MIS3以来天山黄土沉积速率时空分布规律及其意义

程良清; 宋友桂; 孙焕宇; RustamOrozbaev

doi:10.16562/j.cnki.0256-1492.2017032001

MIS3以来天山黄土沉积速率时空分布规律及其意义

1.
中国科学院地球环境研究所黄土与第四纪地质国家重点实验室，西安 710061

2.
中国科学院大学，北京 100049

3.
福建师范大学地理科学学院，福州 350007

4.
Institute of Geology, National Academy of Sciences of Kyrgyz Republic, Bishkek 720040, Kyrgyzstan

基金项目:
国家重点研发计划全球变化专项“亚洲大陆风尘时空分布及其与全球变化的联系”(2016YFA0601902);国家自然科学基金项目“中亚干旱区黄土记录的末次冰期以来气候变化与驱动机制”(41572162);中国科学院国际合作局对外合作重点项目“中亚黄土与第四纪变化”(132B61KYS20160002)

详细信息

作者简介: 程良清(1990—)，男，硕士，第四纪地质与古气候专业, E-mail：chenglq@ieecas.cn

中图分类号: P535

文凤英编辑

收稿日期: 2017-03-20

修回日期: 2017-05-11

刊出日期: 2019-02-28

Spatio-temporal distribution of dust sedimentation rate of Tianshan loess since MIS3 and its implications

1.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China

2.
University of Chinese Academy of Sciences, Beijing 100049, China

3.
College of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China

4.
Institute of Geology, National Academy of Sciences of Kyrgyz Republic, Bishkek 720040, Kyrgyzstan

Received Date: 20 March 2017

Revised Date: 11 May 2017

Publish Date: 28 February 2019

摘要

摘要:
风尘堆积沉积速率的变化对揭示大气环流与古气候变化具有重要意义。基于中亚东北部天山及其周边黄土剖面已有的释光和放射性¹⁴C年代数据的分析筛选整理，初步获得了该区深海氧同位素MIS3以来黄土沉积速率的时空变化特征，并探讨了可能的原因。结果表明：(1)末次盛冰期(LGM)沉积速率总体上表现出天山西部低、伊犁盆地高的特征。这种空间变化特征可能与地形、大气环流以及伊犁盆地黄土的近源堆积有关。(2)LGM和MIS3b时期是MIS3阶段以来主要的粉尘沉积阶段。MIS3b时期沉积速率最高，LGM次之，而全新世沉积速率较低。MIS3b时期高的沉积速率可能与大规模的冰川发育有关。在全新世期间，中全新世的沉积速率相对较高，可能与中全新世气候湿润、地表捕获粉尘的能力强有关。
- 沉积速率 /
- 全新世 /
- LGM /
- MIS3b /
- 天山黄土
Abstract:
Eolian loess is an important archive for understanding Quaternary environmental changes. The sedimentation rate of loess, as an important proxy to environmental changes, is helpful to revealing atmospheric circulation and paleoenvironmental changes. With the application of various dating methods especially the high-accuracy Optically Stimulated Luminescence (OSL), sedimentation rate has been widely applied to the orbital-scale and millennial-scale paleoclimatic changes recently in the study of Chinese Loess Plateau (CLP). Central Asia is also one of the main distribution areas of world loess. This paper is specially devoted to the spatio-temporal distribution pattern of dust sedimentation rate of the Tianshan loess in order to provide a new horizon for understanding paleoclimatic patterns in Central Asia, where sedimentation rate has been poorly studied. Therefore, we collected the available geochronological data including OSL and ¹⁴C of the last glacial loess sections from the Tianshan Mountains of Central Asia in this paper, analyzed the reliability of age data and discussed spatial and temporal distribution pattern of the sedimentation rate. The results suggest that: (1) During the Last Glacial Maximum (LGM), sedimentation rate is relatively low in the west of Tianshan, but high in the Ili Basin. This spatial pattern of distribution is closely related to geographic and atmospheric conditions as well as proximal accumulation. (2) LGM and MIS3b are the main dust deposition stages since MIS3. In the Tianshan area, the sedimentation rate of MIS3b is higher than that of LGM. Since the solar insolation in the MIS3b stage is higher than that in the LGM stage, the westerly will bring more moisture from the Atlantic Ocean, Caspian Sea and Mediterranean Sea. In the Tianshan area, moisture is believed the main factor affecting glaciers. In this regard, the scale of glacier in the wetter MIS3b period is larger than that in the LGM period, and the intensified abrasion of the glaciers will bring in more fine particulate matters. (3) Sedimentation rate is low in Holocene, and the variations in sedimentation rate are similar to the 'westerly model'. We speculate that the amount of dust in the atmosphere is relatively low in Holocene. Dust is mainly deposited under wet climate since humidity is conducive to vegetation and helpful for dust to settle down. More moisture will result in higher sedimentation rate.
- dust sedimentary rate /
- Holocene /
- the last glacial maximum /
- MIS3b /
- Tianshan loess

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图 1 亚洲大气环流特征(a)和天山黄土分布及剖面位置图(b)

Figure 1.

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图 2 ZKT、TLD、NLK、RSK剖面年代-深度图(数据来源见表 1)

Figure 2.

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图 3 MIS3以来天山黄土沉积速率变化(数据来源见表 1)

Figure 3.

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图 4 古里雅冰芯微粒浓度^[69](a)、区域粉尘沉积年代频率(b)和65°N太阳辐射量^[70](c)对比

Figure 4.

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图 5 中亚天山地区沉积速率空间变化

Figure 5.

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图 6 天山全新世黄土年代分布频数特征(a)及其与西风模式对比(b)(据Chen等^[74])

Figure 6.

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表 1 剖面位置、年代和厚度

Table 1. Locations, ages and thickness

地点	剖面	经纬度坐标及海拔	厚度/m	剖面底部年龄/ka	测年材料及方法	文献来源
	TLD1	43°25′N，83°03′E	(12)	62.5	AMS¹⁴C有机质	[30]
	TLD2	43°24′5″N，83°2′13″E; 1020m	100(5.1)	29	石英(4~11μm)SAR	[17]
	TLD3	43°25′N，83°03′E;	(33.5)	55	TL	[56]
	ZKT1	43°31′53"N，83°18′58"E; 850m	18	62.7	OSL	[25]
	ZKT2	43°32′14"N，83°18′50"E; 900m	23	72	石英(38~63μm)SAR	[47]
	ZKT3	43°32′25"N，83°18′10"E	22.5	46.7	AMS¹⁴C蜗牛和OSL	[45]
伊犁盆地	XY	43°27′N，83°18′E;	(7)	41.4	TL	[25]
	ZSP	42°41′24″N，80°15′00″E; 1875m	6.5	67	AMS¹⁴C和石英(4~11μm)Post-IR	[44]
	ZS	43°08′99″N，81°05′65″E; 1920m	4.5	56.9	AMS¹⁴C沉积物	[25]
	XEBLK	43°25′12″N，83°04′12″E; 1050m	30.7	29	石英(38~63μm)SAR	[23]
	NLK1	43°45′36″N，83°15′00″E; 1253m	21	69	石英(38~63μm)SAR	[20]
	NLK2	43°45′36″N，83°15′00″E; 1253m	21	35.8	石英(63~90μm)SAR	[49]
	YN	44°00′N，82°00′E;	(6)	9.4	TL	[56]
	TEH1	42°56′N，84°E; 2400m	3.05	8.5	钾长石(150~200μm)pIRIR	[55]
	TKLK	43°52′06″N，81°24′8″E; 636m	(5)	9.4	AMS¹⁴C有机质	[56]
	LJW	43°50′23″N，85°07′35″E; 3641m	5(1.1)	7.1	钾长石(63~90μm)MET-pIRIR	[27]
	SXG	43°26′46″N，87°30′27″E; 1636m	2(1.2)	8.7	钾长石(63~90μm)MET-pIRIR	[27]
	LJW10	43°58′29″N，85°20′10"E; 1462m	2.8	12.6	钾长石(38~63μm)pIRIR	[19]
天山北坡	DFS	玛纳斯河洪积扇台地，527m	1.8	7	石英(40~63μm)BLSL	[48]
	BYH10	44°02′27"N，87°47′54"E; 622m	30	71	钾长石(63~90μm)pIRIR	[22]
	URS	43°30′50″N，87°19′48″E; 1603m	9.4	27.4	石英(4~11μm)SMAR	[28]
	RSK1	43°13′N，76°51′E; 1070m	80(40)	83	石英(4~11μm) IRSL	[36]
	RSK2	43°13′N，76°51′E; 1070m	80(8)	34.2	长石(4~11μm)PIR-IRSL	[21]
哈萨克斯坦和吉尔吉斯斯坦	Tramplin	43°12′31″N，76°56′01″E; 1020m	10.5	40	AMS¹⁴C蜗牛	[45]
	Romantic	43°12′31″N，77°01′11″E; 1000m	9(5.9)	35	AMS¹⁴C木炭、沉积物	[45]
	Valikhanov	43°10′30″N，69°19′02″E; 1000m	7.5	25	AMS¹⁴C沉积物	[45]
	BSK	42°42′15″N，74°46′51″E; 1432m	30	60	石英(90~250μm)SAR	[18]
注：X(Y)表示总共X，其中上部Y作为研究对象。TLD-塔勒德，ZKT-则克台，XY-新源，ZSP-昭苏波马，ZS-昭苏，XEBLK-肖尔布拉克，NLK-尼勒克，YN-伊宁，TEH-天鹅湖，TKLK-特克拉克，LJW-鹿角湾，SXG-水西沟，DFS-大佛寺，BYH-白杨河，URS-乌鲁木齐河剖面，RSK-Remizovka，BSK-比什凯克。

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MIS3以来天山黄土沉积速率时空分布规律及其意义

1. 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室，西安 710061 2. 中国科学院大学，北京 100049 3. 福建师范大学地理科学学院，福州 350007 4. Institute of Geology, National Academy of Sciences of Kyrgyz Republic, Bishkek 720040, Kyrgyzstan

作者简介: 程良清(1990—)，男，硕士，第四纪地质与古气候专业, E-mail：chenglq@ieecas.cn

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Spatio-temporal distribution of dust sedimentation rate of Tianshan loess since MIS3 and its implications

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