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大气沉积对英国植物物种丰富度的长期影响。

Long-term effects of atmospheric deposition on British plant species richness.

机构信息

UK Centre for Ecology & Hydrology, Lancaster Environment Centre, Lancaster LA1 4AP, UK.

Lancaster Environment Centre, Pentland Centre for Sustainability in Business, Lancaster University, Lancaster LA1 4YX, UK.

出版信息

Environ Pollut. 2021 Jul 15;281:117017. doi: 10.1016/j.envpol.2021.117017. Epub 2021 Mar 25.

DOI:10.1016/j.envpol.2021.117017
PMID:33813199
Abstract

The effects of atmospheric pollution on plant species richness (n) are of widespread concern. We carried out a modelling exercise to estimate how n in British semi-natural ecosystems responded to atmospheric deposition of nitrogen (N) and sulphur (S) between 1800 and 2010. We derived a simple four-parameter equation relating n to measured soil pH, and to net primary productivity (NPP), calculated with the N14CP ecosystem model. Parameters were estimated from a large data set (n = 1156) of species richness in four vegetation classes, unimproved grassland, dwarf shrub heath, peatland, and broadleaved woodland, obtained in 2007. The equation performed reasonably well in comparisons with independent observations of n. We used the equation, in combination with modelled estimates of NPP (from N14CP) and soil pH (from the CHUM-AM hydrochemical model), to calculate changes in average n over time at seven sites across Britain, assuming that variations in n were due only to variations in atmospheric deposition. At two of the sites, two vegetation classes were present, making a total of nine site/vegetation combinations. In four cases, n was affected about equally by pH and NPP, while in another four the effect of pH was dominant. The ninth site, a chalk grassland, was affected only by NPP, since soil pH was assumed constant. Our analysis suggests that the combination of increased NPP, due to fertilization by N, and decreased soil pH, primarily due to S, caused an average species loss of 39% (range 23-100%) between 1800 and the late 20th Century. The modelling suggests that in recent years n has begun to increase, almost entirely due to reductions in S and consequent increases in soil pH, but there are also indications of recent slight recovery from the eutrophying effects of N.

摘要

大气污染对植物物种丰富度(n)的影响受到广泛关注。我们进行了一项建模研究,以估计 1800 年至 2010 年间,英国半自然生态系统中 n 对氮(N)和硫(S)大气沉降的响应。我们根据四个植被类别的物种丰富度(n=1156)的大量数据集,使用 N14CP 生态系统模型计算出的实测土壤 pH 值和净初级生产力(NPP),推导出一个简单的四参数方程。参数是从四个植被类别的物种丰富度(n=1156)的大量数据集(n=1156)中估算出来的,这四个植被类别的数据是在 2007 年获得的,分别是未改良的草地、矮灌木石南荒地、泥炭地和阔叶林。该方程在与 n 的独立观测结果进行比较时表现相当良好。我们使用该方程,结合 N14CP 模型估算的 NPP(从 N14CP 模型中估算)和 CHUM-AM 水化学模型估算的土壤 pH 值,计算了英国七个地点随时间推移的平均 n 变化,假设 n 的变化仅归因于大气沉降的变化。在其中两个地点,存在两种植被类型,共有九个地点/植被组合。在四种情况下,n 受 pH 值和 NPP 的影响大致相同,而在另外四种情况下,pH 值的影响占主导地位。第九个地点是一个白垩草地,仅受 NPP 影响,因为假设土壤 pH 值保持不变。我们的分析表明,由于 N 的施肥作用导致 NPP 增加,以及由于 S 主要导致土壤 pH 值降低,导致 1800 年至 20 世纪后期物种平均损失 39%(范围 23-100%)。建模表明,近年来 n 开始增加,这几乎完全是由于 S 的减少和随之而来的土壤 pH 值的增加所致,但也有迹象表明,近年来由于 N 的富营养化效应,n 略有恢复。

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