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.
Authors
- Vladimir Shanin (ORCID: https://orcid.org/0000-0002-8294-7796)
- Xingkai Xu
- Yuhua Kong
- Jin Yue
- Weiguo Cheng
- Shuirong Tang
- Dmitriy Khoroshaev
Institutions
- 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)
Publication Details
- 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
- 0.00
Funders
- National Natural Science Foundation of China