添加氮条件下土壤胞外酶对土壤碳储量的驱动作用

Ji Chen, Xiao Chen, ומחן לֹשם, Robert Sinsabaugh, Moorhead Daryl L., Richard Bardgett, Nicolas Fanin, Andrew Nottingham
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引用次数: 0

摘要

人为氮输入增加可能对土壤有机碳循环产生重大影响。将富含物种的土壤微生物与特定的有机碳循环过程联系起来的一种方法是通过土壤胞外酶活性(EEAs)。通过对土壤c -降解EEAs对N添加的响应进行meta分析,我们的研究结果表明,N添加可使降解简单多糖的水解c -降解EEAs增加12.8%,而降解复杂酚类大分子的氧化c -降解EEAs减少11.9%。氮添加对土壤有机碳储量的净效应取决于两种碳降解EEAs之间的平衡,其影响在不同的生态系统类型中有所不同。我们的研究结果有助于确定氮添加下土壤微生物C利用策略的变化。将这种酶的影响纳入地球系统模型可以改善微生物过程的表征以及在变化的环境中对有机碳动态的预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Soil extracellular enzymes as drivers of soil carbon storage under nitrogen addition
Abstract Enhanced anthropogenic nitrogen (N) inputs to ecosystems may have substantial impacts on soil organic carbon (SOC) cycling. One way to link species-rich soil microorganisms with specific SOC cycling processes is via soil extracellular enzyme activities (EEAs). Here, by presenting a meta-analysis on the response of soil C-degrading EEAs to N addition, our results show that N addition increases hydrolytic C-degrading EEAs that target simple polysaccharides by 12.8%, but decreases oxidative C-degrading EEAs that degrade complex phenolic macromolecules by 11.9%. The net effect of N addition on SOC storage is determined by the balance between the two types of C-degrading EEAs, with impacts varying across different ecosystem types. Our results help identify changes in soil microbial C use strategies under N addition. Incorporating this enzymatic influence into Earth system models could improve the representation of microbial processes as well as predictions of SOC dynamics in a changing environment.
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