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关键微生物类群对凋落物微养分和常量化学物质的响应决定了造林后农业土壤的激发强度。

The Response of Critical Microbial Taxa to Litter Micro-Nutrients and Macro-Chemistry Determined the Agricultural Soil Priming Intensity After Afforestation.

作者信息

Yang Hongling, Li Yulin, Wang Shaokun, Zhan Jin, Ning Zhiying, Han Dan

机构信息

Naiman Desertification Research Station, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences (CAS), Lanzhou, China.

College of Resources and Environment, University of Chinese Academy of Sciences, Beijing, China.

出版信息

Front Microbiol. 2021 Sep 16;12:730117. doi: 10.3389/fmicb.2021.730117. eCollection 2021.

Abstract

Afforestation with trees and shrubs around cropland can effectively decrease soil degradation and avoid sand storms, but subsequent modification of litter quality accelerates the degradation of native organic matter the soil priming effect (PE). Although carbon accumulation in agricultural soils after afforestation was widely studied, little is known about the extent to which soil organic carbon (SOC) mineralization is induced by complex residue input in agro-forest-grass composite ecosystems. Here, we mixed corn field soil and litter of afforestation tree and shrub species together in a micro-environment to quantify the effects of litter-mixture input on farmland soil priming associated with afforestation. Additionally, we studied the responses of bacterial and fungal species to litter chemistry, with the aim to identify the litter and microbial driver of soil priming. The results showed that soil priming was accelerated by different litter addition which varied from 24 to 74% of SOC mineralization, suggesting that priming intensity was relatively flexible and highly affected by litter quality. We also find that the macro-chemistry (including litter carbon, nitrogen, lignin, and cellulose) directly affects priming intensity, while micro-chemistry (including litter soluble sugar, water-soluble phenol, methanol-soluble phenol, and condensed tannin) indirectly influences priming alteration to dominant bacterial taxa. The stepwise regression analysis suggested that litter nitrogen and cellulose were the critical litter drivers to soil priming ( = 0.279), and the combination of bacterial phylum , , , , and fungal taxa was a great model to explain the priming intensity ( = 0.407).

摘要

在农田周围种植树木和灌木可以有效减少土壤退化并避免沙尘暴,但随后凋落物质量的改变会加速原生土壤有机质的降解,即土壤激发效应(PE)。尽管造林后农业土壤中的碳积累已得到广泛研究,但对于农林草复合生态系统中复杂残体输入诱导土壤有机碳(SOC)矿化的程度却知之甚少。在这里,我们在微环境中将玉米田土壤与造林树木和灌木物种的凋落物混合在一起,以量化凋落物混合输入对与造林相关的农田土壤激发效应的影响。此外,我们研究了细菌和真菌物种对凋落物化学性质的响应,旨在确定土壤激发效应的凋落物和微生物驱动因素。结果表明,不同的凋落物添加加速了土壤激发效应,其范围为SOC矿化的24%至74%,这表明激发强度相对灵活且受凋落物质量的影响很大。我们还发现,宏观化学性质(包括凋落物碳、氮、木质素和纤维素)直接影响激发强度,而微观化学性质(包括凋落物可溶性糖、水溶性酚、甲醇溶性酚和缩合单宁)则通过改变优势细菌类群间接影响激发效应。逐步回归分析表明,凋落物氮和纤维素是土壤激发效应的关键凋落物驱动因素(R² = 0.279),细菌门、、、、和真菌类群的组合是解释激发强度的一个很好的模型(R² = 0.407)。

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