Saxe Henrik, Cannell Melvin G R, Johnsen Øystein, Ryan Michael G, Vourlitis George
Department of Economics and Natural Resources, Arboretum, The Royal Veterinary & Agricultural University, Hørsholm Kongevej 11, DK-2970 Hørsholm, Denmark.
Centre for Ecology and Hydrology, Bush Estate, Penicuik, Midlothian EH26 0QB, UK.
New Phytol. 2001 Mar;149(3):369-399. doi: 10.1046/j.1469-8137.2001.00057.x.
Although trees have responded to global warming in the past - to temperatures higher than they are now - the rate of change predicted in the 21st century is likely to be unprecedented. Greenhouse gas emissions could cause a 3-6°C increase in mean land surface temperature at high and temperate latitudes. Despite this, few experiments have isolated the effects of temperature for this scenario on trees and forests. This review focuses on tree and forest responses at boreal and temperate latitudes, ranging from the cellular to the ecosystem level. Adaptation to varying temperatures revolves around the trade-off between utilizing the full growing season and minimizing frost damage through proper timing of hardening in autumn and dehardening in spring. But the evolutionary change in these traits must be sufficiently rapid to compensate for the temperature changes. Many species have a positive response to increased temperature - but how close are we to the optima? Management is critical for a positive response of forest growth to a warmer climate, and selection of the best species for the new conditions will be of vital importance. Contents Summary 369 I. Introduction 370 II. Photosynthesis and respiration 370 III. Soil organic matter decomposition and mineralization 373 IV. Phenology and frost hardiness 376 V. Whole tree experimental responses to warming 380 VI. Changes in species distribution at warmer temperatures 381 VII. Adaptation and evolution 383 VIII. Ecosystem level responses to warming 387 Acknowledgements 390 References 390 Appendix I. Temperature response functions 399.
尽管树木在过去对全球变暖有过响应——当时的温度比现在更高——但21世纪预测的变化速度可能是前所未有的。温室气体排放可能导致高纬度和温带地区的陆地表面平均温度升高3-6摄氏度。尽管如此,很少有实验分离出这种情景下温度对树木和森林的影响。本综述聚焦于北方和温带地区从细胞水平到生态系统水平的树木和森林响应。适应温度变化围绕着在充分利用整个生长季节与通过秋季适当的硬化和春季脱硬化来最小化霜冻损害之间的权衡。但这些性状的进化变化必须足够迅速,以补偿温度变化。许多物种对温度升高有积极响应——但我们离最适温度有多近呢?管理对于森林生长对气候变暖的积极响应至关重要,选择最适合新条件的物种将至关重要。目录摘要369 一、引言370 二、光合作用与呼吸作用370 三、土壤有机质分解与矿化373 四、物候与抗冻性376 五、整株树木对变暖的实验响应380 六、温暖温度下物种分布的变化381 七、适应与进化383 八、生态系统水平对变暖的响应387 致谢390 参考文献390 附录一、温度响应函数399