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Variation of Rb/Sr Ratios in the Loess-Paleosol Sequences of Central China during the Last 130,000 Years and Their Implications for Monsoon Paleoclimatology

Published online by Cambridge University Press:  20 January 2017

Jun Chen ,
Zhisheng An  and
John Head
Jun Chen
Affiliation:
Department of Earth Sciences, Nanjing University, Nanjing 210093 China
Zhisheng An
Affiliation:
Xian State Key Laboratory of Loess and Quaternary Geology, Xian 710054 China
John Head
Affiliation:
Xian State Key Laboratory of Loess and Quaternary Geology, Xian 710054 China
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Abstract

Rb, Sr, and magnetic susceptibility have been measured in the last interglacial–glacial loess profiles at Luochuan and Huanxian, central China. A high degree of similarity between the parameters in both profiles suggests that variations of Rb/Sr ratios in the sequence can be regarded as an indicator of East Asian summer monsoon strength. Matching the Rb/Sr record with the SPECMAP δ18O curve suggests that the Rb/Sr ratio responds sensitively to changes of the East Asian monsoon induced by global ice-volume variation.

Keywords

Rb/Sr ratiosloesspaleosolsLoess PlateauChina East Asian monsoon
Type
Original Articles
Information
Quaternary Research , Volume 51 , Issue 3 , May 1999 , pp. 215 - 219
Copyright
University of Washington

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References

An, Z.S, Liu, T.S, Lu, Y, 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 Research 78, 91–95.Google Scholar
An, Z.S, Kukla, G, Porter, S.C, Xiao, J.L, (1991). Magnetic susceptibility evidence of monsoon variation in the Loess Plateau of central China during the last 130,000 years. Quaternary Research 36, 29–36.Google Scholar
An, Z.S, Porter, S.C, (1997). Millennial-scale climatic oscillations during the last interglaciation in central China. Geology 25, 603–606.Google Scholar
Brimhell, G.H, Dietrich, W.E, (1987). Constitutive mass balance relation between chemical composition, volume, density, porosity and stain in metasomatic hydrochemical systems. Geochemica et Cosmochimica Acta 51, 567–587.Google Scholar
Chaudhuri, S, Brookings, D.G, (1979). The Rb–Sr systematics in acid-leached clay minerals. Chemical Geology 24, 231–242.Google Scholar
Chen, J, Ji, J, Qiu, G, Lu, H, (1998). Geochemical studies on the intensity of chemical weathering in Luochuan loess–paleosol sequence, China. Science in China 41, 235–241.Google Scholar
Dasch, E.J, (1969). Strontium isotope in weathering profiles, deep sea sediments and sedimentary rocks. Geochimica et Cosmochimica Acta 33, 1521–1552.Google Scholar
Edmond, J.M, (1992). Himalayan tectonics, weathering processes and the strontium isotope record in marine limestones. Science 258, 1594–1597.Google Scholar
Filippelli, G.M, (1997). Intensification of the Asian monsoon and a chemical weathering event in the last Miocene–early Pliocene: Implications for late Neogene climate change. Geology 25, 27–30.Google Scholar
Forman, S.L, (1990). Late Pleistocene chronology of loess deposition near Luochuan, China. Quaternary Research 36, 19–28.Google Scholar
Gallet, S, John, B.M, Toril, M, (1996). Geochemical characterization of the Luochuan loess–paleosol sequence, China, and paleoclimatic implications. Chemical Geology 133, 67–88.Google Scholar
Han, J, Fyfe, S, Longstaffe, F.J, (1998). Climatic implications of the S5 paleosol complex on the southernmost Chinese Loess Plateau. Quaternary Research 50, 21–33.Google Scholar
Heier, K.S, Billings, G.K, (1970). Rubidium. Handbook of Geochemistry. Springer, Berlin, Heidelberg.p. 37B1–37K3.Google Scholar
Heller, F, Liu, T.S, (1986). Paleoclimatic and sedimentary history from magnetic susceptibility of loess in China. Geophysical Research Letters 13, 1169–1172.Google Scholar
Imbrie, J, Hays, J.D, Martinson, D.G, McIntyre, A, Mix, A.C, Morley, J.J, Pisias, N.G, Prell, W.L, Shackleton, N.J, (1984). The orbital theory of Pleistocene climate: Support from a revised chronology of the marine record. Berge, A.L Milankovitch and Climate Reidel, Boston.169–305.Google Scholar
Kukla, G, An, Z.S, (1989). Loess stratigraphy in central China. Palaeography, Palaeoclimatology, Palaeoecology 72, 203–225.CrossRefGoogle Scholar
Kukla, G, Heller, F, Liu, X.M, Liu, T.S, An, Z.S, (1988). Pleistocene climates in China dated by magnetic susceptibility. Geology 16, 811–814.Google Scholar
Leake, T.C, Hendry, G.L, Kemp, A, Plant, A.G, Harrey, P.K, Wilson, J.R, Coats, J.S, Aucott, J.W, Lunel, T, Howarth, R.J, (1969). The chemical analysis of rock powders by automatic X-ray fluorescence. Chemical Geology 5, 7–86.CrossRefGoogle Scholar
Liu, C.Q, Masuda, A, Okada, A, Yabuki, S, Zhang, J, Fan, Z.L, (1993). A geochemical study of loess and desert sand in northern China: Implications for continental crust weathering and composition. Chemical Geology 106, 359–374.CrossRefGoogle Scholar
Liu, T.S, (1985). Loess and the Environment. Ocean, Beijing.Google Scholar
Maher, B.A, Thompson, R, (1991). Mineral magnetic record of the Chinese loess and paleosols. Geology 19, 3–6.Google Scholar
Maher, B.A, Thompson, R, Zhou, L.P, (1994). Spatial and temporal reconstructions of changes in the Asian paleomonsoon: A new mineral magnetic approach. Earth and Planetary Science Letters 125, 461–471.Google Scholar
Nesbitt, H.W, Markovics, G, Price, R.C, (1980). Chemical processes affecting alkalis and alkaline earths during continental weathering. Geochimica et Cosmochimica Acta 44, 1659–1666.Google Scholar
Porter, S.C, An, Z.S, (1995). Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308.Google Scholar
Pye, F, Li, P.Z, (1989). Late Pleistocene and Holocene aeolian dust deposition in North China and Northwest Pacific Ocean. Palaeography, Palaeoclimatology, Palaeoecology 73, 11–23.CrossRefGoogle Scholar
Shemesh, A, Mortlock, R.A, Froelich, P.N, (1989). Late Cenozoic Ge/Si record of marine biogenic opal: Implications for variations of riverine fluxes to the ocean. Paleoceanography 4, 221–234.Google Scholar
Xiao, J.L, Porter, S.C, An, Z.S, Kumai, H, Yoshikawa, S, (1995). Grain size of quartz as an indicator of winter monsoon strength on the Loess Plateau of central China during the last 130,000 yr. Quaternary Research 43, 22–29.Google Scholar
Zheng, H, Rolph, T, Shaw, J, An, Z, (1995). A detailed paleomagnetic record for the last interglacial period. Earth and Planetary Science Letters 133, 339–351.Google Scholar
Zhou, L.P, Oldfield, F, Wintle, A.G, Robinson, S.G, Wang, J.T, (1990). Partly pedogenic origin of magnetic variations in Chinese loess. Nature 346, 737–739.Google Scholar