Carter Therese S, Clark Christopher M, Fenn Mark E, Jovan Sarah, Perakis Steven S, Riddell Jennifer, Schaberg Paul G, Greaver Tara L, Hastings Meredith G
US Global Change Research Program, ICF Contractor, 1800 G Street NW, Suite 9100, Washington, D.C. 20006 USA.
Department of Chemistry, Brown University, 324 Brook Street, Providence, Rhode Island 02912 USA.
Ecosphere. 2017 Mar 1;8(3). doi: 10.1002/ecs2.1717.
We review the mechanisms of deleterious nitrogen (N) deposition impacts on temperate forests, with a particular focus on trees and lichens. Elevated anthropogenic N deposition to forests has varied effects on individual organisms depending on characteristics both of the N inputs (form, timing, amount) and of the organisms (ecology, physiology) involved. Improved mechanistic knowledge of these effects can aid in developing robust predictions of how organisms respond to either increases or decreases in N deposition. Rising N levels affect forests in micro- and macroscopic ways from physiological responses at the cellular, tissue, and organism levels to influencing individual species and entire communities and ecosystems. A synthesis of these processes forms the basis for the overarching themes of this paper, which focuses on N effects at different levels of biological organization in temperate forests. For lichens, the mechanisms of direct effects of N are relatively well known at cellular, organismal, and community levels, though interactions of N with other stressors merit further research. For trees, effects of N deposition are better understood for N as an acidifying agent than as a nutrient; in both cases, the impacts can reflect direct effects on short time scales and indirect effects mediated through long-term soil and belowground changes. There are many gaps on fundamental N use and cycling in ecosystems, and we highlight the most critical gaps for understanding potential deleterious effects of N deposition. For lichens, these gaps include both how N affects specific metabolic pathways and how N is metabolized. For trees, these gaps include understanding the direct effects of N deposition onto forest canopies, the sensitivity of different tree species and mycorrhizal symbionts to N, the influence of soil properties, and the reversibility of N and acidification effects on plants and soils. Continued study of how these N response mechanisms interact with one another, and with other dimensions of global change, remains essential for predicting ongoing changes in lichen and tree populations across North American temperate forests.
我们回顾了有害氮(N)沉降对温带森林影响的机制,特别关注树木和地衣。森林中人为氮沉降的增加对个体生物有不同影响,这取决于氮输入的特征(形式、时间、数量)以及所涉及生物的特征(生态学、生理学)。对这些影响的机制有更深入的了解有助于更准确地预测生物对氮沉降增加或减少的反应。氮水平的上升从细胞、组织和生物体水平的生理反应到影响单个物种以及整个群落和生态系统,以微观和宏观方式影响森林。对这些过程的综合构成了本文总体主题的基础,本文重点关注温带森林中不同生物组织水平上的氮影响。对于地衣,尽管氮与其他压力源的相互作用值得进一步研究,但在细胞、生物体和群落水平上,氮的直接影响机制相对较为人所知。对于树木,与氮作为一种营养物质相比,人们对其作为酸化剂的影响了解得更好;在这两种情况下,影响都可能反映出短时间尺度上的直接影响以及通过长期土壤和地下变化介导的间接影响。在生态系统中,关于氮的基本利用和循环存在许多空白,我们强调了理解氮沉降潜在有害影响的最关键空白。对于地衣,这些空白包括氮如何影响特定代谢途径以及氮是如何被代谢的。对于树木,这些空白包括了解氮沉降对森林冠层的直接影响、不同树种和菌根共生体对氮的敏感性、土壤性质的影响以及氮和酸化对植物和土壤影响的可逆性。持续研究这些氮响应机制如何相互作用,以及与全球变化的其他方面相互作用,对于预测北美温带森林中地衣和树木种群的持续变化仍然至关重要。