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李楠楠 博士
厦门大学海洋与地球学院(希平楼) C3-114 |
Nannan Li, PhD
Xiping Building C3-322, College of Ocean and Earth Sciences, State Key Laboratory of Marine Environmental Science, Xiamen University, Xiang'an District, Xiamen 361102, Fujian, P.R. China |
Tel:18744047941
Email:linannan@xmu.edu.cn
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个人履历
Brief CV |
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2020.09— ，厦门大学海洋与地球学院，近海海洋环境科学国家重点实验室博士后 （合作导师：余凤玲博士 胡建宇教授） |
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2015.09—2020.06, 东北师范大学地理科学学院，自然地理学，博士研究生 （指导教师：介冬梅 教授）
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2018.10—2019.09, 欧洲地球科学与环境科学教学与研究中心(CEREGE, France)，联合培养博士研究生 |
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2018.04—2018.06, 瑞士联邦水科技研究所(Eawag)和苏黎世联邦理工学院(ETH Zürich)，中国科协资助优秀青年交流，联合培养博士研究生 |
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2010.09—2014.06, 东北师范大学地理科学学院，地理科学 |
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2020.09— ，Postdoctoral Fellow, College of Ocean and Earth Sciences and State Key Laboratory of Marine Environmental Science |
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2015.09—2020.06, PhD in Physical Geography, School of Geographical Sciences, Northeast Normal University |
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2018.10—2019.09, Visiting PhD student, Centre de Recherche et d'Enseignement de Géosciences de l'Environnement (CEREGE), Aix-en-Provence, France |
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2018.04—2018.06, Visiting PhD student, Swiss Federal Institute of Aquatic Science and Technology (eawag), Swiss Federal Institute of Technology Zurich (ETH Zürich), Switzerland |
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2010.09—2014.06, Bachelor, School of Geographical Sciences, Northeast Normal University |
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研究方向
Research Interests |
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东亚季风区全新世气候演化的时空特征及外部驱动 |
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晚第四纪植被演替对气候变化的响应 |
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植硅体三氧同位素地球化学及其古气候意义 |
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My research interests focus on the processes of Holocene environmental change and the role of past climate shifts in shaping the composition and distribution of terrestrial vegetation, using various geological archives. My research covers the fields of palaeoclimatology, palaeoecology, geochemistry, geography, and Quaternary geology. Combining these disciplines, I am trying to develop an improved understanding of the interactions between vegetation dynamics and global change, in the past, present and future. |
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There are currently three main themes that I am working on. (a) Spatio-temporal character of Holocene climate change and its external forcing in the East Asian monsoon area; (b) Response of vegetation dynamics to past climate change in East Asia since the Late Quaternary; (c) Triple oxygen isotopes of phytolith and its paleoclimate significance. |
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代表性论文
Selected Publications |
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Li, N., Li, M., Sack, D., Kang, W., Song, L., Yang, Y., Zong, Y. and Jie, D, 2020. Diatom evidence for mid-Holocene peatland water-table variations and their possible link to solar forcing. Science of the Total Environment, 725, 138272. |
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Li, N., Xie, M., Sack, D., Dubois, N., Yang, X., Gao, G., Li, D., Liu, L., Liu, H. and Jie, D, 2020. Continuous aridification since the mid-Holocene as the main cause of C3/C4 dynamics in the grasslands of northeastern China. European Journal of Soil Science, doi: 10.1111/ejss.12960. |
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Li, N., Sack, D., Sun, J., Liu, S., Liu, B., Wang, J., Gao, G., Li, D., Song, Z. and Jie, D., 2020. Quantifying the carbon content of aeolian sediments: Which method should we use? CATENA, 185, 104276. |
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Li, N., Sack, D., Gao, G., Liu, L., Li, D., Yang, X., Jie, D., Liu, H., Shi, J. and Leng, C., 2018. Holocene Artemisia-Chenopodiaceae-dominated grassland in North China: Real or imaginary? The Holocene, 28, 834–841. |
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Li, N., Chambers, F.M., Yang, J., Jie, D., Liu, L., Liu, H., Gao, G., Gao, Z., Li, D., Shi, J., Feng, Y., and Qiao, Z., 2017. Records of East Asian monsoon activities in Northeastern China since 15.6 ka, based on grain size analysis of peaty sediments in the Changbai Mountains. Quaternary International, 447, 158–169. |
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For further information, please visit my Researchgate at https://www.researchgate.net/profile/Li_Nannan. |
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