13 Zhou W J, Dodson J, Head M J, et al. Environmental variability within the Chinese desert-loess transition zone over the last 20000 years.Holocene, 2002, 12: 107-112
[8]
14 Yang X P, Rost K T, Lehmkuhl F, et al. The evolution of dry land in northern China and in the Republic of Mongolia since the Last GlacialMaximum. Quat Int, 2004, 118-119: 69-85
16 Ding Z L, Sun J M, Rutter N W, et al. Changes in sand content of loess deposits along a north-south transect of the Chinese Loess Plateauand the implications for desert variations. Quat Res, 1999, 52: 56-62
[11]
17 Ding Z L, Derbyshire E, Yang S L, et al. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implicationsfor monsoon evolution. Earth Planet Sci Lett, 2005, 237: 45-55
25 Yang L R, Ding Z L. Expansion and contraction of Hulun Buir Dunefield in north-eastern China in the last late glacial and Holocene asrevealed by OSL dating. Environ Earth Sci, 2013, 68: 1305-1312
[16]
30 Vandenberghe J, Renssen H, Huissteden K V, et al. Penetration of Atlantic westerly winds into Central and East Asia. Quat Sci Rev, 2006,25: 2380-2389
33 Murray A S, Wintle A G. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiat Meas, 2000,32: 57-73
[19]
34 Lu H Y, Mason J A, Stevens T, et al. Response of surface processes to climatic change in the dunefields and Loess Plateau of North Chinaduring the late Quaternary. Earth Surf Proc Land, 2011, 36: 1590-1603
37 Zhou Y L, Lu H Y, Zhang J F, et al. Luminescence dating of sand-loess sequences and response of Mu Us and Otindag sand fields (North China) to climatic changes. J Quat Sci, 2009, 24: 336-344
[23]
38 Mason J A, Lu H Y, Zhou Y L, et al. Dune mobility and aridity at the desert margin of northern China at a time of peak monsoon strength.Geology, 2009, 37: 947-950
[24]
39 Stevens T, Lu H Y, Thomas D S G, et al. Optical dating of abrupt shifts in the late Pleistocene East Asian monsoon. Geology, 2008, 36:415-418
48 Li S H, Sun J M, Zhao H. Optical dating of dune sands in the northeastern deserts of China. Palaeogeogr Palaeoclim Palaeoecol, 2002, 181:419-429
[29]
49 Li S H, Sun J M. Optical dating of Holocene dune sands from the Hulun Buir desert, Northeastern China. Holocene, 2006, 13: 457-462
[30]
50 Li S H, Fan A C. OSL chronology of sand deposits and climate change of last 18 ka in Gurbantunggut Desert, northwest China. J Quat Sci,2011, 26: 813-818
[31]
51 Li B, Li S H, Sun J M. Isochron dating of sand-loess-soil deposits from the Mu Us Desert margin, central China. Quat Geochron, 2011, 6:556-563
60 Guo Z T, Petit-Maire N, Kr?pelin S. Holocene non-orbital climatic events in present-day arid areas of northern Africa and China. GlobPlanet Change, 2000, 26: 97-103
2 Bush A B G, Rokosh D, Rutter N W, et al. Desert margins near the Chinese Loess Plateau during the mid-Holocene and at the Last GlacialMaximum: A model-data intercomparison. Global Planet Change, 2002, 32: 361-374
[39]
3 Timm O, Timmermann A, DeCarlo1 S H. User-friendly data portal provides access to a transient paleoclimate simulation covering the last 21 ka. PAGES News, 2009, 17: 4-5
18 Lu H Y, Miao X D, Zhou Y L, et al. Late Quaternary aeolian activity in the Mu Us and Otindag dune fields (North China) and lagged responseto insolation forcing. Geophys Res Lett, 2005, 32: L21716
[45]
19 Lu H Y, Wang X Y, Li L P. Aeolian sediment evidence that global cooling has driven late Cenozoic stepwise aridification in central Asia.In: Clift P D, Tada R, Zheng H, eds. Monsoon Evolution and Tectonics—Climate Linkage in Asia. London: Geological Society SpecialPublications, 2010, 342: 29-44
21 Yang S L, Ding Z L. Advance-retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last twoglacial-interglacial cycles. Earth Planet Sci Lett, 2008, 274: 499-510
31 Chen F H, Yu Z C, Yang M L, et al. Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoonhistory. Quat Sci Rev, 2008, 27: 351-364
47 Sun J M. Origin of eolian sand mobilization during the past 2300 years in the Mu Us Desert, China. Quat Res, 2000, 53: 78-88
[58]
52 Zhao H, Lu Y C, Yin J H. Optical dating of Holocene sand dune activities in the Horqin sand-fields in Inner Mongolia, China, using theSAR protocol. Quat Geochron, 2007, 2: 29-33
[59]
53 He Z, Zhou J, Lai Z P, et al. Quartz OSL dating of sand dunes of Late Pleistocene in the Mu Us Desert in northern China. Quat Geochron,2010, 5: 102-106
[60]
55 Yang L H, Zhou J, Lai Z P, et al. Lateglacial and Holocene dune evolution in the Horqin dunefield of northeastern China based on luminescencedating. Palaeogeogr Palaeoclim Palaeoecol, 2010, 296: 44-51
[61]
56 Yang L H, Wang T, Zhou J, et al. OSL chronology and possible forcing mechanisms of dune evolution in the Horqin dunefield in northernChina since the Last Glacial Maximum. Quat Res, 2012, 78: 185-196
[62]
57 Yu L P, Lai Z P. OSL chronology and palaeoclimatic implications of aeolian sediments in Qaidam Basin of northeastern Qinghai-TibetanPlateau. Palaeogeogr Palaeoclim Palaeoecol, 2012, 337-338: 120-129
[63]
58 Duller G A T, Wintle A G. A review of the thermally transferred optically stimulated luminescence signal from quartz for dating sediments.Quat Geochron, 2012, 7: 6-20
[64]
64 Lu H Y, Zhou Y L, Liu W G, et al. Organic stable carbon isotopic composition reveals late Quaternary vegetation changes in the dunefields of northern China. Quat Res, 2012, 77: 433-444