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Eolian quartz flux variations in Cheju Island, Korea, during the last 6500 yr and a possible Sun–monsoon linkage

Published online by Cambridge University Press:  20 January 2017

Jaesoo Lim ,
Eiji Matsumoto  and
Hiroyuki Kitagawa
Jaesoo Lim*
Affiliation:
Division of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan
Eiji Matsumoto
Affiliation:
Division of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan
Hiroyuki Kitagawa
Affiliation:
Division of Earth and Environmental Sciences, Graduate School of Environmental Studies, Nagoya University, Nagoya 464-8601, Japan
*
*Corresponding author. Fax: +81 52 789 3436. E-mail address: [email protected] (J. Lim).
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Abstract

We have obtained a high-resolution sedimentary record covering the last 6500 yr from a maar in Cheju Island, Korea, in order to reconstruct the history of variations in the eolian quartz flux (EQF) and hence Asian dust. The long-term variation of EQF reveals three intervals: a period of high EQF (4000–2000 cal yr B.P.) and two periods of low EQF (6500–4000 cal yr B.P. and 2000 cal yr B.P. to present), which have been affected by the East Asian monsoon due to insolation change and the cold air activity in high latitudes correlated with polar high-pressure systems. This long-term variation is superimposed by millennial- and centennial-scale fluctuations with periodicities of 1137, 739, 214, 162, 137, 127, and 111 yr, implying drier conditions in the source areas in China. The detrended EQF record correlates visually and statistically (cross-spectral analysis) with the atmospheric Δ14C record (solar proxy). The centennial-scale variability in EQF may be affected by the solar activity through the Sun–East Asian monsoon linkage.

Keywords

Eolian quartzAsian dustEast Asian monsoonSolar activityHoloceneClimate change
Type
Research Article
Information
Quaternary Research , Volume 64 , Issue 1 , July 2005 , pp. 12 - 20
Copyright
University of Washington

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References

An, Z.S., and Porter, S.C. (1997). Millennial-scale climatic oscillations during the last interglaciation in central China. Geology 25, 7 603–606.Google Scholar
An, Z.S., Kukla, G., Porter, S.C., and Xiao, J.L. (1991). Late Quaternary dust flow on the Chinese loess plateau. CATENA 18, 125–132.Google Scholar
An, Z.S., Sun, D.H., Zhang, X., Zhou, W.J., Porter, S.C., Shaw, J., and Zhang, D. (1995). Accumulation sequence of Chinese loess and climatic records of Greenland ice core during the last 130 ka. Chinese Science Bulletin 40–15, 1272–1276.Google Scholar
An, Z.S., Porter, S.C., Kutzbach, J.E., Xiao, W., Suming, W., Xiaodong, L., Xiaoqiang, L., and Zhou, W.J. (2000). Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19, 743–762.CrossRefGoogle Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Lotti-Bond, R., Hajdas, I., and Bonani, G. (2001). Persistent solar influence on North Atlantic climate during the Holocene. Science 294, 2130–2136.Google Scholar
Carmechael, G., Hong, M.-S., Ueda, H., Chen, L.-L., Murano, K., Park, J., Lee, H., Kim, Y., Kang, C., and Shim, S. (1997). Aerosol composition at Cheju Island, Korea. Journal of Geophysical Research 102, 6047–6061.CrossRefGoogle Scholar
Carslaw, K.S., Harrison, R.G., and Kirkby, J. (2002). Cosmic, clouds, and climate. Science 298, 1732–1737.Google Scholar
Chen, F.H., Shi, Q., and Wang, J.M. (1999). Environmental changes documented by sedimentation of Lake Yiema in China since the late glaciation. Journal of Paleolimnology 22, 159–169.Google Scholar
Clayton, R.N., Rex, R.W., Syers, J.K., and Jackson, M.L. (1972). Oxygen isotope abundance in quartz from Pacific pelagic sediments. Journal of Geophysical Research 77, 3907–3915.Google Scholar
Denton, G.H., and Karlen, W. (1973). Holocene climatic variations; their pattern and possible cause. Quaternary Research 3, 155–205.Google Scholar
Dickinson, R.E. (1975). Solar variability and the lower atmosphere. Bulletin of American Meteorological Society 56, 1240–1248.Google Scholar
Ding, Z.L., Rutter, N.W., Sun, J.M., Yang, S.L., and Liu, T.S. (2000). Re-arrangement of atmospheric circulation at about 2.6 Ma over northern China: evidence from grain size records of loess–palaeosol and red clay sequences. Quaternary Science Reviews 19, 547–558.Google Scholar
Fleitmann, D., Burns, S., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., and Matter, A. (2003). Holocene forcing of the Indian monsoon recorded in a stalagmite from Southern Oman. Science 300, 1737–1739.Google Scholar
Gao, Y.X. (1962). On some problems of Asian monsoon.Gao, Y.X. Some Questions About the East Asian Monsoon Science Press, Beijing.1–49.(in Chinese)Google Scholar
Haigh, J.D. (1999). Modelling the impact of solar variability on climate. Journal of Atmospheric and Solar–Terrestrial Physics 61, 63–72.Google Scholar
Hong, Y.T., Wang, Z.G., Jiang, H.B., Lin, Q.H., Hong, B., Zhu, X.Y., Wang, Y., Xu, L.S., Leng, X.T., and Li, H.D. (2001). A 6000-year record of changes in drought and precipitation in northeastern China based on a δ13C time series from peat cellulose. Earth and Planetary Science Letters 185, 111–119.Google Scholar
Hovan, S.A., Rea, D.K., and Pisias, N.G. (1991). Late Pleistocene continental climate and oceanic variability recorded in northwest Pacific sediments. Paleoceanography 6, 349–370.CrossRefGoogle Scholar
Hu, F.S., Kaufman, D., Yoneji, S., Nelson, D., Shemesh, A., Huang, Y.S., Tian, J., Bond, G., Clegg, B., and Brown, T. (2003). Cyclic variation and solar forcing of Holocene climate in the Alaskan subarctic. Science 301, 1890–1894.Google Scholar
Inoue, K., and Naruse, T. (1987). Physical, chemical, and mineralogical characteristics of modern eolian dust in Japan and rate of dust deposition. Soil Science and Plant Nutrition 33, 3 327–345.Google Scholar
Kitagawa, H. (1997). Radiocarbon dating at the International Research Center for Japanese Studies. Japan Review 9, 223–234.Google Scholar
Kitagawa, H., Masuzawa, T., Nakamura, T., and Matsumoto, E. (1993). A batch preparation method for graphite targets with low background for AMS 14C measurements. Radiocarbon 35, 295–300.Google Scholar
Kretschmer, W., Anton, G., Bergmann, M., Finckh, E., Kowalzik, B., Klein, M., Leigart, M., Merz, S., Morgenroth, G., Piringer, I., Kuster, H., Low, R.D., and Nakamura, T. (1997). 14C dating of sediment samples. Nuclear Instruments and Methods in Physics Research, B 123, 455–459.Google Scholar
Kurosaki, Y., and Mikami, M. (2003). Recent frequent dust events and their relation to surface wind in east Asia. Geophysical Research Letters 30, 14 173610.1029/2003GL017261Google Scholar
Lee, M.W. (1982). Petrology and geochemistry of Jeju volcanic island, Korea. Tohoku University Science Report Series 15, 177–256.Google Scholar
Leinen, M., Prospero, J.M., Arnold, E., and Blank, M. (1994). Mineralogy of Aeolian dust reaching the North Pacific Ocean: I. Sampling and analysis. Journal of Geophysical Research 99, 21017–21023.Google Scholar
Littmann, T. (1991). Dust storm frequency in Asia: climatic control and variability. International Journal of Climatology 11, 393–412.Google Scholar
Liu, X.D., Yin, Z.Y., Zhang, X.A., and Yang, X.C. (2004). Analyses of the spring dust storm frequency of northern China in relation to antecedent and concurrent wind, precipitation, vegetation, and soil moisture conditions. Journal of Geophysical Research 109, D16210 10.1029/2004JD004615CrossRefGoogle Scholar
Mizota, C., Kusakabe, M., and Noto, M. (1990). Oxygen isotope composition of quartz in soils developed on late Quaternary volcanic ashes in Japan. Geoderma 46, 319–327.CrossRefGoogle Scholar
Mizota, C., Endo, H., Um, K.T., Kusakabe, M., Noto, M., and Matsuhisa, Y. (1991). The eolian origin of silty mantle in sedentary soils from Korea and Japan. Geoderma 49, 153–164.CrossRefGoogle Scholar
Nakagawa, T., Kitagawa, H., Yasuda, Y., Tarasov, P.E., Nishida, K., Gotanda, K., Sawai, Y. Yangtse River Civilization Program Members(2003). Asynchronous climate changes in the North Atlantic and Japan during the last termination. Science 299, 688–691.Google Scholar
Nakamura, T., Niu, E., Oda, H., Ikeda, A., Minami, M., Takahashi, H., Adachi, M., Pals, L., Gottdang, A., and Suya, N. (2000). The HVEE Tandetron AMS system at Nagoya University. Nuclear Instruments and Methods in Physics Research, B 172, 52–57.CrossRefGoogle Scholar
Neff, U., Burns, S.J., Mangini, A., Mudelsee, M., Fleitmann, D., and Matter, A. (2001). Strong coherence between solar variability and the monsoon in Oman between 9 and 6 kyr ago. Nature 411, 290–293.Google Scholar
O'Brien, S.R., Mayewski, P.A., Meeker, L.D., Meese, D.A., Twickler, M.S., and Whitlow, S.I. (1995). Complexity of Holocene climate as reconstructed from a Greenland ice core. Science 270, 1962–1964.CrossRefGoogle Scholar
Okamoto, T., Matsumoto, E., and Kawahata, H. (2002). Eolian dust fluctuation during the past 200,000 years revealed from quartz in North Pacific deep-sea sediments. Quaternary Research 41, 35–44.(in Japanese)Google Scholar
Ono, Y., and Naruse, T. (1997). Snowline elevation and eolian dust flux in the Japanese islands during isotope stages 2 and 4. Quaternary International 37, 45–54.Google Scholar
Ono, Y., Naruse, T., Ikeya, M., Kohno, H., and Toyoda, S. (1998). Origin and derived courses of eolian dust quartz deposited during marine isotope stage 2 in East Asia, suggested by ESR signal intensity. Global and Planetary Change 18, 129–135.Google Scholar
Porter, S.C., and An, Z.S. (1995). Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308.Google Scholar
Rea, D.K., and Leinen, M. (1988). Asian aridity and the zonal westerlies: late Pleistocene and Holocene record of eolian deposition in the Northwest Pacific Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 66, 1–8.Google Scholar
Schulz, M., and Stattegger, K. (1997). SPECTRUM: spectral analysis of unevenly spaced paleoclimatic time series. Computer Geoscience 23, 929–945.Google Scholar
Shi, Y., Kong, Z., Wang, S., Tang, L., Yao, T., Zhao, X., Zhang, P., and Shi, S. (1993). Mid-Holocene climates and environments in China. Global and Planetary Change 7, 219–233.Google Scholar
Shindell, D., Schmidt, G.A., Mann, M.E., Rind, D., and Waple, A. (2001). Solar forcing of regional climate change during the Maunder Minimum. Science 294, 2149–2152.Google Scholar
Sridhar, K., Jackson, M.L., and Clayton, R.N. (1975). Quartz oxygen isotopic stability in relation to isolation from sediments and diversity of source. Proceedings–Soil Science Society of America 39, 1209–1213.Google Scholar
Stuiver, M., and Braziunas, T.F. (1993). Sun, ocean, climate and atmospheric 14CO2: an evaluation of causal and spectral relationships. Holocene 3–4, 289–305.Google Scholar
Stuiver, M., Grootes, P.M., and Braziunas, T.F. (1995). The GISP2 δ18O climate record of the past 16,500 years and the role of the sun, ocean, and volcanoes. Quaternary Research 44, 341–354.CrossRefGoogle Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, F.G., Plicht, J., v.d., , and Spurk, M. (1998). INTCAL98 radiocarbon calibration, 24,000–0 cal BP. Radiocarbon 40, 1041–1083.Google Scholar
Sun, J.M., Zhang, M.Y., and Liu, T.S. (2001). Spatial and temporal characteristics of dust storms in China and its surrounding regions, 1960–1999: relations to source area and climate. Journal of Geophysical Research 106, 10325–10333.Google Scholar
Svensmark, H., and Friis-Christensen, E. (1997). Variation of cosmic ray flux and global cloud coverage–A missing link in solar–climate relationships. Journal of Atmospheric and Solar–Terrestrial Physics 59, 1225–1232.CrossRefGoogle Scholar
Syers, J.K., Chapman, S.L., Jackson, M.L., Rex, R.W., and Clayton, R.N. (1968). Quartz isolation from rocks, sediments and soils for determination of oxygen isotopes composition. Geochimica et Cosmochimica Acta 32, 1022–1025.Google Scholar
Toyoda, S., and Naruse, T. (2002). Eolian dust from the Asian deserts to the Japanese islands since the last glacial maximum: the basis for the ESR method. Transactions–Japanese Geomorphological Union 23-5, 811–820.Google Scholar
Wang, F.B., and Fan, C.Y. (1987). Climatic changes in the Qinghai-Xizang (Tibetan) region of China during the Holocene. Quaternary Research 28, 50–60.Google Scholar
Xiao, J.L., Poter, S.C., An, Z.S., Kumai, H., and Yoshikawa, S. (1995). Grain size of quartz as an indicator winter monsoon strength on the loess plateau of central China during the last 130,000 yrs. Quaternary Research 43, 22–29.Google Scholar
Xiao, J.L., Inouchi, I., Kumai, H., Yoshikawa, S., Kondo, Y., Liu, T.S., and An, Z.S. (1997). Eolian quartz flux to Lake Biwa, central Japan, over the past 145,000 years. Quaternary Research 48, 48–57.Google Scholar
Xiao, J., Nakamura, T., Lu, H., and Zhang, G. (2002). Holocene climate changes over the desert/loess transition of north-central China. Earth and Planetary Science Letters 197, 11–18.Google Scholar
Yatagai, S., Takemura, K., Naruse, T., Kitagawa, H., Fukusawa, H., Kim, M.H., and Yasuda, Y. (2002). Monsoon changes and eolian dust deposition over the past 30,000 years in Cheju Island, Korea. Transactions–Japanese Geomorphological Union 23–5, 821–831.Google Scholar
Yi, S.H., Saito, Y., Zhao, Q., and Wang, P. (2003). Vegetation and climate changes in the Changjiang (Yangtze River) Delta, China, during the past 13,000 years inferred from pollen records. Quaternary Science Reviews 22, 1501–1519.CrossRefGoogle Scholar
Yoshinaga, S. (1996). Variations in rates of accumulation of tropospheric fine quartz in tephra, loess, and associated paleosols since the last interglacial stage, Tokachi plain, northern Japan, and paleoclimatic inferences. Quaternary International 34–36, 139–146.CrossRefGoogle Scholar
Zhang, H.C., Ma, Y.Z., Wunnemann, B., and Pachur, H.-J. (2000). A Holocene climatic record from arid northwestern China. Palaeogeography, Palaeoclimatology, Palaeoecology 162, 389–401.Google Scholar
Zhou, W.J., Head, M.J., Lu, X.F., An, Z.S., Jull, A.J.T., and Donahue, D. (1999). Teleconnection of climatic events between East Asia and polar, high latitude areas during the last deglaciation. Palaeogeography, Palaeoclimatology, Palaeoecology 152, 163–172.CrossRefGoogle Scholar
Zhou, W.J., Head, M.J., and Deng, L. (2001). Climate changes in northern China since the late Pleistocene and its response to global change. Quaternary International 83–85, 285–292.Google Scholar