Advances in the Study of Sandy Land Evolution and Driving Mechanism in the Monsoonal Marg in Area in China during the Holocene Epoch

doi:10.7522/j.issn.1000-694X.2018.00084

Journal of Desert Research ›› 2019, Vol. 39 ›› Issue (3): 163-171.DOI: 10.7522/j.issn.1000-694X.2018.00084

Previous Articles Next Articles

Advances in the Study of Sandy Land Evolution and Driving Mechanism in the Monsoonal Marg in Area in China during the Holocene Epoch

Xue Wenping^1,2, Jin Heling¹, Liu Bing¹, Sun Liangying¹, Liu Zhenyu^1,2

1. Key Laboratory of Desert and Desertification, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China;
2. University of Chinese Academy of Sciences, Beijing 100049, China

Received:2018-04-11 Revised:2018-06-11 Published:2019-06-10

Abstract

Abstract: Study of the evolution and climatic variation in the monsoonal margin area in China during the Holocene epoch shows there are obviously differences from the east to the west. Firstly, a typical three-stage evolution process is presented in the eastern Horqin Sandy Land and central Mu Us Sandy Land, while the western Gonghe Basin is characterized by multi-stage evolution. Secondly, in the eastern Horqin Sandy Land and central Mu Us Sandy Land the climate change is also presented in three phases, while the change of the western Gonghe Basin is relatively complicated due to the regional features. Thirdly, the Holocene abrupt climate events have different effects on different regions. The Asian monsoon circulation controlled by the solar isolation and the change of the effective humidity has great influence on the sandy evolution.

Key words: Holocene Epoch, sandy land evolution, climatic change, abrupt events, driving mechanism

CLC Number:

P531

Xue Wenping, Jin Heling, Liu Bing, Sun Liangying, Liu Zhenyu. Advances in the Study of Sandy Land Evolution and Driving Mechanism in the Monsoonal Marg in Area in China during the Holocene Epoch[J]. Journal of Desert Research, 2019, 39(3): 163-171.

References

[1] 苏志珠,吴宇婧,孔梦园,等.常量元素记录的毛乌素沙地东南缘全新世气候变化[J].中国沙漠,2018,38(3):516-523.
[2] Lowell T,Heusser B,Anderson B,et al.Interhemispheric correlation of Late Pleistocene glacial events[J].Science,1995,269:1541-1549.
[3] Liu J Q,Lu H Y,Negendank J,et al.Periodicity of Holocene climatic variations in the Huguangyan Maar Lake[J].Chinese Science Bulletin,2000,45(18):1712-1717.
[4] Shi Y F.Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau andin East Asia[J].Quaternary International,2002,97/98:79-91.
[5] 丁一汇,王绍武,郑景云,等.中国气候[M].北京:科学出版社,2013:419-466.
[6] 鹿化煜,周亚利,Mason J,等.中国北方晚第四纪气候变化的沙漠与以光释光年代为基础的直接对比[J].第四纪研究,2006,26(6):888-894.
[7] 刘东生,田斌,余登兵,等.黄土与干旱环境[M].合肥:安徽科学技术出版社,2009:3-20.
[8] Wang T,Chen G T,Zhao H L,et al.Deserts and Aeolian Desertification in China[M].Beijing:Science Press,2011:110-148.
[9] 董光荣,陈惠忠,王贵勇,等.150 ka以来中国北方沙漠-沙地演化和气候变化[J].中国科学,1995,25(12):1303-1312.
[10] 董光荣,金炯,李保生,等.科尔沁沙地沙漠化的几个问题——以南部地区为例[J].中国沙漠,1994,14(1):1-9.
[11] 董光荣,靳鹤龄,陈惠忠,等.末次间冰期以来沙漠-黄土边界带移动与气候变化[J].第四纪研究,1997,17(2):158-167.
[12] 黄赐璇.毛乌素沙地南缘全新世自然环境[J].地理研究,1991,10(2):52-59.
[13] 裘善文.试论科尔沁沙地的形成与演变[J].中国科学,1989,9(4):317-327.
[14] 裘善文,李取生,夏玉梅.东北平原西部沙地古土壤与全新世环境变迁[J].第四纪研究,1992,12(3):224-232.
[15] 陈渭南,高尚玉,孙忠.毛乌素沙地全新世地层化学元素特点及其古气候意义[J].中国沙漠,1994,14(1):22-30.
[16] 曹红霞,张云翔,岳乐平.毛乌素沙地全新世地层粒度组成特征及古气候意义[J].沉积学报,2003,21(3):482-486.
[17] 靳鹤龄,董光荣,左昕昕.滴哨沟湾地层沉积特征记录的毛乌素沙漠变迁[J].中国沙漠,2008,28(6):1064-1072.
[18] 徐叔鹰,徐德馥,石生仁.青海共和盆地的风沙堆积[J].中国沙漠,1982,2(3):1-8.
[19] 徐叔鹰,张维信,徐德馥,等.青藏高原东北边缘地区冰缘发展探讨[J].冰川冻土,1984,6(2):15-24.
[20] 陶贞,董光荣.末次冰期以来贵南沙地土地沙漠化与气候变化的关系[J].中国沙漠,1994,14(2):42-48.
[21] 刘冰,靳鹤龄,孙忠.末次盛冰期以来青藏高原东北部共和盆地气候与环境变化研究进展[J].冰川冻土,2012,34(2):403-410.
[22] He Z,Zhou J,Yang L L,et al.Holocene dune mobility and forcing mechanisms at the Northern margin of the East Asian Monsoon[J].Acta Geological Sinica,2013,87(4):1168-1178.
[23] Zhao H,Lu Y C,Yin J H.Optical dating of Holocene sand dune activities in the Horqin sand-fields in inner Mongolia,China,using the SAR protocol[J].Quaternary Geochronology,2007,2:29-33.
[24] Yang L H,Wang T,Zhou J,et al.OSL chronology and possible forcing mechanisms of dune evolution in the Horqin dunefield in northern China since the Last Glacial Maximum[J].Quaternary Research,2012,78,185-196.
[25] Yang L H,Zhou J,Lai Z P,et al.Lateglacial and Holocene dune evolution in the Horqin dunefield of northeastern China based on luminescence dating[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,296:44-51.
[26] 弋双文,鹿化煜,周亚利,等.晚第四纪科尔沁沙地干湿变化的黄土记录[J].中国沙漠,2006,26(6):869-874.
[27] 弋双文,鹿化煜,曾琳,等.末次盛冰期以来科尔沁沙地古气候变化及其边界重建[J].第四纪研究,2013,33(2):206-217.
[28] Sun J M,Li S H,Han P,et al.Holocene environmental changes in the central Inner Mongolia,based on single-aliquotquartz op tical dating and mu lti-p roxy study of dune sands[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2006,233(1/2):51-62.
[29] Liu B,Jin H L,Sun L Y,et al.Holocene moisture change revealed by the Rb/Sr ratio of aeolian deposits in the southeastern Mu Us Desert,China[J].Aeolian Research,2014,13:109-119.
[30] Jia F F,Lu R J,Gao S Y,et al.Holocene aeolian activities in the southeastern Mu Us Desert,China[J].Aeolian Research,2015,19:267-274.
[31] 马冀,岳乐平,杨利荣,等.毛乌素沙漠东南缘全新世剖面光释光年代及古气候意义[J].第四纪研究,2011,31(1):120-129.
[32] 徐志伟,鹿化煜,弋双文,等.末次盛冰期和全新世大暖期毛乌素沙地的空间变化[J].第四纪研究,2013,33(2):218-227.
[33] 刘冰,靳鹤龄,孙忠,等.全新世共和盆地沙地时空演化及其驱动机制[J].中国沙漠,2014,34(4):982-991.
[34] Qiang M R,Chen F H,Song L,et al.Late Quaternary aeolian activity in Gonghe Basin,northeastern Qinghai-Tibetan Plateau,China[J].Quaternary Research,2013,79,403-412.
[35] Qiang M R,Jin Y X,Liu X X,et al.Late Pleistocene and Holocene aeolian sedimentation in Gonghe Basin,northeastern Qinghai-Tibetan Plateau:variability,processes,and climatic implications[J].Quaternary Science Reviews,2016,132:57-73.
[36] Liu X J,Lai Z P,Yu L P,et al.Luminescence chronology of aeolian deposits from the Qinghai Lake area in the Northeastern Qinghai-Tibetan Plateau and its palaeoenvironmental implications[J].Quaternary Geochronology,2012,10:37-43.
[37] Lu H Y,Zhao C F,Mason J,et al.Holocene climatic changes revealed by aeolian deposits from the Qinghai Lake area (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms[J].The Holocene,2011,21:297-304.
[38] Stauch G.Geomorphological and palaeoclimate dynamics recorded by the formation of aeolian archives on the Tibetan Plateau[J].Earth-Science Reviews,2015,150:393-408.
[39] 高尚玉,陈渭南,靳鹤龄,等.全新世中国季风区西北缘沙漠演化初步研究[J].中国科学,1993,23(2):202-208.
[40] Lancaster N.Development of linear dunes in the southwestern Kalahari,southern Africa[J].Journal of Arid Environments,1988,14(3):233-244.
[41] Lu H Y,Miao X D,Zhou Y L,et al.Late Quaternary aeolian activity in the Mu Us and Otindag dune fields (North China) and lagged response to in solation forcing[J].Geophysical Research Letters,2005,32(21):365-370.
[42] Jin H L,Sun L Y,Sun Z.Millennial-scale evolution of Hunshandake Desert and climate change during the Holocene in Inner Mongolia,northern China[J].Sciences in Cold and Arid Regions,2010,2(6):505-513.
[43] Sun J M,Yin G M,Ding Z L,et al.Thermoluminescence chronology of sand profiles in the Mu Us Desert,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1998,144(1/2):225-233.
[44] 刘冰,靳鹤龄,孙忠.中晚全新世科尔沁沙地演化与气候变化[J].中国沙漠,2013,33(1):77-86.
[45] 杨帆,靳鹤龄,李孝泽,等.中晚全新世毛乌素沙地东南部气候变化过程[J].中国沙漠,2017,37(3):431-438.
[46] Feng Z D,An C B,Wang H B.Holocene climatic and environmental changes in the arid and semi-arid areas of China:a review[J].The Holocene,2006,16(1):119-130.
[47] Chen F H,Yu Z,Yang M,et al.Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history[J].Quaternary Science Reviews,2008,27(3/4):351-364.
[48] Mason J A,Lu H Y,Zhou Y L,et al.Dune mobility and aridity at the desert margin of northern China at a time of peak monsoon strength[J].Geology,2009,37:947-950.
[49] 刘冰.末次盛冰期以来青藏高原气候变化与沙地演化[D].兰州:中国科学院寒区旱区环境与工程研究所,2013.
[50] Qiang M R,Liu Y Y,Jin Y X,et al.Holocene record of eolian activity from Genggahai Lake,northeastern Qinghai-Tibetan Plateau,China[J].Geophysical Research Letters,2014,41:589-595.
[51] Madsen D B,Ma H Z,Rhode D,et al.Age constraints on the late Quaternary evolution of Qinghai Lake,Tibetan Plateau[J]. Quaternary Research,2008,69:316-325.
[52] Dietze E,Wünnemann B,Hartmann K,et al.Early to mid-Holocene lake high-stand sediments at Lake Donggi Cona,northeastern Tibetan Plateau,China[J].Quaternary Research,2013,79:325-336.
[53] Hudson A M,Quade J.Long-term east-west asymmetry in monsoon rainfallon the Tibetan Plateau[J].Geology,2013,41:351-354.
[54] Colman S M,Yu S Y,An Z S,et al.Late Cenozoic climate changes in China's western interior:a review of research on Lake Qinghai and comparison with other records[J].Quaternary Science Reviews,2007,26:2281-2300.
[55] Shen J,Liu X Q,Wang S M,et al.Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years[J].Quaternary International,2005,136:131.
[56] Chen F H,Wu D,Chen J H,et al.Holocene moisture and East Asian summer monsoon evolution in the northeastern Tibetan Plateau recorded by Lake Qinghai and its environs:a review of conflicting proxies[J].Quaternary Science Reviews,2016,154:111-129.
[57] Heinrich H.Origin and consequences of cyclic ice rafting in the northeastern Atlantic Ocean during the past 130,000 years[J].Quaternary Research,1988,29:142-152.
[58] Dansgaard W,White J W C,Johnsen S J.The abrupt termination of the Y.D.climate event[J].Nature,1989,339:532-536.
[59] Bond G,Showers W,Cheseby M,et al.A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates[J].Science,1997,278(5341):1257-1266.
[60] Linsley B K.Oxygen-isotope record of sea level and climatic variations in the Sulu Sea over the past 150,000 years[J].Nature,1996,380(6571):234-237.
[61] Schulz H,Rad U,Erlenkeuser H.Correlation betwee Arabian Sea and Greenland climate oscillations of the past 110,000 years[J].Nature,1998,393(6680):54-57.
[62] Genty D,Blamart D,Ouahdi R,et al.Precise dating of Dansgaard-Oeschger climate oscillations in western Europe from stalagmite data[J].Nature,2003,421(6925):833-837.
[63] Fleitmann D,Burns S J,Mudelsee M,et al.Holocene forcing of the Indian monsoon recorded in a stalagmite from Southern Oman[J].Science,2003,300(5626):1737-1739.
[64] Wang Y J,Wu J Y,Liu D B,et al.A quick cooling event of the East Asian monsoon responding to Heinrich Event 1:evidence from stalagmite delta O-18 records[J].Science in China Series D-Earth Sciences,2002,45(1):88-96.
[65] Zhou W J,Lu X F,Wu Z K,et al.Peat record of Holocene climate changes and accelerator radio active timing[J].Chinese Science Bulletin,2001,46(12):1040-1044.
[66] Hong B,Liu C Q,Ling Q H,et al.Temperature evolution from the δ¹⁸O record of Hani peat,Northeast China,in the last 14000 years[J].Science in China Series D:Earth Sciences,2009,52(7):952-964.
[67] Liu J Q,Lu H Y,Negendank J,et al.Periodicity of Holocene climatic variations in the Huguangyan Maar Lake[J].Chinese Science Bulletin,2000,45(18):1712-1717.
[68] Chen F H,Zhu Y,Li J J,et al.Abrupt Holocene changes of the Asian monsoon at millennial-and centennial-scales:evidence from lake sediment document in Minqin Basin,NW China[J].Chinese Science Bulletin,2001,46(23):1942-1947.
[69] An Z S,Porter S C.Millennial-scale climatic oscillations during the last interglaciation in central China[J].Geology,1997,25(7):603-606.
[70] 郭正堂,刘东生,吴乃琴,等.最后两个冰期黄土中记录的Heinrich型气候节拍[J].Quaternary Sciences,1996,16(1):21-30.
[71] 刘冰,靳鹤龄,孙忠.近6 ka以来科尔沁沙地东部气候变化记录[J].中国沙漠,2011,31(6):1398-1405.
[72] Niu D F,Li B S,Du S H,et al.Cold events of Holocene indicated by primary elements distribution of the high-resolution sand dunes in the Salawusu River Valley[J].Journal of Geographical Sciences,2008,18(1):26-36.
[73] Sun A,Feng Z.Holocene climatic reconstructions from the fossil pollen record at Qigai Nuur in the southern Mongolian Plateau[J].Holocene,2013,23:1391-1402.
[74] Liu B,Jin H L,Sun L Y,et al.Geochemical evidence for Holocene millennialscale climaticand environmental changes in the south eastern Mu Us Desert,northern China[J].International Journal of Earth Sciences,2015,104:1889-1900.
[75] Miao Y F,Jin H L,Cui J X.Human activity accelerating the rapid desertification of the Mu Us Sandy Lands,North China[J].Scientific Reports,2016,6:23003.
[76] Liu B,Jin H L,Sun L Y,et al.History of moisture change derived from slope sediments of the eastern Gonghe Basin (northeastern Qinghai-Tibetan Plateau) during the last 17 ka[J].Geological Journal,2016,52:583-593.
[77] 刘冰,靳鹤龄,孙忠,等.共和盆地开额泥炭剖面粒度敏感组分提取与全新世气候环境变化[J].海洋地质与第四纪地质,2013,33(4):125-134.
[78] 于学峰,周卫健,Lars G F,等.青藏高原东部全新世冬夏季风变化的高分辨率泥炭记录[J].中国科学,2006,36(2):182-187.
[79] Lu H Y,Miao X D,Zhou Y L,et al.Late Quaternary aeolian activity in the Mu Us and Otindag dune fields (North China) and lagged respon se to in solation forcing[J].Geophysical Research Letters,2005,32(21):365-370.
[80] Hong Y T,Hong B,Lin Q H,et al.Correlation between Indian Oceansummer monsoon and North Atlantic climate during the Holocene[J].Earth and Planetary Sciences Letters,2003,211:371-380.
[81] 董光荣,李保生,高尚玉,等.鄂尔多斯高原第四纪古风成砂的发现及其意义[J].科学通报,1983,16:998-1001.
[82] 靳鹤龄,苏志珠,孙良英,等.浑善达克沙地全新世气候变化[J].科学通报,2004,9(15):1532-1536.
[83] 靳鹤龄,苏志珠,孙忠.浑善达克沙地全新世中晚期地层化学元素特征及其气候变化[J].中国沙漠,2003,23(4):366-371.
[84] 李森,孙武,李孝泽,等.浑善达克沙地全新世沉积特征与环境演变[J].中国沙漠,1995,15(4):323-331.
[85] 高全洲,陶贞,董光荣,等.巴丹吉林沙漠查格勒布鲁剖面的沉积地球化学特征[J].地理学报,1998,53:44-51.
[86] 陈渭南,高尚玉,孙忠,等.毛乌素沙地全新世地层化学元素特点及其古气候意义[J].中国沙漠,1994,14(1):22-30.
[87] 舒培仙.毛乌素沙漠现代沙丘沙的理化特性及其对重建沙区古环境的指示意义[D].广州:华南师范大学,2015.

Advances in the Study of Sandy Land Evolution and Driving Mechanism in the Monsoonal Marg in Area in China during the Holocene Epoch

PDF

Knowledge

Abstract

Cite this article

share this article

References

Related Articles 15

Recommended Articles

Metrics

Comments

[1]	Zhao Duoping, An Shuo, Miao Hong, Geng Yirui, Zhao Weiyi, Xie Lijuan. Influencing Factors and Driving Mechanism of Desert Non-traditional Festival Tourism-A Case of the Desert E-clan Hero Association in Alxa,China [J]. Journal of Desert Research, 2019, 39(5): 80-87.
[2]	Liu Zhenyu, Jin Heling, Liu Bing, Xue Wenping. Desert Evolution during the Mid Holocene Reflected by Grain-size Variation of Aeolian Sand and Paleosoil Sequence Records from Mu Us Sandy Land [J]. Journal of Desert Research, 2019, 39(1): 88-96.
[3]	Wang Zhigang, Li Zhiwen, Li Wubiao, Ma Zeyuan, Wang Zhenzhen. Climatic Change Recorded by Aeolian Deposition in the Houtian Section of Nanchang during the Last Glacial Period [J]. Journal of Desert Research, 2018, 38(6): 1200-1208.
[4]	Liu Miaomiao, Su Zhizhu, Kong Mengyuan, Zhang Caixia, Li Jinchang, Wang Guoling, Li Xiang. Climatic Change Reflected by Geochemical Features in Datong Basin, North China since 220 ka BP [J]. Journal of Desert Research, 2018, 38(2): 278-285.
[5]	Wan Wei, Yan Changzhen, Xiao Shengchun, Xie Jiali, Qian Dawen. Process, Spatial Pattern and Driving Mechanisms of the Aeolian Desertification in the Alxa Plateau from 1975 to 2015 [J]. JOURNAL OF DESERT RESEARCH, 2018, 38(1): 17-29.
[6]	Xiao Shengchun, Chen Xiaohong, Ding Aijun. Study Process of Climate Changes, Environment Evolution and Its Driving Mechanism in the Last Two Centuries in the Alxa Desert [J]. JOURNAL OF DESERT RESEARCH, 2017, 37(6): 1102-1110.
[7]	Li Xiaoying, Yao Zhengyi, Wang Hongwei, Xiao Jianhua. Driving Mechanism of Sandy Desertification in Guinan, Qinghai, China [J]. JOURNAL OF DESERT RESEARCH, 2016, 36(6): 1539-1546.
[8]	Liu Zhengyao, Dong Zhibao, Wang Jianbo, Cui Xujia, Zhang Yu, Jiao Yuanlei, Luo Wanyin, Lu Junfeng, Yang Linhai, Li Jiyan, Wang Meng. Vegetation Characteristics in the Marginal Areas of the Badain Jaran Desert [J]. JOURNAL OF DESERT RESEARCH, 2016, 36(5): 1348-1356.
[9]	Yao Zhengyi, Li Xiaoying, Xiao Jianhua. Driving Mechanism of Sandy Desertification around the Qinghai Lake [J]. JOURNAL OF DESERT RESEARCH, 2015, 35(6): 1429-1437.
[10]	Cai Xiaomin, Miao Yunfa, Jin Heling, Liu Bing, Yan Yongyao. Mid-Holocene Charcoal Records and Fire History in the East Edge of the Mu Us Sandy Land, China [J]. JOURNAL OF DESERT RESEARCH, 2015, 35(5): 1156-1162.
[11]	Li Xiaoying, Yao Zhengyi, Wang Hongwei, Xiao Jianhua. The Driving Mechanism of Sandy Desertification in the Zoige Basin of China [J]. JOURNAL OF DESERT RESEARCH, 2015, 35(1): 51-59.
[12]	Liu Bing, Jin Heling, Sun Zhong, Su Zhizhu, Zhang Caixia. Spatiotemporal Evolution of Sandy Land in the Gonghe Basin during the Holocene Period and Its Possible Driving Mechanism [J]. JOURNAL OF DESERT RESEARCH, 2014, 34(4): 982-991.
[13]	LU Jun-feng, DONG Zhi-bao, HU Guang-yin, SONG Xiang, WEI Zhen-hai. Aeolian Desertification Development and Its Causes in Maqu County of Gansu Province, China [J]. JOURNAL OF DESERT RESEARCH, 2012, 32(3): 604-609.
[14]	ZHANG Qiang;;LI Yu;CHEN Li-hua. Major Characteristics, Key Issues and Coping Strategies of Climate Change [J]. JOURNAL OF DESERT RESEARCH, 2011, 31(2): 492-499.
[15]	PU Zong-chao;ZHANG Shan-qing;LI Jing-lin;WANG Sheng-lan;LIU Hai-rong;LI Jing. Climate Change of Area around Taklimakan Desert during 1961—2007 [J]. JOURNAL OF DESERT RESEARCH, 2010, 30(2): 413-421.