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Zhu, R. X., Ding, Z. L., Wu, H. N., and Li, C. Y., Details of magnetic polarity transition recorded in Chinese loess, Journal of Geomagnetism and Geoelectricity, 45(1993), 289-299..
Rutter, N. W., Ding, Z. L., and Liu, T. S., Reliability of grain size variation as a climatic proxy and correlation method for loess-paleosol units, north-central China, International Conference on Geology, Geotechnology and Mineral Resources, Thailand, (1995), 45-52.
Liu, T. S., Ding, Z. L., Chinese loess and the paleomonsoon, Annual Reviews of Earth and Planetary Sciences, 26(1998), 111-145.
Sun, J. M., Ding, Z. L., Liu, T. S., Desert distributions during the glacial maximum and climatic optimum: Example of China, Episodes, 21(1998), 28-31.
Sun, J. M., Ding, Z. L., Deposits and soils of the past 130,000 years at the desert-loess transition in northern China, Quaternary Research, 50(1998), 148-156.
Yu, Z. W., Ding, Z. L., An automatic orbital tuning method for paleoclimate records, Geophysical Research Letters, 25(1998), 4525-4528.
Liu, T. S., Ding, Z. L., and Rutter, N.W., Comparison of Milankovitch periods between continental loess and deep sea records over the last 2.5 Ma, Quaternary Science Reviews, 18(1999), 1205-1212.
Sun, J. M., Ding, Z. L., Liu, T. S., Rokosh, D., and Rutter, N., 580,000 year environmental reconstruction from eolian deposits at the Mu Us desert margin, China, Quaternary Science Reviews, 18(1999), 1351-1364.
Xiong, Shangfa, Ding, Zhongli, and Liu, Tungsheng, Climatic implications of loess deposits from the Beijing region, Journal of Quaternary Science, 16(2001), 575-582.
Xiong, Shangfa, Ding, Zhongli, and Yang, Shiling, Abrupt shifts in the late Cenozoic environment of north-western China recorded in loess-palaeosol-red clay sequences, Terra Nova, 13(2001), 376-381.
Xiong, Shangfa, Ding, Zhongli, Liu, Tungsheng, and Zhang, Jingzhao, East Asian monsoon instability at the stage 5a/4 transition, Boreas, 31(2002), 126-132.
Xiong, S. F., Ding, Z. L., Jiang, W. Y., Yang, S. L., and Liu, T. S., Initial intensification of East Asian winter monsoon at about 2.75 Ma as seen in the Chinese eolian loess-red clay deposit, Geophysical Research Letters, 30(2003), Vol. 30, No. 10, 1524, doi: 10.1029/2003GL017059.
Xiong, S. F., Ding, Z. L., Jiang, W. Y., Yang, S. L., and Liu, T. S., Damped fluctuations in Chinese loess grain size, Geophysical Research Letters, 30(2003), 2007, doi:10.1029/ 2003GL018187.
Yang, S. L., Ding, Z. L., Color reflectance of Chinese loess and its implications for climate gradient changes during the last two glacial-interglacial cycles, Geophysical Research Letters, 30(2003), 2058, doi:10.1029/2003GL018346.
Yang, S. L., Ding, Z. L, Comparison of particle size characteristics of the Tertiary “red clay” and Pleistocene loess in the Chinese Loess Plateau: implications for origin and sources of the “red clay”, Sedimentology, 51(2004), 77-93.
Jiang, H. C., Ding, Z. L., Temporal and spatial changes of vegetation cover on the Chinese Loess Plateau through the last glacial cycle: evidence from spore-pollen records, Review of Palaeobotany and Palynology, 133(2005), 23-37.
Yang, S.L., Ding, Z.L., Winter-spring precipitation as the principal control on predominance of C3 plants in Central Asia over the past 1.77 Myr: Evidence from δ13C of loess organic matter in Tajikistan, Palaeogeography, Palaeoclimatology, Palaeoecology, 235(2006), 330-339.
Jiang, H.C., Ding, Z.L., Xiong, S.F., Magnetostratigraphy of the Neogene Sikouzi section at Guyuan, Ningxia, China. Palaeogeography, Palaeoclimatology, Palaeoecology 243 (2007) 223-234.
Jiang, H.C., Ding, Z.L., A 20 Ma pollen record of East-Asian summer monsoon evolution from Guyuan, Ningxia, China. Palaeogeography, Palaeoclimatology, Palaeoecology 265, 30-38.
Yang, S. L, .Ding, Z. L., Advance-retreat history of the East-Asian summer monsoon rainfall belt over northern China during the last two glacial-interglacial cycles. Earth and Planetary Science Letters, 274(2008), 499-510.
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