Zhu Kai, Chiariello Nona R, Tobeck Todd, Fukami Tadashi, Field Christopher B
Department of Global Ecology, Carnegie Institution for Science, Stanford, CA 94305; Department of Biology, Stanford University, Stanford, CA 94305; Department of BioSciences, Rice University, Houston, TX 77005;
Jasper Ridge Biological Preserve, Stanford University, Stanford, CA 94305.
Proc Natl Acad Sci U S A. 2016 Sep 20;113(38):10589-94. doi: 10.1073/pnas.1606734113. Epub 2016 Sep 6.
Global changes in climate, atmospheric composition, and pollutants are altering ecosystems and the goods and services they provide. Among approaches for predicting ecosystem responses, long-term observations and manipulative experiments can be powerful approaches for resolving single-factor and interactive effects of global changes on key metrics such as net primary production (NPP). Here we combine both approaches, developing multidimensional response surfaces for NPP based on the longest-running, best-replicated, most-multifactor global-change experiment at the ecosystem scale-a 17-y study of California grassland exposed to full-factorial warming, added precipitation, elevated CO2, and nitrogen deposition. Single-factor and interactive effects were not time-dependent, enabling us to analyze each year as a separate realization of the experiment and extract NPP as a continuous function of global-change factors. We found a ridge-shaped response surface in which NPP is humped (unimodal) in response to temperature and precipitation when CO2 and nitrogen are ambient, with peak NPP rising under elevated CO2 or nitrogen but also shifting to lower temperatures. Our results suggest that future climate change will push this ecosystem away from conditions that maximize NPP, but with large year-to-year variability.
气候、大气成分和污染物的全球变化正在改变生态系统及其提供的产品和服务。在预测生态系统响应的方法中,长期观测和操纵实验是解决全球变化对诸如净初级生产力(NPP)等关键指标的单因素和交互作用的有力方法。在这里,我们结合了这两种方法,基于生态系统尺度上运行时间最长、重复次数最多、因素最全面的全球变化实验——一项对加利福尼亚草地进行了17年的全因子变暖、增加降水、升高二氧化碳和氮沉降的研究,开发了NPP的多维响应面。单因素和交互作用不依赖于时间,这使我们能够将每年作为该实验的一个单独实现来进行分析,并将NPP提取为全球变化因素的连续函数。我们发现了一个脊状响应面,当二氧化碳和氮处于环境水平时,NPP对温度和降水呈驼峰状(单峰)响应,在二氧化碳或氮升高的情况下,NPP峰值上升,但也会向较低温度转移。我们的结果表明,未来气候变化将使这个生态系统偏离使NPP最大化的条件,但年际变化很大。