Ecoenzymatic stoichiometry reveals microbial phosphorus limitation decreases the nitrogen cycling potential of soils in semi-arid agricultural ecosystems
[Display omitted] •FM increased microbial C metabolism while very small effects on P metabolism.•Increased microbial C metabolism ascribe to increased soil moisture content.•N fertilization increased the microbial demand for P (microbial P limitation).•Changes in nutrient stoichiometry and N availab...
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Published in: | Soil & tillage research Vol. 197; p. 104463 |
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Main Authors: | , , , , , , , , , , |
Format: | Journal Article |
Language: | English |
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Elsevier B.V
01-03-2020
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Abstract | [Display omitted]
•FM increased microbial C metabolism while very small effects on P metabolism.•Increased microbial C metabolism ascribe to increased soil moisture content.•N fertilization increased the microbial demand for P (microbial P limitation).•Changes in nutrient stoichiometry and N availability led to P limitation increase.•Microbial P limitation strongly inhibited nitrification and denitrification potential.
Variations in soil microbial metabolism currently represent one of the greatest areas of uncertainty with regard to soil nutrient cycles and the control of terrestrial carbon (C) and nitrogen (N) loss and are poorly understood in agricultural ecosystems with intensive farming practices. In this study, extracellular enzymatic stoichiometry models and quantitative PCR techniques were used to examine microbial metabolic limitation and its relationship with N-cycling gene expression in semi-arid agricultural ecosystems considering four N fertilization levels (N 0, N 100, N 250, and N 400 kg N ha−1) and two agronomic strategies (film mulching and no mulching). Film mulching increased microbial C limitation (reflecting microbial C metabolism size; 0.189 of the total effects), while very small effects on microbial phosphorus (P) limitation were observed (-0.007 of the total effects). N fertilization increased the microbial demand for P (microbial P limitation; 0.504 of the total effects). Increased microbial C metabolism was mainly attributed to increased soil moisture content after film mulching, which enhanced microbial decomposition of organic C (high C-acquiring enzyme activities). Changes in nutrient stoichiometry and the increase in N availability due to N fertilization were largely responsible for increased microbial P limitation. Furthermore, microbial P limitation negatively affected the abundance of AOA amoA, AOB amoA (involved in nitrification), nirK, nirS, nosZ (involved in denitrification) genes, strongly inhibiting nitrification and denitrification potential (-0.743 and -0.761 of the total effects, respectively). The present results suggest that agricultural ecosystems with film mulching are conducive to organic residue decomposition, while appropriate P limitation under N fertilization could reduce the loss of N due to nitrification and denitrification in soil. This study highlights the importance of elemental stoichiometry-driven microbial metabolic variation in understanding soil nutrient cycles and optimizing agricultural practices. |
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AbstractList | [Display omitted]
•FM increased microbial C metabolism while very small effects on P metabolism.•Increased microbial C metabolism ascribe to increased soil moisture content.•N fertilization increased the microbial demand for P (microbial P limitation).•Changes in nutrient stoichiometry and N availability led to P limitation increase.•Microbial P limitation strongly inhibited nitrification and denitrification potential.
Variations in soil microbial metabolism currently represent one of the greatest areas of uncertainty with regard to soil nutrient cycles and the control of terrestrial carbon (C) and nitrogen (N) loss and are poorly understood in agricultural ecosystems with intensive farming practices. In this study, extracellular enzymatic stoichiometry models and quantitative PCR techniques were used to examine microbial metabolic limitation and its relationship with N-cycling gene expression in semi-arid agricultural ecosystems considering four N fertilization levels (N 0, N 100, N 250, and N 400 kg N ha−1) and two agronomic strategies (film mulching and no mulching). Film mulching increased microbial C limitation (reflecting microbial C metabolism size; 0.189 of the total effects), while very small effects on microbial phosphorus (P) limitation were observed (-0.007 of the total effects). N fertilization increased the microbial demand for P (microbial P limitation; 0.504 of the total effects). Increased microbial C metabolism was mainly attributed to increased soil moisture content after film mulching, which enhanced microbial decomposition of organic C (high C-acquiring enzyme activities). Changes in nutrient stoichiometry and the increase in N availability due to N fertilization were largely responsible for increased microbial P limitation. Furthermore, microbial P limitation negatively affected the abundance of AOA amoA, AOB amoA (involved in nitrification), nirK, nirS, nosZ (involved in denitrification) genes, strongly inhibiting nitrification and denitrification potential (-0.743 and -0.761 of the total effects, respectively). The present results suggest that agricultural ecosystems with film mulching are conducive to organic residue decomposition, while appropriate P limitation under N fertilization could reduce the loss of N due to nitrification and denitrification in soil. This study highlights the importance of elemental stoichiometry-driven microbial metabolic variation in understanding soil nutrient cycles and optimizing agricultural practices. |
ArticleNumber | 104463 |
Author | Yue, Shanchao Li, Shiqing Duan, Chengjiao Fang, Linchuan Zhang, Xingchang Wang, Xia Chen, Hansong Ju, Wenliang Wang, Yunqiang Zhang, Yanle Cui, Yongxing |
Author_xml | – sequence: 1 givenname: Yongxing surname: Cui fullname: Cui, Yongxing organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 2 givenname: Yanle surname: Zhang fullname: Zhang, Yanle organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 3 givenname: Chengjiao surname: Duan fullname: Duan, Chengjiao organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 4 givenname: Xia surname: Wang fullname: Wang, Xia organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 5 givenname: Xingchang surname: Zhang fullname: Zhang, Xingchang organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 6 givenname: Wenliang surname: Ju fullname: Ju, Wenliang organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 7 givenname: Hansong surname: Chen fullname: Chen, Hansong organization: University of Chinese Academy of Sciences, Beijing, 100049, China – sequence: 8 givenname: Shanchao surname: Yue fullname: Yue, Shanchao organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 9 givenname: Yunqiang surname: Wang fullname: Wang, Yunqiang organization: CAS Center for Excellence in Quaternary Science and Global Change, Xi'an, 710061, China – sequence: 10 givenname: Shiqing surname: Li fullname: Li, Shiqing organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China – sequence: 11 givenname: Linchuan surname: Fang fullname: Fang, Linchuan email: flinc629@hotmail.com organization: State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation CAS and MWR, Yangling, 712100, China |
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•FM increased microbial C metabolism while very small effects on P metabolism.•Increased microbial C metabolism ascribe to increased soil... |
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SubjectTerms | Extracellular enzyme activity Functional genes Microbial metabolic limitation |
Title | Ecoenzymatic stoichiometry reveals microbial phosphorus limitation decreases the nitrogen cycling potential of soils in semi-arid agricultural ecosystems |
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