生物地球化学循环
环境科学
土壤碳
陆地生态系统
生物量(生态学)
生态系统
生物地球化学
磷
碳循环
自行车
营养循环
全球变化
氮气循环
营养物
环境化学
土壤科学
氮气
生态学
土壤水分
化学
林业
生物
气候变化
地理
有机化学
作者
Zhiqiang Wang,Mengying Zhao,Zhengbing Yan,Yuanhe Yang,Karl J. Niklas,Heng Huang,Tserang Donko Mipam,Xianjin He,Huifeng Hu,S. Joseph Wright
出处
期刊:Catena
[Elsevier]
日期:2022-01-20
卷期号:211: 106037-106037
被引量:45
标识
DOI:10.1016/j.catena.2022.106037
摘要
Soil microbes play key roles in driving and regulating nutrient cycling in terrestrial ecosystems. However, a lack of global-scale information regarding the distribution of soil microbial biomass carbon (SMB C), nitrogen (SMB N), and phosphorus (SMB P) in terrestrial ecosystems has limited our ability to incorporate the broad-scale soil microbial nutritional properties and the associated processes into biogeochemical models. Here, we synthesized a global dataset including 3801 observations for SMB C, 3154 observations of SMB N, and 2429 observations of SMB P in the top 0–30 cm soil depth. Based on this comprehensive global dataset, we generated quantitative and spatially explicit maps of SMB C, N, and P across terrestrial ecosystems using a random forest approach. We also quantified the relative importance of multiple environmental variables in predicting the spatial variation of SMB C, N, and P concentrations and then made further predictions at a global scale. Soil organic carbon (SOC) was the most important factor in predicting SMB C, N, and P at a global scale. At the global scale, the storage of SMB C, N, and P were estimated to be 23.13 Pg C, 3.93 Pg N and 2.16 Pg P in the top 0–30 cm soil surface, respectively. Our global maps of SMB C, N, and P presented here can be used to constraint Earth system models, and provide the first step forward to predict the roles of soil microbial nutrients in terrestrial nutrient cycling.
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