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Paper Publications
[1] Paleoenvironmental significance of 5α-stigmastanol in surface soil and lake sediment from the Nianbaoyeze Mountains, eastern Qinghai-Tibet Plateau [J]. Journal of Paleolimnology, 2022, 68: 103–118
[2] Organic matter geochemical signatures of sediments of Lake Ngoring (Qinghai-Tibetan Plateau): A record of environmental and climatic changes in the source area of the Yellow River for the last 1500 years PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2020, 551(8): 109729
[3] 太阳辐射影响高原生态系统的湖泊沉积生物标志物证据 地球科学前沿, 2018, 8(1): 9-18
[4] “教学-实践-研究” 三位一体发展模式研究 大学教育, 2016, 5(12): 21-23
[5] Origins of biomarker aliphatic hydrocarbons in sediments of alpine Lake Ximencuo, China PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 2017, 475(11): 106-114
[6] The aliphatic hydrocarbon distributions of terrestrial plants around an alpine lake: a pilot study from Lake Ximencuo, Eastern Qinghai-Tibet Plateau Frontiers of earth science, 2018, 12(3): 600-610
[7] Unusual hydrocarbon waxes detected in Salix oritrepha leaf from Nianbaoyeze Mountains, eastern Qinghai-Tibetan Plateau JOURNAL OF MOUNTAIN SCIENCE, 2018, 15(11): 2445–2452
[8] 干旱盆地古湖相沉积物生物标志物分布特征及环境意义——以柴达木盆地为例 中国沙漠, 2013, 33(4):
[9] 青藏高原东北部柴达木盆地古湖泊沉积物正构烷烃记录的MIS3晚期气候变化 中国科学：地球科学, 2010,
[10] 我国大学自然地理课堂教学发展趋势探讨 大学教育, 2014, 3(10): 25-26
[11] 西北地区晚第四纪沉积地层一元正脂肪酸酰胺分布特征及古气候意义 地球科学进展, 2010,
[12] 柴达木盆地察尔汗湖区古湖相沉积物中含氮类分子化石的检出 地球学报, 2010,
[13] Climate variability recorded by n-alkanes of paleolake sediment in Qaidam Basin on the northeast Tibetan Plateau in late MIS3 SCIENCE CHINA Earth Sciences , 2010, 53(6):
[14] Deposition and regional distribution of HCHsandp,p′-DDX in the western and southern Tibetan Plateau:records from a lake sediment core and the surface soils Environmental Science and Pollution Research, 2013, 20(8):
[15] Paleoclimate changes of the last 1000 yr on the eastern Qinghai–Tibetan Plateau recorded by elemental, isotopic, and molecular organic matter proxies in sediment from glacial Lake Ximencuo Palaeogeography Palaeoclimatology Palaeoecology, 2013, 379(-): 39–53
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