壁酸
化学
氨基酸
氮气
食品科学
碳纤维
生物化学
有机化学
酶
材料科学
肽聚糖
复合材料
复合数
作者
Junxi Hu,Congde Huang,Shixing Zhou,Liu Xiong,Feike A. Dijkstra
标识
DOI:10.1016/j.soilbio.2021.108500
摘要
Increasing anthropogenic nitrogen (N) input has changed the global soil carbon (C) stock, yet the contribution of microbial necromass (amino sugars) to soil C with N addition is poorly understood. Here, we conducted a meta-analysis of 32 publications and evaluated the responses of microbial necromass to N addition. Our results showed that the overall effects of N addition significantly increased the fungal (glucosamine, GluN) and bacterial (muramic acid, MurN; galactosamine, GalN) necromass but did not significantly affect the total microbial necromass (total amino sugars). N addition effects on amino sugars were contingent on ecosystem type. In particular, N addition increased the contents of GluN, MurN, GalN, and total amino sugars in croplands, but in forests N addition only increased the contents of MurN. In croplands, the effects of N addition on microbial necromass depended on whether N was added alone or in combination with phosphorus (P) and potassium (K). Specifically, N addition alone did not significantly affect the contents of bacterial MurN and GalN, fungal GluN, and total amino sugars, while NPK addition significantly increased the contents of all individual (i.e., GluN, MurN, and GalN) and total amino sugars. In addition, high N addition rates (>150 kg N ha−1 yr−1), and long-term N addition (>10 years) significantly increased the contents of all individual and total amino sugars in croplands, possibly because of high N addition rates and long-term N addition may have stimulated microbial growth. Our results demonstrate that N addition increases microbial necromass in croplands and bacterial necromass in forests, providing critical information to improve the sequestration of microbially derived C with continued global anthropogenic N input.
科研通智能强力驱动
Strongly Powered by AbleSci AI