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温带森林中生物多样性对土壤呼吸的季节影响

Seasonal Influence of Biodiversity on Soil Respiration in a Temperate Forest.

作者信息

Zhang Mengxu, Sayer Emma J, Zhang Weidong, Ye Ji, Yuan Zuoqiang, Lin Fei, Hao Zhanqing, Fang Shuai, Mao Zikun, Ren Jing, Wang Xugao

机构信息

CAS Key Laboratory of Forest Ecology and Management, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China.

University of Chinese Academy of Sciences, Beijing 100049, China.

出版信息

Plants (Basel). 2022 Dec 5;11(23):3391. doi: 10.3390/plants11233391.

Abstract

Soil respiration in forests contributes to significant carbon dioxide emissions from terrestrial ecosystems but it varies both spatially and seasonally. Both abiotic and biotic factors influence soil respiration but their relative contribution to spatial and seasonal variability remains poorly understood, which leads to uncertainty in models of global C cycling and predictions of future climate change. Here, we hypothesize that tree diversity, soil diversity, and soil properties contribute to local-scale variability of soil respiration but their relative importance changes in different seasons. To test our hypothesis, we conducted seasonal soil respiration measurements along a local-scale environmental gradient in a temperate forest in Northeast China, analyzed spatial variability of soil respiration and tested the relationships between soil respiration and a variety of abiotic and biotic factors including topography, soil chemical properties, and plant and soil diversity. We found that soil respiration varied substantially across the study site, with spatial coefficients of variation (CV) of 29.1%, 27.3% and 30.8% in spring, summer, and autumn, respectively. Soil respiration was consistently lower at high soil water content, but the influence of other factors was seasonal. In spring, soil respiration increased with tree diversity and biomass but decreased with soil fungal diversity. In summer, soil respiration increased with soil temperature, whereas in autumn, soil respiration increased with tree diversity but decreased with increasing soil nutrient content. However, soil nutrient content indirectly enhanced soil respiration via its effect on tree diversity across seasons, and forest stand structure indirectly enhanced soil respiration via tree diversity in spring. Our results highlight that substantial differences in soil respiration at local scales was jointly explained by soil properties (soil water content and soil nutrients), tree diversity, and soil fungal diversity but the relative importance of these drivers varied seasonally in our temperate forest.

摘要

森林中的土壤呼吸是陆地生态系统中二氧化碳排放的重要组成部分,但其在空间和季节上存在差异。非生物和生物因素都对土壤呼吸有影响,但其对空间和季节变化的相对贡献仍知之甚少,这导致全球碳循环模型和未来气候变化预测存在不确定性。在此,我们假设树木多样性、土壤多样性和土壤性质会导致土壤呼吸的局部尺度变化,但其相对重要性在不同季节会发生变化。为了验证我们的假设,我们在中国东北温带森林的局部尺度环境梯度上进行了季节性土壤呼吸测量,分析了土壤呼吸的空间变异性,并测试了土壤呼吸与各种非生物和生物因素之间的关系,这些因素包括地形、土壤化学性质以及植物和土壤多样性。我们发现,整个研究区域的土壤呼吸差异很大,春季、夏季和秋季的空间变异系数(CV)分别为29.1%、27.3%和30.8%。在高土壤含水量条件下,土壤呼吸始终较低,但其他因素的影响具有季节性。在春季,土壤呼吸随树木多样性和生物量的增加而增加,但随土壤真菌多样性的增加而降低。在夏季,土壤呼吸随土壤温度的升高而增加,而在秋季,土壤呼吸随树木多样性的增加而增加,但随土壤养分含量的增加而降低。然而,土壤养分含量通过其对不同季节树木多样性的影响间接增强了土壤呼吸,而林分结构在春季通过树木多样性间接增强了土壤呼吸。我们的结果表明,局部尺度上土壤呼吸的显著差异是由土壤性质(土壤含水量和土壤养分)、树木多样性和土壤真菌多样性共同解释的,但在我们的温带森林中,这些驱动因素的相对重要性随季节而变化。

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