蒙古全新世气候变化研究进展

doi:10.11867/j.issn.1001-8166.2005.02.0240

地球科学进展 ›› 2005, Vol. 20 ›› Issue (2): 240 -247. doi: 10.11867/j.issn.1001-8166.2005.02.0240

蒙古全新世气候变化研究进展

汪卫国 ¹，冯兆东 ^2,3，P. Khosbayar ⁴，T.Narantsetseg ⁴

1.国家海洋局第三海洋研究所，福建厦门 361005；
2.兰州大学西部环境教育部重点实验室，甘肃兰州 730000；
3.Department of Earth and Environmental Studies, Montclair State University, New Jersey, USA；
4. Institute of Geology and Mineral Resources of the Mongolian Academy of Sciences, Ulaanbaatar, Mongolia

收稿日期:2003-10-17 修回日期:2004-06-01 出版日期:2005-02-25
通讯作者: 汪卫国 E-mail:wangwgg@hotmail.com
基金资助:
国家杰出青年科学基金项目“晚第四纪中东亚干旱—半干旱区环境系统对全球气候变化的贡献与响应”（编号：40025105）；国家自然科学基金重点项目“蒙古高原全新世气候环境时空变化的高分辨率重建”（编号：40331012）资助.

THE STUDIES OF HOLOCENE CLIMATE CHANGES IN MONGOLIA: A REVIEW

WANG Weiguo ¹;FENG Zhaodong ^2,3; P. Khosbayar ⁴;T.Narantsetseg ⁴

1.Third Institutes of Oceanography, SOA, Xiamen 361005, China；
2. Key Laboratory of Weatern China’s Environment Systems, MOE, Lanzhou University, Lanzhou 730000, China；
3. Department of Earth and Environmental Studies, Montclair State University, New Jersey, USA；
4. Institute of Geology and Mineral Resources of the Mongolian Academy of Sciences, Ulaanbaatar, Mongolia

Received:2003-10-17 Revised:2004-06-01 Online:2005-02-25 Published:2005-02-25

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简要地回顾了蒙古全新世气候变化研究。蒙古全新世气候变化研究侧重于对树轮、风成沉积和湖泊沉积物的研究。蒙古的树轮研究恢复了杭爱山（Hangai）地区过去1 783年以来的温度变化及蒙古中东部地区过去340多年以来的降水和径流量变化。蒙古全新世风成沉积主要分布在蒙古北部的走廊地带，全新世古土壤的层数可以和中国北方地区的古土壤层数对比。蒙古的湖泊研究显示蒙古全新世气候演化存在2种模式，即冷干—暖湿型和冷湿—暖干型，这2种模式以杭爱山为分界线。这说明蒙古全新世气候变化的复杂性，其水汽来源和水热组合存在差异。迄今为止，蒙古全新世气候变化的研究仍较薄弱，有待进一步加强研究。

关键词: 蒙古, 全新世, 气候变化

This article has a brief review on Holocene climate changes in Mongolia. The studies of Mongolian Holocene climate changes mainly focused on the records of tree-rings, eolian sediments and lacustrine sediments. 1 783years of temperature variability were inferred from tree-ring widths of Siberian pine at Hangai Mountain and about 340 years of precipitation and stream flow variability were reconstructed according to the data of tree-rings in east-central Mongolia. Eolian strata are distributed in the corridor running from Ulaanbaatar to Lake Baikal. The Holocene paleosols there can be correlated with that in Northern China. According to the studies of lacustrine sediments, there occur two Holocene climatic models, cool-dry/ warm-wetter model and cool-wetter/ warm-dry modelin Mongolia, bordered by Hangai Mountain, suggesting the complex of Mongolian Holocene climate changes. The water resource, combination of water and heat, atmospheric circulation may be different between the north and south of Mongolia. In a word, the studies of Mongolian Holocene climate changes are relatively poor and should be enhanced.

Key words: Mongolia, Holocene, Climate change

中图分类号:

[1] Xiong Shangfa, Ding Zhongli, Liu Tungsheng. The problems and progresss in the studies of mechanisms for Quaternary [J]. Advances in Earth Science , 1998, 13 (3): 265-272. [熊尚发, 丁仲礼, 刘东生. 第四纪气候变化机制研究的进展与问题 [J]. 地球科学进展, 1998, 13(3): 265-272.] 
[2] Wang Pinxian. Earth system science in China Quo Vadis ?[J]. Advances in Earth Science , 2003, 18 (6): 837-851. [汪品先. 我国的地球系统科学研究向何处去[J]. 地球科学进展, 2003, 18 (6):837-851.] 
[3] Lovelius N V, Davaajamts T S, Gunin P D. Dendroindications of Forest Growth Conditions in Mongolia and Possibilities of Foresting[M]. Moscow: Puschino, 1992. 32-49(in Russian). 
[4] Jacoby G, D'Arrigo R, Davaajamts T. Mongolian tree rings and 20th-century warming[J]. Science , 1996, 273: 771-773. 
[5] Jacoby G, Pederson N, D'Arrigo R. Temperature and precipitation in Mongolia based on dendroclimatic investingations[J]. Chinese Science Bulletin , 2003, 48(14): 1 474-1 479. 
[6] D'Arrigo R, Jacoby G, Frank D, et al. 1738 Years of Mongolian temperature variability inferred from a tree-ring width chronology of Siberian Pine[J]. Geophysical Research Letters , 2001, 28(3): 543-546. 
[7] D'Arrigo R, Jacoby G, Pederson N, et al . Mongolian tree-rings, temperature sensitivity and reconstructions of Northern Hemisphere temperature[J]. Holocene , 2000, 10(6): 669-672. 
[8] Pederson N, Jacoby G, D'Arrigo R, et al . Hydrometeorological reconstructions for Northeastern Mongolia derived from tree rings: 1651-1995[J]. Journal of Climate , 2001, 14: 872-881. 
[9] Feng Z-D. Gobi dynamics in the Northern Mongolian Plateau during the past 20,000+a: Preliminary results[J]. Quaternary International , 2001, 76/77: 77-83. 
[10] O'Brien S R, Mayevoski P A, Meeker L D, et al. Complexity of Holocene climate as reconstructed from a Greenland ice core[J]. Science , 1995, 270: 1 962-1 964. 
[11] Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in north Atlantic Holocene and glacial climates [J]. Science , 1997, 278: 1 257 -1 266. 
[12] Liu X M, Hesse P, Rolph T, et al. Properties of magnetic mineralogy of Alaskan loess: Evidence for pedogenesis[J]. Quaternary International , 1999, 62: 93-102. 
[13] Zhu Rixiang, Kazansky A, Matasova G, et al . Magnetic properties of loess in southern Siberia [J]. Chinese Science Bulletin , 2000, 45(11): 1 200-1 205. [朱日祥, Kazansky A, Matasova G, 等. 西伯利亚南部黄土沉积物的磁学性质 [J]. 科学通报, 2000, 45(11): 1 200-1 205.] 
[14] Li Sen, Sun Wu, Li Xiaoze, et al . Sedimentary characteristics and environmental evolution of Otindag Sandy Land in Holocene [J]. Journal of Desert Research , 1995, 15(4): 323-331. [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.] 
[15] Chen Huizhong, Jin Jiong, Dong Guangrong. Holocene evolution processes of Gurbantunggut Desert and climaticchanges [J]. Journal of Desert Research, 2001, 21(4): 334-339. [陈惠中, 金炯, 董光荣. 全新世古尔班通古特沙漠演化和气候变化 [J]. 中国沙漠, 2001, 21(4): 334-339.] 
[16] Dorofeyuk N I, Tarasov P E. Vegetation and lake level in Northern Mongolia in the last 12500 years as Indicated by data of pollen and diatom analyses[J]. Stratigraphy and Geologial Correlation , 1998, 6: 70-83(in Russian). 
[17] Tarasov P, Dorofeyuk N, Metel'Tseva E. Holocene vegetation and climate change in Hoton-Nur basin, northwest Mongolia[J]. Boreas, 2000, 29: 117-126. 
[18] Gunin P D, Vostokova E A, Dorofeyuk N I, et al. Vegetation Dynamics of Mongolia[M]. Boston: Kluwer Academic, 1999. 
[19] Grunert J, Lehmkuhl F, Walther M. Paleoclimatic evolution of the Uvs Nuur basin and adjacent areas (Western Mongolia)[J]. Quaternary International, 2000, 65/66: 171-192. 
[20] Lehmkuhl F, Haselein F. Quaternary paleoenvironmental change on the Tibetan Plateau and adjacent areas (western China and Western Mongolia)[J]. Quaternary International, 2000, 65/66: 121-145. 
[21] Lehmkuhl F, Lang A. Geomorphological investingations and luminescence dating in the southern part of the Khangay and the Valley of the Gobi Lakes (Central Mongolia)[J]. Journal of Quaternary Science, 2001, 16(1): 69-87. 
[22] Fowell S J, Hansen B C S, Peck J A, et al. Mid to late Holocene climate evolution of the Lake Telmen Basin, North Central Mongolia, based on Palynological data[J]. Quaternary Research ,2003, 59: 353-363. 
[23] Peck J A, Khosbayar P, Fowell S J, et al . Mid to late Holocene climate change in north central Mongolia as recorded in the sediments of Lake Telmen[J]. Palaeogeography, Palaeoclimatology, Palaeoecology , 2002, 183: 135-153. 
[24] Wang W G, Feng Z D, Lee X Q, et al . Holocene abrupt climate shifts recorded in Gun Nuur lake core, northern Mongolia[J]. Chinese Science Bulletin, 2004, 49(5): 520-526. 
[25] Harrison S P, Yu G, Tarasov P E. Late Quaternary lake-level record from northern Eurasia[J]. Quaternary Research , 1996, 45: 138-159. 
[26] Tarasov P E, Harrison S P, Saarse L, et al . Lake status records form the former Soviet Union and Mongolia, database documentation[A]. In: NOAA Paleoclimatology Publications Series Report No. 2 [C]. Colorado: Boulder, 1994. 
[27] Mitchell J F B, Grahame N S, Needham K J. Climate simulations for 9 000 years before present: seasonal variations and effect of the Laurentide ice sheet[J]. Journal of Geophysical Research , 1988, 93: 8 283-8 303. 
[28] Liao X, Street-Perrott F A, Mitchell J F B. GCM experiments with different cloud parameterization: Comparisons with palaeoclimatic reconstructions for 6 000 years BP[J]. Palaeoclimates: Data and Modelling , 1994, 1: 99-123. 
[29] Kutzbach J E, Guetter P J, Behling P J, et al . Simulated climatic changes: results of the COHMAP climatmodel experiments[A]. In: Wright H E, Kutzbach J E, Webb Ⅲ, et al , eds. Global Climates since the Last Glacial Maximum [C]. Minneapolis: University of Minnesota Press, 1993. 24-93. 
[30] Tarasov P E, Guinot J, Cheddadi R, et al. Climate in northern Eurasia 6000 years ago reconstructed from pollen data[J]. Earth and Planetary Science Letters, 1999, 171: 635-645. 
[31] COHMAP Members. Climate changes of the last 18 000 years: Observations and model simulations[J]. Science , 1988, 241: 1 043-1 052. 
[32] Tarasov P E, Pushenko M Y, Harrison S P, et al . Lake status records from the former Soviet Union and Mongolia: documentation of the second version of the database[A]. In: NOAA Paleoclimatology Publications Series Report No.5 [C]. Colorado: Boulder, 1996.

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