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Contribution of acidification and eutrophication to declines in species richness of calcifuge grasslands along a gradient of atmospheric nitrogen deposition

机译:酸化和富营养化对沿大气氮沉积梯度的钙化草原草地物种丰富度下降的贡献

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摘要

1. Atmospheric deposition of nitrogen (N) is a global problem resulting in negative consequences for biodiversity due to direct toxicity, increases in invasive species, increased susceptibility to environmental stresses and soil-mediated effects of acidification and eutrophication. 2. Reductions in plant species richness related to N deposition have been observed in a number of habitats including calcifuge (acid) grasslands but the mechanisms of this decline have not been fully investigated. We test the hypotheses that along a large-scale gradient of N deposition there is (i) an increase in species tolerant of low pH conditions as a result of soil acidification and (ii) an increase in competitive and nitrophilic species as a result of soil eutrophication. As competitive species can occur in low pH habitats, both of these hypotheses could be true. 3. Using plant characteristics, we examined changes in vegetation species composition along the gradient of N deposition in the UK. Mean C–S–R signatures were used to identify the competitive response of plant communities together with Ellenberg N (nitrogen) scores to identify increases in nitrophilic species. Ellenberg R (reaction, pH) scores were used to identify change in response to soil pH together with an index of soil acidity preference developed using regional survey data. 4. Mean C–S–R signatures showed no significant correlation with N deposition, nor did mean Ellenberg N scores. Ellenberg R scores and the index of soil acidity preference showed significant relationships with N deposition indicating an increased dominance of acid-tolerant species. 5. The results suggest that soil acidification as opposed to eutrophication and consequent competition between species is contributing to shifts in species composition and diversity linked to N deposition in calcifuge grasslands. Soil acidification may be leading to reduced nutrient availability preventing the effects of N addition from being apparent.
机译:1.大气中氮的沉积是一个全球性问题,由于直接毒性,入侵物种的增加,对环境压力的敏感性增加以及酸化和富营养化对土壤介导的影响,导致对生物多样性产生不利影响。 2.在包括生化钙(酸性)草原在内的许多生境中都观察到了与氮沉降有关的植物物种丰富度的降低,但是这种降低的机理尚未得到充分研究。我们检验了以下假设:沿着土壤氮的大规模沉积,(i)由于土壤酸化而增加了对低pH条件的耐受性,并且(ii)由于土壤使竞争性和嗜氮性物种增加了富营养化。由于竞争性物种可能发生在低pH的栖息地中,所以这两个假设都是正确的。 3.利用植物特征,我们研究了英国沿N沉积梯度的植被物种组成的变化。平均C–S–R签名用于鉴定植物群落的竞争反应,并使用Ellenberg N(氮)评分来鉴定嗜氮物种的增加。 Ellenberg R(反应,pH)评分用于识别对土壤pH的响应变化,以及使用区域调查数据得出的土壤酸度偏好指数。 4.平均C–S–R签名显示与N沉积无显着相关性,平均Ellenberg N评分也无显示。 Ellenberg R评分和土壤酸度偏好指数显示出与N沉积的显着关系,表明耐酸物种的优势度增加。 5.结果表明,土壤酸化与富营养化以及物种之间的竞争相反,是导致钙质草地氮素沉积相关物种组成和多样性发生变化的原因。土壤酸化可能导致养分利用率降低,从而阻止氮的添加效果明显。

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