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Luminescence-dated aeolian deposits of late Quaternary age in the southern Tibetan Plateau and their implications for landscape history

Published online by Cambridge University Press:  20 January 2017

ZhongPing Lai ,
Knut Kaiser  and
Helmut Brückner
ZhongPing Lai*
Affiliation:
Luminescence Dating Group, Key Laboratory of Salt Lake Resources and Chemistry, Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China Faculty of Geography, University of Marburg, D-35032 Marburg, Germany
Knut Kaiser
Affiliation:
German Academy of Science and Engineering, D-14473 Potsdam, Germany Faculty of Geography, University of Marburg, D-35032 Marburg, Germany
Helmut Brückner
Affiliation:
Faculty of Geography, University of Marburg, D-35032 Marburg, Germany
*
⁎Corresponding author. E-mail addresses:zplai@isl.ac.cn (Z. Lai), knut.kaiser@gmx.net (K. Kaiser), h.brueckner@staff.uni-marburg.de (H. Brückner).
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Abstract

Aeolian deposits are widely distributed in the interior of the Tibetan Plateau, and their chronology is poorly known. It is not yet clear whether they accumulated only after the last deglaciation, or over a longer time. We applied quartz OSL dating to aeolian samples from the Lhasa area with OSL ages ranging from 2.9 ± 0.2 to at least 118 ± 11 ka. The probability density frequency (PDF) distribution of 24 ages reveals age clusters at about 3, 8, 16–21, 33, and 79–83 ka, indicating enhanced sediment accumulation then. The results show that aeolian deposition occurred throughout most of the last 100 ka. This implies that: 1) an ice sheet covering the whole Tibetan Plateau during the last glacial maximum (LGM) could not have existed; and 2) erosion during the last deglaciation was not as strong as previously proposed, such that not all pre-Holocene loess was removed. The age distribution shown in the PDF indicates that aeolian accumulation is episodic. Sand-formation events revealed by age clusters at 3, 8, and 16–21 ka imply roughly synchronous environmental responses to corresponding global-scale arid events.

Keywords

Aeolian depositsQuartz luminescence datingPalaeoenvironmental changeTibetan Plateau
Type
Research Article
Information
Quaternary Research , Volume 72 , Issue 3 , November 2009 , pp. 421 - 430
Copyright
University of Washington

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References

Aitken, M.J. An Introduction to Optical Dating. (1998). Oxford University Press, Oxford. 262 pp CrossRefGoogle Scholar
Alley, R.B., and Ágústsdóttir, A.M. The 8 k event: cause and consequences of a major Holocene abrupt climate change. Quaternary Science Reviews 24, (2005). 1123–1149.Google Scholar
An, Z.S., Kukla, G.J., Porter, S.C., and Xiao, J. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quaternary Research 36, (1991). 29–36.Google Scholar
An, Z.S., Kutzbach, J.E., Prell, W.L., and Porter, S.C. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times. Nature 411, (2001). 62–66.Google Scholar
Atlas of Tibet Plateau, (1990). Edited by the Institute of Geography, Chinese Academy of Sciences, Beijing. (in Chinese).Google Scholar
Berger, A.L. Long-term variations of caloric insolation resulting from the Earth's orbital elements. Quaternary Reseasrch 9, (1978). 139–167.Google Scholar
Böhner, J. Circulation and representativeness of precipitation and air temperature in the southeast of the Qinghai-Xizang Plateau. GeoJournal 34, (1994). 55–66.Google Scholar
Bond, G., Kromer, B., Beer, J., Muscheler, R., Evans, M.N., Showers, W., Hoffmann, S., Rusty Lotti-Bond, R., Hajdas, I., and Bonani, G. Persistent solar influence on North Atlantic climate during the Holocene. Science 294, (2001). 2130–2136.CrossRefGoogle ScholarPubMed
Bøtter-Jensen, L., Bulur, E., Duller, G.A.T., and Murray, A.S. Advances in luminescence instrumentation. Radiation Measurements 32, (2000). 523–528.Google Scholar
Bøtter-Jensen, L., McKeever, S.W.S, and Wintle, A.G. Optically Stimulated Luminescence Dosimetry. (2003). Elsevier, Amsterdam.Google Scholar
Bryson, R.A. Airstream climatology of Asia. Proceedings of International Symposium on the Qinghai-Xizang Plateau and Mountain Meteorology. (1986). American Meteorological Society, Boston, MA. 604–617.Google Scholar
Derbyshire, E., Shi, Y., Li, J., Zheng, B., Li, S., and Wang, J. Quaternary glaciation of Tibet: the geological evidence. Quaternary Science Reviews 10, (1991). 485–510.Google Scholar
Ding, Z.L., Rutter, N., Han, J.T., and Liu, T.S. A coupled environmental system formed at about 2.5 Ma in East Asia. Palaeogeography, Palaeoclimatology, Palaeoecology 94, (1992). 223–242.Google Scholar
Domrös, M., and Peng, G. The Climate of China. (1988). Springer, Berlin.Google Scholar
Fan, Q.S., Lai, Z.P., Long, H., Sun, Y.J., Liu, X.J., in press. OSL chronology for lacustrine sediments recording high stands of Gahai Lake in Qaidam Basin, northeastern Qinghai-Tibetan Plateau. Quaternary Geochronology. doi:10.1016/j.quageo.2009.02.012.Google Scholar
Fang, X.M. The origin and provenance of the Malan loess along the eastern margin of the Qinghai–Xizang (Tibetan) Plateau and its adjacent area. Science in China (B) 38, (1995). 876–887.Google Scholar
Fang, X., Lü, L., Mason, J.A., Yang, S., An, Z., and Li, J. Pedogenic response to millennial summer monsoon enhancements on the Tibetan Plateau. Quaternary International 106/107, (2003). 79–88.Google Scholar
Fielding, E., Isacks, B., Barazangi, M., and Duncan, C. How flat is Tibet?. Geology 22, (1994). 163–167.Google Scholar
Gasse, F., Fontes, J.Ch., Van Campo, E., and WeiHolocene, K. Environmental changes in Bangong Co basin (Western Tibet). Part 4: discussion and conclusions. Palaeogeography, Palaeoclimatology, Palaeoecology 120, (1996). 79–92.Google Scholar
Herzschuh, U., Winter, K., Wünnemann, B., and Li, S. A general cooling trend on the central Tibetan Plateau throughout the Holocene recorded by the Lake Zigetang pollen spectra. Quaternary International 154/155, (2006). 113–121.Google Scholar
Kaiser, K., (2007). Soils and terrestrial sediments as indicators of Holocene environmental changes on the Tibetan Plateau. Habilitation thesis, Faculty of Geography, University of Marburg., 192 pp.Google Scholar
Kaiser, K., Lai, Z.P., Schneider, B., Reudenbach, C., Miehe, G., and Brückner, H. Stratigraphy and palaeoenvironmental implications of Pleistocene and Holocene aeolian sediments in the Lhasa area, southern Tibet (China). Palaeogeography, Palaeoclimatology, Palaeoecology 271, (2009). 329–342.Google Scholar
Kaiser, K., Opgenoorth, L., Schoch, W.H., and Miehe, G. Charcoal and fossil wood from palaeosols, sediments and artificial structures indicating Late Holocene woodland decline in southern Tibet. Quaternary Science Reviews 28, (2009). 1539–1554.Google Scholar
Kaiser, K., Lai, Z.-P., Schneider, B., Schoch, W.H., Shen, X.H., Miehe, G., and Brückner, H. Sediment sequences and paleosols in the Kyichu Valley, southern Tibet (China), indicating Late Quaternary environmental changes. The Island Arc 18, 3 (2009). 404–427.Google Scholar
Kaiser, K., Lai, Z.P., Schneider, B., Junge, F.W., (2009d). Late Pleistocene genesis of the middle Yarlung Zhangbo Valley, southern Tibet (China), as deduced by sedimentological and luminescence data. Quaternary Geochronology, doi:10.1016/j.quageo.2009.01.005.Google Scholar
Kuhle, M. Reconstruction of the 2.4 million km2 late Pleistocene ice sheet on the Tibetan Plateau and its impact on the global climate. Quaternary International 45, /46 (1998). 71–108.CrossRefGoogle Scholar
Kuhle, M. Glacial geomorphology and ice ages in Tibet and the surrounding mountains. The Island Arc 14, (2005). 346–367.Google Scholar
Kukla, G., and An, Z. Loess stratigraphy in central China. Palaeogeography, Palaeoclimatology, Palaeoecology 72, (1989). 203–225.CrossRefGoogle Scholar
Lamb, H.F., Gasse, F., Benkaddour, A., Hamouti, N., Kaars, S., Perkins, W.T., Pearce, N.J., and Roberts, C.N. Relation between century-scale Holocene arid intervals in tropical and temperate zones. Nature 373, (1995). 134–137.CrossRefGoogle Scholar
Lai, Z.P., in press. Chronology and the upper dating limit for loess samples from Luochuan section in the Chinese Loess Plateau using quartz OSL SAR protocol. Journal of Asian Earth Sciences. doi:10.1016/j.seaes.2009.08.003.Google Scholar
Lai, Z.P., and Brückner, H. Effects of feldspar contamination on equivalent dose and the shape of growth curve for OSL of silt-sized quartz extracted from Chinese loess. Geochronometria 30, (2008). 49–53.Google Scholar
Lai, Z.P., and Wintle, A.G. Locating the boundary between the Pleistocene and the Holocene in Chinese loess using luminescence. The Holocene 16, (2006). 893–899.Google Scholar
Lai, Z.P., Singhvi, A.K., Chen, H.Z., and Zhou, W.J. Luminescence chronology of Holocene sediments from Taipingchuan in loess/desert transitional zone, China and its implication. Man and Environment 14, (1999). 91–97.Google Scholar
Lai, Z.P., Wintle, A.G., and Thomas, D.S.G. Rates of dust deposition between 50 ka and 20 ka revealed by OSL dating at Yuanbao on the Chinese Loess Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology 248, (2007). 431–439.CrossRefGoogle Scholar
Lai, Z.P., Zöller, L., Fuchs, M., and Brückner, H. Alpha efficiency determination for OSL of quartz extracted from Chinese loess. Radiation Measurements 43, (2008). 767–770.Google Scholar
Lai, Z.P., Brückner, H., Zöller, L., and Fülling, A. Effects of thermal treatment on the growth curve shape for OSL of quartz extracted from Chinese loess. Radiation Measurements 43, (2008). 763–766.Google Scholar
Lancaster, N. Palaeoclimatic evidence from sand seas. Palaeogeography, Palaeoclimatology, Palaeoecology 76, (1990). 279–290.Google Scholar
Lancaster, N. Desert dune dynamics and development: insights from luminescence dating. Boreas 37, (2008). 559–573.Google Scholar
Lehmkuhl, F. The spatial distribution of loess and loess-like sediments in the mountain areas of Central and High Asia. Zeitschrift für Geomorphologie Supplement 111, (1997). 97–116.Google Scholar
Lehmkuhl, F., Klinge, M., Rees-Jones, J., and Rhodes, E.J. Late Quaternary eolian sedimentation in central and south-eastern Tibet. Quaternary International 68-71, (2000). 117–132.Google Scholar
Lehmkuhl, F., Klinge, M., and Lang, A. Late Quaternary glacier advances, lake level fluctuations and aeolian sedimentation in Southern Tibet. Zeitschrift für Geomorphologie Supplement 126, (2002). 183–218.Google Scholar
Li, S.H., Sun, J.M., and Zhao, H. Optical dating of dune sands in the northeastern deserts of China. Palaeogeography, Palaeoclimatology, Palaeoecology 181, (2002). 419–429.Google Scholar
Li, X.Z., Yi, C.L., Chen, F.H., Yao, T.D., and Li, X. Formation of proglacial dunes in front of the Puruogangri Icefield in the central Qinghai-Tibet Plateau: implications for reconstructing paleoenvironmental changes since the Lateglacial. Quaternary International 154/155, (2006). 122–127.Google Scholar
Liu, T.S. Loess and the Environment. (1985). China Ocean Press, Beijing. 251 pp Google Scholar
Liu, X.Q., Shen, J., Wang, S.M., Yang, X.D., Tong, G.B., and Zhang, E.L. A 16000-year pollen record of Qinghai Lake and its paleoclimate and paleoenvironment. Chinese Science Bulletin 47, (2002). 1931–1936.Google Scholar
Liu, X.J., Lai, Z.P., Long, H., Fan, Q.S., Sun, Y.J., in press. Timing for high lake level of Qinghai lake in the Qinghai-Tibet Plateau based on quartz optically stimulated luminescence dating. Quaternary Geochronology. doi:10.1016/j.quageo.2009.03.010.Google Scholar
Long, H., Lai, Z.P., Fan, Q.S., Sun, Y.J., Liu, X.J., in press. Applicability of a quartz OSL standardised growth curve for De determination up to 400 Gy for lacustrine sediments from the Qaidam Basin of the Qinghai-Tibetan Plateau. Quaternary Geochronology. doi:10.1016/j.quageo.2009.05.005.Google Scholar
Lu, H.Y., Wang, X.Y., Ma, H.Z., Tan, H.B., Vandenberghe, J., Miao, X.D., Li, Z., Sun, Y.B., An, Z.S., and Cao, G.C. The plateau monsoon variation during the past 130 kyr revealed by loess deposit at northeast Qinghai-Tibet (China). Global and Planetary Change 41, (2004). 207–214.Google Scholar
Lu, H.Y., Miao, X.D., Zhou, Y.L., Joseph, M., James, S., Zhang, J.F., Zhou, L.P., and Yi, S.W. Late Quaternary Aeolian activity in the Mu Us and Otindag dune fields (North China) and lagged response to insolation forcing. Geophysical Research Letters 32, (2005). L21716 Google Scholar
Madsen, D.B., Ma, H.Z., Rhode, D., Brantingham, P.J., and Forman, S.T. Age constraints on the late Quaternary evolution of Qinghai Lake, Tibetan Plateau. Quaternary Research 69, (2008). 316–325.Google Scholar
Martinson, D.G., Pisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C., Shackleton, N.J., (1987). Age dating and the Orbital Theory of the Ice Ages: Development of a High-Resolution 0 to 300,000-Year Chronostratigraphy 27. 1–29.Google Scholar
McFarlane, M.J., Eckardt, F.D., Ringrose, S., Coetzee, S.H., and Kuhn, J.R. Degradation of linear dunes in Northwest Ngamiland, Botswana and the implications for luminescence dating of periods of aridity. Quaternary International 135, (2005). 83–90.Google Scholar
Miehe, G., Winiger, M., Böhner, J., and Zhang, Y.L. The climatic diagram map of High Asia. Purpose and concepts. Erdkunde 55, (2001). 94–97.Google Scholar
Miehe, G., Miehe, S., Schlütz, F., Kaiser, K., and La, Duo Palaeoecological and experimental evidence of former forests and woodlands in the treeless desert pastures of Southern Tibet (Lhasa, A.R. Xizang, China). Palaeogeography, Palaeoclimatology, Palaeoecology 242, (2006). 54–67.CrossRefGoogle Scholar
Murray, A.S., and Wintle, A.G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32, (2000). 57–73.CrossRefGoogle Scholar
Nanson, G.C., Chen, X.Y., and Price, D.M. Lateral migration, thermoluminescence chronology and color variation of longitudinal dunes near Birdsville in the Simpson Desert, Central Australia. Earth Surface Processes and Landforms 17, (1992). 807–819.Google Scholar
Ou, X.J., Lai, Z.P., Xu, L.B., Long, H., He, Z., Fan, Q.S., Zhou, S.Z., in press. Potential of quartz OSL dating on morainic deposits from eastern Tibetan Plateau using SAR protocol. Quaternary Geochronology. doi:10.1016/j.quageo.2009.02.004.Google Scholar
Owen, L.A., Finkel, R.C., and Caffee, M.W. A note on the extent of glaciation in the Himalaya during the global Last Glacial Maximum. Quaternary Science Reviews 21, (2002). 147–157.Google Scholar
Owen, L.A., Finkel, R.C., Ma, H.Z., and Barnard, P.L. Late Quaternary landscape evolution in the Kunlun Mountains and Qaidam Basin, Northern Tibet: a framework for examining the links between glaciation, lake level changes and alluvial fan formation. Quaternary International 154/155, (2006). 73–86.Google Scholar
Péwé, T.L., Liu, T.S., Slatt, R.M., and Li, B.Y. Origin and character of loesslike silt in the southern Qinghai-Xizang (Tibet) Plateau, China. US Geological Survey Professional Paper 1549, (1995). 1–55.Google Scholar
Porter, S.C., and An, Z.S. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, (1995). 305–308.CrossRefGoogle Scholar
Porter, S.C., and Zhou, W.J. Synchronism of Holocene East Asian monsoon variations and North Atlantic drift-ice tracers. Quaternary Research 65, (2006). 443–449.Google Scholar
Porter, S.C., Singhvi, A., Zhisheng, A., and Zhongping, L. Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the Northeastern Tibetan Plateau. Permafrost and Periglacial Processes 12, (2001). 203–210.Google Scholar
Prescott, J.R., and Hutton, J.T. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements 23, (1994). 497–500.Google Scholar
Roberts, H.M., Muhs, D.R., Wintle, A.G., Duller, G.A.T., Bettis, E.A. III Unprecedented last-glacial mass accumulation rates determined by luminescence dating of loess from western Nebraska. Quaternary Research 59, (2003). 411–419.CrossRefGoogle Scholar
Ruddimann, W.F., and Kutzbach, J.E. Forcing of Late Cenozoic Northern Hemisphere climate by plateau uplift in southern Asia and the America west. Journal of Geophysical Research 94, (1989). 18,409–18,427.Google Scholar
Shen, J., Liu, X.Q., Wang, S.M., and Matsumoto, R. Palaeoclimatic changes in the Qinghai Lake area during the last 18,000 years. Quaternary International 136, (2005). 131–140.Google Scholar
Shi, Y., Zheng, B., and Li, S. Last glaciation and maximum glaciation in the Qinghai-Xizang (Tibet) Plateau: a controversy to M. Kuhle's ice sheet hypothesis. Zeitschrift für Geomorphologie Supplement 84, (1992). 19–35.Google Scholar
Singhvi, A.K., and Porat, N. Impact of luminescence dating on geomorphological and palaeoclimate research in drylands. Boreas 37, (2008). 536–558.Google Scholar
Singhvi, A.K., Bronger, A., Sauer, W., and Pant, R.K. Thermoluminescence dating of loess/palaeosol sequences in the Carpathian Basin (east Central Europe): a suggestion for a revised chronology. Chemical Geology (Isotopic Geosciences Section) 73, (1989). 307–317.Google Scholar
Singhvi, A.K., Bluszcz, A., Bateman, M.D., and Rao, M.S. Luminescence dating of loess-palaeosol sequences and coversands: methodological aspects and palaeoclimatic implications. Earth-Science Reviews 54, (2001). 193–211.Google Scholar
Sun, J.M., Li, S.H., Han, P., and Chen, Y.Y. Holocene environmental changes in central Inner Mongolia, based on single-aliquot-quartz optical dating and multi-proxy study of dune sands. Palaeogeography, Palaeoclimatology, Palaeoecology 233, (2006). 51–62.Google Scholar
Sun, J.M., Li, S.H., Muhs, D.R., and Li, B. Loess sedimentation in Tibet: provenance, processes, and link with Quaternary glaciations. Quaternary Science Reviews 26, (2007). 2265–2280.Google Scholar
Sun, Y.J., Lai, Z.P., Long, H., Liu, X.J., Fan, Q.S., in press. Quartz OSL dating of archaeological sites in Xiao Qaidam Lake of the NE Qinghai-Tibetan Plateau and its implication for palaeoenvironmental changes. Quaternary Geochronology. doi:10.1016/j.quageo.2009.02.013.Google Scholar
Telfer, M.W., and Thomas, D.S.G. Late Quaternary linear dune accumulation and chronostratigraphy of the southwestern Kalahari: implications for aeolian palaeoclimatic reconstructions and predictions of future dynamics. Quaternary Science Reviews 26, (2007). 2617–2630.Google Scholar
Thompson, L.G., Mosley-Thompson, E., Davis, M.E., Bolzan, J.F., Dai, J., Yao, T., Gundestrup, N., Wu, X., Klein, L., and Xie, Z. Holocene-Late Pleistocene climatic ice core records from Qinghai-Tibetan Plateau. Science 246, (1989). 474–477.Google Scholar
Thompson, L.G., Yao, T., Davis, M.E., Henderson, K.A., Mosley-Thompson, E., Lin, P.-N., Beer, J., Synal, H.-A., Cole-Dai, J., and Bolzan, J.F. Tropical climate instability: the last glacial cycle from a Qinghai-Tibetan ice core. Science 276, (1997). 1821–1825.Google Scholar
van Campo, E., and Gasse, F. Pollen- and diatom-inferred climatic and hydrological changes in Sumxi Co Basin (Western Tibet) since 13,000 yr B.P. Quaternary Research 39, (1993). 300–313.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., Kong, X.G., Shao, X.H., Chen, S.T., Wu, J.Y., Jiang, X.Y., Wang, X.F., and An, Z.S. Millennial- and orbital-scale changes in the East Asian monsoon over the past 224,000 years. Nature 451, (2008). 1090–1092.Google Scholar
Wanner, H., Beer, J., Buetikofer, J., Crowley, T.J., Cubasch, U., Flueckiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J.O., Kuettel, M., Mueller, S.A., Prentice, C., Solomina, O., Stocker, T.F., Tarasov, P., Wagner, M., and Widmannm, M. Mid- to Late Holocene climate change: an overview. Quaternary Science Reviews 27, (2008). 1791–1828.Google Scholar
Wintle, A.G., and Murray, A.S. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41, (2006). 369–391.CrossRefGoogle Scholar
Wu, Y.H., Lücke, A., Jin, Z.D., Wang, S.M., Schleser, G.H., Battarbee, R.W., and Xia, W.L. Holocene climate development on the central Tibetan Plateau: a sedimentary record from Cuoe Lake. Palaeogeography, Palaeoclimatology, Palaeoecology 234, (2006). 328–340.Google Scholar
Yao, T.D., Thompson, L.G., Shi, Y.F., Qin, D.H., Jiao, K.Q., Yang, Z.H., Tian, L.D., and Thompson, E.M. Climate variation since the last interglaciation recorded in the Guliya ice core. Science in China (Ser. D) 40, 6 (1997). 662–668.Google Scholar
Ye, D.Z., and Gao, Y.X. Meteorology of the Tibetan Plateau. (1988). Science Press, Beijing. (1988). 420 pp. (in Chinese) Google Scholar
Zheng, B.X., and Rutter, N. On the problem of Quaternary glaciations, and the extent and patterns of Pleistocene ice cover in the Qinghai-Xizang (Tibet) Plateau. Quaternary International 45/46, (1998). 109–122.Google Scholar
Zhou, S., and Li, J. The sequence of Quaternary glaciation in the Bayan Har Mountains. Quaternary International 45/46, (1998). 135–142.Google Scholar
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