戴云山土壤微生物碳利用效率的海拔变异规律及影响因素
Elevational pattern and control factors of soil microbial carbon use efficiency in the Daiyun Mountain
微生物碳源利用效率 (CUE) 是指微生物将吸收的碳 (C) 转化为自身生物量C的效率,对土壤微生物CUE的量化及其影响机制的研究有利于深入认识土壤C循环过程及其对全球变化的响应。利用18O-H2O-DNA标记法,研究亚热带森林戴云山6个海拔梯度上的土壤微生物CUE、微生物生长速率 (Cgrowth)、呼吸速率 (Crespiration)和单位微生物生物量 (qGrowth) 及呼吸熵 (qCO2) 的海拔变异规律,分析微生物CUE、生长和呼吸与土壤有机碳 (C)、全氮(N) 和全磷 (P),微生物生物量碳、氮、磷和土壤-微生物计量不平衡的关系。结果表明:微生物CUE在0.1~0.4之间变化,并且随海拔升高呈线性增加;微生物CUE与Cgrowth、Crespiration和qGrowth正相关,而与qCO2负相关,说明随着海拔的增加,微生物通过同时增加个体生长和抑制个体呼吸的策略提高微生物CUE;逐步回归分析表明,微生物CUE与温度负相关,说明随着海拔的增加,温度的下降是促进土壤微生物CUE升高的主导因素。
Microbial carbon use efficiency (CUE) refers to the C transformation to microbial biomass from C uptake. Quantification of microbial CUE and its controlling factors can deepen our understanding of soil C cycle process and feedback to global change parameters. CUE, Cgrowth, Crespiration, qGrowth, qCO2 were measured by 18O-H2O-DNA labeling method at six elevational sites in the Daiyun Mountain, a subtropical montane forest, soil organic carbon, total nitrogen and phosphorus, microbial biomass carbon, nitrogen and phosphorus, stoichiometry imbalance of soil-microorganisms were measured to understand their controls on microbial CUE, microbial growth and respiration. We found: CUE varied from 0.1 to 0.4, and increased linearly with elevation; CUE was positively correlated with Cgrowth, Crespiration and qGrowth, but negatively correlated with qCO2, indicating that CUE increased with elevation by increasing microbial growth and inhibiting respiration; Stepwise regression analysis revealed that temperature was the first controlling factor for the elevation variation of microbial CUE in the subtropical forest ecosystem.
黄刚、苏延桂、王晶晶、吕坤
环境科学理论环境科学基础理论微生物学
温度土壤元素计量比土壤-微生物计量不平衡亚热带山地森林
temperaturesoil element stoichiometric ratiosoil-microbial stoichiometric imbalancesubtropical regionmontane forest
黄刚,苏延桂,王晶晶,吕坤.戴云山土壤微生物碳利用效率的海拔变异规律及影响因素[EB/OL].(2021-12-02)[2025-08-06].http://www.paper.edu.cn/releasepaper/content/202112-7.点此复制
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