Inhibition by Nitrogen Addition of Moss-Mediated CH4 Uptake and CO2 Emission Under a Well-Drained Temperate Forest, Northeastern China

Nitrogen (N) deposition poses a multi-pronged threat to the carbon (C)-regulating services of moss understories. For forest C-cycle modeling under increasing N deposition, failure to mechanistically incorporate the moss-mediated processes risks severely overestimating the C sink potential of global forests. To explore whether and how N input affects the moss-mediated CH<sub>4</sub> and carbon dioxide (CO<sub>2</sub>) fluxes, a five-year field measurement was performed in the N manipulation experimental plots treated with 22.5 and 45 kg N ha<sup>-1</sup> yr<sup>-1</sup> as ammonium chloride for nine years under a well-drained temperate forest in northeastern China. In the presence of mosses, the average annual CH<sub>4</sub> uptake and CO<sub>2</sub> emission in all N-treated plots ranged from 0.96 to 1.48 kg C-CH<sub>4</sub> ha<sup>-1</sup> yr<sup>-1</sup> and from 4.04 to 4.41 Mg C-CO<sub>2</sub> ha<sup>-1</sup> yr<sup>-1</sup>, respectively, with a minimum in the high-N-treated plots, which were smaller than those in the control (1.29-1.83 kg C-CH<sub>4</sub> ha<sup>-1</sup> yr<sup>-1</sup> and 4.82-6.51 Mg C-CO<sub>2</sub> ha<sup>-1</sup> yr<sup>-1</sup>). However, no significant differences in annual cumulative CO<sub>2</sub> and CH<sub>4</sub> fluxes across all treatments occurred without moss cover. Based on the differences in C fluxes with and without mosses, the average annual moss-mediated CH<sub>4</sub> uptake and CO<sub>2</sub> emission in the control were 0.77 kg C-CH<sub>4</sub> ha<sup>-1</sup> yr<sup>-1</sup> and 2.40 Mg C-CO<sub>2</sub> ha<sup>-1</sup> yr<sup>-1</sup>, respectively, which were larger than those in the two N treatments. The N effects on annual moss-mediated C fluxes varied with annual meteorological conditions. Soil pH, available N and C contents, and microbial activity inferred from δ<sup>13</sup>C shifts in respired CO<sub>2</sub> were identified as the main driving factors controlling the moss-mediated CH<sub>4</sub> and CO<sub>2</sub> fluxes. The results highlighted that this inhibitory effect of increasing N deposition on moss-mediated C fluxes in the context of climate change should be reasonably taken into account in model studies to accurately predict C fluxes under well-drained forest ecosystems.

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Journal
Plants
Published
2026-01-05
DOI
https://doi.org/10.3390/plants15010166
Primary Topic
Peatlands and Wetlands Ecology
Type
article
Field-Weighted Citation Impact
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article

Inhibition by Nitrogen Addition of Moss-Mediated CH4 Uptake and CO2 Emission Under a Well-Drained Temperate Forest, Northeastern China

Vladimir Shanin, Xingkai Xu, Yuhua Kong, Jin Yue et al.
Plants
Peatlands and Wetlands Ecology
article

Inhibition by Nitrogen Addition of Moss-Mediated CH4 Uptake and CO2 Emission Under a Well-Drained Temperate Forest, Northeastern China

Vladimir Shanin, Xingkai Xu, Yuhua Kong, Jin Yue, Weiguo Cheng, Shuirong Tang, Dmitriy Khoroshaev
article en

Abstract

Nitrogen (N) deposition poses a multi-pronged threat to the carbon (C)-regulating services of moss understories. For forest C-cycle modeling under increasing N deposition, failure to mechanistically incorporate the moss-mediated processes risks severely overestimating the C sink potential of global forests. To explore whether and how N input affects the moss-mediated CH<sub>4</sub> and carbon dioxide (CO<sub>2</sub>) fluxes, a five-year field measurement was performed in the N manipulation experimental plots treated with 22.5 and 45 kg N ha<sup>-1</sup> yr<sup>-1</sup> as ammonium chloride for nine years under a well-drained temperate forest in northeastern China. In the presence of mosses, the average annual CH<sub>4</sub> uptake and CO<sub>2</sub> emission in all N-treated plots ranged from 0.96 to 1.48 kg C-CH<sub>4</sub> ha<sup>-1</sup> yr<sup>-1</sup> and from 4.04 to 4.41 Mg C-CO<sub>2</sub> ha<sup>-1</sup> yr<sup>-1</sup>, respectively, with a minimum in the high-N-treated plots, which were smaller than those in the control (1.29-1.83 kg C-CH<sub>4</sub> ha<sup>-1</sup> yr<sup>-1</sup> and 4.82-6.51 Mg C-CO<sub>2</sub> ha<sup>-1</sup> yr<sup>-1</sup>). However, no significant differences in annual cumulative CO<sub>2</sub> and CH<sub>4</sub> fluxes across all treatments occurred without moss cover. Based on the differences in C fluxes with and without mosses, the average annual moss-mediated CH<sub>4</sub> uptake and CO<sub>2</sub> emission in the control were 0.77 kg C-CH<sub>4</sub> ha<sup>-1</sup> yr<sup>-1</sup> and 2.40 Mg C-CO<sub>2</sub> ha<sup>-1</sup> yr<sup>-1</sup>, respectively, which were larger than those in the two N treatments. The N effects on annual moss-mediated C fluxes varied with annual meteorological conditions. Soil pH, available N and C contents, and microbial activity inferred from δ<sup>13</sup>C shifts in respired CO<sub>2</sub> were identified as the main driving factors controlling the moss-mediated CH<sub>4</sub> and CO<sub>2</sub> fluxes. The results highlighted that this inhibitory effect of increasing N deposition on moss-mediated C fluxes in the context of climate change should be reasonably taken into account in model studies to accurately predict C fluxes under well-drained forest ecosystems.

PlantsVol. 15(1)
Yamagata University (JP), Chinese Academy of Sciences (CN), Hainan University (CN), Institute of Physical-Chemical and Biological Problems in Soil Science (RU), Sanya University (CN), Institute of Atmospheric Physics (CN), University of Chinese Academy of Sciences (CN), Henan Agricultural University (CN)
National Natural Science Foundation of China
Life in Land
Openalex Percentile: Top 98%
Peatlands and Wetlands Ecology
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