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- [4] Variations in air temperature during the last 100 years revealed by δ18O in the Malan ice core from the Tibetan Plateau CHINESE SCIENCE BULLETIN, 2003, 48 (19): : 2134 - 2138
- [9] Reply to the comment of Sternberg on "Zech et al. (2014) Oxygen isotope ratios (18O/16O) of hemicellulose-derived sugar biomarkers in plants, soils and sediments as paleoclimate proxy I: Insight from a climate chamber experiment. GCA 126, 614-623." GEOCHIMICA ET COSMOCHIMICA ACTA, 2014, 141 : 680 - 682