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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第32卷

期数:

2010年第01期

页码:

81-88

栏目:

水资源与环境

出版日期:

2010-03-15

文章信息/Info

Title:

Holocene Climate and Environmental Changes in the Eolian Sand Section of Yulin, Shaanxi Province

文章编号:

1672-6561(2010)01-0081-08

作者:

陈淑娥; 樊双虎; 刘秀花; 董汉文; 陆璐; 王莉丽

(长安大学 地球科学与资源学院,陕西 西安 710054)

Author(s):

CHEN Shu-e;  FAN Shuang-hu;  LIU Xiu-hua;  DONG Han-wen;  LU Lu;  WANG Li-li

(School of Earth Sciences and Resources, Chang'an University, Xi'an 710054, China)

关键词:

全新世; 气候; 风沙活动; 环境变化; 榆林

Keywords:

Holocene;  climate;  eolian sand activity;  environmental change;  Yulin

分类号:

P532

DOI:

-

文献标志码:

A

摘要:

榆林长城沿线处于环境变化敏感带,其风沙滩区沉积剖面的磁化率和粒度分析结果显示,该区全新世早期11500～10000aBP随着全球气候的逐渐转暖,磁化率、黏粒和粉沙含量逐渐增高;全新世中期的10000～4500aBP气候相对比较湿润,植被覆盖度增大,风沙活动减弱,地表沉积物当中粉沙和黏土成分含量显著增大,风化成壤作用增强,地表发育沙质弱古土壤;全新世中期后段的4500～3000aBP期间,气候以比较温和湿润为主,但在4200～4000aBP出现一个气候干旱事件,风沙活动强烈;近3000a以来,气候显著干旱化,波动频繁,地表风沙沉积物显著变粗,表现出有5次沙漠扩张。该区生态环境演化、人文历史变迁基本上是自然因素与人为活动综合作用的结果,以自然演化为主,近代人为因素对环境变化起着加强和放大作用。

Abstract:

The eolian-sand section along the Great Wall in Yulin, Shaanxi province, is sensitive to climate and environmental changes. The magnetic susceptibility and particle-size analysis in Dabaodang profile showed that the early Holocene(11 500～10 000 a BP), was a transition during the change in eolian regime and dust source because of the weakened northwesterly monsoon along with the global climatic amelioration; the middle Holocene(10 000～4 500 a BP)was relatively humid, while vegetation coverage increased, aeolian activities weakened, silt and clay compositions were significantly increased, weathering pedogenesis was enhanced, and sandy weak paleosols were developed; the late stage of the middle Holocene(4 500～3 000 a BP)was mild and humid in general, but at 4 200～4 000 a BP an arid climate event occurred, with intensive eolian sand activities; the climate was droughty and fluctuating frequently in recent 3 000 a, while eolian sand was significantly coarser, which showing 5 times desert expansions. Natural factors played an important role in the environmental changes in this area, and human activities greatly strengthened and amplified the changes at the modern times.

参考文献/References:

[1] 邓 辉,夏正楷,王琫瑜.从统万城的兴废看人类活动对生态环境脆弱地区的影响[J]. 中国历史地理论丛,2001,16(2):104-113.
[2] 王尚义,董靖保.统万城的兴废与毛乌素沙地之变迁[J].地理研究,2001,20(3):347-353.
[3] Denton G H,Karlen W.Holocene Climatic Variations:Their Pattern and Possible Cause[J]. Quaternary Research,1973,3(2):155-174.
[4] O'Brien S R,Mayewski P A,Meeker L D,et al.Complexity of Holocene Climate as Reconstructed from a Greenland Ice Core[J].Science,1995,270:1962-1964.
[5] 施雅风,孔昭宸,王苏民,等.中国全新世大暖期的气候波动与重要事件[J].中国科学(B辑),1992,22(12):1300-1308.
[6] 魏明建,李虎侯.全新世黑垆土中千年尺度的全球变化记录[M].香港:国际科学出版社,1998.
[7] 郭正堂, Petit-Maire N,刘东生.全新世期间亚洲和非洲干旱区环境的短尺度变化[J]. 古地理学报,1999,1(1):68-74.
[8] 黄春长,庞奖励,黄 萍,等.关中盆地西部黄土台塬全新世气候事件研究[J].干旱区地理,2002,25(1):10-15.
[9] Mayewski P A,Rohling E E,Stager J C,et al.Holocene Climate Variability[J].Quaternary Research,2004,62(3):243-255.
[10] 施少华.中国全新世高温气候环境与新石器时代古文化的发展[C]∥施雅风.中国全新世大暖期气候与环境.北京:海洋出版社,1992:185-191.
[11] 付淑清,陈淑娥,魏明建,等.甘肃通渭县黄土堆积区全新世环境变迁[J].地球科学与环境学报,2005,27(4):71-75.
[12] 许靖华.太阳、气候、饥荒与民族大迁移[J].中国科学(D辑),2000,28(4):366-384.
[13] Huang C C,Zhou J, Pang J L,et al.A Regional Aridity Phase and Its Possible Cultural Impact During the Holocene Megathermal in the Guanzhong Basin,China[J].The Ho-locene,2000,10(1):135-142.
[14] 周群英,黄春长.渭河流域全新世环境演变对人类文化发展的影响[J].地理科学进展,2008,27(5):12-18.
[15] 钟 巍,熊黑钢,舒 强.全新世以来南疆地区气候环境演变与人类活动的关系[J].地理科学进展,2000,19(4):307-316.
[16] Hoelzmann P,Keding B,Berke H,et al.Environmental Change and Archaeology:Lake Evolution and Human Occupation in the Eastern Sahara During the Holocene[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2001,169(3):193-217.
[17] 成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京:地质出版社,1978.
[18] Huang C C,Pang J L,Zhao J B.Chinese Loess and the Evolution of the East Asia Monsoon[J].Progress in Physical Geography,2000,24(1):75-96.
[19] Porter S C,An Z S.Correlation Between Climate Events in the North Atlantic and China During the Last Glaciation[J].Nature,1995,375:305-308.
[20] Ding Z,Yu Z,Rutter N W,et al.Towards an Orbital Time Scale for Chinese Loess Deposits[J].Quaternary Science Reviews,1994,13(1):39-70.
[21] 孙东怀,安芷生,苏瑞侠,等.古环境中沉积物粒度组分分离的数学方法及其应用[J].自然科学进展,2001,11(3):269-276.
[22] 李智佩,岳乐平,薛祥煦,等.毛乌素沙地东南部边缘不同地质成因类型土地沙漠化粒度特征及其地质意义[J].沉积学报,2006,24(2):267-275.
[23] 孙东怀,鹿化煜,Rea D,等.中国黄土粒度的双峰分布及其古气候意义[J].沉积学报,2000,18(3):327-335.
[24] Kukla G,Heller F,Liu X M,et al.Pleistocene Climates in China Dated by Magnetic Susceptibility[J].Geology,1988,16(9):811-814.
[25] An Z S,Kukla G J,Porter S C,et al.Magnetic Susceptibility Evidence of Monsoon Variation on the Loess Plateau of Central China During the Last 130 000 Years[J].Quaternary Research,1991,36(1):29-36.
[26] Huang C C,Pang J L,Chen S E,et al.Holocene Dust Accumulation and the Formation of Polycyclic Cinnamon Soils(Luvisols)in the Chinese Loess Plateau[J].Earth Surface Processes and Landforms,2003,28(12):1259-1270.
[27] 周群英,黄春长.西周沣镐遗址全新世土壤研究[J].地理科学, 2003,23(3):310-315.
[28] 丁仲礼,孙继敏,刘东生.联系沙漠—黄土演变过程中耦合关系的沉积学指标[J].中国科学(D辑),1999,29(1):82-87.
[29] 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黄土记录——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.
[30] 周卫建,卢雪峰,武振坤,等.若尔盖高原全新世气候变化的泥炭记录与加速器放射性碳测年[J].科学通报,2001,46(12):1040-1044.
[31] 刘嘉麒,吕厚远,Negendank J,等.湖光岩玛珥湖全新世气候波动的周期性[J].科学通报,2000,45(11):1190-1195.
[32] 安成邦,冯兆东,唐领余,等.甘肃中部4 000年前环境变化与古文化变迁[J].地理学报,2003,58(5):743-748.
[33] 马振兴,黄俊华,魏 源,等.鄱阳湖沉积物近8 ka来有机质碳同位素记录及其古气候变化特征[J].地球化学,2004,33(3):279-285.
[34] 邵晓华,汪永进,程 海,等.全新世季风气候演化与干旱事件的湖北神农架石笋记录[J].科学通报,2006,51(1):80-86.
[35] 谭亮成,安芷生,蔡演军,等.4.2 ka BP 气候事件在中国的降雨表现及其全球联系[J].地质论评,2008,54(1):94-104.
[36] Chen F H,Shi Q,Wang J M.Environmental Changes Documented by Sedimentation of Lake Yiema in Arid China Since the Late Glaciation[J].Journal of Paleolimnology,1999,22(2):159-169.
[37] Huang C C,Zhao S C,Pang J L,et al.Climatic Aridity and the Relocations of the Zhou Culture in the Southern Loess Plateau of China[J].Climatic Change,2003,61(3):361-378.
[38] Huang C C,Jia Y F,Pang J L,et al.Holocene Colluviation and Its Implications for Tracing Human-induced Soil Erosion and Redeposition on the Piedmont Loess Lands of the Qinling Mountains,Northern China[J].Geoderma,2006,136(3/4):838-851.
[39] Dahl S O,Nesje A.Holocene Glacier Fluctuations at Hardangerjokulen,Central-southern Norway:a High-resolution Compo-site Chronology from Lacustrine and Terrestrial Deposits[J].The Holocene,1994,4(3):269-277.
[40] Gasse F.Diatom-inferred Salinity and Carbonate Oxygen Isotopes in Holocene Waterbodies of the Western Sahara and Sahel(Africa)[J].Quaternary Science Reviews,2002,21(7):737-767.
[41] Arz H W,Lamy F, Pätzold J.A Pronounced Dry Event Recorded Around 4.2 ka in Brine Sediments from the Northern Red Sea[J].Quaternary Research,2006,66(3):432-441.
[42] Booth R K,Jackson S T,Forman S L,et al.A Severe Centennial-scale Drought in Midcontinental North America 4 200 Years Ago and Apparent Global Linkages[J].The Holocene,2005,15(3):321-328.
[43] 黄春长.渭河流域3 100年前资源退化与人地关系演变[J].地理科学,2001,21(1):30-35.
[44] 姚檀栋,杨志红,皇翠兰,等.近2 ka来高分辨的连续气候环境变化记录——古里雅冰芯近2 ka记录初步研究[J].科学通报,1996,41(12):1103-1106.
[45] 姚檀栋.古里雅冰芯近2000年来气候环境变化记录[J].第四纪研究,1997,17(1):52-61.
[46] Booth R K,Notaro M,Jackson S T,et al.Widespread Drought Episodes in the Western Great Lakes Region During the Past 2 000 Years:Geographic Extent and Potential Mechanisms[J].Earth and Planetary Science Letters,2006,242(3/4):415-427.
[47] Lamb H H.The Early Medieval Warm Epoch and Its Sequel[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1965,1:13-37.
[48] 竺可桢.中国近五千年来气候变迁的初步研究[J].考古学报,1972(1):15-38.
[49] 张德二.我国“中世纪温暖期”气候的初步推断[J].第四纪研究,1993,13(1):7-15.
[50] 吴宏岐,党安荣.隋唐时期气候冷暖特征与气候波动[J].第四纪研究,1998,18(1):31-38.
[51] 陕西省地方志编纂委员会.陕西省志第十三卷:水利志[M].西安:陕西人民出版社,1999.
[52] 赵景波,顾 静,邵天杰.唐代渭河流域与泾河流域涝灾研究[J].自然灾害学报,2009,18(2):50-55.
[53] 王绍武.小冰期气候的研究[J].第四纪研究,1995,15(3):202-212.
[54] 王苏民,刘 健,周 静.我国小冰期盛期的气候环境[J].湖泊科学,2003,15(4):369-376.
[55] 王会昌.2 000年来中国北方游牧民族南迁与气候变化[J].地理科学,1996,16(3):274-279.
[56] 王 川,杜继稳,杜川利,等.530年来陕北气候变化与东部地区关系分析[J].西北大学学报:自然科学版,2004,34(2):238-241.
[57] 邢福来.统万城遗址考古发掘的新收获[J].中国历史地理论丛,2003,18(专辑):89-94.

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备注/Memo

备注/Memo:

收稿日期:2009-07-20
基金项目: 陕西省自然科学基金项目(2006D04)
作者简介: 陈淑娥(1964-),女,陕西三原人,理学博士,从事第四纪地质学和古生物地层学的教学与研究。E-mail:shuechen@chd.edu.cn

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更新日期/Last Update: 2010-03-20