Global synthesis on the response of soil microbial necromass carbon to climate‐smart agriculture

土壤碳 环境科学 固碳 生物量(生态学) 碳循环 温室气体 碳纤维 农学 生态系统 生态学 土壤水分 土壤科学 二氧化碳 生物 复合数 材料科学 复合材料
作者
Yüze Li,Shengnan Wang,Yang Ya-li,Liang Ren,Ziting Wang,Yuncheng Liao,Taiwen Yong
出处
期刊:Global Change Biology [Wiley]
卷期号:30 (5) 被引量:4
标识
DOI:10.1111/gcb.17302
摘要

Abstract Climate‐smart agriculture (CSA) supports the sustainability of crop production and food security, and benefiting soil carbon storage. Despite the critical importance of microorganisms in the carbon cycle, systematic investigations on the influence of CSA on soil microbial necromass carbon and its driving factors are still limited. We evaluated 472 observations from 73 peer‐reviewed articles to show that, compared to conventional practice, CSA generally increased soil microbial necromass carbon concentrations by 18.24%. These benefits to soil microbial necromass carbon, as assessed by amino sugar biomarkers, are complex and influenced by a variety of soil, climatic, spatial, and biological factors. Changes in living microbial biomass are the most significant predictor of total, fungal, and bacterial necromass carbon affected by CSA; in 61.9%–67.3% of paired observations, the CSA measures simultaneously increased living microbial biomass and microbial necromass carbon. Land restoration and nutrient management therein largely promoted microbial necromass carbon storage, while cover crop has a minor effect. Additionally, the effects were directly influenced by elevation and mean annual temperature, and indirectly by soil texture and initial organic carbon content. In the optimal scenario, the potential global carbon accrual rate of CSA through microbial necromass is approximately 980 Mt C year −1 , assuming organic amendment is included following conservation tillage and appropriate land restoration. In conclusion, our study suggests that increasing soil microbial necromass carbon through CSA provides a vital way of mitigating carbon loss. This emphasizes the invisible yet significant influence of soil microbial anabolic activity on global carbon dynamics.
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