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Nine years of change in the flora of Ellerburn Bank, a limestone grassland in the North York Moors

机译:北约克郡高地石灰岩草原埃勒本银行(Ellerburn Bank)的植物区系发生了九年的变化

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Limestone grassland is one of the most biodiverse habitats on Earth at a small scale (Wilson er al., 2012). Floristic richness within Europe can reach 80 species per m2 (Butaye er al., 2005) and many plants are found in no other habitat. Limestone grassland also supports important invertebrate communities as well as specialist birds (UK Steering Group, 1998). However, it is also one of Europe's most threatened habitats (WallisDeVries ef al., 2002). In 1998 there was a maximum of 41,000 hectares of lowland calcareous grassland remaining in the UK (UK Steering Group, he. cit.). Loss of habitat continues from forestry, conversion of pastureland to crops and land abandonment (WallisDeVries er al., loc. cit.), leading to reductions in the area and increasesin the isolation of habitat patches (Fisher & Stocklin, 1997). Quality reductions come from the abandonment of traditional agricultural practices leading to land-use intensification such as increased fertilization, herbicides, reseeding and frequent or early mowing (WallisDeVries et al., loc. cit). They may also result from overgrazing, undergrazing leading to the encroachment of scrub, Bracken Pteridium aquilinum and coarse grasses (Bobbink & Willems, 1987), and atmospheric nitrogen deposition leadingto loss of richness (van den Berg et al., 2011). The latter threats mean that their quality may decline even if sites are enclosed in protected areas, due to pervasive forces beyond the control of reserve managers (van den Berg et al., loc. cit.) or as aconsequence of suboptimal management. Indeed, JNCC declared that only 29% of Sites of Special Scientific Interest (SSSI) and 27% of Special Areas of Conservation (SAC) on lowland calcareous grassland in the UK were in favourable condition in 2006, belowthe average for habitats in general (Williams, 2006). Optimal management is difficult to achieve because the effects of different practices can vary depending on local conditions (Klimek et al., 2007) and the taxonomic group under consideration (WallisDeVries et al., loc. cit.).
机译:石灰石草原是地球上生物多样性最丰富的栖息地之一(Wilson等,2012)。欧洲的植物丰富度可以达到每平方米80种(Butaye等,2005),而且在其他栖息地也找不到许多植物。石灰石草原还为重要的无脊椎动物群落和鸟类提供了支持(英国指导小组,1998)。但是,它也是欧洲受威胁最大的栖息地之一(WallisDeVries等,2002)。 1998年,英国最多剩下41,000公顷的低地钙质草原(英国督导小组,他引述)。栖息地的丧失继续发生于林业,牧场转换为农作物以及土地被遗弃(WallisDeVries er等人,同上),导致面积减少,栖息地斑块的隔离增加(Fisher&Stocklin,1997)。降低质量的原因是放弃了传统的耕作方式,导致土地利用集约化,例如增加了施肥,除草剂,播种以及频繁或早割(WallisDeVries等,同上)。它们也可能是由于过度放牧,放牧而导致灌木丛,蕨菜蕨和粗草的侵占(Bobbink&Willems,1987),以及大气中的氮沉降导致丰富度的损失(van den Berg等,2011)。后一种威胁意味着,由于保护区管理者无法控制的普遍力量(范登·伯格等人,同上),或者由于管理不善,即使将保护区封闭在保护区内,其质量也会下降。实际上,JNCC宣布,2006年英国低地钙质草原上只有29%的具有特殊科学兴趣的遗址(SSSI)和27%的特殊保护区(SAC)处于有利条件,低于一般生境的平均水平(威廉斯,2006)。由于不同实践的影响可能会因当地条件(Klimek等,2007)和所考虑的分类组(WallisDeVries等,同上)而不同,因此难以实现最佳管理。

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