Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil

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  • Institute of Subtropical Agriculture, Chinese Academy of Sciences
  • Lund University
  • Ningbo University
  • Ludong University
  • Russian Academy of Sciences (RAS)
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Details

Original languageEnglish
Pages (from-to)1193-1203
Number of pages11
JournalLand Degradation and Development
Volume33
Issue number8
Early online date4 May 2022
Publication statusPublished - 15 May 2022

Abstract

Root exudates can significantly modify microbial activity and soil organic matter (SOM) mineralization. However, how root exudates and their C/N stoichiometric ratios control rice field (paddy) soil C mineralization is poorly understood. This study used a mixture of glucose, oxalic acid, and alanine as root exudate mimics for three C/N stoichiometric ratios (CN6, CN10, and CN80) to explore the underlying mechanisms involved in SOM mineralization. The input of root exudates enhanced CO2 emissions by 1.8–2.3-fold that of soil with only C additions (C-only). Artificial root exudates with low C/N ratios (CN6 and CN10) increased the metabolic quotient (qCO2) by 12% over those with higher stoichiometric ratios (CN80 and C-only), suggesting a relatively high energy demand for microorganisms to acquire organic N from SOM by increasing N-hydrolase production. The increase of stoichiometric ratios of C- to N-hydrolase [β-1,4-glucosidase to β-1,4-N-acetyl glucosaminidase (NAG)] promoted SOM degradation compared to those involved in organic C- and N-degradation, which had a significant positive correlation with qCO2. The stoichiometric ratios of microbial biomass were positively correlated with C use efficiency, indicating root exudates with higher C/N ratios provide an undersupply of N for microorganisms that trigger the release of N-degrading extracellular enzymes. Our findings showed that the C/N stoichiometry of root exudates controlled SOM mineralization by affecting the specific response of the microbial biomass through the activity of C- and N-releasing extracellular enzymes to adjust the microbial C/N ratio.

Keywords

    carbon use efficiency, extracellular enzymes, metabolic quotients, microbial biomass, root exudates, stoichiometric ratios

ASJC Scopus subject areas

Cite this

Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil. / Cai, Guan; Shahbaz, Muhammad; Ge, Tida et al.
In: Land Degradation and Development, Vol. 33, No. 8, 15.05.2022, p. 1193-1203.

Research output: Contribution to journalArticleResearchpeer review

Cai, G, Shahbaz, M, Ge, T, Hu, Y, Li, B, Yuan, H, Wang, Y, Liu, Y, Liu, Q, Shibistova, O, Sauheitl, L, Wu, J, Guggenberger, G & Zhu, Z 2022, 'Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil', Land Degradation and Development, vol. 33, no. 8, pp. 1193-1203. https://doi.org/10.1002/ldr.4198
Cai, G., Shahbaz, M., Ge, T., Hu, Y., Li, B., Yuan, H., Wang, Y., Liu, Y., Liu, Q., Shibistova, O., Sauheitl, L., Wu, J., Guggenberger, G., & Zhu, Z. (2022). Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil. Land Degradation and Development, 33(8), 1193-1203. https://doi.org/10.1002/ldr.4198
Cai G, Shahbaz M, Ge T, Hu Y, Li B, Yuan H et al. Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil. Land Degradation and Development. 2022 May 15;33(8):1193-1203. Epub 2022 May 4. doi: 10.1002/ldr.4198
Cai, Guan ; Shahbaz, Muhammad ; Ge, Tida et al. / Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil. In: Land Degradation and Development. 2022 ; Vol. 33, No. 8. pp. 1193-1203.
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title = "Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil",
abstract = "Root exudates can significantly modify microbial activity and soil organic matter (SOM) mineralization. However, how root exudates and their C/N stoichiometric ratios control rice field (paddy) soil C mineralization is poorly understood. This study used a mixture of glucose, oxalic acid, and alanine as root exudate mimics for three C/N stoichiometric ratios (CN6, CN10, and CN80) to explore the underlying mechanisms involved in SOM mineralization. The input of root exudates enhanced CO2 emissions by 1.8–2.3-fold that of soil with only C additions (C-only). Artificial root exudates with low C/N ratios (CN6 and CN10) increased the metabolic quotient (qCO2) by 12% over those with higher stoichiometric ratios (CN80 and C-only), suggesting a relatively high energy demand for microorganisms to acquire organic N from SOM by increasing N-hydrolase production. The increase of stoichiometric ratios of C- to N-hydrolase [β-1,4-glucosidase to β-1,4-N-acetyl glucosaminidase (NAG)] promoted SOM degradation compared to those involved in organic C- and N-degradation, which had a significant positive correlation with qCO2. The stoichiometric ratios of microbial biomass were positively correlated with C use efficiency, indicating root exudates with higher C/N ratios provide an undersupply of N for microorganisms that trigger the release of N-degrading extracellular enzymes. Our findings showed that the C/N stoichiometry of root exudates controlled SOM mineralization by affecting the specific response of the microbial biomass through the activity of C- and N-releasing extracellular enzymes to adjust the microbial C/N ratio.",
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TY - JOUR

T1 - Root exudates with low C/N ratios accelerate CO2 emissions from paddy soil

AU - Cai, Guan

AU - Shahbaz, Muhammad

AU - Ge, Tida

AU - Hu, Yajun

AU - Li, Baozhen

AU - Yuan, Hongzhao

AU - Wang, Yi

AU - Liu, Yuhuai

AU - Liu, Qiong

AU - Shibistova, Olga

AU - Sauheitl, Leopold

AU - Wu, Jinshui

AU - Guggenberger, Georg

AU - Zhu, Zhenke

N1 - Funding information: National Natural Science Foundation of China, Grant/Award Numbers: 41877104, 41977156, 42177330, 42177334; the Alexander von Humboldt Foundation of Germany, Grant/Award Number: The grants or other support to Tida Ge from the Al; the Natural Science Foundation of Hunan Province, Grant/Award Number: 2020JJ4653; The Youth Innovation Promotion Association of the Chinese Academy of Sciences, Grant/Award Number: 2019357

PY - 2022/5/15

Y1 - 2022/5/15

N2 - Root exudates can significantly modify microbial activity and soil organic matter (SOM) mineralization. However, how root exudates and their C/N stoichiometric ratios control rice field (paddy) soil C mineralization is poorly understood. This study used a mixture of glucose, oxalic acid, and alanine as root exudate mimics for three C/N stoichiometric ratios (CN6, CN10, and CN80) to explore the underlying mechanisms involved in SOM mineralization. The input of root exudates enhanced CO2 emissions by 1.8–2.3-fold that of soil with only C additions (C-only). Artificial root exudates with low C/N ratios (CN6 and CN10) increased the metabolic quotient (qCO2) by 12% over those with higher stoichiometric ratios (CN80 and C-only), suggesting a relatively high energy demand for microorganisms to acquire organic N from SOM by increasing N-hydrolase production. The increase of stoichiometric ratios of C- to N-hydrolase [β-1,4-glucosidase to β-1,4-N-acetyl glucosaminidase (NAG)] promoted SOM degradation compared to those involved in organic C- and N-degradation, which had a significant positive correlation with qCO2. The stoichiometric ratios of microbial biomass were positively correlated with C use efficiency, indicating root exudates with higher C/N ratios provide an undersupply of N for microorganisms that trigger the release of N-degrading extracellular enzymes. Our findings showed that the C/N stoichiometry of root exudates controlled SOM mineralization by affecting the specific response of the microbial biomass through the activity of C- and N-releasing extracellular enzymes to adjust the microbial C/N ratio.

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KW - extracellular enzymes

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