戴云山土壤微生物碳源利用效率的海拔变异规律及影响因素 |
摘要点击 6873 全文点击 969 投稿时间:2021-10-11 修订日期:2021-12-22 |
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中文关键词 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 |
英文关键词 temperature soil element stoichiometric ratio soil-microbial stoichiometric imbalance subtropical region montane forest |
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中文摘要 |
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,土壤微生物CUE的研究对深入认识土壤C循环过程十分重要.利用18 O-H2 O-DNA标记法,研究戴云山不同海拔(980~1765 m)天然林土壤微生物CUE、微生物生长速率(Cgrowth)和呼吸速率(Crespiration)的变化特征和影响机制.结果表明,微生物CUE在0.1~0.4之间变化,并随海拔升高而增加;微生物CUE与Cgrowth、Crespiration和单位微生物生长正相关,而与呼吸熵负相关,说明随海拔的增加,微生物通过增加个体生长和抑制个体呼吸来提高CUE;温度是影响CUE的主要因素,微生物CUE与温度负相关,说明随海拔增加,温度下降是促进土壤微生物CUE升高的关键因素. |
英文摘要 |
Microbial carbon use efficiency (CUE) refers to the C transformation to microbial biomass from C uptake. The study of soil microbial CUE is very important for understanding the soil C cycle. Here, CUE, Cgrowth, and Crespiration were measured using the 18O-H2O-DNA labeling method at six elevational sites (980-1765 m) in Daiyun Mountain, a subtropical montane forest, to understand the variation characteristics and influencing mechanisms. The results showed that: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; and temperature was the first controlling factor for the elevation variation in microbial CUE in the subtropical forest ecosystem. |