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土壤微生物中养分限制的全球模式。

Global patterns of nutrient limitation in soil microorganisms.

作者信息

Cui Yongxing, Peng Shushi, Rillig Matthias C, Camenzind Tessa, Delgado-Baquerizo Manuel, Terrer César, Xu Xiaofeng, Feng Maoyuan, Wang Mengjie, Fang Linchuan, Zhu Biao, Du Enzai, Moorhead Daryl L, Sinsabaugh Robert L, Peñuelas Josep, Elser James J

机构信息

Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.

Department of Biology, Chemistry, and Pharmacy, Institute of Biology, Freie Universität Berlin, Berlin 14195, Germany.

出版信息

Proc Natl Acad Sci U S A. 2025 May 20;122(20):e2424552122. doi: 10.1073/pnas.2424552122. Epub 2025 May 13.

Abstract

The availability of nitrogen (N) and phosphorus (P) is essential for soil microbial activity and growth, yet global patterns of N and P limitation in soil microbial metabolism remain largely unknown. We modeled ecoenzyme stoichiometry data from 5,259 field observations of natural ecosystems to assess microbial N and P limitation in global surface soils. We found that microbial P limitation, which was especially strong at low latitudes, was more prevalent globally than microbial N limitation, which prevailed in cold environments. We also found widespread N and P colimitation in soil microorganisms in the tropics, contradicting the long-held paradigm that P, and not N, is the primary limiting nutrient at low latitudes. This colimitation could be attributable to elevated microbial N demand for the synthesis of P-acquiring enzymes under P limitation. Upscaling (0.1 × 0.1° spatial resolution) suggested that soil microorganisms were limited by N and P in 39% and 57%, respectively, of natural terrestrial surface areas, with 21% of areas with N and P colimitation. As a global assessment of spatial variation in microbial N and P limitation, our results highlight the importance of N availability in supporting microbial P acquisition at low latitudes and improve our understanding of microbial nutrient limitation on a global scale.

摘要

氮(N)和磷(P)的有效性对于土壤微生物的活动和生长至关重要,然而土壤微生物代谢中N和P限制的全球模式仍 largely 未知。我们对来自5259个自然生态系统实地观测的生态酶化学计量数据进行建模,以评估全球表层土壤中微生物的N和P限制。我们发现,微生物P限制在低纬度地区尤为强烈,在全球范围内比微生物N限制更为普遍,微生物N限制在寒冷环境中占主导。我们还发现热带地区土壤微生物中普遍存在N和P共同限制,这与长期以来认为在低纬度地区P而非N是主要限制养分的范式相矛盾。这种共同限制可能归因于在P限制下微生物对合成获取P的酶的N需求增加。向上扩展(0.1×0.1°空间分辨率)表明,在自然陆地表面积的39%和57%中,土壤微生物分别受到N和P的限制,21%的区域存在N和P共同限制。作为对微生物N和P限制空间变化的全球评估,我们的结果强调了N有效性在支持低纬度地区微生物获取P方面的重要性,并增进了我们对全球范围内微生物养分限制的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/9434/12107151/7e52bc28d59e/pnas.2424552122fig01.jpg

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