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首页> 外文期刊>Science of the total environment >Site conditions interact with litter quality to affect home-field advantage and rhizosphere effect of litter decomposition in a subtropical wetland ecosystem
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Site conditions interact with litter quality to affect home-field advantage and rhizosphere effect of litter decomposition in a subtropical wetland ecosystem

机译:网站条件与垃圾质量相互作用,影响亚热带湿地生态系统中凋落物分解的主场优势和根际效果

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The home-field advantage (HFA) hypothesis predicts that plant litter would decompose more quickly beneath its own plant species in the soil than beneath other plant species. Theoretically, HFA can be induced by the rhizosphere of growing plants, due to so-called rhizosphere effect (RE). Despite growing evidence for the site condition-dependence of both effects, few work has be conducted to explore how site climate, vegetation type and soil properties interact to affect RE and HFA, and especially limited in situ representation from subtropical wetland systems. In a field experiment, we reciprocally incubated three root litter species (Rumex dentatus L., Carex thunbergii Steud., and Polygonum cripolitartum Hance) along a hydroperiod gradient in a subtropical wetland, which differed mainly with respect to vegetation and soil microclimate, with and without growing plants. The occurrence and magnitude of HFA and RE were mainly determined by litter quality and were stage-specific. Collectively, we detected significant HFA with chemically-recalcitrant litter from C. thunbergii and P. cripolitanum, but only at the first stage of decomposition. The presence of growing plants generally reduced litter decomposition, but the magnitude of the response was species-specific, with the positive effects detected only for root litters from C. thunbergii at the first stage of decomposition. In addition, we did not find a significant relationship between HFA and RE, indicating that plant species that produce litters exhibiting HFA may not accelerate litter decomposition via RE at same time. Structural equation models (SEM) revealed that site microclimate factors were conducive with soil properties in regulating C dynamics. Overall, soil microclimate in this wetland ecosystem was likely important in driving C cycling, either directly by changing environmental conditions, litter quality, and plant trait spectra, or indirectly by interrupting the interactions between litter and decomposers.
机译:主场优势(HFA)假设预测,植物垃圾将在土壤中的植物种类下方比其他植物物种下方更快地分解。从理论上讲,由于所谓的根际效果(RE),种植植物的根际可以诱导HFA。尽管现场条件的证据依赖于两种效果,但甚至探索了如何探索地区气候,植被类型和土壤性质的相互作用,以影响Re和HFA,特别是亚热带湿地系统的原位表示。在野外实验中,我们在亚热带湿地中沿着亚热带湿地孵育三种根垃圾物种(Rumex Dentatus L.,Carex Thunbergii Steud,和Polygonum Cripolitartum Hance),其主要是关于植被和土壤微动物的植被和土壤微动物。没有种植的植物。 HFA和RE的发生和幅度主要由垃圾质量决定,并且是特异性的。统称,我们用来自C.Thunbergii和P.Ripolitanum的化学醋酸垃圾检测到显着的HFA,但仅在分解的第一阶段。生长植物的存在通常降低凋落物分解,但响应的幅度是特异性的,其仅针对来自C.Thunbergii的Root凋落物在分解的第一阶段检测到的正效应。此外,我们没有在HFA和RE之间找到重要的关系,表明产生凋落物的植物物种在表现出HFA的凋落物可以同时通过RE加速凋落物分解。结构方程模型(SEM)透露,现场微气候因子有利于调节C动力学的土壤性质。总体而言,这种湿地生态系统中的土壤微动物在驾驶C循环中可能是重要的,无论是通过改变环境条件,垃圾质量和植物特质光谱,还是间接地通过中断垃圾和分解器之间的相互作用间接。

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