Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.catena.2023.107122 |
Chironomid-based reconstruction of 500-year water-level changes in Daihai Lake, northern China | |
Ni, Zhenyu; Zhang, Enlou; Meng, Xianqiang; Sun, Weiwei; Ning, Dongliang | |
通讯作者 | Zhang, EL |
来源期刊 | CATENA
![]() |
ISSN | 0341-8162 |
EISSN | 1872-6887 |
出版年 | 2023 |
卷号 | 227 |
英文摘要 | In recent decades, lakes in arid and semi-arid regions of northern China have been rapidly shrinking, threatening the area's ecological security. However, the impacts of climate change and human activities on lake shrinkage remains unclear due to short instrumental records and a lack of long-term lake-level change records. To address this issue, we reconstructed the water depth changes of Daihai Lake, a typical lake experiencing rapid shrinkage in northern China, over the last 500 years using lake-level-sensitive chironomid assemblages. We established a regional quantitative transfer function of chironomid water-depth using 54 surface sediments from Daihai Lake and Bosten Lake in northern China. The partial least squares (PLS) model yielded a coefficient of determination (R2jack) of 0.85, a maximum bias of 1.75 m, and a root mean square error prediction (RMSEP) of 1.58 m demonstrating the reliability of inferred water depth. Several diagnostic methods were used to verify the results, and they were compared with a 60-years instrumental record. The reconstructed data revealed that the lake level was low during 1500-1780 CE, gradually increasing to its peak in the 1960s and then rapidly decreasing by approximately 10 m in the last few decades. By comparing the results with regional historical documents, palynology and stalagmite records, and meteorological data, we concluded that climate change was the main driver of lake level dynamics before the 1960s, while human activities dominated the rapid shrinkage of the lake in recent decades. Our results provide a valuable limnological dataset for the water management in Daihai Lake and a reliable method for reconstruct the lake-level changes. |
英文关键词 | Chironomid subfossil Quantitative transfer function Arid and semi-arid areas Water-level change Climate change Human activities |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000975150700001 |
WOS关键词 | ASIAN SUMMER MONSOON ; HOLOCENE CLIMATE ; INFERENCE MODELS ; TIBETAN PLATEAU ; AIR-TEMPERATURE ; BOSTEN LAKE ; DEPTH ; VEGETATION ; XINJIANG ; SHALLOW |
WOS类目 | Geosciences, Multidisciplinary ; Soil Science ; Water Resources |
WOS研究方向 | Geology ; Agriculture ; Water Resources |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/395682 |
推荐引用方式 GB/T 7714 | Ni, Zhenyu,Zhang, Enlou,Meng, Xianqiang,et al. Chironomid-based reconstruction of 500-year water-level changes in Daihai Lake, northern China[J],2023,227. |
APA | Ni, Zhenyu,Zhang, Enlou,Meng, Xianqiang,Sun, Weiwei,&Ning, Dongliang.(2023).Chironomid-based reconstruction of 500-year water-level changes in Daihai Lake, northern China.CATENA,227. |
MLA | Ni, Zhenyu,et al."Chironomid-based reconstruction of 500-year water-level changes in Daihai Lake, northern China".CATENA 227(2023). |
条目包含的文件 | 条目无相关文件。 |
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。