1992年生,江西峡江人。
2024.12--至今 中国科学院南京地质古生物研究所 助理研究员
2021.09--2024.11 中国科学院青藏高原研究所 特别研究助理(博士后)
2018.09--2021.06 中国科学院青藏高原研究所 自然地理学博士学位
2015.09--2018.06 中国科学院青藏高原研究所 自然地理学硕士学位
2011.09--2015.06 湖南师范大学 地理科学学士学位
长期从事新生代孢粉与古气候研究,研究兴趣涉及东亚早新生代气候环境演变、亚洲季风干旱环境演化及古新世-始新世极热事件等。
[1] 中国科学院朱李月华优秀博士生奖(2021年)
[2] 博士研究生国家奖学金(2020年)
[3] 中国科学院大学三好学生(2020年)
[4] 中国科学院大学三好学生(2018年)
[1] 中国博士后科学基金面上项目,江汉盆地深钻记录的古新世—始新世极热事件期间的植被与气候变化,2023.1-2025.12,主持
[2] 国家自然科学基金委面上项目,青藏高原尼玛盆地孢粉记录的早新生代生态环境演变及古高度,2020.1-2023.12,参与
[3] 第二次青藏高原科学考察项目之专题7《高原风化剥蚀历史及气候环境效应》,2019.1-2024.10,参与
[4] 中国科学院战略性先导专项A《季风区古地理重建与古环境演化》,2018.3-2023.3,参与
[5] 国家自然科学基金委重点国际合作项目《青藏高原南北晚新生代古气候记录对比与印度季风-内陆干旱耦合系统的演化》,2017.1-2021.12,参与
[1] Xie,Y.L., Wu, F.L*.,Wang,H.T,Jiang,Y.X,Yang,L.Y,2024. Onset of aridification in mid-latitude Asia at 41 Ma linked to the proto-Paratethys Sea retreat. Gondwana Research,131,196-207.
[2] Xie,Y.L., Wu, F.L*., Jiang, Y.X.,Yang,L.Y.,2024. Stepwise hydroclimate changes in Northeast China linked to proto-Paratethys Sea retreats and global cooling during the Eocene. Palaeogeography,Palaeoclimatology,Palaeoecology, 648,1-10.
[3] Xie, Y.L., Wu, F.L*., Ning, W.X., Jiang, Y.X., 2024. Orbitally-forced meridional shifts of the westerlies modulated the hydroclimate of Northeast China during the late Eocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 633, 1-12.
[4] Xie, Y.L., Wu, F.L*., Fang, X.M., 2022. A transient south subtropical forest ecosystem in central China driven by rapid global warming during the Paleocene-Eocene Thermal Maximum. Gondwana Research, 101:192-202.
[5] Xie, Y.L., Wu, F.L*., Fang, X.M*., 2022. Abrupt collapse of a swamp ecosystem in northeast China during the Paleocene–Eocene Thermal Maximum. Palaeogeography, Palaeoclimatology, Palaeoecology, 595, 1-12.
[6] Xie, Y.L., Wu, F.L*., Fang, X.M*., Song, J., Niu, Z., 2022. Late Eocene onset of the East Asian Monsoon in the Qingjiang Basin of Central Jiangxi Province (Southeast China) revealed by a major vegetation transition from desert to forest. Palaeogeography, Palaeoclimatology, Palaeoecology, 602, 1-13.
[7] Xie, Y.L., Wu, F.L*., Fang, X.M*., Zhang, D.W., Zhang, W.L., 2020. Early Eocene South China dominated by desert: Evidence from a palynological record of the Hengyang Basin, Hunan Province. Global and Planetary Change, 195: 1-10.
[8] Xie, Y.L., Wu, F.L*., Fang, X.M*., 2020. A major environmental shift by the middle Eocene in southern China: Evidence from palynological records. Review of Palaeobotany and Palynology, 278:1-16.
[9] Xie, Y.L., Wu, F.L*., Fang, X.M*., 2019. Middle Eocene East Asian monsoon prevalence over southern China: Evidence from palynological records. Global and Planetary Change, 175: 13-26.
[10] 谢宇龙, 吴福莉, 方小敏. 云南新生代孢粉组合与气候环境演变. 2019. 海洋地质与第四纪地质, 39(2): 164-176.
[11] 谢宇龙,章新平*,姚天次,黄煌. 长沙近地面水汽中稳定同位素的监测与分析. 2016. 环境科学, 37(2): 475-481.
[12] Wu, F.L., Tang, F.J., Gao, S.J., Xie, Y.L., Jiang, Y.X., Fang, X.M., Wang, H.T., 2024. Northward expansion of Cenozoic Asian humid climate recorded by sporopollen. Palaeogeography, Palaeoclimatology, Palaeoecology, 637, 1-9.a
[13] Khatri, D.B., Zhang, W.L*, Fang, X.M, Meng, Q.Q, Zhang, D.W, Zhang, T., Yan, M.D, Xie, Y.L., Paudayal, K. N., 2024. Magnetostratigraphy of the Late Cretaceous to Early Eocene sediments from the Tulsipur section, western Nepal: Tectonic implications for the Indian northern passive margin. Palaeogeography, Palaeoclimatology, Palaeoecology, 647, 1-19.