A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

王乃昂; 高顺尉

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A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

王乃昂, 高顺尉

文章导航 > Chinese Geographical Science > 1999 > 9(4): 335-341

王乃昂, 高顺尉. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. 中国地理科学, 1999, 9(4): 335-341.

引用本文:

王乃昂, 高顺尉. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. 中国地理科学, 1999, 9(4): 335-341.

Wang Nai'ang, Gao Shunwei. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. Chinese Geographical Science, 1999, 9(4): 335-341.

Citation:

Wang Nai'ang, Gao Shunwei. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. Chinese Geographical Science, 1999, 9(4): 335-341.

A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

王乃昂^1,2,
高顺尉¹

1.
Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China;
2.
Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China

基金项目: An great project of National Natural Science Foundation of China(NO.49731010);a project supported by Postdoctoral Science Fund

A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

Wang Nai'ang^1,2,
Gao Shunwei¹

1.
Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China;
2.
Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China

摘要: A preliminary study on the advance and the retreat of Qingtu Lake and its climatic records of the Holocene lacustrine deposits has been made through comprehensive analysis. The study shows that the modes characteristics of climatic change in Eastern Hexi Corridor was provided with the corresponding relationship of warm moist and cold dry during the scale longer than hundred years. As a result of climatic changes and human activities, Qingtu Lake cycle has undergone four lake retreated and three lake advanced stages since 6000 a B.P. Based on the study on lacustrine sedimentary color, grain size, Fe³⁺/Fe²⁺ and organic matter, the authors put forward that a warm period existed during the phase of 335-480 A.D. in the studied area. This warm period could be further testified by a lot of evidences obtained from the historical documents and the natural records of Qingtu Lake. In brief, the evolution of lakes in Eastern Hexi Corridor is characterized by sedimentary continuity, fast sedimentary rate and high resolution, it not only indicate the paleoenvironmental and climatic change in Holocene, but also can reflect the intensity of Eastern Asia monsoon.
- Qingtu Lake /
- Holocene /
- lacustrine deposits /
- climatic records /
- warm period of 355-480 A.D.
Abstract: A preliminary study on the advance and the retreat of Qingtu Lake and its climatic records of the Holocene lacustrine deposits has been made through comprehensive analysis. The study shows that the modes characteristics of climatic change in Eastern Hexi Corridor was provided with the corresponding relationship of warm moist and cold dry during the scale longer than hundred years. As a result of climatic changes and human activities, Qingtu Lake cycle has undergone four lake retreated and three lake advanced stages since 6000 a B.P. Based on the study on lacustrine sedimentary color, grain size, Fe³⁺/Fe²⁺ and organic matter, the authors put forward that a warm period existed during the phase of 335-480 A.D. in the studied area. This warm period could be further testified by a lot of evidences obtained from the historical documents and the natural records of Qingtu Lake. In brief, the evolution of lakes in Eastern Hexi Corridor is characterized by sedimentary continuity, fast sedimentary rate and high resolution, it not only indicate the paleoenvironmental and climatic change in Holocene, but also can reflect the intensity of Eastern Asia monsoon.
- Qingtu Lake /
- Holocene /
- lacustrine deposits /
- climatic records /
- warm period of 355-480 A.D.

[1]	Xuelian GUO, Lusheng HE, Guoyong ZHAO, Weibin WANG, Huairen CAO, Hao WU. Spatial-temporal Characteristics of Holocene Paleosols in the Chinese Loess Plateau and Paleoclimatic Significance . Chinese Geographical Science, 2022, 32(6): 1110-1118. doi: 10.1007/s11769-022-1285-1
[2]	WANG Chunling, ZHAO Hongyan, WANG Guoping. Vegetation Development and Water Level Changes in Shenjiadian Peatland in Sanjiang Plain, Northeast China . Chinese Geographical Science, 2015, 25(4): 451-461. doi: 10.1007/s11769-015-0768-8
[3]	WANG Shaowu, GE Quansheng, WANG Fang, WEN Xinyu, HUANG Jianbin. Abrupt Climate Changes of Holocene . Chinese Geographical Science, 2013, 23(1): 1-12.
[4]	LU Yingxia, LI Baosheng, WEN Xiaohao, QIU Shifan, WANG Fengnian, NIU Dongfeng, LI Zhiwen. Millennial-centennial Scales Climate Changes of Holocene Indicated by Magnetic Susceptibility of High-resolution Section in Salawusu River Valley, China . Chinese Geographical Science, 2010, 20(3): 243-251. doi: 10.1007/s11769-010-0243-5
[5]	ZHENG Yinghua, WU Yongqiu, LI Sen, TAN Lihua, GOU Shiwei, ZHANG Hongyan. Grain-size Characteristics of Sediments Formed Since 8600 yr B.P. in Middle Reaches of Yarlung Zangbo River in Tibet and Their Paleoenvironmental Significance . Chinese Geographical Science, 2009, 19(2): 113-119. doi: 10.1007/s11769-009-0113-1
[6]	XUE Jibin, ZHONG Wei, ZHENG Yanming, MA Qiaohong, CAI Ying, OUYANG Jun. A New High-resolution Late Glacial-Holocene Climatic Record from Eastern Nanling Mountains in South China . Chinese Geographical Science, 2009, 19(3): 274-282. doi: 10.1007/s11769-009-0274-y
[7]	XUE Jibin, ZHONG Wei, ZHAO Yinjuan, PENG Xiaoying. Holocene Abrupt Climate Shifts and Mid-Holocene Drought Intervals Recorded in Barkol Lake of Northern Xinjiang of China . Chinese Geographical Science, 2008, 18(1): 54-61. doi: 10.1007/s11769-008-0054-0
[8]	LONG Hao, TAN Hongbin, WANG Naiang, TAN Liangcheng, LI Yu. Mid-Holocene Climate Variations Recorded by Palaeolake in Marginal Area of East Asian Monsoon: A Multi-proxy Study . Chinese Geographical Science, 2007, 17(4): 325-332. doi: 10.1007/s11769-007-0325-1
[9]	YIN Yong, FANG Nian-qiao, HU Chao-yong, NIE Hao-gang, QING Zun-li. RELATIVE BRIGHTNESS INDEX AND IT'S CLIMATIC SIGNIFICANCE FROM LACUSTRINE SEDIM ENT OF NAPAHAI LAKE,NORTHWESTERN YUNNAN PLATEAU,CHINA . Chinese Geographical Science, 2002, 12(3): 249-253.
[10]	HAN Mei, LI Dao-gao, ZHAO Ming-hua, JIANG Ai-xia. A STUDY OF THE SURFACE EMERGING PALAEOCHANNELS ON THE SOUTH COAST PLAIN OF LAIZHOU BAY . Chinese Geographical Science, 2000, 10(3): 245-253.
[11]	王瑜, 宋长青, 孙湘君. PALYNOLOGICAL RECORD OF PALEOVEGETATION CHANGE DURING HOLOCENE AT NORTH TUMD PLAIN IN INNER MONGOLIA, CHINA . Chinese Geographical Science, 1999, 9(1): 87-91.
[12]	李有利, 杨景春. RESPONSE OF RIVER TERRACES TO HOLOCENE CLIMATIC CHANGES IN HEXI CORRIDOR, GANSU, CHINA . Chinese Geographical Science, 1998, 8(1): 53-57.
[13]	张虎才. CLIMATIC CHANGE AND HUMAN ACTIVITIES OF NORTHEASTERN SAHARA IN HOLOCENE . Chinese Geographical Science, 1998, 8(4): 377-382.
[14]	钟巍, 熊黑钢. ISOTOPIC EVIDENCE FOR HOLOCENE CLIMATIC CHANGES IN BOSTEN LAKE, SOUTHERN XINJIANG, CHINA . Chinese Geographical Science, 1998, 8(2): 176-182.
[15]	吴敬禄, 王苏民, 吴艳宏. THE HOLOCENE SEDIMENTAL CHARACTERISTIC AND PALEOCLIMATIC EVOLUTION OF EBINUR LAKE, XINJIANG . Chinese Geographical Science, 1996, 6(1): 78-88.
[16]	钟巍, 王建民. PRELIMINARY STUDY ON THE HOLOCENE ENVIRONMENT CHANGES IN XINJIANG──GEOLOGIC RECORDS AND SEQUENCE . Chinese Geographical Science, 1996, 6(2): 166-176.
[17]	周子康, 夏越炯, 刘为纶, 吴维棠. RECONSTRUCTION OF PALEOVEGETATION AND PALEOCLIMATE OF HOLOCENE HYPSITHERMAL IN THE HEMUDU REGION . Chinese Geographical Science, 1995, 5(3): 232-241.
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[20]	张仲英, 刘瑞华. THE HOLOCENE ALONG THE COAST OF HAINAN ISLAND, CHINA . Chinese Geographical Science, 1991, 1(2): 188-196.

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A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

王乃昂^1,2,
高顺尉¹

1. Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China;

2. Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China

基金项目: An great project of National Natural Science Foundation of China(NO.49731010);a project supported by Postdoctoral Science Fund

收稿日期: 1999-06-22
刊出日期: 1999-12-20

关键词:

Qingtu Lake /

Holocene /

lacustrine deposits /

climatic records /

warm period of 355-480 A.D.

摘要: A preliminary study on the advance and the retreat of Qingtu Lake and its climatic records of the Holocene lacustrine deposits has been made through comprehensive analysis. The study shows that the modes characteristics of climatic change in Eastern Hexi Corridor was provided with the corresponding relationship of warm moist and cold dry during the scale longer than hundred years. As a result of climatic changes and human activities, Qingtu Lake cycle has undergone four lake retreated and three lake advanced stages since 6000 a B.P. Based on the study on lacustrine sedimentary color, grain size, Fe³⁺/Fe²⁺ and organic matter, the authors put forward that a warm period existed during the phase of 335-480 A.D. in the studied area. This warm period could be further testified by a lot of evidences obtained from the historical documents and the natural records of Qingtu Lake. In brief, the evolution of lakes in Eastern Hexi Corridor is characterized by sedimentary continuity, fast sedimentary rate and high resolution, it not only indicate the paleoenvironmental and climatic change in Holocene, but also can reflect the intensity of Eastern Asia monsoon.

English Abstract

王乃昂, 高顺尉. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. 中国地理科学, 1999, 9(4): 335-341.

引用本文:

王乃昂, 高顺尉. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. 中国地理科学, 1999, 9(4): 335-341.

Wang Nai'ang, Gao Shunwei. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. Chinese Geographical Science, 1999, 9(4): 335-341.

Citation:

Wang Nai'ang, Gao Shunwei. A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS[J]. Chinese Geographical Science, 1999, 9(4): 335-341.

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A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

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出版历程

A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

1. Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China; 2. Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China

English Abstract

A PRELIMINARY RESEARCH ON THE CLIMATIC RECORDS OF LACUSTRINE DEPOSITS OF QINGTU LAKE IN THE LAST 6000 YEARS

1. Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China; 2. Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China

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目录

1. Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China;

2. Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China

1. Department of Geography, Lanzhou University, Lanzhou 730000, P. R. China;

2. Lanzhou Institute of Desert, the Chinese Academy of Sciences, Lanzhou 730000, P. R. China