Geographic gradients reshape dissolved organic matter activity to regulate microbial metabolic strategies and greenhouse gas production across alpine aquatic systems

Abstract As a sensitive region of global climate change, the Qinghai‐Tibet Plateau is experiencing permafrost degradation, leading to the release of sequestered carbon and nitrogen into aquatic ecosystems. However, the spatial heterogeneity and underlying drivers of greenhouse gas concentrations across diverse water body types remain unclear. Here, we investigated the concentration patterns of greenhouse gases (CO 2 , CH 4 , and N 2 O) in rivers, lakes, and thermokarst lakes along an elevational gradient of 4382 m on the plateau. Results showed that mean CO 2 , CH 4 , and N 2 O concentrations were 74.39, 0.67, and 0.065 μ mol L −1 , respectively. Rivers exhibited the highest CO 2 , thermokarst lakes the highest CH 4 , and N 2 O followed a lakes > thermokarst lakes > rivers pattern. The concentrations of CH 4 and N 2 O declined with elevation, especially in lakes. Mechanistic analyses revealed that complex macromolecules, especially highly unsaturated and phenolic compounds, were closely involved in microbial carbon and nitrogen cycling. Dissolved organic matter meta‐metabolomics further indicated a high proportion of lignin compounds within the active dissolved organic matter pool, suggesting that these traditionally recalcitrant molecules play a more dynamic biogeochemical role in alpine waters than previously recognized. Moreover, microbial life‐history strategy analyses demonstrated that communities adapt to variations in dissolved organic matter bioavailability by shifting metabolic priorities from central metabolism toward polymer degradation. Our findings elucidate how macro‐geographic gradients shape the spatial patterns of greenhouse gas by driving microenvironmental differentiation. These insights have important implications for predicting future trajectories of carbon and nitrogen cycling on the plateau and for informing adaptive management strategies in fragile alpine ecosystems.

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Publication Details

Journal
Limnology and Oceanography
Published
2026-10-30
DOI
https://doi.org/10.1002/lno.70534
Primary Topic
Peatlands and Wetlands Ecology
Type
article
Field-Weighted Citation Impact
0.00

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article

Geographic gradients reshape dissolved organic matter activity to regulate microbial metabolic strategies and greenhouse gas production across alpine aquatic systems

Yiwen Zhou, Yaoqing Peng, Chuanqiao Zhou, Liangang Chen et al.
2 links
Limnology and Oceanography
Peatlands and Wetlands Ecology
article

Geographic gradients reshape dissolved organic matter activity to regulate microbial metabolic strategies and greenhouse gas production across alpine aquatic systems

Yiwen Zhou, Yaoqing Peng, Chuanqiao Zhou, Liangang Chen, Qiu Jin, Weizheng Xie, Yao Yu, Chao Wu, Jiasen Yang, Jianjun Wang, Xiaoguang Xu
article en

Abstract

Abstract As a sensitive region of global climate change, the Qinghai‐Tibet Plateau is experiencing permafrost degradation, leading to the release of sequestered carbon and nitrogen into aquatic ecosystems. However, the spatial heterogeneity and underlying drivers of greenhouse gas concentrations across diverse water body types remain unclear. Here, we investigated the concentration patterns of greenhouse gases (CO 2 , CH 4 , and N 2 O) in rivers, lakes, and thermokarst lakes along an elevational gradient of 4382 m on the plateau. Results showed that mean CO 2 , CH 4 , and N 2 O concentrations were 74.39, 0.67, and 0.065 μ mol L −1 , respectively. Rivers exhibited the highest CO 2 , thermokarst lakes the highest CH 4 , and N 2 O followed a lakes > thermokarst lakes > rivers pattern. The concentrations of CH 4 and N 2 O declined with elevation, especially in lakes. Mechanistic analyses revealed that complex macromolecules, especially highly unsaturated and phenolic compounds, were closely involved in microbial carbon and nitrogen cycling. Dissolved organic matter meta‐metabolomics further indicated a high proportion of lignin compounds within the active dissolved organic matter pool, suggesting that these traditionally recalcitrant molecules play a more dynamic biogeochemical role in alpine waters than previously recognized. Moreover, microbial life‐history strategy analyses demonstrated that communities adapt to variations in dissolved organic matter bioavailability by shifting metabolic priorities from central metabolism toward polymer degradation. Our findings elucidate how macro‐geographic gradients shape the spatial patterns of greenhouse gas by driving microenvironmental differentiation. These insights have important implications for predicting future trajectories of carbon and nitrogen cycling on the plateau and for informing adaptive management strategies in fragile alpine ecosystems.

Limnology and OceanographyVol. 71(11)
Nanjing Normal University (CN), Chinese Academy of Sciences (CN), Kyoto University (JP), State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering (CN), Guangdong Academy of Sciences (CN), Nanjing Hydraulic Research Institute (CN), Nanjing Institute of Geography and Limnology (CN), State Key Laboratory of Hydrology Water Resources and Hydraulic Engineering (CN), State Key Laboratory of Lake Science and Environment (CN), Institute of Eco-environmental and Soil Sciences, Guangdong Academy of Sciences (CN)
National Natural Science Foundation of China, Ministry of Water Resources, Natural Science Foundation of Jiangsu Province, Guangdong Provincial Applied Science and Technology Research and Development Program, Joint Fund of the National Natural Science Foundation of China and the Karst Science Research Center of Guizhou Province, Guangdong Academy of Sciences, National Key Research and Development Program of China
Climate action, Clean water and sanitation
Openalex Percentile: Top 16%
Peatlands and Wetlands Ecology
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