生态系统
矿化(土壤科学)
氮气循环
生态学
陆地生态系统
生物量(生态学)
微生物
环境化学
生物地球化学循环
土壤生物学
生物
环境科学
农学
化学
土壤水分
氮气
细菌
遗传学
有机化学
作者
Paul Dijkstra,Corinne M. LaViolette,Jeffrey S. Coyle,Richard R. Doucett,Egbert Schwartz,Stephen C. Hart,Bruce A. Hungate
标识
DOI:10.1111/j.1461-0248.2008.01154.x
摘要
Abstract Organic carbon (C) and nitrogen (N) are essential for heterotrophic soil microorganisms, and their bioavailability strongly influences ecosystem C and N cycling. We show here that the natural 15 N abundance of the soil microbial biomass is affected by both the availability of C and N and ecosystem N processing. Microbial 15 N enrichment correlated negatively with the C : N ratio of the soil soluble fraction and positively with net N mineralization for ecosystems spanning semiarid, temperate and tropical climates, grassland and forests, and over four million years of ecosystem development. In addition, during soil incubation, large increases in microbial 15 N enrichment corresponded to high net N mineralization rates. These results support the idea that the N isotope composition of an organism is determined by the balance between N assimilation and dissimilation. Thus, 15 N enrichment of the soil microbial biomass integrates the effects of C and N availability on microbial metabolism and ecosystem processes.
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