College of Life Sciences, Hebei University, Baoding, China.
International Joint Research Laboratory for Global Change Ecology, School of Life Sciences, Henan University, Kaifeng, China.
Nat Ecol Evol. 2019 Sep;3(9):1309-1320. doi: 10.1038/s41559-019-0958-3. Epub 2019 Aug 19.
Direct quantification of terrestrial biosphere responses to global change is crucial for projections of future climate change in Earth system models. Here, we synthesized ecosystem carbon-cycling data from 1,119 experiments performed over the past four decades concerning changes in temperature, precipitation, CO and nitrogen across major terrestrial vegetation types of the world. Most experiments manipulated single rather than multiple global change drivers in temperate ecosystems of the USA, Europe and China. The magnitudes of warming and elevated CO treatments were consistent with the ranges of future projections, whereas those of precipitation changes and nitrogen inputs often exceeded the projected ranges. Increases in global change drivers consistently accelerated, but decreased precipitation slowed down carbon-cycle processes. Nonlinear (including synergistic and antagonistic) effects among global change drivers were rare. Belowground carbon allocation responded negatively to increased precipitation and nitrogen addition and positively to decreased precipitation and elevated CO. The sensitivities of carbon variables to multiple global change drivers depended on the background climate and ecosystem condition, suggesting that Earth system models should be evaluated using site-specific conditions for best uses of this large dataset. Together, this synthesis underscores an urgent need to explore the interactions among multiple global change drivers in underrepresented regions such as semi-arid ecosystems, forests in the tropics and subtropics, and Arctic tundra when forecasting future terrestrial carbon-climate feedback.
直接量化陆地生物圈对全球变化的响应对于地球系统模型中未来气候变化的预测至关重要。在这里,我们综合了过去四十年间进行的 1119 项实验中的生态系统碳循环数据,这些实验涉及到世界主要陆地植被类型中温度、降水、CO 和氮的变化。大多数实验在中美欧的温带生态系统中只操纵了单一而非多种全球变化驱动因素。增温和 CO 处理的幅度与未来预测的范围一致,而降水变化和氮输入的幅度往往超过了预测的范围。全球变化驱动因素的增加一直加速,但降水减少减缓了碳循环过程。全球变化驱动因素之间的非线性(包括协同和拮抗)效应很少见。地下碳分配对增加的降水和氮添加呈负响应,对减少的降水和升高的 CO 呈正响应。碳变量对多种全球变化驱动因素的敏感性取决于背景气候和生态系统条件,这表明地球系统模型应该使用特定地点的条件进行评估,以充分利用这个大型数据集。总的来说,这一综合研究强调了在预测未来陆地碳-气候反馈时,迫切需要探索未被充分代表的地区(如半干旱生态系统、热带和亚热带森林以及北极苔原)中多种全球变化驱动因素之间的相互作用。