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Atmospheric nitrogen deposition explains patterns of plant species loss

机译:大气氮沉积解释了植物物种流失的模式

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Atmospheric nitrogen (N) deposition across Europe increased substantially from the 1950s to the 1990s. Targeted surveys suggest a negative correlation between N deposition and species richness within quadrats in sensitive habitats. However, it remains unclear whether plant species losses at national recording scales are correlated with nitrogen deposition. We relate plant species losses before 1987 in Great Britain to reduced and oxidized N deposition, land use change and climate change. The mean Ellenberg fertility (N) indices of plant species lost in each 100 km(2) cell before 1987 was compared with those of species that were recorded between 1987 and 1999. In 45% of squares, indices of species lost were significantly lower than those for species present after 1986. For 17%, primarily upland, squares, the opposite effect was found. A generalized least squares regression model, with difference in the mean Ellenberg N index between samples as the dependent variable, showed that higher deposition of reduced N was significantly associated with selective loss of species with a lower index. Arable land use and change in arable land use also demonstrated this positive relationship. Rough grazing, change in rough grazing, change in pasture and change in annual precipitation showed negative effects. Difference in Ellenberg R index was highly correlated with difference in Ellenberg N and was negatively correlated with oxidized N deposition, suggesting that the lack of a significant effect of oxidized N deposition on Ellenberg N was because it had effects through both acidification and eutrophication, while the effect of reduced N deposition was primarily through eutrophication. Our results suggest that N deposition, along with land use and precipitation changes, has been a significant driver of local plant extinctions. With N deposition increasing in many parts of the world, local extinctions of plant species may be experienced in other regions.
机译:从1950年代到1990年代,整个欧洲的大气氮(N)沉积量大幅增加。有针对性的调查表明,敏感生境中四方类动物的氮沉积与物种丰富度之间呈负相关。但是,尚不清楚国家记录规模的植物物种损失是否与氮沉积有关。我们将1987年之前英国的植物物种丧失与氮氧化物的减少和氧化,土地利用的变化和气候变化联系起来。将1987年之前每100 km(2)单元中损失的植物物种的平均Ellenberg育性(N)指数与1987年至1999年之间记录的物种的平均Ellenberg育性(N)指数进行比较。在45%的正方形中,物种损失的指数显着低于1986年以后出现的物种的影响为正。对于17%(主要是高地)的正方形,发现了相反的效果。广义最小二乘回归模型以样品之间的平均Ellenberg N指数差异作为因变量,表明还原N的较高沉积与具有较低指数的物种的选择性损失显着相关。耕地利用和耕地利用变化也证明了这种积极关系。粗放牧,粗放牧变化,牧场变化和年降水量变化均显示出负面影响。 Ellenberg R指数的差异与Ellenberg N的差异高度相关,与氧化N的沉积呈负相关,这表明氧化N沉积对Ellenberg N缺乏显着的影响是因为它同时具有酸化和富营养化的作用,而氮沉积减少的影响主要是富营养化。我们的结果表明,氮的沉积,以及土地利用和降水的变化,已成为当地植物灭绝的重要驱动力。随着世界许多地方氮沉降的增加,其他地区可能会经历局部物种灭绝。

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