitors, while also provid<strong>in</strong>g small scale localsoil disturbance <strong>in</strong> frost heave; both processes will be reduced.It will be hard to disentangle responses to chang<strong>in</strong>g weather from other changes (land-use, habitatextent), particularly for species whose ecology, distribution, and past and current status are poorlyknown.Recommendation: Ground water scenarios should be explored by models that comb<strong>in</strong>e temperature andprecipitation <strong>in</strong> equations for potential evapo-transpiration. Attempt to mitigate <strong>in</strong>creased vegetation productivity from milder and wetter w<strong>in</strong>ters bygreater use of soil disturbance transpiration and adjustments <strong>in</strong> graz<strong>in</strong>g regimes to removeexcess biomass.97

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