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Shifts in plant functional community composition under hydrological stress strongly decelerate litter decomposition

机译:在水文压力下植物功能群落组成的转变强烈减速凋落物分解

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Litter decomposition is a key process of nutrient and carbon cycling in terrestrial ecosystems. The decomposition process will likely be altered under ongoing climate change, both through direct effects on decomposer activity and through indirect effects caused by changes in litter quality. We studied how hydrological change indirectly affects decomposition via plant functional community restructuring caused by changes in plant species’ relative abundances (community‐weighted mean (CWM) traits and functional diversity). We further assessed how those indirect litter quality effects compare to direct effects. We set up a mesocosm experiment, in which sown grassland communities and natural turf pieces were subjected to different hydrological conditions (dryness and waterlogging) for two growing seasons. Species‐level mean traits were obtained from trait databases and combined with species’ relative abundances to assess functional community restructuring. We studied decomposition of mixed litter from these communities in a common “litterbed.” These indirect effects were compared to effects of different hydrological conditions on soil respiration and on decomposition of standard litter (direct effects). Dryness reduced biomass production in sown communities and natural turf pieces, while waterlogging only reduced biomass in sown communities. Hydrological stress caused profound shifts in species’ abundances and consequently in plant functional community composition. Hydrologically stressed communities had higher CMW leaf dry matter content, lower CMW leaf nitrogen content, and lower functional diversity. Lower CWM leaf N content and functional diversity were strongly related to slower decomposition. These indirect effects paralleled direct effects, but were larger and longer‐lasting. Species mean traits from trait databases had therefore considerable predictive power for decomposition. Our results show that stressful soil moisture conditions, that are likely to occur more frequently in the future, quickly shift species’ abundances. The resulting functional community restructuring will decelerate decomposition under hydrological stress.
机译:凋落物分解是陆地生态系统中营养和碳循环的关键过程。通过对分解器活动的直接影响以及通过垃圾质量变化引起的间接影响,分解过程可能会在持续的气候变化下改变。我们研究了如何通过植物物种相对丰富的变化(社区加权平均值(CWM)特征和功能多样性)的植物功能社区重组间接影响水文变化如何影响分解。我们进一步评估了那些间接垃圾质量效应如何与直接效应进行比较。我们建立了一个Mesocosm实验,其中播种草原群落和天然草坪碎片对两个生长季节进行了不同的水文条件(干燥和涝渍)。物种级别的平均特征是从特征数据库获得的,并与物种的相对丰富相结合,以评估功能社区重组。我们研究了在普通的“垃圾箱”中的这些社区中混合垃圾的分解。将这些间接效应与不同水文条件对土壤呼吸的影响和标准垃圾分解(直接效应)进行比较。干燥在播种社区和天然草坪件中减少生物量产量,而涝渍仅减少生物量。水文应激引起物种丰度的深刻偏移,因此在植物功能群落组合物中。水文应激群落具有较高的CMW叶片干物质含量,较低的CMW叶片氮含量和较低的功能多样性。降低CWM叶N内容和功能多样性与较慢的分解强烈相关。这些间接效应平行直接效果,但持久较大。来自特征数据库的物种平均特征因此具有相当大的预测力量来分解。我们的研究结果表明,在未来的可能会频繁地发生压力土壤湿度条件,迅速换档物种丰富。由此产生的功能性群落重组将在水文压力下减速分解。

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