国家自然科学基金（42276069）:南海北部绿素氮同位素研究及古海洋学意义, 2023-1-1至2026-12-31

国家自然科学基金（41876042）:晚渐新世-中中新世东亚低纬区降水演化历史及其全球影响, 2019-1-1至2022-12-31

国家自然科学基金（41673042） :南海沉积物中支链四醚膜脂的组成和碳同位素特征及其对古气候研究的启示，2017-1-1至2020-12-31

近3年研究成果：

Yu, J., Li, L.*,Zhang, X., He, J., Jia, G., Kuhnt, W., Mangrove sediment erosion in the SundaShelf during meltwater pulses: Insights from biomarker records, OrganicGeochemistry, 2023, 175, 104542. doi:https://doi.org/10.1016/j.orggeochem.2022.104542

Udoh E. C., Li L.*,Chen M.Y., Dan S.F., Chen L.D., Zhang J.Y., Jia G.D., He J.*, Distributioncharacteristics of terrestrial and marine lipid biomarkers in surface sedimentand their implication for the provenance and palaeoceanographic application inthe northern South China Sea. Marine Geology, 2022, 452, 106899https://doi.org/10.1016/j.margeo.2022.106899

梁栋, 李丽*, 贺娟, 贾国东. 运用生物标志物重建古盐度的研究进展[J]. 地球化学,  2022, 51(03)，316-332. doi:10.19700/j.0379-1726.2020.04.008

杨迎雪, 李丽*, 郁金勇, 贺娟, 贾国东. 有机脂类分子重建海洋古温度研究进展. 海洋地质与第四纪地质, 2022, 42(6): 131-149.

Umoh U.U., Li L*., He J., Chen L.D., Dong L., Jia G.D., Lahajnar N.,Massoth G., Schwarz-Schampera U., Unusual aliphatic hydrocarbon profiles athydrothermal vent fields of the Central and Southeast Indian Ridges andMid-Indian Basin. Deep–Sea Research II, 2021, 194, 104996, https://doi.org/10.1016/j.dsr2.2021.104996.

郁金勇, 李丽*, 贺娟, 贾国东, 巽他陆架末次冰期植被之谜, 海洋地质与第四纪地质, 2021, 41,129-141.


朱艳宸, 李丽*, 王鹏, 贺娟, 贾国东, 海洋氮循环中稳定氮同位素变化与地质记录研究进展. 地球科学进展, 2020, 35,167-179.

Liu Zh., Li L*., He J., Chen L.D., Wang J.J, Jia G.D., Operational laboratorymethods for GDGTs groups separation. Journal of Ocean University of China, 2020,19, 1073-1080, https://doi.org/10.1007/s11802-020-4339-y.

Dong L., Zhang X., Jia G., Du Y., Li L., Li Q. CO2‐induceddecoupling of tropical surface and thermocline water temperature at the onsetof interglacials. Geophysical Research Letters, 2020, 47, e2020GL088805. https://doi.org/10.1029/2020GL088805.

Umoh U.U., Li L.*, Luckge A.,Schwartz-Schampera U., Naafs B.D.A., Influence of hydrothermal vent activity onGDGT pool in marine sediments might be less than previously thought. OrganicGeochemistry 2020, 149, 104102 doi: https://doi.org/10.1016/j.orggeochem.2020.104102.