Temporal variations of δ13C-CH4 in rice paddies dominated by the plant-mediated pathway

The stable carbon isotope signature of methane (δ<sup>13</sup>C-CH<sub>4</sub>) helps constrain CH<sub>4</sub> emissions on regional to global scales, yet observations in rice paddies remain limited. The temporal dynamics of δ<sup>13</sup>C-CH<sub>4</sub> and its drivers in rice paddies are still not fully understood. Here, we conducted continuous <i>in situ</i> observations of CH<sub>4</sub> and δ<sup>13</sup>C-CH<sub>4</sub> at three canopy heights throughout a rice growing season. We investigated the emission source signature (δ<sup>13</sup>C<sub>source</sub>) and partitioned it into plant-mediated (δ<sup>13</sup>C<sub>P</sub>) and non-plant-mediated (δ<sup>13</sup>C<sub>NP</sub>) pathways. δ<sup>13</sup>C<sub>source</sub> exhibited significant temporal and vertical variability, influenced by transport pathways and external sources. We found that temporal variations in δ<sup>13</sup>C<sub>source</sub> were strongly correlated with rice photosynthesis and predominantly driven by δ<sup>13</sup>C<sub>P</sub>. Our results show that plant-mediated transport, rather than CH<sub>4</sub> production, dominates δ<sup>13</sup>C<sub>source</sub> variability. These findings provide new insight into the δ<sup>13</sup>C<sub>source</sub> dynamics in rice paddies and will be crucial for improving regional-to-global estimates of CH<sub>4</sub> fluxes from rice agriculture.

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Publication Details

Journal
iScience
Published
2025-06-16
DOI
https://doi.org/10.1016/j.isci.2025.112886
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
0.00

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article

Temporal variations of δ13C-CH4 in rice paddies dominated by the plant-mediated pathway

Shushi Peng, Jing M. Chen, Guirui Yu, Huilin Chen et al.
iScience
Atmospheric and Environmental Gas Dynamics
article

Temporal variations of δ13C-CH4 in rice paddies dominated by the plant-mediated pathway

Shushi Peng, Jing M. Chen, Guirui Yu, Huilin Chen, Weimin Ju, Xuguang Chi, Philippe Ciais, Yongguang Zhang, Zeqing Ma, Aijun Ding, Wenping Yuan
article en

Abstract

The stable carbon isotope signature of methane (δ<sup>13</sup>C-CH<sub>4</sub>) helps constrain CH<sub>4</sub> emissions on regional to global scales, yet observations in rice paddies remain limited. The temporal dynamics of δ<sup>13</sup>C-CH<sub>4</sub> and its drivers in rice paddies are still not fully understood. Here, we conducted continuous <i>in situ</i> observations of CH<sub>4</sub> and δ<sup>13</sup>C-CH<sub>4</sub> at three canopy heights throughout a rice growing season. We investigated the emission source signature (δ<sup>13</sup>C<sub>source</sub>) and partitioned it into plant-mediated (δ<sup>13</sup>C<sub>P</sub>) and non-plant-mediated (δ<sup>13</sup>C<sub>NP</sub>) pathways. δ<sup>13</sup>C<sub>source</sub> exhibited significant temporal and vertical variability, influenced by transport pathways and external sources. We found that temporal variations in δ<sup>13</sup>C<sub>source</sub> were strongly correlated with rice photosynthesis and predominantly driven by δ<sup>13</sup>C<sub>P</sub>. Our results show that plant-mediated transport, rather than CH<sub>4</sub> production, dominates δ<sup>13</sup>C<sub>source</sub> variability. These findings provide new insight into the δ<sup>13</sup>C<sub>source</sub> dynamics in rice paddies and will be crucial for improving regional-to-global estimates of CH<sub>4</sub> fluxes from rice agriculture.

iScienceVol. 28(7)
Fujian Normal University (CN), Centre National de la Recherche Scientifique (FR), Cyprus Institute (CY), University of Toronto (CA), Université de Versailles Saint-Quentin-en-Yvelines (FR), Chinese Academy of Sciences (CN), Peking University (CN), Ministry of Natural Resources (CN), Commissariat à l'Énergie Atomique et aux Énergies Alternatives (FR), Université Paris-Saclay (FR), Laboratoire des Sciences du Climat et de l'Environnement (FR), CEA Paris-Saclay (FR), Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application (CN), Institute of Geographic Sciences and Natural Resources Research (CN), University of Chinese Academy of Sciences (CN), Nanjing University (CN)
National Natural Science Foundation of China, Chinese Academy of Sciences, Government of Jiangsu Province, Jiangsu Collaborative Innovation Center for Climate Change, National Key Research and Development Program of China, Fundamental Research Funds for the Central Universities
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Atmospheric and Environmental Gas Dynamics
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