同位素地球化学、有机地球化学

  2012至2013大一年度国家励志奖学金（福建省教育厅）

  2012至2013大一上学年校二等综合奖学金

  2013至2014大一下学年校三等综合奖学金

  2012至2013大一下学年三好学生，优秀学生干部、校社会工作突出贡献奖

  2013至2014大二学年校社会工作突出贡献奖两次

  2014至2015大三上、下学年校三等综合奖学金两次

  2017至2018研一学年中国科学院西北生态环境资源研究院优秀学生干部

  2017至2018研一学年中国科学院大学“三好学生”

  2019年09月第二届全国气体同位素技术与地球科学应用大会“优秀志愿者”

  2019年12月第十七届有机地球化学会议优秀青年论文展板报告奖（5/200）

  2020至2021博二学年，获得中国科学院大学“三好学生”

  2023至2024年度，中国科学院西北生态环境资源研究院，优秀工作者

 2025至2026年度，中国科学院西北生态环境资源研究院，优秀工作者

1. Ma, X.Y., Wei, Z.F., Wang, T.L., Wang, G., Zhang, T., Zhang, X.M., Guo, Z.G., Liang, K.K., Li, S.K., Chen, J.Z., Wang, Y.L., Fan, Q.H., 2026. Prehistoric anthropogenic heavy metal pollution and its correlations with climate evolution on the NE Tibetan Plateau. Geoscience Frontiers, https://doi.org/10.1016/j.gsf.2026.102287. (中科院1区Top, IF: 8.9).

2. Ma, X.Y., Wei, Z.F., Wang, G., Zhang, T., Zhang, P.Y., Liang, K.K., Guo, Z.G., Li, S.K., Zhang, X.M., Chen, J.Z., Li, Z.L., He, W., Wang, Y.L., 2025. Lake level variability on the Northeastern Tibetan Plateau linked to interaction between Westerlies and Asian monsoon since the last deglaciation, Catena, 250. (中科院1区Top, IF: 5.7).

3. Ma, X.Y., Wei, Z.F., Wang, Y.L., Wang, G., Zhang, T., He, W., Yu, X.L., Ma, H., Zhang, P.Y., Li, S.K., Fan, Q.H., 2023a. Links between geochemical weathering on the NE Tibetan Plateau and global climate change since the Last Deglacial. Catena, 224, 106971, (中科院1区Top, IF: 5.7).

4. Ma, X.Y., Wei, Z.F., Wang, Y.L., Wang, G., Zhang, T., Ma, H., He, W., Yu, X.L., Zhang, P.Y., 2023b. Temperature and climatic seasonality affecting C3 vs C4 plants since the Last Deglacial on the northeastern Tibetan Plateau. Geochemistry Geophysics Geosystems, doi: 10.1029/2022GC010847, (中科院2区, IF: 3.0).

5. Ma, X.Y., Wei, Z.F., Wang, Y.L., Wang, G., Zhang, T., He, W., Yu, X.L., Ma, H., Zhang, P.Y., Li, S.K., Wei, J.Y., Fan, Q.H., 2021. Reconstruction of climate changes based δ18Ocarb on northeastern Tibetan Plateau: a 16.1-cal kyr BP record from Hurleg Lake. Front. Earth Sci. doi: 10.3389/feart.2021.745972, (Q2, IF：2.9).

6. Ma, X.Y., Wei, Z.F., Wang,Y.L., Wang, G., Zhang, T., Ma, H., He, W., Yu, X.L., Li, S.K., Fan, Q.H., 2021. Speculation for quantifying increased C4 plants under future climate conditions: Inner Mongolia, China case study. Quaternary International, 592, 97-110, (Q2, IF: 2.130).

7. Ma, X.Y., Wei, Z.F., Wang, YL., 2020. Reconstructing of C3/C4 Vegetation Evolution and Climate Variety Since the Last Glacial Maximum in the Northeast Tibetan Plateau. Goldschmidt2020. (会议摘要).

8. 马雪云, 魏志福, 王永莉,等. 末次冰盛期以来东北地区霍拉盆地湖泊沉积物记录的C3/C4植被演化[J]. 第四纪研究, 2018, 038(005):1193-1202.(影响因子：2.55).

9. Li, S., Ma, X., Jiang, S., Wang, G., Zhang, T., He, W., ... & Wei, Z., 2022. Long-term drying trend during 51.8–37.5 Ma in the Nangqian Basin, central-eastern Qinghai–Tibet Plateau. Front. Earth Sci. 10, 866304. (Q2, IF：2.9).

10. Yu, X., Wang, G., Zhang, T., Ma, X*., Zhang, X., Li, L., ... & Zhou, S., 2023. Chemical weathering intensity as a reliable indicator for southwest summer monsoon reconstruction: Evidence from clay minerals of Qionghai Lake sediments since the Last Glacial Maximum. Geochemistry Geophysics Geosystems, 24(7), e2023GC010900, (中科院2区, IF: 3.0).

11. Wang, G., Wang, Y.L., Wei, ZF., He, W., Ma, X.Y., Zhang, T., 2021. Reconstruction of temperature and precipitation spanning the past 28kyr based on branched tetraether lipids from Qionghai Lake, southwestern China. Palaeogeography, Palaeoclimatology, Palaeoecology,  doi:10.1016/j.palaeo.2020. 110094, (Q1, IF: 3).

12. Wang, G., Wang, Y.L., Wei, ZF., He, W., Zhang, T., Ma, X.Y., Yu, X.L., 2021. Distribution of n-alkan-2-ones in Qionghai Lake sediments, southwest China, and its potential for late Quaternary paleoclimate reconstruction. Journal of Quaternary Science. doi: 10.1002/jqs.3271, (Q1, IF: 2.3).

13. Ma, H., Wang, Y.L., Jin, C.S., Wei, Z.F., Wang, G., Zhang, T., He, W., Ma, X.Y., 2021. Relative paleointensity correction of radiocarbon reservoir effect for lacustrine sediments on the northeast Tibetan Plateau. Quaternary Geochronology, doi:10.1016/j.quageo.2021.101193, (Q1, IF: 2.7).