中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Can sustained climate warming intensify the carbon source potential of saline lakes on the Qingzang Plateau?

文献类型:期刊论文

作者Shen, Di2,3; Gao, Yang1,4; Wang, Yafeng2; Jia, Junjie1,4
刊名JOURNAL OF ENVIRONMENTAL MANAGEMENT
出版日期2025-11-01
卷号394页码:127533
关键词Ecosystem metabolism Saline lakes Qingzang Plateau Climate warming Carbon source
ISSN号0301-4797
DOI10.1016/j.jenvman.2025.127533
产权排序3
文献子类Article
英文摘要Under global climate change intensification, the debate over whether high-altitude saline lakes act as carbon (C) emission sinks or sources remains unresolved. Moreover, there is currently a lack of systematic metabolic and mechanistic C assessments for saline lake ecosystems on the Qingzang Plateau (QZP), especially regarding their associative changes under climate change. Here, we used 18/16O technology and regression models to assess saline lake C metabolism on the QZP between 2000 and 2020. Additionally, we predicted the C metabolism of these lakes between 2030 and 2050 under three future scenario models: SSP126, SSP245, and SSP585. Results showed that saline lakes on the QZP have long acted as C sources. The average annual GPP of these lakes is 12.26 +/- 0.23 g O2 m-2 d-1, the average annual ER is 23.96 +/- 0.46 g O2 m-2 d-1, and the average annual NEP is-11.70 +/- 0.22 g O2 m-2 d-1. Higher temperatures, wind speeds, and total nitrogen (TN) concentrations in low-altitude saline lakes collectively promote GPP and ER. Between 2000 and 2020, under increases in temperature, surface pressure, wind speed, and TN, both GPP and ER significantly increased while NEP significantly decreased. Between 2030 and 2050, GPP and ER will gradually increase under the three future scenario models while NEP will decrease. However, under the SSP126 scenario, saline lakes on the QZP will emit the least amount of atmospheric carbon dioxide (CO2). These findings not only enhance our understanding of aquatic plateau C cycling processes but also provide a theoretical basis for the future C management of saline lakes on the QZP.
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WOS关键词RIVER ECOSYSTEM METABOLISM ; TEMPERATURE-DEPENDENCE ; TIBETAN PLATEAU ; NITROGEN ; LEVEL ; WATER
WOS研究方向Environmental Sciences & Ecology
语种英语
WOS记录号WOS:001597583400001
出版者ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
源URL[http://ir.igsnrr.ac.cn/handle/311030/217513]  
专题生态系统网络观测与模拟院重点实验室_外文论文
通讯作者Jia, Junjie
作者单位1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Beijing 100101, Peoples R China;
2.Chinese Acad Sci, Inst Tibetan Plateau Res, State Key Lab Tibetan Plateau Earth Syst Environm, Beijing 100101, Peoples R China;
3.Lanzhou Univ, Coll Earth & Environm Sci, Lanzhou 730000, Peoples R China;
4.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100049, Peoples R China
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GB/T 7714
Shen, Di,Gao, Yang,Wang, Yafeng,et al. Can sustained climate warming intensify the carbon source potential of saline lakes on the Qingzang Plateau?[J]. JOURNAL OF ENVIRONMENTAL MANAGEMENT,2025,394:127533.
APA Shen, Di,Gao, Yang,Wang, Yafeng,&Jia, Junjie.(2025).Can sustained climate warming intensify the carbon source potential of saline lakes on the Qingzang Plateau?.JOURNAL OF ENVIRONMENTAL MANAGEMENT,394,127533.
MLA Shen, Di,et al."Can sustained climate warming intensify the carbon source potential of saline lakes on the Qingzang Plateau?".JOURNAL OF ENVIRONMENTAL MANAGEMENT 394(2025):127533.

入库方式: OAI收割

来源:地理科学与资源研究所

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