古尔班通古特沙漠及周边区域全新世环境演变研究进展

doi:10.12118/j.issn.1000-6060.2022.306

Abstract

Abstract:

The Gurbantunggut Desert (GGD), the largest fixed and semi-fixed desert in northwestern China, is the region most obviously affected by westerly circulation in China. Holocene environmental evolution and its response to global climate change have important scientific significance in understanding the modern surface process and future environmental evolution trends in the GGD. The previously studies on the Holocene environmental evolution of the GGD and its surrounding areas are controversial: some studies have concluded that optimal periods of precipitation/humidity happened in the Middle-Late Holocene, while others concluded that the optimal periods occurred in the Middle Holocene and that the genetic mechanism is in dispute between the monsoon intruding inland and the overall control by the westerly. This study reconstructs the Holocene climate/humidity variation using dimensionality reduction and integrated analysis based on the multiarchive records published in the study area, and synthesizes the Holocene aeolian sand activity history by sorting out the chronological distribution of the regional aeolian sedimentary stratigraphy. The coupling relationship between regional aeolian activity and humidity change is also examined. The results show that the early Middle Holocene (12-6 ka) in this area was arid, with considerable aeolian activity; the humidity gradually increased and the aeolian activity gradually weakened from the Middle to the Late Holocene. According to the comparative analysis on the regional and hemispheric scales, it is concluded that the environmental evolution process in the GGD is mainly controlled by the westerly circulation.

Key words: Holocene, humidity change, aeolian activities, genetic mechanism, Gurbantonggut Desert

XU Yujie, LIU Bing, SUN Aijun, WANG Keqi, LI Dongxue, ZHAO Hui. Research progress of Holocene environmental evolution in the Gurbantunggut Desert and its surrounding areas[J].Arid Land Geography, 2023, 46(4): 550-562.

Figures/Tables 7

Fig. 1

Tab. 1

Tab. 2

Fig. 2

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Fig. 5

References 46

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序号	类型	剖面名称	剖面位置	时间跨度/ka	测年手段	年代数/个	参考文献
A	黄土-古土壤序列	LJW剖面	43.975°N，85.336°E	12.0~0.0	OSL	14	Chen等^[16]
B	黄土-古土壤序列	ZKT剖面	43.537°N，83.314°E	12.0~0.5	¹⁴C	5	Chen等^[16]
C	黄土-古土壤序列	TLD16剖面	43.335°N，83.018°E	12.0~0.0	OSL	15	Jia等^[17]
D	黄土-古土壤序列	KS16剖面	43.432°N，83.943°E	11.5~1.0	OSL	14	Jia等^[17]
E	黄土-古土壤序列	HC14剖面	44.600°N，87.563°E	10.5~2.0	¹⁴C	5	Jia等^[17]
F	黄土-古土壤序列	TLD剖面	43.401°N，83.037°E	11.5~1.0	OSL	8	Kang等^[18]
G	黄土-古土壤序列	XEB剖面	43.422°N，82.933°E	12.0~1.0	OSL	8	Kang等^[18]
H	黄土-古土壤序列	ZS剖面	42.934°N，80.956°E	11.5~0.5	OSL	10	Kang等^[18]
I	湖泊沉积	博斯腾湖钻孔	41.978°N，87.244°E	8.5~0.0	OSL、¹⁴C	12	Huang等^[31]
J	湖泊沉积	乌伦古湖钻孔	47.273°N，87.137°E	9.5~0.0	¹⁴C	6	蒋庆丰等^[25]
K	湖泊沉积	赛里木湖钻孔	44.609°N，81.117°E	12.0~0.0	¹⁴C	12	Jiang等^[19]
L	湖泊沉积	喀纳斯湖钻孔	48.730°N，87.020°E	12.0~0.0	¹⁴C	9	Huang等^[23]
M	湖泊沉积	巴里坤湖钻孔	43.629°N，92.808°E	11.0~0.0	¹⁴C	12	An等^[32]
N	湖泊沉积	艾比湖钻孔	44.906°N，82.904°E	12.0~0.0	¹⁴C	8	Wang等^[33]
O	泥炭沉积	铁力沙汗泥炭	48.809°N，86.920°E	9.0~0.0	¹⁴C	5	Zhang等^[28]
P	泥炭沉积	柴窝堡泥炭	43.496°N，87.910°E	8.5~0.0	¹⁴C	19	Hong等^[29]
Q	泥炭沉积	克拉沙子泥炭	48.117°N，88.370°E	11.5~3.5	¹⁴C	14	Wang等^[24]
R	泥炭沉积	那仁夏泥炭	48.800°N，86.900°E	11.5~0.0	¹⁴C	9	Feng等^[26]
S	泥炭沉积	温泉-1泥炭	44.972°N，81.030°E	10.0~0.0	¹⁴C	8	Li等^[27]
T	石笋沉积	布鲁克石笋	42.433°N，88.733°E	9.0~0.5	ICP-MS	19	Liu等^[30]

序号	类型	剖面名称	剖面位置	时间跨度/ka	测年手段	年代数/个	代用指标	参考文献
1	风成沙序列	梧桐沟钻孔	44.467°N，87.864°E	12.0~0.0	OSL	10	粒度、磁化率等	Li等^[7]
2	风成沙-河湖相序列	沙漠钻孔	44.497°N，88.183°E	8.0~5.0	TL	5	粒度、孢粉等	黄强等^[34]
3	风成沙-古土壤序列	莫索湾剖面	44.667°N，86.333°E	11.0~0.5	¹⁴C、TL	9	粒度、CaCO₃等	陈惠中等^[6]
4	风成沙-河湖相序列	MGDD	44.325°N，86.238°E	4.5~4.0	¹⁴C	2	粒度、有机质等	马妮娜^[35]
5	风成沙-河湖相序列	4C2L	44.619°N，86.624°E	5.5~5.0	¹⁴C	2	粒度、有机质等	马妮娜^[35]
6	风成沙-河湖相序列	23SGZ	45.143°N，85.958°E	1.0~0.0	¹⁴C	1	粒度、有机质等	马妮娜^[35]
7	风成沙-河湖相序列	TDG-A	44.696°N，86.766°E	6.0~5.0	¹⁴C	1	粒度、有机质等	马妮娜^[35]
8	湖泊沉积	东道海子B剖面	44.666°N，87.570°E	5.0~0.0	¹⁴C	8	粒度、孢粉等	马妮娜等^[36]
9	湖泊沉积	东道海子剖面DDH	44.604°N，87.590°E	6.5~0.0	OSL	5	粒度、磁化率等	何冬^[37]
10	湖泊沉积	东道海子钻孔	44.643°N，87.575°E	12.0~0.0	¹⁴C	5	粒度、孢粉等	李志忠等^[38-39]
11	湖泊沉积	BLK-1	43.700°N，92.833°E	9.4~0.0	¹⁴C	7	粒度	薛积彬等^[40]
12	风成沙-土壤序列	THE-1~THE-8	42°420′~43°120′N，83°150′~84°450′E	12.0~0.0	OSL	79	粒度、磁化率等	Long等^[8]

Research progress of Holocene environmental evolution in the Gurbantunggut Desert and its surrounding areas

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