Niklaus P A, Alphei J, Kampichler C, Kandeler E, Körner C, Tscherko D, Wohlfender M
Institute of Botany, Schönbeinstrasse 6, University of Basel, CH-4056 Basel, Switzerland.
Ecology. 2007 Dec;88(12):3153-63. doi: 10.1890/06-2100.1.
Terrestrial ecosystems consist of mutually dependent producer and decomposer subsystems, but not much is known on how their interactions are modified by plant diversity and elevated atmospheric CO2 concentrations. Factorially manipulating grassland plant species diversity and atmospheric CO2 concentrations for five years, we tested whether high diversity or elevated CO2 sustain larger or more active soil communities, affect soil aggregation, water dynamics, or nutrient cycling, and whether plant diversity and elevated CO2 interact. Nitrogen (N) and phosphorus (P) pools, symbiotic N2 fixation, plant litter quality, soil moisture, soil physical structure, soil nematode, collembola and acari communities, soil microbial biomass and microflora community structure (phospholipid fatty acid [PLFA] profiles), soil enzyme activities, and rates of C fluxes to soils were measured. No increases in soil C fluxes or the biomass, number, or activity of soil organisms were detected at high plant diversity; soil H2O and aggregation remained unaltered. Elevated CO2 affected the ecosystem primarily by improving plant and soil water status by reducing leaf conductance, whereas changes in C cycling appeared to be of subordinate importance. Slowed-down soil drying cycles resulted in lower soil aggregation under elevated CO2. Collembola benefited from extra soil moisture under elevated CO2, whereas other faunal groups did not respond. Diversity effects and interactions with elevated CO2 may have been absent because soil responses were mainly driven by community-level processes such as rates of organic C input and water use; these drivers were not changed by plant diversity manipulations, possibly because our species diversity gradient did not extend below five species and because functional type composition remained unaltered. Our findings demonstrate that global change can affect soil aggregation, and we advocate that soil aggregation should be considered as a dynamic property that may respond to environmental changes and feed back on other ecosystem functions.
陆地生态系统由相互依存的生产者和分解者子系统组成,但对于植物多样性和大气二氧化碳浓度升高如何改变它们之间的相互作用,我们了解得并不多。通过对草地植物物种多样性和大气二氧化碳浓度进行五年的析因操纵,我们测试了高多样性或高二氧化碳浓度是否能维持更大或更活跃的土壤群落、影响土壤团聚、水分动态或养分循环,以及植物多样性和高二氧化碳浓度是否会相互作用。我们测量了氮(N)和磷(P)库、共生固氮、植物凋落物质量、土壤湿度、土壤物理结构、土壤线虫、弹尾虫和螨类群落、土壤微生物生物量和微生物群落结构(磷脂脂肪酸[PLFA]谱)、土壤酶活性以及碳通量进入土壤的速率。在高植物多样性水平下,未检测到土壤碳通量或土壤生物的生物量、数量或活性增加;土壤水分和团聚状况未发生改变。高二氧化碳浓度主要通过降低叶片导度来改善植物和土壤的水分状况,从而影响生态系统,而碳循环的变化似乎次要。在高二氧化碳浓度下,土壤干燥周期减缓导致土壤团聚程度降低。弹尾虫受益于高二氧化碳浓度下额外的土壤湿度,而其他动物类群则无反应。可能由于土壤响应主要由群落水平的过程驱动,如有机碳输入速率和水分利用,而这些驱动因素并未因植物多样性操纵而改变,这可能是因为我们的物种多样性梯度未延伸至五个物种以下,且功能类型组成保持不变,所以未观察到多样性效应以及与高二氧化碳浓度的相互作用。我们的研究结果表明,全球变化会影响土壤团聚,我们主张应将土壤团聚视为一种动态属性,它可能对环境变化做出响应并反馈于其他生态系统功能。