人类受精
分解
化学
环境化学
土壤碳
土壤有机质
土壤水分
化学分解过程
氮气
营养物
亚热带
微生物
微生物种群生物学
氮气循环
农学
微观世界
碳纤维
环境科学
磷
碳循环
总有机碳
固碳
土壤生物学
异养
矿化(土壤科学)
野外试验
水槽(地理)
土壤化学
孵化
作者
Yanli Jing,Jing Li,Xuechao Zhao,Peng Tian,Jiaping Yang,Yan Li,Qingkui Wang
摘要
Microbial necromass is an important contributor to soil organic carbon (C) in subtropical forests. However, how microbial necromass decomposition responds to nitrogen (N) fertilization and whether this process depends on phosphorus (P) availability remain poorly understood. This study assessed the impact of long-term N fertilization and P addition on microbial necromass decomposition using soils collected from a subtropical Cunninghamia lanceolata forest. We combined a seven-year field N fertilization experiment with a laboratory incubation using 13C-labeled microbial necromass. We found that N fertilization accelerated decomposition of the fast degradable pool by 54.3% while reducing its proportional size by 66.9%, indicating intensified microbial processing of readily available C. This shift was mechanistically linked to N-induced relative microbial C limitation, evidenced by depleted dissolved organic C, elevated oxidase activities, and microbial communities shifted toward taxa favoring labile substrates (e.g. increased Rozellomycota and decreased Basidiomycota). Moreover, P addition moderated N effects on stable pool decomposition, resulting in more necromass-13C retention in N + P than N-only treatments at the end of incubation. These findings demonstrate that N enrichment accelerates the turnover of the fast degradable necromass pool through inducing microbial C limitation. Our study reveals that microbial necromass constitutes a vulnerable C sink under N enrichment, suggesting that N-driven acceleration of decomposition may reduce soil C sequestration capacity in subtropical forests, which could be mitigated by concurrent P addition.
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