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Late Quaternary aeolian activity in Gonghe Basin, northeastern Qinghai-Tibetan Plateau, China

Published online by Cambridge University Press:  20 January 2017

Mingrui Qiang ,
Fahu Chen ,
Lei Song ,
Xingxing Liu ,
Mingzhi Li  and
Qin Wang
Mingrui Qiang*
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Research school of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, PR China
Fahu Chen
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Research school of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, PR China
Lei Song
Affiliation:
Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang 050061, PR China
Xingxing Liu
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Research school of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, PR China
Mingzhi Li
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Research school of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, PR China
Qin Wang
Affiliation:
MOE Key Laboratory of Western China’s Environmental Systems, Research school of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, PR China
*
*Corresponding author at: Research school of Arid Environment and Climate Change, Lanzhou University, No. 222, South Tianshui Road, Lanzhou 730000, PR China. Fax: + 86 931 891 2330. E-mail address:[email protected] (M. Qiang).
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Abstract

Aeolian deposits at four sites in the Gonghe Basin were used to reconstruct the history of aeolian activity over the late Quaternary. These deposits include well-sorted aeolian sand, paleosols and/or loess. Aeolian sand represents dune-field expansion and/or dune buildup, whereas paleosols indicate stabilization of dunes, accompanying ameliorated vegetation cover. On the basis of 25 dates by optically stimulated luminescence (OSL), it appears that aeolian activities occurred episodically at 33.5, 20.3, 13.9, 11.8–11.0, 9.4, 7.8, and 5.7 (5.5) ka, which is largely consistent with the recent findings from the adjacent semi-arid areas. Aeolian sand mobility occurring during the early to mid Holocene conflicts with a climatic optimum inferred from lacustrine records in the northeastern Qinghai-Tibetan Plateau. This inconsistency may be resolved by interpreting aeolian activity as a response to decreased effective moisture due to enhanced evaporation, induced by higher summer insolation at that time, together with local terrain and its effects on moisture. Our results suggest that aeolian sand and paleosol cannot be simply ascribed to regional dry and wet climates, respectively, and they most likely reflect changes in effective moisture.

Keywords

Aeolian activityAeolian sandPaleosolLuminescence datingGonghe Basin
Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 3 , May 2013 , pp. 403 - 412
Copyright
University of Washington

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References

An, Z.S., Kukla, G.J., Porter, S.C., and Xiao, J.L. Late Quaternary dust flow on the Chinese loess plateau. Catena 18, (1991). 125–132.Google Scholar
An, Z.S., Porter, S.C., Kutzbach, J.E., Wu, X.H., Wang, S.M., Liu, X.D., Li, X.Q., and Zhou, W.J. Asynchronous Holocene optimum of the East Asian monsoon. Quaternary Science Reviews 19, (2000). 743–762.CrossRefGoogle 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
Berger, A., and Loutre, M.F. Isolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, (1991). 297–317.Google Scholar
Chen, F.H., Yu, Z.C., Yang, M.L., Ito, E., Wang, S.M., Madsen, D.B., Huang, X.Z., Zhao, Y., Sato, T., Birks, H.J.B., Boomer, I., Chen, J.H., An, C.B., and Wünnermann, B. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with monsoon history. Quaternary Science Reviews 27, (2008). 351–364.Google Scholar
Colman, S.M., Yu, S.-Y., An, Z.S., Shen, J., and Henderson, A.G.G. Late Cenozoic climate changes in China’s western interior: a review of research on Lake Qinghai and comparison with other records. Quaternary Science Reviews 26, (2007). 2281–2300.CrossRefGoogle Scholar
Dong, G.R., Gao, S.Y., and Jin, J. Desertification and Controls in the Gonghe Basin, Qinghai Province. (1993). Science Press, Beijing. 1–166. (in Chinese with English abstract) Google Scholar
Dykoski, C.A., Edwards, R.L., Cheng, H., Yuan, D.X., Cai, Y.J., Zhang, M.L., Lin, Y.S., Qing, J.M., An, Z.S., and Revenaugh, J. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record form Dongge Cave, China. Earth and Planetary Science Letters 233, (2005). 71–86.CrossRefGoogle Scholar
Feng, Z.-D., An, C.B., and Wang, H.B. Holocene climatic and environmental changes in the arid and semi-arid areas of China: a review. The Holocene 16, (2006). 119–130.Google Scholar
Fleitmann, D., Burns, S.J., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., and Matter, A. Holocene forcing of Indian monsoon recorded in a stalagmite from southern Oman. Science 300, (2003). 1737–1739.CrossRefGoogle Scholar
Gao, Y.X., Xu, S.Y., Guo, Q.Y., and Zhang, M.L. Monsoon regions in China and regional climates. Gao, Y.X. Some Problems on East-Asia monsoon. (1962). Science Press, Beijing. 49–63. (in Chinese) Google Scholar
Gao, S.Y., Chen, W.N., Jin, H.l, Dong, G.R., Li, B.S., Yang, G.S., Lin, L.Y., Guan, Y.Z., Sun, Z., Jin, J., Zhang, Y.T., and Cao, J.S. Preliminary study on the Holocene evolution of the NW desert margin in the monsoon region of China. Science in China Series B 23, (1993). 202–208. (in Chinese) Google Scholar
Guo, Z.T., Ruddiman, W.F., Hao, Q.Z., Wu, H.B., Qiao, Y.S., Zhu, R.X., Peng, S.Z., Wei, J.J., Yuan, B.Y., and Liu, T.S. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature 416, (2002). 159–162.CrossRefGoogle ScholarPubMed
Gupta, A.K., Anderson, D.M., and Overpeck, J.T. Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature 421, (2003). 354–357.CrossRefGoogle ScholarPubMed
He, Y., Theakstone, W.H., Zhang, Z.L., Zhang, D., Yao, T.D., Chen, T., Shen, Y.P., and Pang, H.X. Asynchronous Holocene climatic change across China. Quaternary Research 61, (2004). 52–63.Google Scholar
Henderson, A.C.G., Holmes, J.A., and Leng, M.J. Late Holocene isotope hydrology of Lake Qinghai, NE Tibetan Plateau: effective moisture variability and atmospheric circulation changes. Quaternary Science Reviews 29, (2010). 2215–2223.CrossRefGoogle Scholar
Herzschuh, U. Palaeo-moisture evolution in monsoonal Central Asia during the last 50,000 years. Quaternary Science Reviews 25, (2006). 163–178.Google Scholar
Herzschuh, U., Zhang, C.J., Mischke, S., Herzschuh, R., Mohammadi, F., Mingram, B., Kqrschner, H., and Riedel, F. A late Quaternary lake record from the Qilian Mountains (NW China): evolution of the primary production and the water depth reconstructed from macrofossil, pollen, biomarker, and isotope data. Global and Planetary Change 46, (2005). 361–379.CrossRefGoogle Scholar
Herzschuh, U., Kramer, A., Mischke, S., and Zhang, C.J. Quantitative climate and vegetation trends since the late glacial on the northeastern Tibetan Plateau deduced from Kuocha Lake pollen spectra. Quaternary Research 71, (2009). 162–171.Google Scholar
Ji, J.F., Shen, J., Balsam, W., Chen, J., Liu, L.W., and Liu, X.Q. Asian monsoon oscillations in the northeastern Qinghai–Tibet Plateau since the late glacial as interpreted from visible reflectance of Qinghai Lake sediments. Earth and Planetary Science Letters 233, (2005). 61–70.CrossRefGoogle Scholar
Jin, L.Y., Chen, F.H., Morrill, C., Otto-Bliesner, B.L., and Rosenbloom, N. Causes of early Holocene desertification in arid central Asia. Climate Dynamics 38, (2012). 1577–1591.CrossRefGoogle Scholar
Kelts, K.R., Chen, K.Z., Lister, G.S., Yu, J.Q., Gao, Z.H., Niessen, N., and Bonani, G. Geological fingerprints of climate history: a cooperative study of Qinghai Lake, China. Eclogae Geologicae Helvetiae 82, (1989). 167–182.Google Scholar
Kramer, A., Herzschuh, U., Mischke, S., and Zhang, C.J. Holocene treeline shifts and monsoon variability in the Hengduan Mountains (southeastern Tibetan Plateau), implications form palynological investigations. Palaeogeography, Palaeoclimatology, Palaeoecology 286, (2010). 23–41.Google 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.CrossRefGoogle Scholar
Lai, Z.P., Kaiser, K., and Brückner, H. Luminescence-dated aeolian deposits of late Quaternary age in the southern Tibetan Plateau and their implications for landscape history. Quaternary Research 72, (2009). 421–430.Google Scholar
Lancaster, N. Geomorphology of Desert Dunes. (1995). Routledge, London and New York. 228–254.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
Lister, G.S., Kelts, K., Chen, K.Z., Yu, Z.Q., and Niessen, F. Lake Qinghai, China: closed-basin lake levels and the oxygen isotope record for ostracoda since the latest Pleistocene. Palaeogeography, Palaeoclimatology, Palaeoecology 84, (1991). 141–162.CrossRefGoogle Scholar
Liu, T.S. Loess and Environment. (1985). China Ocean Press, Beijing.Google Scholar
Liu, T.S., and Ding, Z.L. Chinese loess and the paleomonsoon. Annual Review of Global Earth and Planetary Sciences 26, (1998). 111–145.Google Scholar
Liu, X.Q., Dong, H.L., Rech, J.A., Matsumoto, R., Yang, B., and Wang, Y.B. Evolution of Chaka Salt Lake in NW China in response to climatic change during the Latest Pleistocene–Holocene. Quaternary Science Reviews 27, (2008). 867–879.Google Scholar
Liu, X.J., Lai, Z.P., Yu, L.P., Sun, Y.J., and Madsen, D. Luminescence chronology of aeolian deposits from the Qinghai Lake area in the Northeastern Qinghai-Tibetan Plateau and its palaeoenvironmental implications. Quaternary Geochronology 10, (2012). 37–43.Google Scholar
Liu, B., Jin, H.L., Sun, L.Y., Sun, Z., Su, Z.Z., Zhang, C.X., in press. Holocene climatic change revealed by aeolain deposits from the Gonghe Basin, northeastern Qinghai-Tibetan Plaeau. Quaternary International, doi: 10.1016/j.quaint.2012.05.003.Google Scholar
Lu, H.Y., Miao, X.D., Zhou, Y.L., Mason, J., Swinehart, J., 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 http://dx.doi.org/10.1029/2005GL024560CrossRefGoogle Scholar
Lu, Y.C., Wang, X.L., and Wintle, A.G. A new OSL chronology for dust accumulation in the last 130,000 yr for the Chinese Loess Plateau. Quaternary Research 67, (2007). 152–160.CrossRefGoogle Scholar
Lu, H.Y., Zhao, C.F., Mason, J., Yi, S.W., Zhao, H., Zhou, Y.L., Ji, J.F., Swinehart, J., and Wang, C.M. Holocene climatic changes revealed by aeolian deposits from the Qinghai Lake area (northeastern Qinghai-Tibetan Plateau) and possible forcing mechanisms. The Holocene 21, (2011). 297–304.Google Scholar
Maher, B.A., and Hu, M.Y. A high-resolution record of Holocene rainfall variations from the western Chinese Loess Plateau: antiphase behaviour of the African/Indian and East Asian summer monsoons. The Holocene 16, (2006). 309–319.CrossRefGoogle Scholar
Mason, J.A., Swinehart, J.B., Lu, H.Y., Miao, X.D., Cha, P., and Zhou, Y.L. Limited change in dune mobility in response to a large decrease in wind power in semi-arid north China since 1970s. Geomophology 102, (2008). 351–363.Google Scholar
Mason, J.A., Lu, H., Zhou, Y., Miao, X., Swinehart, J.B., Liu, Z., Goble, R.J., and Yi, S. Dune mobility and aridity at the desert margin of northern China at a time of peak monsoon strength. Geology 37, 10 (2009). 947–950.Google Scholar
Mischke, S., Zhang, C.J., Börner, A., and Herzschuh, U. Lateglacial and Holocene variation in aeolian sediment flux over the northeastern Tibetan Plateau recorded by laminated sediments of a saline meromictic lake. Journal of Quaternary Science 25, (2010). 162–177.Google Scholar
Morrill, C. The influence of Asian summer monsoon variability on the water balance of a Tibetan lake. Journal of Paleolimnology 32, (2004). 273–286.CrossRefGoogle Scholar
Morrill, C., Overpeck, J.T., and Cole, J.E. A synthesis of abrupt changes in the Asian summer monsoon since the last deglaciation. The Holocene 13, (2003). 465–476.CrossRefGoogle Scholar
Morrill, C., Overpeck, J.T., Cole, J.E., Liu, K.B., Shen, C.M., and Tang, L.Y. Holocene variations in the Asian monsoon inferred from geochemistry of lake sediments in central Tibet. Quaternary Research 65, (2006). 232–243.Google Scholar
Murray, A.S., and Wintle, A.G. Luminescence dating of quarts using an improved single-aliquot regenerative-dose procedure. Radiation Measurement 32, (2000). 57–73.CrossRefGoogle Scholar
Overpeck, J.T., Anderson, D.M., Trumbore, S., and Prell, W.L. The southwest Indian Monsoon over the last 18,000 years. Climate Dynamics 12, (1996). 213–225.Google Scholar
Partridge, T.C. Warming phases in the Southern Africa during the last 150,000 years—an overview. Palaleogeography, Palaeoclimatology, Palaeoecology 101, (1993). 237–244.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.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 variations. Radiation Measurements 23, (1994). 497–500.Google Scholar
Qiang, M.R., Chen, F.H., Wang, Z.T., Niu, G.M., and Song, L. Aeolian deposits at the southeastern margin of the Tengger Desert (China): Implications for surface wind strength in the Asian dust source area over the past 20,000 years. Palaeogeoraphy, Palaeoclimatology, Palaeoecology 286, (2010). 66–80.Google Scholar
Qiang, M.R., Song, L., Chen, F.H., Li, M.Z., Liu, X.X., Wang, Q., in press. A 16-ka lake-level record inferred from macrofossils in a sediment core from Genggahai Lake, northeastern Qinghai-Tibetan Plateau (China). Journal of Paleolimnology, doi: 10.1007/s10933-012-9660-z.CrossRefGoogle Scholar
Rhode, D., Zhang, H.Y., Madsen, D.B., Gao, X., Brantingham, P.J., Ma, H.Z., and Olsen, J.W. Epipaleolithic/early Neolithic settlements at Qinghai Lake, western China. Journal of Archaeological Science 34, (2007). 600–612.Google Scholar
Schlütz, F., and Lehmkuhl, F. Holocene climatic change and the nomadic Anthropocene in Eastern Tibet: palynological and geomorphological results from the Nianbaoyeze Mountains. Quaternary Science Reviews 28, (2009). 1449–1471.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
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
Stauch, G., IJmaker, J., Pötsch, S., Zhao, H., Hilgers, A., Diekmann, B., Dietze, E., Hartmann, K., Opitz, S., Wünnemann, B., and Lehmkuhl, F. Aeolian sediments on the north-eastern Tibetan Plateau. Quaternary Science Reviews 57, (2012). 71–84.Google Scholar
Stevens, T., Thomas, D.S.G., Armitage, S.J., Lund, H.R., and Lu, H.Y. Reinterpreting climate proxy records from late Quaternary Chinese Loess: A detailed OSL investigation. Earth-Science Reviews 80, (2007). 111–136.Google Scholar
Stuiver, M., Groots, P.M., and Braziunas, T.F. The GISP2 δ18O climate record of the past 16,500 years and the roles of the sun, ocean and volcanoes. Quaternary Research 44, (1995). 341–354.Google Scholar
Sun, J.G., Li, B.G., and Lu, Q. Temporal-spatial analysis of temperature and its effect on climate and water in Qinghai Gonghe Basin. Progress in Geography 23, (2004). 100–106. (in Chinese with English abstract) Google Scholar
Sun, J.M., Li, S.-H., Han, P., and Chen, Y.Y. Holocene environmental changes in the central Inner Mongolian, based on single-aliquot-quartz optical dating and multi-proxy study of dune sands. Palaeogeoraphy, Palaeoclimatology, Palaeoecology 233, (2006). 51–62.Google Scholar
Sun, Y.J., Lai, Z.P., Long, H., Liu, X.J., and Fan, Q.S. Quartz OSL dating of archaeological sites in Xiao Qaidam Lake of the NE Qinghai-Tibetan Plateau and its implications for palaeoenvironmental changes. Quaternary Geochronology 5, (2010). 360–364.Google Scholar
Sun, Y.J., Lai, Z.P., Madsen, D., and Hou, G.L. Luminescence dating of a hearth from the archaeological site of Jiangxigou in the Qinghai Lake area of the northeastern Qinghai-Tibetan Plateau. Quaternary Geochronology 12, (2012). 107–110.CrossRefGoogle 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
Wang, Y.J., Cheng, H., Edwards, L.R., An, Z.S., Wu, J.Y., Shen, C.-C., and Dorale, J.A. A high-resolution absolute-dated late Pleistocene monsoon record from Hulu Cave, China. Science 294, (2001). 2345–2348.Google Scholar
Wang, Y.J., Cheng, H., Edwards, R.L., He, Y.Q., Kong, X.G., An, Z.S., Wu, J.Y., Kelly, M.J., Dykoski, C.A., and Li, X.D. The Holocene Asian Monsoon: links to solar changes and North Atlantic Climate. Science 308, (2005). 854–857.Google Scholar
Wang, Y.B., Liu, X.Q., and Herzschuh, U. Asynchronous evolution of the Indian and East Asian Summer monsoon indicated by Holocene moisture patterns in monsoonal central Asia. Earth-Science Reviews 103, (2010). 135–153.Google Scholar
Wang, L., Li, J.J., Lu, H.Y., Gu, Z.Y., Rioual, P., Hao, Q.Z., Mackay, A.W., Jiang, W.Y., Cai, B.G., Xu, B., Han, J.T., and Chu, G.Q. The East Asian winter monsoon over the last 15,000 years: its links to high-latitudes and tropical climate systems and complex correlation to the summer monsoon. Quaternary Science Reviews 32, (2012). 131–142.Google Scholar
Wintle, A.G., and Murray, A.S. A review of Quartz optically stimulated luminescence characteristics and their relevance in single aliquot regeneration protocols. Radiation Measurements 41, (2006). 369–391.Google Scholar
Wischnewski, J., Mischke, S., Wang, Y.B., and Herzschuh, U. Reconstructing climate variability on the northeastern Tibetan Plateau since the last Lateglacial―a multi-proxy, dual-site approach comparing terrestrial and aquatic signals. Quaternary Science Review 30, (2011). 82–97.Google Scholar
Xiao, J.L., Nakamura, T., Lu, H.Y., and Zhang, G.Y. Holocene climate changes over the desert/loess transition of north-central China. Earth and Planetary Science Letter 197, (2002). 11–18.Google Scholar
Xu, S.Y., Xu, D.F., and Shi, S.R. Aeolian sand deposits in the Gonghe Basin, Qinghai province. Journal of Desert Research 2, (1982). 1–8. (in Chinese with English abstract) Google Scholar
Xu, S.Y., Xu, D.F., and Shi, S.R. A discussion on the development of landforms and evolution of environments in the Gonghe Basin. Journal of Lanzhou University 20, (1984). 146–157. (in Chinese with English abstract) Google Scholar
Yang, L.H., Wang, T., Zhou, J., Lai, Z.P., and Long, H. OSL chronology and possible forcing mechanisms of dune evolution in the Horqin dunefield in northern China since the Last Glacial Maximum. Quaternary Research 78, (2012). 185–196.CrossRefGoogle Scholar
Yang, X.P., Li, H.W., and Conacher, A. Large-scale controls on the development of sand seas in northern China. Quaternary International 250, (2012). 74–83.Google Scholar
Yu, L.P., and Lai, Z.P. OSL chronology and palaeoclimatic implications of aeolian sediments in the eastern Qaidam Basin of northeastern Qinghai-Tibetan Plateau. Palaeogeoraphy, Palaeoclimatology, Palaeoecology 337–338, (2012). 120–129.CrossRefGoogle Scholar
Yu, X.F., Zhou, W.J., Liu, Z., and Kang, Z.H. Different patterns of changes in the Asian summer and winter monsoons on the eastern Tibetan Plateau during the Holocene. The Holocene 21, (2011). 1031–1036.CrossRefGoogle Scholar
Zeng, Y.N., Ma, H.Z., Sha, Z.J., Li, L.Q., Li, Z., and Cao, G.C. The record of Younger Drays event in eolian sand deposits in Qaidam Basin. Chinese Geographical Science 9, (1999). 92–95. (in Chinese with English abstract) CrossRefGoogle Scholar
Zeng, Y.N., Feng, Z.D., and Cao, G.C. Desert formation and evolution in Qaidam Basin since the Last Glacial epoch. Acta Geographica Sinica 58, (2003). 452–457. (in Chinese with English abstract) Google Scholar
Zhang, J.W., Chen, F.H., Holmes, J.A., Li, H., Guo, X.Y., Wang, J.L., Li, S., Lü, Y.B., Zhao, Y., and Qiang, M.R. Holocene monsoon climate documented by oxygen and carbon isotopes from lake sediments and peat bogs in China: a review and synthesis. Quaternary Science Reviews 30, (2011). 1973–1987.CrossRefGoogle Scholar
Zhao, Y., and Yu, Z.C. Vegetation response to Holocene climate change in East Asian monsoon-margin region. Earth-Science Reviews 113, (2012). 1–10.Google Scholar
Zhao, Y., Yu, Z.C., Chen, F.H., Zhang, J.W., and Yang, B. Vegetation response to Holocene climate change in monsoon-influenced region of China. Earth-Science Reviews 97, (2009). 242–256.Google Scholar
Zhao, C., Yu, Z., Zhao, Y., Ito, E., Kodama, K.P., and Chen, F. Holocene millennial-scale climate variations documented by multiple lake-level proxies in sediment cores from Hurleg Lake, Northwest China. Journal of Paleolimnology 44, (2010). 995–1008.CrossRefGoogle Scholar
Zhao, H., Lu, Y.C., Wang, C.M., Chen, J., Liu, J.F., and Mao, H.L. ReOSL dating of aeolian and fluvial sediments from Nihewan Basin, northern China and its environmental application. Quaternary Geochronology 5, (2010). 159–163.Google Scholar
Zhu, Z.D. An Outline on Chinese Deserts. (1980). Science Press, Beijing. (in Chinese) Google Scholar
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