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Above- and belowground carbon inputs affect seasonal variations of soil microbial biomass in a subtropical monsoon forest of southwest China

机译:地上和地下碳输入影响西南亚热带季风森林土壤微生物生物量的季节性变化

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摘要

Soil microbial activity drives carbon and nutrient cycling in terrestrial ecosystems. Soil microbial biomass is commonly limited by environmental factors and soil carbon availability. We employed plant litter removal, root trenching and stem-girdling treatments to examine the effects of environmental factors, above- and belowground carbon inputs on soil microbial C in a subtropical monsoon forest in southwest China. During the experimental period from July 2006 through April 2007, 2 years after initiation of the treatments, microbial biomass C in the humus layer did not vary with seasonal changes in soil temperature or water content. Mineral soil microbial C decreased throughout the experimental period and varied with soil temperature and water content. Litter removal reduced mineral soil microbial C by 19.0% in the ungirdled plots, but only 4.0% in girdled plots. Root trenching, stem girdling and their interactions influenced microbial C in humus layer. Neither root trenching nor girdling significantly influenced mineral soil microbial C. Mineral soil microbial C correlated with following-month plant litterfall in control plots, but these correlations were not observed in root-trenching plots or girdling plots. Our results suggest that belowground carbon retranslocated from shoots and present in soil organic matter, rather than aboveground fresh plant litter inputs, determines seasonal fluctuation of mineral soil microbial biomass.
机译:土壤微生物活动推动了陆地生态系统中的碳和养分循环。土壤微生物生物量通常受环境因素和土壤碳利用率的限制。我们采用了植物凋落物去除,根部挖沟和茎环处理的方法,研究了环境因子,地上和地下碳输入对西南亚热带季风森林土壤微生物碳的影响。在2006年7月至2007年4月的实验期内,即开始处理2年后,腐殖质层中的微生物生物量C不会随土壤温度或水含量的季节性变化而变化。在整个实验期间,矿质土壤微生物碳含量下降,并且随土壤温度和水分含量的变化而变化。去除垃圾后,在未耕地的地块中矿物质土壤中的微生物C减少了19.0%,但在散落地的地块中仅降低了4.0%。根沟,茎环和它们的相互作用影响腐殖质层中的微生物碳。根部开沟和环剥都没有显着影响矿质土壤微生物C。矿质土壤微生物C与控制区次月的植物凋落率相关,但是在根部沟壑或环剥环境中没有观察到这些相关性。我们的结果表明,地下碳从新芽中转移出来并存在于土壤有机质中,而不是地上新鲜的植物凋落物输入,决定了矿质土壤微生物生物量的季节性波动。

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