B-WARE Research Centre, Radboud University Nijmegen, P.O. Box 9010, 6500 GL Nijmegen, The Netherlands.
Ecol Appl. 2010 Jan;20(1):30-59. doi: 10.1890/08-1140.1.
Atmospheric nitrogen (N) deposition is a recognized threat to plant diversity in temperate and northern parts of Europe and North America. This paper assesses evidence from field experiments for N deposition effects and thresholds for terrestrial plant diversity protection across a latitudinal range of main categories of ecosystems, from arctic and boreal systems to tropical forests. Current thinking on the mechanisms of N deposition effects on plant diversity, the global distribution of G200 ecoregions, and current and future (2030) estimates of atmospheric N-deposition rates are then used to identify the risks to plant diversity in all major ecosystem types now and in the future. This synthesis paper clearly shows that N accumulation is the main driver of changes to species composition across the whole range of different ecosystem types by driving the competitive interactions that lead to composition change and/or making conditions unfavorable for some species. Other effects such as direct toxicity of nitrogen gases and aerosols, long-term negative effects of increased ammonium and ammonia availability, soil-mediated effects of acidification, and secondary stress and disturbance are more ecosystem- and site-specific and often play a supporting role. N deposition effects in mediterranean ecosystems have now been identified, leading to a first estimate of an effect threshold. Importantly, ecosystems thought of as not N limited, such as tropical and subtropical systems, may be more vulnerable in the regeneration phase, in situations where heterogeneity in N availability is reduced by atmospheric N deposition, on sandy soils, or in montane areas. Critical loads are effect thresholds for N deposition, and the critical load concept has helped European governments make progress toward reducing N loads on sensitive ecosystems. More needs to be done in Europe and North America, especially for the more sensitive ecosystem types, including several ecosystems of high conservation importance. The results of this assessment show that the vulnerable regions outside Europe and North America which have not received enough attention are ecoregions in eastern and southern Asia (China, India), an important part of the mediterranean ecoregion (California, southern Europe), and in the coming decades several subtropical and tropical parts of Latin America and Africa. Reductions in plant diversity by increased atmospheric N deposition may be more widespread than first thought, and more targeted studies are required in low background areas, especially in the G200 ecoregions.
大气氮(N)沉积是温带和欧洲北部及北美的植物多样性面临的一个公认威胁。本文评估了来自田间实验的证据,以了解在从北极和北方系统到热带森林的主要生态系统类别纬度范围内,陆地植物多样性保护的 N 沉积效应和阈值。然后,利用当前关于 N 沉积对植物多样性影响的机制的认识、G200 生态区的全球分布以及当前和未来(2030 年)大气 N 沉积速率的估计,来确定现在和未来(2030 年)所有主要生态系统类型中植物多样性面临的风险。这篇综述文章清楚地表明,N 积累是通过驱动导致组成变化和/或使某些物种条件不利的竞争相互作用,成为不同生态系统类型物种组成变化的主要驱动因素。其他影响,如氮气体和气溶胶的直接毒性、增加的铵和氨可用性的长期负面影响、酸化的土壤介导效应以及次生胁迫和干扰,更具生态系统和地点特异性,通常起辅助作用。现在已经确定了地中海生态系统中的 N 沉积效应,从而首次估计了一个效应阈值。重要的是,被认为不受 N 限制的生态系统,如热带和亚热带系统,在再生阶段可能更加脆弱,在这种情况下,大气 N 沉积减少了 N 可用性的异质性,在沙质土壤上或在山区。临界负荷是 N 沉积的效应阈值,临界负荷概念帮助欧洲政府在减少敏感生态系统上的 N 负荷方面取得了进展。欧洲和北美,特别是包括几个具有高保护价值的生态系统在内的更敏感的生态系统类型,还需要做更多的工作。这项评估的结果表明,欧洲和北美以外没有得到足够重视的脆弱地区是东亚和南亚(中国、印度)的生态区、地中海生态区的重要部分(加利福尼亚、南欧),以及未来几十年拉丁美洲和非洲的几个亚热带和热带地区。由于大气 N 沉积增加而导致的植物多样性减少可能比最初认为的更为广泛,需要在低背景地区,特别是在 G200 生态区进行更有针对性的研究。