阿拉善高原古湖岸堤释光测年与晚第四纪湖面变化

李国强; 陶淑娴; 佘琳琳; 金明; 魏海涛; 李芳亮; 黄新; 王中; 杨和; 王晓艳; 杨丽萍; 陈发虎

doi:10.11928/j.issn.1001-7410.2019.04.02

阿拉善高原古湖岸堤释光测年与晚第四纪湖面变化

- 1.
  兰州大学资源环境学院, 西部环境教育部重点实验室, 甘肃兰州 730000
- 2.
  中国科学院青藏高原研究所, 中国科学院青藏高原地球科学卓越创新中心, 北京 100101
- 3.
  长安大学地质工程与测绘学院, 陕西西安 710054
基金项目:
国家自然科学基金项目（批准号：41571181和41790423）资助

详细信息

作者简介:
李国强, 男, 32岁, 研究员, 释光测年与古环境变化, E-mail:gqli@lzu.edu.cn

中图分类号: P467;P534.63;P941.7

收稿日期: 2019-03-26

修回日期: 2019-05-24

刊出日期: 2019-07-30

Optically stimulated luminescence dating of paleoshorelines revealed Late Quaternary lake evolution in Alxa Plateau

- 1.
  Key Laboratory of Western China's Environmental Systems(Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, Gansu
- 2.
  CAS Center for Excellence in Tibetan Plateau Earth Sciences, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101
- 3.
  School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi

Received Date: 26 March 2019

Revised Date: 24 May 2019

Publish Date: 30 July 2019

摘要

摘要:
阿拉善高原位于现代西风环流与东亚季风环流过渡带，该地区分布的湖泊对全球性气候变化响应极为敏感，阿拉善高原广泛分布的古湖岸堤为较准确地重建晚第四纪湖泊水位变化提供了良好载体。近年对黑河、石羊河尾闾湖泊以及吉兰泰盐池、雅布赖盆地等地的古湖岸堤的沉积地层以及石英和钾长石释光测年研究，重建了不同区域较高分辨率的末次间冰期以来湖泊时空演化过程。发现早在300 ka以前阿拉善高原就已经形成了高水位湖泊，黑河尾闾额济纳盆地在MIS 11或更早、MIS 9、MIS 7、MIS 5和MIS 1形成了高湖面湖泊，高湖面湖泊形成存在100 ka的周期。阿拉善高原在末次间冰期及全新世形成了稳定高湖面湖泊，但间冰期内部湖面波动具有空间差异性，东部区域湖泊高湖面出现在MIS 5e~5c和中全新世，西部湖泊高湖面出现在MIS 5a~5c和晚全新世。湖面变化的空间差异性很可能与冰期-间冰期旋回尺度及间冰期内部东亚夏季风与西风气候系统在阿拉善高原的相互作用密切相关。
- 阿拉善高原 /
- 古湖岸堤 /
- 释光测年 /
- 湖泊演化 /
- 间冰期 /
- 全新世
Abstract:
The arid Alxa Plateau (37°~42°N, 99°107°E) is located at a major climatic transition zone between the East Asian Summer Monsoon (EASM) and the Westerlies. Endorheic rivers terminating in closed lake systems in this region are sensitive to changes in the EASM and westerlies. Well-preserved palaeoshorelines provide a record of lake-level change during the Late Quaternary. Quartz-OSL and post-IR IRSL (pIRIR) luminescence methods have been systematically applied to survey (using d-GPS) palaeoshorelines preserved in the terminal-lake systems of the Heihe River, Shiyang River, Jilantai Salt Lake and the Yabulai Basin to derive chronologies of lake evolution. The earliest shorelines are preserved in the Ejina Basin (> 300 ka). A systematic relation between glacial-interglacial cycles and lake highstands (MIS 9, 7, 5, 1) in Ejina Basin has been identified, attesting to the impact of orbital forcing on the EASM/Westerlies precipitation and lake level changes in Alxa Plateau. However, spatio-temporal variations in lake level changes are indicated in different regions of the Alxa Plateau:(1) Eastern part of the plateau sustained lake highstands during MIS 5e~5c and the mid-Holocene; whereas (2) the western part of the plateau sustained lake highstands during MIS 5c~5a and the Late Holocene. The complex interactions between the East Asian summer monsoon and the Westerlies on glacial-interglacial cycles and inside interglacial is likely responsible for spatial difference of lake level changes inside interglacial at Alxa Plateau.
- Alxa Plateau /
- palaeolake shorelines /
- luminescence dating /
- lake evolution /
- last interglacial /
- the Holocene

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图 1

阿拉善高原遥感影像及已有主要研究点分布图

Figure 1.

Map showing the locations of the Alxa Plateau(AP)and the studied shoreline sections

下载: 全尺寸图片幻灯片

图 2

阿拉善高原黑河及白碱湖尾闾湖泊晚第四纪湖面变化及间冰期内部湖面变化的空间差异性(依据Li等^[49~50]改绘)

Figure 2.

The reconstructed lake level changes during Late Quaternary and spatial variation during insides interglacial in the terminal-lake basin of Heihe River and Shiyang River of Alxa Plateau, modified from Li et al. ^[49~50]. (a) and (b) are distribution of paleolake shorelines at Gaxun Nur-Sogu Nur Basin^[48] and Juyanze Basin^{[47, 51]}, respectively. (c) is distribution of paleolake shorelines at Baijian Lake Basin^{[35, 50]}. (d) is the map of study area, the blue dotted line is the boundary of modern East Asia summer monsoon^[52] and red dash line is the boundary of possible maximum EASM precipitation dominance at study area^[50]. (e) is the reconstructed lake level changes in Ejina Basin on glacial-interglacial cycles^[49]. (f) and (g) are the reconstructed lake level changes at Alexa Plateau since last interglacial and during Holocene, respectively^[50], and the cycles age data used in the fig are cited from Long et al. ^[35]

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表 1

阿拉善高原古湖岸堤探槽剖面信息

Table 1.

The summary of paleolake shoreline sections in Alxa Plateau

序号	剖面	纬度(N)	经度(E)	海拔(m)	对应水深(m)	湖岸堤海拔(m)	剖面深度(m)	湖盆
1	GXNT-1	42°27′30.73″	100°35′33.19″	902.5	8	903	2.5	嘎顺诺尔-苏古诺尔^[48]
2	GXNT-2	42°27′29.45″	100°35′16.41″	910.1	16	910	4.0
3	GXNT-3	42°27′30.78″	100°35′07.96″	911.4	17	911	4.6
4	GXNT-4	42°29′01.84″	100°35′44.94″	913.4	19	913	4.0
5	GXNT-5	42°29′01.28″	100°35′40.46″	914.8	20	915	6.4
6	GXNT-6	42°32′36.10″	100°51′47.85″	919.1	25	919	5.0
7	WT-4	41°54′15.66″	101°45′25.17″	920.7	20	920	1.5	西居延泽^[50~51]
8	WT-2	41°54′18.22″	101°45′15.32″	917.6	14	914	1.5
9	WT-1	41°54′19.03″	101°45′0.02″	912.0	12	912	1.2
10	JYZXT-2	41°54′18″	101°45′40.1″	926.9	27	927	4.0
11	JYZXT-1	41°54′26.1″	101°45′1″	914.0	14	914	2.8
12	ET-11	41°54′07″	101°45′28″	944.3	44	944	10.0	东居延泽^{[47, 49, 51]}
13	ET-8	41°56′22.87″	101°48′47.08″	939.9	40	940	9.0
14	ET-7	41°51′16.37″	101°58′07.93″	927.1	27	927	6.1
15	ET-6	41°51′15.76″	101°58′05.28″	926.4	26	927	1.7
16	ET-5	41°51′18.71″	101°57′51.87″	923.9	24	924	5.5
17	ET-2	41°51′23.50″	101°57′0.13″	917.7	18	918	4.1
18	ET-9	41°49′25.98″	101°58′34.44″	939.6	40	940	9.0
19	ET-10	41°44′42″	101°54′24″	944.0	44	944	1.0
20	BJHT-1	39°09′41.7″	104°09′35.2″	1303.0	11	1303	4.7	白碱湖^{[35, 50]}
21	BJHT-3	39°09′59.7″	104°09′26.8″	1317.0	25	1317	2.4
22	BJHT-2	39°09′52.7″	104°09′32.8″	1314.0	22	1314	1.8
23	BJ-S1	39°08′46″	104°08′57″	1314.0	22	1314	2.5
24	BJ-S2	39°08′42″	104°08′01″	1307.0	15	1307	2.5

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表 2

阿拉善高原古湖岸堤剖面石英OSL年龄与钾长石pIRIR年龄结果

Table 2.

Summary of quartz OSL and K-feldspar pIRIR ages of samples from paleolake shorelines at Alxa Plateau

嘎顺淖尔^[48]	石英OSL年龄(ka)	钾长石pIRIR年龄(ka)	居延泽^[48~50]	钾长石pIRIR年龄(ka)	居延泽^{[47~48, 50~51]}	石英OSL年龄(ka)	白碱湖^[50]	石英OSL年龄(ka)	钾长石pIRIR年龄(ka)	白碱湖^[35]	石英OSL年龄(ka)
GXNT-6-256	56.7±6.0	84.1±6.4	ET-11-600	> > 460	ET-7-070	1.9±0.2	BJHT-3-42		97.1±8.1	BJ-S1-1	84.5±8.1
GXNT-6-374	66.3±10.3	76.8±4.8	ET-10-26	> > 352	ET-7-122	2.6±0.2	BJHT-3-165		86.3±6.5	BJ-S1-2	95.6±7.7
GXNT-6-434	75.5±9.0	84.6±5.8	ET-10-72	> > 473	ET-7-190	60.6±4.0	BJHT-3-194		86.4±4.8	BJ-S1-3	91.6±9.2
GXNT-5-472	7.3±0.5	6.2±0.5	ET-9-M	3.3±0.6	ET-7-245	65.0±4.1	BJHT-3-237		124.7±6.7	BJ-S1-4	85.8±6.9
GXNT-5-480	6.3±0.3	6.4±0.4	ET-9-272	313±19	ET-7-365	89.2±6.3	BJHT-2-64	7.8±0.7	6.8±1.6	BJ-S1-5	74.7±5.3
GXNT-5-515	16.2±1.2	28.2±4.0	ET-9-530	322±22	ET-6-090	1.4±0.1	BJHT-2-94		83.2±4.2	BJ-S1-6	90.0±6.6
GXNT-5-555	7.4±0.5	23.5±3.3	ET-9-560	324±18	ET-6-140	0.9±0.1	BJHT-2-121		93.5±5.9	BJ-S1-7	85.4±7.4
GXNT-5-580	10.6±0.7	22.7±3.3	ET-8-220	238±17	ET-5-080	1.1±0.1	BJHT-2-162		101.3±6.3	BJ-S1-8	86.5±6.6
GXNT-4-210	2.5±0.2	2.3±0.3	ET-8-270	196±12	ET-5-100	1.0±0.1	BJHT-1-52	0.9±0.1		BJ-S2-1	6.5±0.4
GXNT-4-295	6.3±0.5	5.4±0.4	ET-8-290	183±10	ET-5-232	1.0±0.1	BJHT-1-112	1.4±0.1		BJ-S2-2	7.4±0.5
GXNT-4-315	8.4±0.6	14.9±1.3	ET-8-340	178±15	ET-5-435	2.0±0.1	BJHT-1-142	4.1±0.3		BJ-S2-3	7.2±0.5
GXNT-3-120	3.1±0.2	2.7±0.3	ET-8-380	> > 389	ET-5-534	2.9±0.2	BJHT-1-207	6.5±0.8		BJ-S2-4	9.6±0.6
GXNT-3-215	6.3±0.4	7.1±1.1	ET-8-420	> > 386	ET-2-060	3.3±0.2	BJHT-1-225	8.7±0.7		BJ-S2-5	9.4±0.6
GXNT-3-290	4.9±0.4	7.4±0.5	ET-7-190	73.4±3.9	ET-2-205	4.6±0.3	BJHT-1-243	22.8±2.4	20.4±2.3	BJ-S2-6	12.7±0.8
GXNT-2-220	0.8±0.1	2.4±0.5	ET-7-245	96.9±4.8	WT-4-130	1.0±0.1				BJ-S2-7	13.8±0.9
GXNT-2-240	1.0±0.1	1.7±0.5	ET-7-365	116.6±6.2	WT-2-120	1.0±0.1
GXNT-2-290	4.6±0.3	6.0±0.4	ET-7-525	89.3±4.6	WT-1-060	0.3±0.1
GXNT-2-386	59.6±10.0	89.2±4.6	ET-7-610	122.3±6.6	JYZXT-2-52	1.5±0.1
GXNT-1-160	68.6±8.7	120.5±8.3	JYZXT-2-202	1.0±1.6	JYZXT-2-202	1.7±0.2
					JYZXT-2-278	1.6±0.2
					JYZXT-2-298	1.3±0.1
					JYXZT-2-362	1.4±0.1
					JYZXT-1-107	1.3±0.1

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阿拉善高原古湖岸堤释光测年与晚第四纪湖面变化

作者简介: 李国强, 男, 32岁, 研究员, 释光测年与古环境变化, E-mail:gqli@lzu.edu.cn

Optically stimulated luminescence dating of paleoshorelines revealed Late Quaternary lake evolution in Alxa Plateau

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作者简介:
李国强, 男, 32岁, 研究员, 释光测年与古环境变化, E-mail:gqli@lzu.edu.cn