垃圾箱
生物群落
植物凋落物
生态学
环境科学
土壤碳
土壤生物学
温带森林
生态系统
背景(考古学)
土壤动物
碎石
自行车
温带气候
温带雨林
土壤有机质
陆地生态系统
无脊椎动物
动物群
营养循环
土壤质量
碳循环
有机质
土壤水分
生物
分解者
食物网
森林生态学
土层
表土
氮气循环
生物地球化学
碎屑岩
作者
Sergey M. Tsurikov,Andrew D. Barnes,Ulrich Brose,Felicity V. Crotty,Anton A. Goncharov,Anastasia Yu. Gorbunova,Fujio Hyodo,Malte Jochum,Bernhard Klarner,Daniil I. Korobushkin,Z L Li,Dana Liebke,I. I. Lyubechanskii,Melanie M. Pollierer,Di Ajeng Prameswari,Oksana L. Rozanova,Ruslan A. Saifutdinov,Nicole Scheunemann,Winda Ika Susanti,Irina V. Zenkova
摘要
ABSTRACT Soil fauna regulates litter decomposition and soil organic matter transformation, acting as both litter and microbial feeders. Whether these feeding modes shift along environmental gradients remains unclear. We tested if microbivory increases with decreasing litter quality and in colder climates, both factors limiting detritus digestion by fauna. Using stable isotope composition (δ 13 C, δ 15 N) of 7408 soil invertebrate samples from 228 forest sites across temperate to tropical biomes, we determined δ 15 N values are positively associated with litter C:N ratio and mean annual temperature, indicating a shift from detritivory toward microbivory under low litter quality with additional modulation by climate. In contrast, δ 13 C values showed no consistent association with litter C:N ratio or climate, reflecting context dependent microbial carbon routing. Our findings highlight litter quality as the primary driver of the detritivory‐to‐microbivory shift in soil fauna, with implications for predicting changes in climate and plant communities on carbon cycling in terrestrial ecosystems.
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