内蒙古查干淖尔湖2000a以来气候环境演变的沉积记录

江南; 王永; 董进; 杨劲松; 田飞; 刘瑾; 汤文坤

内蒙古查干淖尔湖2000a以来气候环境演变的沉积记录

1. 中国地质科学院地质研究所, 北京 100037;
2. 中国地质科学院水文地质环境地质研究所, 河北石家庄 050061

收稿日期: 2015-08-15

修回日期: 2016-02-24

刊出日期: 2016-06-15

Sedimentary record of environmental evolution since ca 2000 cal yr B P ago in Qehan Lake, Inner Mongolia

1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
2. Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang 050061, Hebei, China

Received Date: 15 August 2015

Revised Date: 24 February 2016

Publish Date: 15 June 2016

摘要

摘要: 以内蒙古东部查干淖尔湖西湖深97cm的浅井剖面为对象,根据取得的7个AMS¹⁴C测年数据建立其2070cal a BP以来的年代序列,结合孢粉组合特征与粒度组成的综合分析,重建该地区2070cal a BP以来气候环境变化过程。研究结果表明,查干淖尔湖2070cal a BP以来气候环境变化具体可以分为3个阶段:2070~1150cal a BP,孢粉总浓度较高,以蒿属、藜科为主,沉积物各粒级组分变幅较小且以粉砂为主,水动力条件较弱,湖水位较高,气候温凉偏湿;1150~825cal a BP,孢粉总浓度显著降低,耐旱的麻黄属达到最高值,沉积物粗颗粒含量显著增加,水动力条件增强,湖水位降低,气候冷干,其中940~870cal a BP期间气候极端干旱;825cal a BP以来,总体温暖偏湿,有冷干事件发生。太阳活动可能是导致查干淖尔湖过去2000a气候变化的主要驱动力。
Abstract: A 97cm long lacustrine section from Qehan Lake, situated in eastern Inner Mongolia, was used to reestablish the environ-ment and climate changes since the last 2070cal a BP. The chronological framework was built on seven AMS¹⁴C ages. On the basis of pollen-spore characteristics and grain size distribution, three environmental stages can be recognized. From 2070~1150cal a BP, this interval was featured by high total pollen concentration, with the dominance of Artemisia and Chenopodiaceae; lacustrine sediments were mainly composed of silt and each fraction presented quite low amplitudes of increases, indicating the weak hydrological condi-tions and high lake level; this period was characterized by a warm, cool and slightly humid climate. During the period of 1150~825cal a BP, the total pollen concentration significantly decreased and the pollen percentages of xerophyte, especially Ephedra, reached the maximum; the coarse particle content showed obviously increase, sugge sting strong hydrodynamic conditions and low lake level; so in this period, the climate was cold and dry,especially from 940cal a BP to 870cal a BP. Since 825cal a BP, the climate mainly tend-ed to become warm and slightly humid with the occurrence of cold and dry oscillations. Solar activities might have been the domi-nant force that drove the climate changes in Qehan Lake area since 2000 years ago.
- 2000a /
- pollen /
- grain size /
- climate change /
- Qehan Lake /
- Inner Mongolia

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参考文献(79)

[1]	Pèrez-Obiol R, Julià R. Climatic Change on the Iberian Peninsula Recorded in a 30000-Yr Pollen Record from Lake Banyoles[J]. Quaternary Research, 1994, 41(1):91-98.
[2]	Wang H, Liu H, Liu Y, et al. Mineral magnetism of lacustrine sedi-ments and Holocene palaeoenvironmental changes in Dali Nor area, southeast Inner Mongolia Plateau, China[J]. Palaeogeography, Pal-aeoclimatology, Palaeoecology, 2004, 208(3/4):175-193.
[3]	董进,王永,张世红,等.内蒙古黄旗海全新世湖泊沉积物粒度分析及其沉积学意义[J]. 地质通报, 2014, 33(10):1514-1522.
[4]	关友义,王永,姚培毅,等. 内蒙古克什克腾旗浩来呼热古湖泊全新世以来的环境演变[J]. 地质通报, 2010, 29(6):891-900.
[5]	吴健,沈吉. 兴凯湖沉积物有机碳和氮及其稳定同位素反映的28kaBP以来区域古气候环境变化[J]. 沉积学报, 2010, 28(2):365-372.
[6]	孙青,储国强,李圣强,等. 硫酸盐型盐湖中的长链烯酮及古环境意义[J]. 科学通报, 2004, 49(17):1789-1792.
[7]	Mann M E, Zhang Z, Hughes M K, et al. Proxy-based reconstruc-tions of hemispheric and global surface temperature variations over the past two millennia[J]. Proc. Natl. Acad. Sci. USA, 2008, 105(36):13252-13257.
[8]	IPCC. Climate Change 2014:Synthesis Report[C]//Contribution of Working Groups Ⅰ, Ⅱ and Ⅲ to the Fifth Assessment Report of the Intergovernmental Panel. Geneva, Switzerland:IPCC, 2014:1-155.
[9]	Consortium P K. Continental-scale temperature variability during the last two millennia[J]. Nature Geoscience, 2013, 6:339-346.
[10]	Reinemann S A, Porinchu D F, Macdonald G M, et al. A 2000-yr reconstruction of air temperature in the Great Basin of the United States with specific reference to the Medieval Climatic Anomaly[J]. Quaternary Research, 2014, 82(2):309-317.
[11]	葛全胜,郑景云,郝志新. 过去2000年亚洲气候变化(PAGESAsia2k)集成研究进展及展望[J]. 地理学报, 2015, 70(3):355-363.
[12]	葛全胜,郑景云,郝志新,等. 过去2000年中国气候变化研究的新进展[J]. 地理学报, 2014, 69(9):1248-1258.
[13]	Holmes J A, Cook E R, Yang B. Climate change over the past 2000 years in Western China[J]. Quaternary International, 2009, 194(1/2):91-107.
[14]	Ge Q, Hao Z, Zheng J, et al. Temperature changes over the past 2000 yr in China and comparison with the Northern Hemisphere[J]. Cli-mate of the Past, 2013, 9(3):1153-1160.
[15]	竺可桢. 中国近五千年来气候变迁的初步研究[J]. 中国科学, 1973, 2:168-189.
[16]	郑景云,郝志新,方修琦,等. 中国过去2000年极端气候事件变化的若干特征[J]. 地理科学进展, 2014, 33(1):3-12.
[17]	Yao T, Masson-Delmotte V, Gao J, et al. A review of climatic con-trols on δ18 O in precipitation over the Tibetan Plateau:Observa-tions and simulations[J]. Reviews of Geophysics, 2013, 51(4):525-548.
[18]	Baiqing X, Tandong Y. Dasuopu ice core record of atmospheric methane over the past 2000 years[J]. Science in China (Series D), 2001, 44(8):689-695.
[19]	Li H, Lee Z, Wan N, et al. The δ¹⁸O and δ¹³C records in an ara-gonite stalagmite from Furong Cave, Chongqing, China:A-2000-year record of monsoonal climate[J]. Journal of Asian Earth Scienc-es, 2011, 40(6):1121-1130.
[20]	张振克,吴瑞金,沈吉,等. 近2000年来云南洱海沉积记录的气候变化[J]. 海洋地质与第四纪地质, 2001, 21(2):31-35.
[21]	谢宏琴,贾国东,彭平安,等. 艾比湖二千余年来环境演变的地球化学记录[J]. 干旱区地理, 2005, 28(2):205-209.
[22]	Zhu H, Shao X, Yin Z, et al. August temperature variability in the southeastern Tibetan Plateau since AD 1385 inferred from tree rings[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2011, 305(1/4):84-92.
[23]	杨保,康兴成,施雅风. 近2000年都兰树轮10年尺度的气候变化及其与中国其它地区温度代用资料的比较[J]. 地理科学, 2000, (5):397-402.
[24]	Wang X, Cui L, Xiao J, et al. Stable carbon isotope of black carbon in lake sediments as an indicator of terrestrial environmental chang-es:An evaluation on paleorecord from Daihai Lake, Inner Mongo-lia, China[J]. Chemical Geology, 2013, 347:123-134.
[25]	Xiao J, Fan J, Zhai D, et al. Testing the model for linking grainsize component to lake level status of modern clastic lakes[J]. Qua-ternary International, 2015, 355:34-43.
[26]	Zhang J, Lai Z, Jia Y. Luminescence chronology for late Quaterna-ry lake levels of enclosed Huangqihai lake in East Asian monsoon marginal area in northern China[J]. Quaternary Geochronology, 2012, 10:123-128.
[27]	Wen R, Xiao J, Chang Z, et al. Holocene climate changes in the mid-high-latitude-monsoon margin reflected by the pollen re-cord from Hulun Lake, northeastern Inner Mongolia[J]. Quaterna-ry Research, 2010, 73(2):293-303.
[28]	王苏民,窦鸿身. 中国湖泊志[M]. 北京市:科学出版社, 1998:580.
[29]	任国玉. 内蒙古湖相沉积~¹⁴C年代测定中"硬水"影响的发现[J]. 湖泊科学, 1998, 10(3):80-82.
[30]	汪勇,沈吉,吴健,等. 湖泊沉积物~¹⁴C年龄硬水效应校正初探——以青海湖为例[J]. 湖泊科学, 2007, 19(5):504-508.
[31]	孙千里,周杰,肖举乐. 岱海沉积物粒度特征及其古环境意义[J]. 海洋地质与第四纪地质, 2001, 21(1):93-95.
[32]	王永,姚培毅,迟振卿,等. 内蒙古黄旗海全新世中晚期环境演变的沉积记录[J]. 矿物岩石地球化学通报, 2010, 29(2):149-156.
[33]	陈敬安,万国江,张峰,等. 不同时间尺度下的湖泊沉积物环境记录——以沉积物粒度为例[J]. 中国科学(D辑), 2003, 33(6):563-568.
[34]	Peng Y, Xiao J, Nakamura T, et al. Holocene East Asian mon-soonal precipitation pattern revealed by grain-size distribution of core sediments of Daihai Lake in Inner Mongolia of north-central China[J]. Earth and Planetary Science Letters, 2005, 233(3/4):467-479.
[35]	Campbell C. Late Holocene Lake Sedimentology and Climate Change in Southern Alberta, Canada[J]. Quaternary Research, 1998, 49(1):96-101.
[36]	强明瑞,陈发虎,周爱锋,等. 苏干湖沉积物粒度组成记录尘暴事件的初步研究[J]. 第四纪研究, 2006, 26(6):915-922.
[37]	沈吉,汪勇,羊向东,等. 湖泊沉积记录的区域风沙特征及湖泊演化历史:以陕西红碱淖湖泊为例[J]. 科学通报, 2006, 51(1):87-92.
[38]	Wentworth C K. A Scale of Grade and Class Terms for Clastic Sed-iments[J]. The Journal of Geology, 1992, 30(5):377-392.
[39]	黄思静. 用EXCEL计算沉积物粒度分布参数[J]. 成都理工学院学报, 1999, 26(2):98-100.
[40]	李月丛,许清海,阳小兰,等. 中国草原区主要群落类型花粉组合特征[J]. 生态学报, 2005, 25(3):555-564.
[41]	许清海,李月丛,阳小兰,等. 北方草原区主要群落类型表土花粉分析[J]. 地理研究, 2005, 24(3):394-402.
[42]	El-Moslinmany A P. Ecological significance of common nonarbo-real pollen:examples from drylands of the Middle East[J]. Review of Palaeobotony and Palynology, 1990, 64:343-350.
[43]	Huang X Z, Chen F H, Fan Y X, et al. Dry late-glacial and early Holocene climate in arid central Asia indicated by lithological and palynological evidence from Bosten Lake, China[J]. Quaternary In-ternational, 2009, 194(1/2):19-27.
[44]	Xu Q, Li Y, Tian F, et al. Pollen assemblages of tauber traps and surface soil samples in steppe areas of China and their relationships with vegetation and climate[J]. Review of Palaeobotany and Paly-nology, 2009, 153(1/2):86-101.
[45]	Xiao J, Xu Q, Nakamura T, et al. Holocene vegetation variation in the Daihai Lake region of north-central China:a direct indication of the Asian monsoon climatic history[J]. Quaternary Science Re-views, 2004, 23(14/15):1669-1679.
[46]	蒋庆丰,季峻峰,沈吉,等. 赛里木湖孢粉记录的亚洲内陆西风区全新世植被与气候变化[J]. 中国科学(D辑), 2013, 43(2):243-255.
[47]	张美良,程海,林玉石,等. 贵州荔波地区2000年来石笋高分辨率的气候记录[J]. 沉积学报, 2006, 24(3):339-348.
[48]	赵志丽,王永,迟振卿,等. 内蒙古辉腾锡勒全新世中晚期环境变迁的孢粉记录[J]. 地质力学学报, 2011, 17(1):103-110.
[49]	孙千里,周杰,沈吉,等. 北方环境敏感带岱海湖泊沉积所记录的全新世中期环境特征[J]. 中国科学(D辑), 2006, 36(9):838-849.
[50]	赵志丽,王永,姚培毅,等. 内蒙古中部达尔罕茂明安联合旗腾格尔诺尔湖泊沉积物记录的全新世晚期环境演变[J]. 地质通报, 2011, 31(8):1251-1255.
[51]	姚檀栋,徐柏青,段克勤,等. 青藏高原达索普冰心2ka来温度与甲烷浓度变化记录[J]. 中国科学(D辑), 2002, 32(4):346-352.
[52]	靳鹤龄,肖洪浪,张洪,等. 粒度和元素证据指示的居延海1.5ka BP来环境演化[J]. 冰川冻土, 2005, 27(2):233-240.
[53]	张美良,朱晓燕,程海,等. 贵州荔波1200年来石笋高分辨率的古气候环境记录[J]. 地球学报, 2009, 30(6):831-840.
[54]	张丽华,李钟模. 北京地区3500a来的气候与环境变迁——兼论昆明湖的沧桑[J]. 中国煤田地质, 2003, 15(5):42-43.
[55]	许清海,李月丛,赵登海,等. 中国北方典型灌丛群落表土花粉组合特征[J]. 古地理学报, 2006, 8(2):157-164.
[56]	Miao Y, Jin H, Liu B, et al. Natural ecosystem response and recov-ery after the 8.2 ka cold event:Evidence from slope sediments on the northeastern Tibetan Plateau[J]. Journal of Arid Environments, 2014, 104:17-22.
[57]	Zhang P, Cheng H, Edwards R L, et al. A test of climate, sun, and culture relationships from an 1810-year Chinese cave record[J]. Science, 2008, 322(5903):940-942.
[58]	Bard E, Raisbeck G, Yiou F O, et al. Solar irradiance during the last 1200 years based on cosmogenic nuclides[J]. Tellus B, 2000, 52B:985-992.
[59]	Lamb H H. The early medieval epoch and its sequel[J]. Palaeogeog-raphy, Palaeoclimatology, Palaeoecology, 1965, 1:13-37.
[60]	Lamb H H. Climate history and the modern world[M]. London:Methuen, 1982:171.
[61]	Bao Y. Late Holocene temperature fluctuations on the Tibetan Pla-teau[J]. Quaternary Science Reviews, 2003, 22(21/22):2335-2344.
[62]	金章东,沈吉,王苏民,等. 岱海的"中世纪暖期"[J]. 湖泊科学, 2002, 14(3):209-216.
[63]	葛全胜,郑景云,满志敏,等. 过去2000年中国温度变化研究的几个问题[J]. 自然科学进展, 2004, 14(4):91-97.
[64]	Dahljensen D, Mosegaord K, Gundestrup N, et al. Past Tempera-tures Directly from the Greenland Ice Sheet[J]. Science, 1998, 282(5387):268-271.
[65]	Gerald H H, Konrad A Hn, Daniel M S, et al. Southward Migration of the Intertropical Convergence Zone Through the Holocene[J]. Science, 2001, 293:1304-1308.
[66]	Frank McDermott, David P M, Hawkesworth C. Centennial-Scale Holocene Climate Variability Revealed by a High-Resolu-tion Speleothem δ¹⁸O Record from SW Ireland[J]. Science, 2001, 294:1328-1331.
[67]	王绍武. 中世纪暖期与小冰期[J]. 气候变化研究进展, 2010, 6(5):388-390.
[68]	曹建廷,王苏民,沈吉,等. 近千年来内蒙古岱海气候环境演变的湖泊沉积记录[J]. 地理科学, 2000, 20(5):391-396.
[69]	王绍武. 小冰期气候的研究[J]. 第四纪研究, 1995, 25(3):202-212.
[70]	许清海,肖举乐,中村俊夫,等. 孢粉记录的岱海盆地1500年以来气候变化[J]. 第四纪研究, 2004, 24(3):341-347.
[71]	Bond G, Kromer B, Beer J, et al. Persistent solar influence on North Atlantic climate during the Holocene[J]. Science, 2001, 294(5549):2130-2136.
[72]	Wang Y, Cheng H, Edwards R L, et al. The Holocene Asian Mon-soon:Links to Solar Changes and North Atlantic Climate[J]. Sci-ence, 2005, 308(5723):854-857.
[73]	Perry C A, Hsu K J. Geophysical, archaeological, and historical evi-dence support a solar-output model for climate change[J]. Proc Natl Acad Sci U S A, 2000, 97(23):12433-12438.
[74]	Stuiver M, Braziunas T F. Anthropogenic and solar components of hemispheric¹⁴C[J]. Geophysical Research Letters, 1998, 25(3):329-332.
[75]	Eddy J A. Climate and the changing sun[J]. Climatic Change, 1977, 1:173-190.
[76]	Tinsley B A. Influence of solar wind on the global electric circuit, and inferred effects on cloud microphysics,temperature,and dynam-ics in the troposphere[J]. Space Science Reviews, 2000, 94:231-258.
[77]	Shindell D, Rind D, Balachandran N, et al. Solar Cycle Variability, Ozone, and Climate[J]. Science, 1999, 284(5412):305-308.
[78]	Van Geel B, Raspopov O M, Renssen H, et al. The role of solar forcing upon climate change[J]. Quaternary Science Reviews, 1999, 18:331-338.
[79]	陈隆勋,朱乾根,罗会邦. 东亚季风[M]. 北京:气象出版社, 1991:28-45.

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内蒙古查干淖尔湖2000a以来气候环境演变的沉积记录

1. 中国地质科学院地质研究所, 北京 100037;2. 中国地质科学院水文地质环境地质研究所, 河北 石家庄 050061

Sedimentary record of environmental evolution since ca 2000 cal yr B P ago in Qehan Lake, Inner Mongolia

1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;2. Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang 050061, Hebei, China

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1. 中国地质科学院地质研究所, 北京 100037;
2. 中国地质科学院水文地质环境地质研究所, 河北石家庄 050061

1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China;
2. Institute of Hydrogeology and Environmental Geology, CAGS, Shijiazhuang 050061, Hebei, China