Optical Stimulation Luminescence Dating of Deltas Revealed the Early to Mid-Holocene Lake-level Fluctuations of Daihai, Inner Mongolia, Northern China

被引:3
|
作者
Huang, Shixin [1 ,2 ,3 ]
Chun, Xi [1 ,4 ]
机构
[1] Inner Mongolia Normal Univ, Inner Mongolia Restorat Engn Lab Wetland Ecoenvir, Hohhot, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing, Peoples R China
[3] Univ Chinese Acad Sci, Beijing, Peoples R China
[4] Inner Mongolia Normal Univ, Lab Mongolian Plateau Environm & Global Change, Hohhot, Peoples R China
基金
中国国家自然科学基金;
关键词
lake-level fluctuation; high lake level; early to mid-Holocene; fluvial delta; optical stimulation luminescence; East Asian summer monsoon; monsoon precipitation; GRAIN-SIZE COMPONENT; ARID CENTRAL-ASIA; HUANGQIHAI LAKE; LACUSTRINE SEDIMENTS; CORE SEDIMENTS; DALI LAKE; OSL AGES; QUARTZ; EVOLUTION; LOESS;
D O I
10.3389/feart.2021.702843
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Lake-level reconstruction of inland enclosed lakes especially for monsoon-sensitive areas is of great significance to reveal regional climate changes. Daihai, a typical enclosed lake at the marginal of the East Asian summer monsoon (EASM) area in north China, is sensitive to climate changes due to its unique regional characteristics. There were a series of lakeshore terraces, highstand lacustrine sediments, and braided river deltas, providing sufficient geomorphologic and stratigraphic evidence for the reconstruction of lake-level fluctuations of Daihai. Reconstructed lake-level variations during the early and mid-Holocene were constructed based on 22 quartz optical stimulated luminescence (OSL) ages from six well-preserved profiles around Daihai Basin. Our results indicated Daihai showed a relatively low level at 10.2 ka, and a gradually increasing lake level following the enhanced monsoon precipitation during the mid-Holocene. Specifically, the high lake level began to develop at 8.1 ka and reached the maximum at 5.2 ka, with similar to 40 m higher than present. At this time, the lake area expanded to similar to 400 km(2), approximately six times as large as that of present, corresponding to the maximum monsoon precipitation and intensity of EASM during the mid-Holocene. However, our stratigraphic records showed a part of the depositional records in the north and east of the Daihai was missed after 5.2 ka, probably indicating a sudden drop of the Daihai lake level. These rapid level fluctuations were likely to be interpreted by some local scenarios and need to be further investigated in the future. Overall, the lake-level fluctuation of Daihai during the early and mid-Holocene was slightly different from that observed in the previously published regional records. Possibly, the interaction of the EASM and regional feedback from topography, and hydrology factors might have contributed to the spatial complexity and distinction.
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页数:15
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