Precipitation differentially regulates above- and belowground productivity in response to nitrogen enrichment in an alpine meadow

被引:1
|
作者
Peng, Jinlong [1 ,2 ]
Zhang, Ruiyang [1 ]
Ma, Fangfang [1 ]
Quan, Quan [1 ]
Liao, Jiaqiang [1 ,2 ]
Zhou, Qingping [3 ,4 ]
Niu, Shuli [1 ,2 ,4 ]
机构
[1] Chinese Acad Sci, Key Lab Ecosyst Network Observat & Modeling, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
[2] Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
[3] Southwest Univ Nationalities, Inst Qinghai Tibetan Plateau, Chengdu 610041, Peoples R China
[4] Sichuan Zoige Alpine Wetland Ecosyst Natl Observat, Chengdu 610041, Peoples R China
基金
中国国家自然科学基金;
关键词
Productivity; Aboveground; Belowground; Carbon; Nitrogen; Water; TIBETAN PLATEAU; PHOSPHORUS LIMITATION; PLANT DIVERSITY; SOIL CARBON; DEPOSITION; ECOSYSTEMS; REDUCTION; DYNAMICS; WATER;
D O I
10.1016/j.agrformet.2024.110257
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
The fertilization effect of nitrogen (N) deposition on global productivity may be limited by water availability due to the coupling effect of N and water on ecosystem carbon cycling. However, it remains unclear whether this limitation is synchronized between above- and belowground productivity. Based on a long-term field manipulation experiment in an alpine meadow of the Qinghai-Tibetan Plateau, we found that precipitation played differential roles in regulating above- and belowground productivity responses to N addition. In experimental years with higher precipitation, N addition increased belowground productivity more. The main underlying mechanism was that higher precipitation mitigated excessive accumulation of soil inorganic N under N addition and shifted background plant community composition towards more N-favored species, which increased plant biomass allocation belowground and consequently stimulated the return of belowground productivity from N addition. In contrast, while N addition increased aboveground productivity, its effect didn't change with precipitation. This was mainly due to the trade-off between positive and negative effects of precipitation on the N response of aboveground productivity. Specifically, the precipitation-induced changes in soil inorganic N accumulation and background plant species composition reduced the return of aboveground productivity from N addition, while precipitation also offset this effect by mitigating the N-induced plant species loss, resulting in an overall insignificant effect of precipitation on the N response of aboveground productivity. Our findings imply that the trends of belowground productivity under N deposition can't be inferred solely from the easily measured aboveground parts, especially in the context of climate change. The work underscores an urgent need for more belowground measurements to improve the assessment of terrestrial carbon sinks.
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页数:9
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