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Landscape evolution of the Ulan Buh Desert in northern China during the late Quaternary

Published online by Cambridge University Press:  20 January 2017

Fahu Chen ,
Guoqiang Li ,
Hui Zhao ,
Ming Jin ,
Xuemei Chen ,
Yuxin Fan ,
Xiaokang Liu ,
Duo Wu  and
David Madsen
Fahu Chen*
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
Guoqiang Li
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
Hui Zhao
Affiliation:
Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Ming Jin
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
Xuemei Chen
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
Yuxin Fan
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
Xiaokang Liu
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
Duo Wu
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
David Madsen
Affiliation:
MOE Key Laboratory of West China's Environmental System, Research School of Arid Environment and Climate Change, Lanzhou University, Lanzhou 730000, China
*
*Corresponding author. Fax: + 86 931 8912330. E-mail address:[email protected] (F. Chen).
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Abstract

The evolution of arid environments in northern China was a major environmental change during the Quaternary. Here we present the dating and environmental proxy results from a 35 m long core (A-WL10ZK-1) collected from the Ulan Buh Desert (UBD), along with supplemental data from four other cores. The UBD is one of the main desert dune fields in China and our results indicate the UBD has undergone complex evolution during the late Quaternary. Most of the present UBD was covered by a Jilantai-Hetao Mega-paleolake lasting until ~ 90 ka ago. A sandy desert environment prevailed throughout the UBD during the last glacial period and early Holocene. A wetland environment characterized by the formation of numerous interdunal ponds in the northern UBD occurred at ~ 8–7 ka, although a dune field persisted in the southern UBD. The modern UBD landscape formed after these wetlands dried up. During the last 2000 years, eolian sand from the Badain Jaran Desert has invaded the northern UBD, while farming and overgrazing resulted in the formation of the eastern UBD. We suggest that the formation of UBD landforms is related to the disintegration of the megalake Jilantai-Hetao and to summer monsoon changes during the last glaciation and Holocene.

Keywords

Arid landscape evolutionUlan Buh DesertLast glacial periodHoloceneChina
Type
Articles
Information
Quaternary Research , Volume 81 , Issue 3 , May 2014 , pp. 476 - 487
Copyright
University of Washington

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References

Aitken, M.J. An Introduction to Optical Dating. (1998). Oxford University Press, Oxford, UK.CrossRefGoogle Scholar
Banerjee, D., Murray, A.S., Bøter-Jensen, L., and Lang, A. Equivalent dose estimation using a single aliquot of polymineral fine grains. Radiation Measurements 33, (2001). 73–94.CrossRefGoogle Scholar
Biscaye, P.E., Grousset, F.E., Revel, M., Van der Gaast, S., Zielinski, G.A., Vaars, A., and Kukla, G. Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2 Ice Core, summit, Greenland. Journal of Geophysical Research 102, (1997). 26765–26781.Google Scholar
Bøtter-Jensen, L., McKeever, S.W.S., and Wintle, A.G. Optically Stimulated Luminescence Dosimetry. (2003). Elsevier, Amsterdam. 355 Google Scholar
Bush, A. CO2/H2O and orbitally driven climate variability over central Asia through the Holocene. Quaternary International 136, (2005). 15–23.CrossRefGoogle Scholar
Cai, Y.J., Tan, L.C., Cheng, H., An, Z.S., Edwards, L.R., Kelly, M.J., Kong, X.G., and Wang, X.F. The variation of summer monsoon precipitation in central China since the last deglaciation. Earth and Planetary Science Letters 291, (2010). 21–31.CrossRefGoogle Scholar
Chen, F.H., Fan, Y.X., Chun, X., Madsen, D.B., Oviatt, C.G., Zhao, H., Yang, L.P., and Sun, Y. Preliminary research on Megalake Jilantai-Hetao in the arid areas of China during the late Quaternary. Chinese Science Bulletin 53, (2008). 1725–1739.CrossRefGoogle 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 Wünnemann, B. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews 27, (2008). 351–364.Google Scholar
Chen, F.H., Fan, Y.X., Madsen, D.B., Chun, X., Zhao, H., and Yang, L.P. Preliminary study on the formation mechanism of the “Jilantai-Hetao” megalake and the lake evolutionary history in Hetao region. Quaternary Sciences 28, (2008). 866–873. (in Chinese with English abstract) Google Scholar
Chen, F.H., Qiang, M.R., Zhou, A.F., Xiao, S., and Chen, J.H. A 2000-year dust storm record from Lake Sugan in the dust source area of arid China. Journal of Geophysical Research (2013). http://dx.doi.org/10.1002/jgrd.50140/pdf (http://onlinelibrary.wiley.com/)Google Scholar
Chun, X., Chen, F.H., and Fan, Y.X. Formation of Ulan Buh Desert and its environmental changes during the Holocene. Frontiers of Earth Science in China 2, (2008). 327–332.CrossRefGoogle Scholar
Clark, P.U., Dyke, A.S., Shakun, J.D., Carlson, A.E., Clark, J., Wohlfarth, B., Mitrovica, J.X., Hostetler, S.W., and McCabe, A.M. The Last Glacial Maximum. Science 325, (2009). 710–714.CrossRefGoogle ScholarPubMed
Ding, Z.J., Sun, J.M., and Liu, T.S. The sedimentological indicator: linking the coupling relationship on the loess-desert evolutionary course. Science in China Series D 29, (1999). 82–87.Google Scholar
Dong, G. Studies on Deserts' Formation and Evolution, Climate Changes and Desertification in China. (2002). China Ocean Press, Beijing. (in Chinese) Google Scholar
Dykoski, C.A., Edwards, R.L., Cheng, H., Yuan, D.X., Cai, Y.J., Zhang, M.L., Lin, Y.F., Qing, J.M., An, Z.S., and Revenaugh, J. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth and Planetary Science Letters 233, (2005). 71–86.CrossRefGoogle Scholar
Faegri, K., and Iversen, J. Test Book of Pollen Analysis (3rd). (1989). Blackwell, Oxford.Google Scholar
Fan, Y.X. Study on the Evolution of the Jilantai-Hetao Megalake Focusing on Optical Dating of Lakeshore Sediments. (Ph.D. Thesis) (2008). Lanzhou University, China. (in Chinese with English abstract) Google Scholar
Fan, Y.X., Chen, F.H., Fan, T.L., Zhao, H., and Yang, L.P. Sedimentary documents and Optically Stimulated Luminescence (OSL) dating for formation of the present landform of the northern Ulan Buh Desert, northern China. Science in China Series D 53, (2010). 1675–1682.Google Scholar
Fan, Y.X., Chen, F.H., Wei, G.X., Madsen, D.B., Oviatt, C.G., Zhao, H., Chun, X., Yang, L.P., Fan, T.L., and Li, G.Q. Potential water sources for late Quaternary Megalake Jilantai-Hetao, China, inferred from mollusk shell 87Sr/86Sr ratios. Journal of Paleolimnology 43, (2010). 577–587.CrossRefGoogle Scholar
Geological and Mineral Bureau of Inner Mongolia Autonomous Region, Areal Geological Survey for Inner Mongolia Autonomous Region. (1991). Geological Publishing House, Beijing. 327–329. (in Chinese) Google Scholar
Heiri, O., Lotter, A.F., and Lemcke, G. Loss on ignition as a method for estimating organic and carbonate content in sediments: reproducibility and comparability of results. Journal of Paleolimnology 25, (2001). 101–110.Google Scholar
Hou, The Theory and Case Study of Historical Geography. (1979). Shanghai People's Publishing House, Shanghai, China. (in Chinese) Google Scholar
Hou, R.Z., and Yu, C.W. Environmental variance and archaeological findings in the Ulan Buh Desert. Archaeology 2, (1973). 92–107. (in Chinese) Google Scholar
Jia, T.F., Yin, S., He, Y., Zhao, M., and Bao, G.L. Holocene sediment texture and its environmental meaning of Donghaizi Lake in Ulan Buh Desert. Journal of Desert Research 23, (2003). 165–170. (in Chinese with English abstract) Google Scholar
Jing, A. An Introduction to Desert Archaeology. (2001). Forbidden City Publishing House, Beijing. (in Chinese) Google Scholar
Lai, Z.P. 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 37, (2009). 176–185.CrossRefGoogle Scholar
Li, S.H. Identification of well-bleached grains in the optical dating of quartz. Quaternary Science Reviews 20, (2001). 1365–1370.Google Scholar
Li, B., and Li, S.-H. Luminescence dating of K-feldspar from sediments: a protocol without anomalous fading correction. Quaternary Geochronology 6, (2011). 468–479.CrossRefGoogle Scholar
Li, B., and Li, S.-H. Luminescence dating of Chinese loess beyond 130 ka using the non-fading signal from K-feldspar. Quaternary Geochronology 10, (2012). 24–31.CrossRefGoogle Scholar
Li, B.Y., Ge, Q.S., and Zhen, J.Y. Evolution of the Yellow River in the Hetao Plain of Inner Mongolia in the past 2000 years. Acta Geographica Sinica 58, (2003). 239–246. (in Chinese with English abstract) Google Scholar
Li, J.B., Ran, Y.K., and Guo, W.S. Research on the lacustrine strata of the Tuoketuo mesa, Hetao basin, China. Quaternary Sciences 25, (2005). 630–639. (in Chinese with English abstract) Google Scholar
Li, S.H., Chen, Y.Y., Li, B., Sun, J.M., and Yang, L.R. OSL dating of sediments from deserts in northern China. Quaternary Geochronology 2, (2007). 23–28.CrossRefGoogle Scholar
Li, G.J., Chen, J., Ji, J.F., Yang, J.D., and Conway, T.M. Natural and anthropogenic sources of East Asian dust. Geology 37, (2009). 727–730.Google Scholar
Liu, C.Q., Akimasa, M., Akihiko, O., Sadayo, Y., and Fan, Z.L. Isotope geochemistry of Quaternary deposits from the arid lands in northern China. Earth and Planetary Science Letters 127, (1994). 25–38.Google Scholar
Long, H., Lai, Z.P., Wang, N.A., and Li, Y. Holocene climate variations from Zhuyeze terminal lake records in East Asian monsoon margin in arid northern China. Quaternary Research 74, (2010). 46–56.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/10.1029/2005GL024560Google Scholar
Maher, L.J. Statistics for microfossil concentration measurements employing samples spiked with marker grains. Review of Palaeobotany and Palynology 32, (1981). 153–191.Google Scholar
Markey, B.G., Bøtter-Jensen, L., and Duller, G.A.T. A new flexible system for measuring thermally and optically stimulated luminescence. Radiation Measurements 27, (1997). 83–89.Google Scholar
Pang, X.L., and Hu, D.S. Environment evolution and salt forming process of Jilantai salt lake since 22 ka BP. Journal of Desert Research 29, (2009). 193–199. (in Chinese with English abstract) Google Scholar
Peng, Y.J., Xiao, J.L., Nakamura, T., Liu, B.L., and Inouchi, Y. Holocene East Asian monsoonal precipitation pattern revealed by grainsize distribution of core sediments of Daihai Lake in Inner Mongolia of north-central China. Earth and Planetary Science Letters 233, (2005). 467–479.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
Qiang, M.R., Chen, F.H., Zhang, J.W., Zu, R.P., Jin, M., Zhou, A.F., and Xiao, S. Grain size in sediments from Lake Sugan: a possible linkage to dust storm events at the northern margin of the Qinghai–Tibetan Plateau. Environmental Geology 51, (2006). 1229–1238.CrossRefGoogle Scholar
Qin, D.H. Environment Changes Assessment for Western China. (2002). Science Press, Beijing, China. (in Chinese) Google Scholar
Santisteban, J.I., Mediavilla, R., López-Pamo, E., Dabrio, C.J., Zapata, M.B.R., García, M.J.G., Castaño, S., and Martínez-Alfaro, P.E. Loss on ignition: a qualitative or quantitative method for organic matter and carbonate mineral content in sediments?. Journal of Paleolimnology 32, (2004). 287–299.Google Scholar
Sun, J.M., and Liu, T.S. The age of the Taklimakan Desert. Science 312, (2006). 1621 Google Scholar
Sun, J.M., Zhang, M.Y., and Liu, T.S. 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, (2001). 10325–10333.Google Scholar
Sun, Y.B., Tada, R.J., Chen, J., Liu, Q.S., Toyoda, S., Tani, A., Ji, J.F., and Isozaki, Y. Tracing the provenance of fine-grained dust deposited on the central Chinese Loess Plateau. Geophysical Research Letters 35, (2008). L01804 http://dx.doi.org/10.1029/2007GL031672Google Scholar
Sun, J.M., Zhang, Z.Q., and Zhang, L.Y. New evidence on the age of the Taklimakan Desert. Geology 37, (2009). 159–162.CrossRefGoogle Scholar
Tan, Q.X. Historical Atlas of China. (1991). Xiao Yuan Press, Taipei.Google Scholar
Uno, I., Eguchi, K., Yumimoto, K., Takemura, T., Shimizu, A., Uematsu, M., Liu, Z.Y., Wang, Z.F., Hara, Y., and Sugimoto, N. Asian dust transported one full circuit around the globe. Nature Geoscience 2, (2009). 557–560.Google Scholar
Wang, T. Desert and Desertification in China. (2003). Hebei Science and Technology Press, Shijiazhuang. (in Chinese) Google Scholar
Wang, F.X., Qian, N.F., and Zhang, Y.L. Pollen Flora of China. 2nd ed. (1995). Science Press, Beijing. (in Chinese) 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.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 224000 years. Nature 451, (2008). 1090–1093.Google Scholar
Xi, Y.Z., and Ning, J.C. Study on pollen morphology of plants from dry and semidry area in China. Yushania 11, (1994). 119–191. (in Chinese with English abstract) Google Scholar
Xiao, J.L., Xu, Q.G., Nakamura, T., Yang, X.L., Liang, W.D., and Inouchi, Y. Holocene vegetation variation in the Daihai Lake region of north-central China: a direct indication of the Asian monsoon climate history. Quaternary Science Reviews 23, (2004). 1669–1679.Google Scholar
Xu, Q.H., Xiao, J.L., Toshio, N., Yang, X.L., Yang, Z.J., Liang, W.D., Biro, I., and Yang, S.Y. Quantitative reconstructed climatic changes of Daihai basin by pollen data. Marine Geology & Quaternary Geology 23, (2003). 99–108. (in Chinese with English abstract) Google Scholar
Yan, C.M., Dong, G.R., Tao, Z. et al. Late Tertiary eolian sand accumulation and its environment in the southeastern marginal Tengger Desert. Journal of Desert Research 12, (1992). 10–15. (in Chinese with English abstract) Google Scholar
Yang, X.P., and Williams, M.A.J. The ion chemistry of lakes and late Holocene desiccation in the Badain Jaran desert, Inner Mongolia, China. Catena 51, (2003). 45–60.Google Scholar
Yang, G.S., Liu, L.Y., and Liu, Z.M. Land desertification and its integrated transformation of Dengkou County. Journal of Arid Land Resources and Environment 5, (1991). 1–11. (in Chinese with English abstract) Google Scholar
Yang, D., Fang, X.M., Dong, G.R., Peng, Z.C., and Li, J.J. Aeolian deposit evidence for formation and evolution of the Tengger Desert in the north of China since early Pleistocene. Marine Geology & Quaternary Geology 26, (2006). 93–100. (in Chinese with English abstract) Google Scholar
Yang, L.P., Chen, F., Chun, X., Fan, Y., Sun, Y., Madsen, D.B., and Zhang, X. The Jilantai Salt Lake shorelines in Northwestern arid China revealed by remote sensing images. Journal of Arid Environments 72, (2008). 861–866.CrossRefGoogle Scholar
Yang, L.H., Zhou, J., Lai, Z.P., Long, H., and Zhang, J.R. Late glacial and Holocene dune evolution in the Horqin dune field of northeastern China based on luminescence dating. Palaeogeography, Palaeoclimatology, Palaeoecology 296, (2010). 44–51.Google Scholar
Yang, X.P., Scuderi, L., Liu, T., Paillou, P., Li, H.W., Dong, J.F., Zhu, B.Q., Jiang, W.W., Jochems, A., and Weissmann, G. Formation of the highest sand dunes on Earth. Geomorphology 135, (2011). 108–116.Google Scholar
Yao, T.D., Thompson, L.G., Shi, Y.F., 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 Series D 27, (1997). 447–452.Google Scholar
Yin, Z.Q., Qin, X.G., Wu, J.S., and Ning, B. The multimodal grain-size distribution characteristics of loess, desert, lake and river sediment in some areas of northern China. Acta Sedimentologica Sinica 27, (2009). 343–351. (in Chinese with English abstract) Google Scholar
Yuan, D.X., Cheng, H., Edwards, R.L., Dykoski, C.A., Kelly, M.J., Zhang, M.L., Qing, J.M., Lin, Y.S., Wang, Y.J., Wu, J.Y., Dorale, J.A., An, Z.S., and Cai, Y.J. Timing, duration, and transitions of the last interglacial Asian monsoon. Science 304, (2004). 575–578.Google Scholar
Zhang, J.F., and Zhou, L.P. Optimization of the ‘double SAR’ procedure for polymineral fine grains. Radiation Measurements 42, (2007). 1475–1482.CrossRefGoogle Scholar
Zhang, J.F., Zhou, L.P., and Yue, S.Y. Dating fluvial sediments by optically stimulated luminescence: selection of equivalent doses for age calculation. Quaternary Science Reviews 22, (2003). 1123–1129.CrossRefGoogle Scholar
Zhang, H.C., Peng, J.L., Ma, Y.Z., Chen, G.J., Feng, Z.D., Li, B., Fan, H.F., Chang, F.Q., Lei, G.L., and Wünnemann, B. Late Quaternary paleolake levels in Tengger Desert, NW China. Palaeogeography, Palaeoclimatology, Palaeoecology 211, (2004). 45–58.Google Scholar
Zhao, H., and Li, S.H. Internal dose rate to K-feldspar grains from radioactive elements other than potassium. Radiation Measurements 40, (2005). 84–93.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.CrossRefGoogle Scholar
Zhao, H., Li, G.Q., Sheng, Y.W., Jin, M., and Chen, F.H. Early-middle Holocene lake-desert evolution in northern Ulan Buh Desert, China. Palaeogeography, Palaeoclimatology, Palaeoecology 331–332, (2012). 31–38.CrossRefGoogle Scholar
Zhu, Z., Wu, Z., Liu, S., and Di, X. An Outline of Chinese Deserts (in Chinese). (1980). Science Press, Beijing. (in Chinese) Google Scholar