临汾盆地黄土沉积记录的末次冰期千年尺度气候事件

doi:10.13866/j.azr.2022.04.04

Abstract

Abstract:

Global change is a hotspot of current geography research, among which the millennium-scale climate events during the last glacial stage are the focus of global change research. Optical luminescence dating was conducted on the Dingcun section of the Linfen Basin, and the grain age model was used to reconstruct the chronological sequence of the area. In addition, the climate proxy indicators such as grain size, frequency magnetic susceptibility, and chromaticity were compared and analyzed to investigate the change of millennium-scale climate abrupt events in the Linfen Basin. The performance and regional characteristics revealed the relationship between climate instability in the East Asian monsoon region since the last glacial period and that in the North Atlantic region. Results showed that the median particle size and frequency magnetic susceptibility curves of the Dingcun section clearly recorded five Heinrich events and 19 Dansgaard-Oeschger cycles between 80 and 20 ka BP. The change was evident, followed by the H5 event, and the H3 and H4 events were the smallest, indicating the local climate was not only controlled by large-scale climate changes, but also affected by regional climate changes. Moreover, climatic events recorded in the Dingcun section had a good correlation with the Greenland ice core δ¹⁸O, Lijiayuan section in the western Loess Plateau, and Zeketai and Tajikistan sections in the westerly region. Furthermore, the magnitude was affected by the westerly wind and East Asian summer monsoon.

Key words: last glacial, Heinrich event, Dansgaard-Oeschger cycle, Dingcun section, Linfen Basin

TIAN Qingchun,SHI Xiaojing,HAO Xiaolong. Last glacial millennium-scale climate event recorded by loess sediments in Linfen Basin[J].Arid Zone Research, 2022, 39(4): 1027-1035.

Figures/Tables 6

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样品	深度/m	U/(mg·kg^-1)	Th/(mg·kg^-1)	K/％	环境剂量率/(Gy·ka^-1)	含水量/％	测片	等效剂量/Gy	年代/ka
DC1-1	1.35	2.46±0.4	11.41±0.7	2.03±0.04	3.85±0.20	15±7	6	160.61±2.74	41.773±2.43
DC3-1	3	2.20±0.4	12.21±0.7	2.12±0.04	3.87±0.20	15±7	6	247.30±13.38	63.85±4.99
DC5-1	4	2.17±0.4	12.34±0.7	2.16±0.04	3.87±0.21	15±7	6	279.23±7.88	72.09±4.57
DC7-1	5	2.04±0.4	10.26±0.7	1.94±0.04	3.53±0.19	15±7	6	345.19±8.10	97.76±5.98
DC8-1	5.5	1.86±0.3	11.09±0.7	1.93±0.04	4.09±0.24	15±7	6	449.59±20.94	109.96±8.63

Last glacial millennium-scale climate event recorded by loess sediments in Linfen Basin

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[1]	TIAN Qingchun,YIN Jianan,HAO Xiaolong. MIS3 climate change assessed according to loess deposition in the Linfen Basin, China [J]. Arid Zone Research, 2022, 39(1): 10-20.
[2]	DI Xin-Wei, WU Song, LI Fu-Qiang. Geochemistry Characteristics of Elements in Loess in the Huining Profile in MIS3 and Climate Change [J]. , 2013, 30(1): 156-161.