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A grain-size record from Beijing region in Northern China: Late Quaternary paleoclimate oscillation in response to global change |
Guifang YANG1( ), Zhiliang GE1, Qing DAI1, Jie CHENG1, Gongming YIN2, Lihong ZAN1, Jingwei LIU3 |
| 1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 2. Institute of Geology, China Earthquake Administration, Beijing 100029, China; 3. The Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China |
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Abstract Numerous samples taken from one core at the Beijing plain were utilized to characterize the paleoclimatic configuration of the study area and its possible relation to global control since the last interglaciation. We presented here a detailed grain-size record for the full length of Late Pleistocene, along with the optical simulated luminescence (OSL) dating. Our findings revealed that Late Pleistocene of the study area started approximately at 110 ka B.P. represented by the thick sediments of 31 m in Changping depression. Four sedimentary cycles were outlined in the core during Late Pleistocene, corresponding to marine isotope stage (MIS) 5 to 2. Controlled by regional geology and global climatic setting, eight paleoclimatic periods were identified simultaneously in the study area on the time scale of 104 year, with the warm and moist climate being found at 110-96, 92-76, 67-56, and 28-18 ka B.P.. The climatic instabilities on a millennial scale in Late Pleistocene were characterized largely by the occurrence of 6 strong Heinrich events shown by comparatively coarse groups. These variations correlate well with those documented in the GRIP Greenland and in the Northern Atlantic Ocean, though more complex features may exist on the long time scale.
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| Keywords
paleoclimatic variations
103-104 year scale oscillations
grain-size analysis
the Beijing plain
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Corresponding Author(s):
YANG Guifang,Email:yangguifang@cugb.edu.cn
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Issue Date: 05 June 2009
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| 1 |
An Z S, Liu T S, Lu Y C, Porter S C, Kukla G, Wu X H, Hua Y M (1990). The long-term paleomonsoon variation recorded by the loess-paleosol sequence in Central China. Quaternary International , 7-8: 91–95
|
| 2 |
Bond G, Broecker W, Johnsen S, Mamanus J, Labeyrie L, Jouzel J, Bonan G (1993). Correlations between climate records from North Atlantic sediments and Greenland ice. Nature , 365: 143–147
doi: 10.1038/365143a0
|
| 3 |
Bond G, Showers W, Cheseby M, Lotti R, Almasi P, deMenocal P, Cullen H, Hajdas I, Bonani G (1997). A pervasive millennial-scale cycle in North Atlantic Holocene and glacial climates. Science , 278: 1257–1266
doi: 10.1126/science.278.5341.1257
|
| 4 |
Bradley R S (1985). Quaternary Paleoclimatology: Methods of Paleoclimatic Reconstruction. London: Chapman and Hall. 472
|
| 5 |
Chen F H, Bloemendal J, Wang J M (1997). High-resolution multi-proxy climate records from Chinese loess: evidence for rapid climatic changes over the last 75 kyr. Palaeogeography, Palaeoclimatology, Palaeoecology , 130: 323–335
doi: 10.1016/S0031-0182(96)00149-6
|
| 6 |
Dansgaard W, Johnsen S J, Clausen H B, Jensen D D, Gundestrup N S, Hammer C U, Hvidberg C S, Steffensen J P, Sveinbj?rnsdottir A E, Jouzel J, Bond G (1993). Evidence for general instability of past climate from a 250-kyr ice-core record. Nature , 364: 218–220
doi: 10.1038/364218a0
|
| 7 |
Greenland Ice-Core Project (GRIP) Members (1993). Climate instability during the last interglacial period recorded in the GRIP ice core. Nature , 364: 203–207
doi: 10.1038/364203a0
|
| 8 |
Grigg L D, Whitlock C (2002). Patterns and causes of millennial-scale climate change in the Pacific Northwest during Marine Isotope Stages 2 and 3. Quaternary Science Reviews , 21: 2067–2083
doi: 10.1016/S0277-3791(02)00017-3
|
| 9 |
Grimm E C, Jacobson Jr G L, Watts W A, Hansen B C S, Maasch K A (1993). A 50000-year record of climate oscillations from Florida and its temporal correlation with Heinrich events. Science , 261: 198–200
doi: 10.1126/science.261.5118.198
|
| 10 |
Guo Z, Liu T, Guiot J, Wu N, Lü H, Han J, Liu J, Gu Z (1996). High frequency pulses of East Asian monsoon climate in the last two glaciations: link with the North Atlantic. Climate Dynamics , 12: 701–709
doi: 10.1007/s003820050137
|
| 11 |
Heinrich H (1988). Origin and consequences of cyclic ice rafting in the Northeast Atlantic Ocean during the past 130,000 years. Quaternary Research , 29: 142–152
doi: 10.1016/0033-5894(88)90057-9
|
| 12 |
Jouzel J, Lorius J C, Petit J R, Genthon C, Barkov N I, Kotlyakov V M, Petrov V M (1987). Vostok ice core: a continuous isotope temperature record over the last climatic cycle (160,000 years). Nature , 329: 403–408
doi: 10.1038/329403a0
|
| 13 |
Kong Z C, Du N Q (1980). Vegetational and climatic changes in the past 30000-10000 years in Beijing. Acta Botanica Sinica , 22(4): 330–338 (in Chinese)
|
| 14 |
Li C A (1993). Changes of Quaternary paleoclimate in the plain area of Beijing. Regional Geology of China , (4): 336–343 (in Chinese with English abstract)
|
| 15 |
Li H Z (1995). Quaternary Paleogeographic Study of Beijing Area. Beijing: Geological Publish House. 165 (in Chinese)
|
| 16 |
Lu H Y, Wang X Y, Ma H Z (2004). The Plateau monsoon variation during the past 130 kyr revealed by loess deposit at northeast Qinghai-Tibet (China). Global and Planetary Change , 41: 207–214
doi: 10.1016/j.gloplacha.2004.01.006
|
| 17 |
Lu H Y, Zhou J (1996). Heinrich events and instability of palaeoclimate in last glacial period. Advances in Earth Sciences , 11(1): 40–44 (in Chinese with English abstract)
|
| 18 |
Lü L Q, Fang X M, Lu H Y, Han Y X, Yang S L, Li J J, An Z S (2004). Millennial-scale climate change since the last glaciation recorded by grain sizes of loess deposits on the northeastern Tibetan Plateau. Chinese Science Bulletin , 49(11): 1157–1164
doi: 10.1360/03wd0467
|
| 19 |
Pan B T, Wang J M (1999). Monsoon variations in the east Qinghai-Tibetan Plateau recorded by loess deposit since the last interglacial period. Quaternary Sciences , 4: 330–335 (in Chinese with English abstract)
|
| 20 |
Petit J R, Jouzel J, Raynaud D, Barkov N I, Barnola J M, Basile I, Bender M, Chappellaz J, Davis J, Delaygue G, Delmotte M, Kotlyakov V M, Legrand M, Lipenkov V, Lorius C, Pépin L, Ritz C, Saltzman E, Stievenard M (1999). Climate and atmospheric history of the past 420, 000 years from the Vostok ice core, Antarctica. Nature , 399: 429–436
doi: 10.1038/20859
|
| 21 |
Porter S C (2001). Chinese loess record of monsoon climate during the last glacial-interglacial cycle. Earth Science Reviews , 54: 115–128
doi: 10.1016/S0012-8252(01)00043-5
|
| 22 |
Porter S C, An Z S (1995). Correlation between climate events in the North Atlantic and China during the last glaciations. Nature , 375: 305–308
doi: 10.1038/375305a0
|
| 23 |
Ren J Z, Ding Z L, Liu T S, Sun J M, Zhou X Q (1996). Climate changes on millennial time scale: evidence from a high-resolution loess record. Science in China (D) , 39(5): 449–459
|
| 24 |
Schmitter A, Yoshimori M, Weaver A J (2002). Instability of glacial climate in a model of the ocean-atmosphere-cryophere system. Science , 295: 1489–1493
doi: 10.1126/science.1066174
|
| 25 |
Sun J H, Kong Z C, Du N Q (1999). Vegetation and environmental changes in the Gangshan area of Beijing from 16000-7000 yr BP. Acta Micropalaeontologica Sinica , 16(4): 421–430
|
| 26 |
Tang M C (1998). Formation, evolution and fluctuation of the Plateau Monsoon. In: Tang, M C, Cheng G D, Lin Z Y, Eds. The Recent Climatic Changes in Qinghai-Tibetan Plateau and Its Influences on Environment . Guangzhou: Guangdong Science and Technology Press. 163–183 (in Chinese)
|
| 27 |
Thouveny N, de Beaulleu J L, Bonifay E, Creer K M, Guiot J, Icole M, Johnsen S, Jouzel J, Reille M, Willams T, Willamson D (1994). Climate variations in Europe over the last 140 kyr deduced from rock magnetism. Nature , 371: 503–506
doi: 10.1038/371503a0
|
| 28 |
Thunell R C, Mortyn P G (1995). Glacial climate instability in the Northeast Pacific Ocean. Nature , 376: 504–506
doi: 10.1038/376504a0
|
| 29 |
Yao T D, Thompson L G, Shi Y F, Qin D H, Jiao K Q (1997). Climate variation since the last interglaciation recorded in Guliya ice core. Science in China (D) , 27(5): 447–452
|
| 30 |
Yao Y F, Ye C, Kou X Y, Xu J X, Jia S M, Du N Q, Li C S (2007). Vegetation succession and climate changing since the Late Pliocene in Tianzhu Region in Beijing. Journal of Palaeogeography , 9(1): 49–62 (in Chinese with English abstract)
|
| 31 |
Yu T, Wei M J, Xiao H M, Zhang Y H (2005). Study on the sequence of vegetation change during the middle stage of the last glacial in Xishan Mountain of Beijing area. Journal of Capital Normal University (Natural Science Edition) , 26(3): 81–86 (in Chinese with English abstract)
|
| 32 |
Zhang J H (1998). Reanalysis of principal component analysis to resume past vegetation and environment: kaking Fenzhuang profile in Beijing as an example. Chinese Geographical Science , 8(3): 225–231
|
| 33 |
Zhang P Z, Wang X B, Wang S M, Chen J F, Fang X M, Liu G X (1998). Climate instability of East Tibetan Plateau during last interglacial cycle. Chinese Science Bulletin , 43(1): 17–21
|
| 34 |
Zhao X T, Sun X P, Zhang Y L, Huang X G (1984). Paleogeographic evolution of the Beijing Plain during the past 30,000 years. Science in China (B) , 11: 1184–1196
|
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