[1] 刘东生.黄土与环境[M].北京:科学出版社,1985:1-481.
[2] Guo Z,Ruddiman W,Hao Q,et al.Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J].Nature,2002,416(6877):159-163.
[3] Liu T,Ding Z.Chinese loess and the paleomonsoon[J].Annual Review of Earth & Planetary Sciences,1998,26(26):111-145.
[4] An Z,Wu G,Li J,et al.Global monsoon dynamics and climate change[J].Annual Review of Earth & Planetary Sciences,2015,42(1):29-77.
[5] 鹿化煜,安芷生,刘洪滨,等.洛川黄土记录的最近2500 ka东亚冬夏季风变化周期[J].地质论评,1998,44(5):553-558.
[6] Lu H,Wang X,Li L.Aeolian sediment evidence that global cooling has driven late Cenozoic stepwise aridification in central Asia[J].Geological Society London Special Publications,2010,342:29-44.
[7] 鹿化煜,王先彦,李郎平.晚新生代亚洲干旱气候发展与全球变冷联系的风尘沉积证据[J].第四纪研究,2008,28(5):949-956.
[8] Ding Z,Sun J,Rutter N,et al.Changes in sand content of loess deposits along a North-South transect of the Chinese Loess Plateau and the implications for desert variations[J].Quaternary Research,1999,52(1):56-62.
[9] Ding Z,Derbyshire E,Yang S,et al.Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution[J].Earth & Planetary Science Letters,2005,237(1/2):45-55.
[10] 曾琳,鹿化煜,弋双文,等.我国东北地区黄土堆积的磁性地层年代与古气候变化[J].科学通报,2011,56(27):2267-2275.
[11] Yi S,Lu H,Stevens T.SAR TT-OSL dating of the loess deposits in the Horqin dunefield (northeastern China)[J].Quaternary Geochronology,2012,10(7):56-61.
[12] Yi S,Buylaert J,Murray A,et al.High resolution OSL and post-IR IRSL dating of the last interglacial-glacial cycle at the Sanbahuo loess site (northeastern China)[J].Quaternary Geochronology,2015,30:200-206.
[13] 裘善文.试论科尔沁沙地的形成与演变[J].地理科学,1989,9(4):317-328.
[14] 董光荣,金炯,李保生,等.科尔沁沙地沙漠化的几个问题:以南部地区为例[J].中国沙漠,1994,14(1):1-9.
[15] 弋双文,鹿化煜,周亚利,等.晚第四纪科尔沁沙地干湿变化的黄土记录[J].中国沙漠,2006,26(6):869-874.
[16] 鹿化煜,张红艳,曾琳,等.温度影响东北地区更新世植被变化的黄土记录[J].第四纪研究,2015,35(4):828-836.
[17] Vandenberghe J,Renssen H,Huissteden K,et al.Penetration of Atlantic westerly winds into Central and East Asia[J].Quaternary Science Reviews,2006,25(17/18):2380-2389.
[18] Zeng L,Lu H,Yi S,et al.New magnetostratigraphic and pedostratigraphic investigations of loess deposits in north-east China and their implications for regional environmental change during the Mid-Pleistocene climatic transition[J].Journal of Quaternary Science,2016,31(1):20-32.
[19] Zeng L,Lu H,Yi S,et al.Long-term Pleistocene aridification and possible linkage to high-latitude forcing:new evidence from grain size and magnetic susceptibility proxies from loess-paleosol record in northeastern China[J].Catena,2017,154:2132.
[20] Lisiecki L E,Raymo M E.A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records[J].Paleoceanography,2005,20(1):1-16.
[21] 鹿化煜,安芷生.洛川黄土粒度组成的古气候意义[J].科学通报,1997,42(1):66-69.
[22] Lu H,Vandenberghe J,An Z.Aeolian origin and palaeoclimatic implications of the ‘red clay’ (north China) as evidenced by grain-size distribution[J].Journal of Quaternary Science,2001,16(1):89-97.
[23] 丁仲礼,孙继敏.联系沙漠-黄土演变过程中耦合关系的沉积学指标[J].中国科学,1999,29(1):82-87.
[24] Ding Z,Liu T,Rutter N W,et al.Ice-volume forcing of East Asian Winter Monsoon variations in the past 800000 years[J].Quaternary Research,1995,44(2):149-159.
[25] 鹿化煜,安芷生.黄土高原黄土粒度组成的古气候意义[J].中国科学:地球科学,1998,(3):278-283.
[26] Lu H,Zhang F,Liu X,et al.Periodicities of palaeoclimatic variations recorded by loess-paleosol sequences in China[J].Quaternary Science Reviews,2004,23(18):1891-1900.
[27] Lu H,Yi S,Xu Z,et al.Chinese deserts and sand fields in Last Glacial Maximum and Holocene Optimum[J].Science Bulletin,2013,58(23):2775-2783.
[28] 陈骏,李高军.亚洲风尘系统地球化学示踪研究[J].中国科学:地球科学,2011,41(9):1211-1232.
[29] 谢静,杨石岭,丁仲礼.黄土物源碎屑锆石示踪方法与应用[J].中国科学:地球科学,2012,42(6):133-143.
[30] Lu H,Zhou Y,Liu W,et al.Organic stable carbon isotopic composition reveals late Quaternary vegetation changes in the dune fields of northern China[J].Quaternary Research,2012,77(3):433-444.
[31] 胡亚萍,贾玉连,张智,等.粒度揭示的末次间冰期以来长江中游风沙-风尘体系[J].中国沙漠,2013,33(5):1324-1332.
[32] Zan J,Fang X,Yang S,et al.Evolution of the arid climate in High Asia since~1 Ma:evidence from loess deposits on the surface and rims of the Tibetan Plateau[J].Quaternary International,2013,313-314(4):210-217.
[33] 昝金波,杨胜利,方小敏.西昆仑山黄土1 Ma以来的粒度变化特征及其古气候意义[J].地球环境学报,2014,5(2):120-126.
[34] Rea D K,Snoeckx H,Joseph L H.Late Cenozoic eolian deposition in the North Pacific:Asian drying,Tibetan uplift,and cooling of the northern hemisphere[J].Paleoceanography,1998,13(3):215-224.
[35] Lu H,Guo Z.Evolution of the monsoon and dry climate in East Asia during late Cenozoic:a review[J].Science China Earth Sciences,2014,57(1):70-79.
[36] Zhang W,Chen J,Ji J,et al.Evolving flux of Asian dust in the North Pacific Ocean since the late Oligocene[J].Aeolian Research,2016,23:11-20.
[37] 沈亚萍,张春来,李庆,等.中国东部沙区表层沉积物粒度特征[J].中国沙漠,2016,36(1):150-157.