State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing, China.
Earth and Biological Sciences Directorate, Ecosystem Sciences Team, Pacific Northwest National Laboratory, Richland, Washington.
Mol Ecol. 2018 Dec;27(24):5238-5251. doi: 10.1111/mec.14914. Epub 2018 Nov 25.
Belowground microbial communities strongly influence ecosystem function such that predicting function may rely on understanding ecological processes that assemble communities. Uncertainty remains, however, in what governs the relative contributions of different ecological processes. To help fill this knowledge gap, we test the general hypothesis that both initial state and degree of change in environmental conditions govern the relative contributions of different ecological assembly processes. To do so, we leveraged regional-scale nutrient and organic matter addition experiments and used soil organic matter (SOM) as a proxy of integrated soil environmental conditions. Consistent with our hypothesis, we found that both the initial amount of SOM and the degree of change in SOM-in response to nutrient addition-influenced the relative contributions of different ecological assembly processes. These influences were most clearly observed at the regional scale, suggesting potential scale dependence. More specifically, nutrient additions homogenized bacterial community composition due to enhanced influences of homogenizing dispersal when SOM content was initially high. In contrast, nutrient additions led to divergence in community composition due to variable selection when initial SOM was low and/or when SOM increased significantly in response to nutrient additions. Our findings indicate important connections among initial conditions, degree of change in environmental variables and microbial community assembly processes that may influence ecosystem processes. These conceptual inferences highlight a need to strengthen connections between ecological theory and biogeochemical modelling.
地下微生物群落强烈影响生态系统功能,因此预测功能可能依赖于理解组装群落的生态过程。然而,对于什么控制不同生态过程的相对贡献,仍然存在不确定性。为了帮助填补这一知识空白,我们检验了一个普遍假设,即环境条件变化的初始状态和程度决定了不同生态组装过程的相对贡献。为此,我们利用区域尺度的养分和有机质添加实验,并将土壤有机质 (SOM) 用作综合土壤环境条件的替代物。与我们的假设一致,我们发现 SOM 的初始量和 SOM 对养分添加的变化程度都影响了不同生态组装过程的相对贡献。这些影响在区域尺度上最为明显,表明存在潜在的尺度依赖性。更具体地说,养分添加由于初始 SOM 含量较高时均匀化扩散的影响增强,导致细菌群落组成均匀化。相比之下,当初始 SOM 较低且/或 SOM 因养分添加而显著增加时,养分添加会导致群落组成的分歧,这是由于可变选择的影响。我们的研究结果表明,初始条件、环境变量变化程度和微生物群落组装过程之间存在重要联系,这些联系可能影响生态系统过程。这些概念推断强调了加强生态理论和生物地球化学模型之间联系的必要性。