Institute of Environmental Sustainability, Loyola University Chicago, Chicago, Illinois.
Department of Plant and Microbial Biology, University of Minnesota, St Paul, Minnesota.
Glob Chang Biol. 2019 Mar;25(3):885-899. doi: 10.1111/gcb.14541. Epub 2019 Jan 6.
Understanding the effects of global change in terrestrial communities requires an understanding of how limiting resources interact with plant traits to affect productivity. Here, we focus on nitrogen and ask whether plant community nitrogen uptake rate is determined (a) by nitrogen availability alone or (b) by the product of nitrogen availability and fine-root mass. Surprisingly, this is not empirically resolved. We performed controlled microcosm experiments and reanalyzed published pot experiments and field data to determine the relationship between community-level nitrogen uptake rate, nitrogen availability, and fine-root mass for 46 unique combinations of species, nitrogen levels, and growing conditions. We found that plant community nitrogen uptake rate was unaffected by fine-root mass in 63% of cases and saturated with fine-root mass in 29% of cases (92% in total). In contrast, plant community nitrogen uptake rate was clearly affected by nitrogen availability. The results support the idea that although plants may over-proliferate fine roots for individual-level competition, it comes without an increase in community-level nitrogen uptake. The results have implications for the mechanisms included in coupled carbon-nitrogen terrestrial biosphere models (CN-TBMs) and are consistent with CN-TBMs that operate above the individual scale and omit fine-root mass in equations of nitrogen uptake rate but inconsistent with the majority of CN-TBMs, which operate above the individual scale and include fine-root mass in equations of nitrogen uptake rate. For the much smaller number of CN-TBMs that explicitly model individual-based belowground competition for nitrogen, the results suggest that the relative (not absolute) fine-root mass of competing individuals should be included in the equations that determine individual-level nitrogen uptake rates. By providing empirical data to support the assumptions used in CN-TBMs, we put their global climate change predictions on firmer ground.
理解全球变化对陆地群落的影响需要了解限制资源如何与植物特性相互作用,从而影响生产力。在这里,我们关注氮,并探讨植物群落氮吸收速率是由氮供应单独决定(a)还是由氮供应和细根质量的乘积决定(b)。令人惊讶的是,这一问题尚未得到经验性解决。我们进行了控制微宇宙实验,并重新分析了已发表的盆栽实验和野外数据,以确定 46 种独特物种组合、氮水平和生长条件下群落水平氮吸收速率、氮供应和细根质量之间的关系。我们发现,在 63%的情况下,植物群落氮吸收速率不受细根质量的影响,在 29%的情况下,细根质量达到饱和(总计 92%)。相比之下,植物群落氮吸收速率明显受到氮供应的影响。研究结果支持以下观点,即尽管植物可能为个体竞争过度增殖细根,但这并不会增加群落水平的氮吸收。研究结果对耦合碳氮陆地生物圈模型(CN-TBM)中包含的机制具有启示意义,与在个体尺度上运行且在氮吸收速率方程中忽略细根质量的 CN-TBM 一致,但与在个体尺度上运行且在氮吸收速率方程中包含细根质量的大多数 CN-TBM 不一致。对于极少数明确模拟氮个体地下竞争的 CN-TBM,研究结果表明,应将竞争个体的相对(而非绝对)细根质量纳入确定个体水平氮吸收速率的方程中。通过提供支持 CN-TBM 中使用的假设的经验数据,我们使它们的全球气候变化预测更加可靠。