中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Hydro-environmental shifts in Laolike peatland of Northeast China: Evidence from grain size distributions and end-member modeling analysis

文献类型:期刊论文

作者Li, Jing1,2,3; Dong, Yanmin1,3; Li, Hongkai1,3; Xu, Zhiwei1,3; Wang, Shengzhong1,3
刊名CATENA
出版日期2026-04-01
卷号265页码:109845
关键词End-member modeling analysis Grain size distributions Peatland Hydrological evolution Holocene
ISSN号0341-8162
DOI10.1016/j.catena.2026.109845
产权排序3
文献子类Article
英文摘要Peat serves as a critical geological archive in terrestrial ecosystems because of its ability to preserve high-resolution climatic and environmental records throughout its development. The hydrological conditions of peatlands are highly sensitive to climate variability and are commonly employed as key indicators for paleoclimate reconstruction. However, hydrological conditions within peatlands can exhibit notable spatial heterogeneity, influenced by local environmental factors such as paleotopography and autogenic self-organizing processes, which have not been sufficiently addressed. In this study, two peat cores (LLK17C and LLK-D-2019) from the Laolike peatland in the Changbai Mountains were analyzed using grain size distributions (GSDs) and end-member modeling analysis. Supported by a robust chronological framework and paleotopographic reconstruction, GSDs were examined under contrasting paleotopographic settings to evaluate hydrological dynamics and their driving mechanisms. The results demonstrated that hydrological evolution within the peatland exhibited evident spatial heterogeneity. The LLK17C core contained fine-grained sediments in which aeolian and aquatic components could not be effectively separated, whereas the LLK-D-2019 core yielded four distinct end members. On a millennial scale, climate acted as the primary control on hydrological evolution in the Laolike peatland between 11 and 4.2 kyr BP. After 4.2 kyr BP, the LLK-D-2019 core, located at the lowest topographic position, transitioned into a stable peat accumulation phase as water levels declined, as evidenced by abrupt shifts in GSDs, total organic carbon, and C/N ratios. In addition, local paleotopography and autogenic self-organization further modulated the internal hydrological conditions and their evolutionary trajectories. These findings highlight the importance of spatial heterogeneity in peatland hydrological evolution and indicate that paleohydrological reconstructions based on a single core may suffer from limited representativeness. This study contributes to improving our understanding of internal hydrological variability within peatlands and their longterm developmental dynamics.
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WOS关键词HOLOCENE CLIMATE-CHANGE ; ASIAN WINTER MONSOON ; CARBON ACCUMULATION ; BAYESIAN-ANALYSIS ; HIGH-RESOLUTION ; RECORDS ; VEGETATION ; LOESS ; SEDIMENTS ; DYNAMICS
WOS研究方向Geology ; Agriculture ; Water Resources
语种英语
WOS记录号WOS:001677441400001
出版者ELSEVIER
源URL[http://ir.igsnrr.ac.cn/handle/311030/220958]  
专题陆地表层格局与模拟院重点实验室_外文论文
通讯作者Dong, Yanmin
作者单位1.Northeast Normal Univ, Inst Peat & Mire Res, Key Lab Wetland Ecol & Vegetat Restorat, Minist Ecol & Environm, Changchun 130024, Peoples R China;
2.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing, Peoples R China
3.Northeast Normal Univ, Sch Geog Sci, Key Lab Geog Proc & Ecol Secur Changbai Mt, Minist Educ, Changchun 130024, Peoples R China;
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GB/T 7714
Li, Jing,Dong, Yanmin,Li, Hongkai,et al. Hydro-environmental shifts in Laolike peatland of Northeast China: Evidence from grain size distributions and end-member modeling analysis[J]. CATENA,2026,265:109845.
APA Li, Jing,Dong, Yanmin,Li, Hongkai,Xu, Zhiwei,&Wang, Shengzhong.(2026).Hydro-environmental shifts in Laolike peatland of Northeast China: Evidence from grain size distributions and end-member modeling analysis.CATENA,265,109845.
MLA Li, Jing,et al."Hydro-environmental shifts in Laolike peatland of Northeast China: Evidence from grain size distributions and end-member modeling analysis".CATENA 265(2026):109845.

入库方式: OAI收割

来源:地理科学与资源研究所

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