高原泥炭记录揭示的全新世季风快速变化

鲜锋; 周卫健; 于学峰; 卢雪峰; A J T Jull; Lars G Franz&#233;n

高原泥炭记录揭示的全新世季风快速变化

1 中国科学院地球环境研究所黄土与第四纪地质国家重点实验室, 西安 710075;
2 中国科学院研究生院, 北京 100039;
3 NSF-AMS Facility, University of Arizona, Arizona, AZ85721, USA;
4 Department of Earth Sciences, Göteborg University, P. O. Box 460 SE-405 30 Göteborg, Sweden

基金项目:

国家自然科学基金(40531003,40121303)

国家重点基础研究发展规划项目(NBRPC 2004 CB720200)

黄土与第四纪地质国家重点实验室基金(SKLLQG0322)

详细信息

作者简介:
鲜锋(1979-),男,博士生,从事地质数据分析及全新世气候演化研究,E-mail:xianf@ieecas.cn

中图分类号: P532
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- 文章访问数: 1682
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出版历程
- 收稿日期: 2005-06-26
- 修回日期: 2005-10-16

EVIDENCE FOR ABRUPT CHANGES OF THE ASIAN MONSOON DURING THE HOLOCENE: FROM THE PEAT RECORDS OF TIBETAN PLATEAU

1 Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China;
2 Graduate School of the Chinese Academy of Sciences, Beijing 100039, China;
3 NSF-AMS Facility, University of Arizona, Arizona AZ 85721, USA;
4 Department of Earth Sciences, Göteborg University, P. O. Box 460 SE-405 30 Göteborg, Sweden

摘要

摘要: 利用青藏高原东北缘的泥炭沉积记录,重建了该地区全新世冬、夏季风快速波动历史,清晰地识别出9次可与北大西洋浮冰碎屑事件及低纬海面降温事件相对比的气候干冷事件。总有机碳含量频谱分析揭示的1 428、512、255、217 a气候准周期,表明中纬度地区百年至千年尺度气候韵律的存在,全新世气候快速变化具有全球性。
- 泥炭记录 /
- 季风 /
- 浮冰碎屑事件 /
- 百年至千年尺度 /
- 青藏高原
Abstract: Based on the proxies of peat such as TOC, grey scale and ash content, we reconstruct the evolution history of the Asian monsoon during the Holocene. Nine cold and dry events which can be correlated to both ice rafting events recorded in high latitude North Atlantic Ocean sediment cores and cooling events in the low latitude SST are recognized. Spectral analysis of the TOC data indicates that there exists series of periodicities of 1.428 ka,0.512 ka,0.255 ka and 0.217 ka.This further confirms the existence of centennial-millennial scale climatic rhythm in mid-latitude areas, reflecting the global significance of the rapid changes of climate during the Holocene.
- peat /
- Asian monsoon /
- ice rafting events /
- centennial-millennial scale /
- Tibetan Plateau

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参考文献(35)

[1]	Dansgaard W, Johnsen S J, Clausen H B, et al. Evidence for general instability of past climate from a 250-kyr ice-core record[J]. Nature, 1993, 364:218-220.
[2]	McManus J F, Bond G C, Broecker W S, et al. High resolution climate records from the Atlantic during the last interglacial[J]. Nature, 1994, 371:326-329.
[3]	Bender M, Sowers T, Dickson M L, et al. Climate correlations between Greenland and Antarctica during the past 100000 years[J]. Nature, 1994, 372:663-666.
[4]	Chen F H, Bloemendal J, Wang J M, et al. High-resolution multi-proxy climate records from Chinese loess:Evidence for rapid climatic changes between 70 ka and 10 ka[J]. Paleo.Paleo.Palaeo., 1997, 130:323-335.
[5]	GUO Zheng-tang, Petit-Maire N, LIU Tung-sheng. Holocene abrupt environmental changes in the arid regions in Africa and Asia[J]. Paleogeography, 1999, 1(1):68.
[6]	Zhou S Z, Chen F H, Pan B T, et al. Environmental changes during the Holocene in the Western China on millennial timescale[J]. The Holocene, 1991, 1(2):151-156.
[7]	Oppo D W, McManus J F, Cullen J L. Abrupt climate events 500000 to 340000 years ago:evidence from subpolar North Atlantic sediments[J]. Science, 1998, 277:1867-1870.
[8]	McManus J F, Oppo D W, Cullen J L. A 0.5-million-year record of millennial-scale climate variability in the North Atlantic[J]. Science, 1999, 283(5404):971-975.
[9]	Orien 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.
[10]	Bond G, Showers W, Cheseby M, et al. A pervasive millennial-scale cycle in North Atlantic Holocene and Glacial climates[J]. Science, 1997, 278:1257-1266.
[11]	ZHOU Wei-jian, LU Xue-feng, WU Zhen-kun, et al. Peat record reflecting Holocene climatic change in the Zoige Plateau and AMS radiocarbon dating.[J]. Chinese Science Bulletin, 2002, 47(1):66-70.
[12]	Campbell I D, Campbell C, Apps M J, et al. Late Holocene~1500 year climatic periodficities and their implications[J]. Geology, 1998, 26:471-473.
[13]	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,1992,12:1300-1308.[SHI Ya-feng, KONG Zhao-chen, WANG Su-min, et al. Climatic fluctuations and special events during the Holocene Optimum of China[J]. Science in China(Series B), 1992 , 12:1300-1308.]
[14]	Gasse F, Van C E. Abrupt post-glacial climate events in West Asia and North Africa monsoon domains[J]. Earth and Planetary Science Letters, 1994,126:435-456.
[15]	Huang C C, Zhao J, Pang J L, et al.A regional aridity phase and its possible cultureal impact during the Holocene Magathermal in the Guanzhong Basin[J]. The Holocene, 2000, 10(1):135-142.
[16]	CHEN Fa-hu, ZHU Yan, LI Ji-jun, et al. Abrupt Holocene changes of the Asian monsoon at millenial and centennial scales[J]. Chinese Science Bulletin, 2001, 46(23):1942-1947.
[17]	孙广友, 罗新正, Turner R E. 青藏东北部若尔盖高原全新世泥炭沉积年代学研究[J].沉积学报, 2001, 19(2):177-181. [SUN Guang-you, LUO Xin-zheng,Turner R E.A study on peat deposition chronology of Holocene of Zoigê Plateau in the northeast Qinghai Tibetan Plateau[J]. Acta Sedimentologica Sinica, 2001, 19(2):177-181.]
[18]	徐海, 洪业汤, 林庆华, 等. 红原泥炭纤维素氧同位素指示的距今6000年温度变化[J]. 科学通报, 2002, 47(15):1181-1186. [XU Hai, HONG Ye-tang, LIN Qing-hua, et al. Temperature variations in past 6000 years inferred from δ¹⁸O of Peat Cellulose from Hongyuan, China[J]. Chinese Science Bulletin, 2002, 47(15):1181-1186.]
[19]	Gasse F, Arnold M, Fontes J C, et al. A 13000-year climate record from western Tibet[J]. Nature, 1991, 353:742.
[20]	ZHOU Wei-jian, Doinahue D J, Porter S C, et al. Variability of monsoon climate in east Asia at the end of the last glaciation[J]. Quaternary Research, 1996,46:219.
[21]	ZHOU Wei-jian, LU Xue-feng, WU Zhen-kun, et al. Peat record reflecting Holocene climatic change in the Zoigê Plateau and AMS radiocarbon dating[J]. Chinese Science Bulletin, 2002, 47(1):66-70.
[22]	Wanyner R K.Peat in Greens:knows, unknowns and speculations[M]. Soil Science,1987:5-8.
[23]	Stuiver M, Reimer B, Braziunas T. High-precision radiocarbon age calibration for terrestrial and marine samples[J]. Radiocarbon, 1998,49(3):1127-1151
[24]	XIAO Jia-yi, ZHOU Wei-jian, AN Zhi-sheng, et al. Evidence for the Younger Dryas event in the eastern part of Nanling region[J]. Acta Botanic Sinica(in Chinese), 1998, 40(11):1079.
[25]	Bond G, Kromer B, Beer J, et al. Persistent solar influence on North Atlantic climate during the Holocene[J]. Science, 2001, 294:2130-2136.
[26]	Sirocko F, Samthein M, Erlenkeuser H. Century-scale events in monsoonal climate over the past 24000 years[J]. Nature, 1993,364:322-324.
[27]	Thomson D. Spectrum estimation and harmonic analysis[C]. Proceedings of the IEEE, 1982, 70(9):1055.
[28]	Stuiver M, Braziunas T. Sun, ocean, climate and atmospheric ¹⁴CO₂:an evaluation of causal and spectral relationships[J]. Holocene, 1993, 3(4):289.
[29]	Gleissberg W. A table of secular variations of the solar cycle[J]. Terrestrial Magnetism and Atmospheric Electricity, 1994, 49:243.
[30]	Sirocko F, Garbe-Schonberg D, McIntyre A, et al. Teleconnections between the subtropical monsoon and high-latitude climates during the last deglaciation[J]. Science, 1996, 272:526.
[31]	许靖华. 太阳、气候、饥饿与民族大迁移[J]. 中国科学D辑, 1998, 28(4):366-384. [XU Jing-hua. The sun, climate, starvation and nation's migration[J].Science in China(Series D), 1998, 28(4):366-384.]
[32]	Bianchi G G, McCave I N. Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland[J]. Nature, 1999, 397:515-517.
[33]	ZHOU Wei-jian, Head M J, LU Xue-feng, et al. Teleconnection of climatic events between east Asia and polar high latitude areas during the last deglaciation[J]. Palaeo. Palaeo.Palae., 1999, 152:163.
[34]	Hoyt D V, Schatten K H. The Role of The Sun in Climate Change[M]. Oxford:Oxford University Press, 1997.
[35]	Beer J, Mende W,Stellmacher R. The role of The sun in climate forcing[J]. Quaternary Science Review, 2000, 19:403-415.