Name:Tingjiang Peng
Title: Associate Professor  Master advisor 
Gender:male
Graduate College:Lanzhou University
Education:
Academic degree:PhD
On-the-job information:Incumbency
Unit:
Initiation time:
Office location:
Mail box:pengtj@lzu.edu.cn
Learning Experience
2007-2012: PhD, Physical Geography, Lanzhou University 2003-2007: B.A., Geography Science, Lanzhou University
Research Direction
Molecular Paleoclimatology, Cenozoic Environmental Evolution
Work Experience
2013- 2019: Lecturer, Key laboratory of west China’s Environmental System (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University 2019- present: Associate Professor, Key laboratory of west China’s Environmental System (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University
Courses
1. Graduate Class: The Principles, Methods of Geochemistry and its Environmental Applications
Publications
First Author and Corresponding Author* [1] Guo B H, Peng T J*, Yu H, Hui Z C*, Ma Z H, Li X M, Feng Z T, Liu J, Liu S P, Zhang J, Ye X Y, Song C H, Li J J, 2020. Magnetostratigraphy and palaeoclimatic significance of the Late Pliocene red clay-Quaternary loess sequence in the Lanzhou Basin, western Chinese Loess Plateau. Geophysical Research Letters, 47, e2019GL086556. [2] Li X M, Peng T J*, Ma Z H, Li M, Feng Z T, Guo B H, Yu H, Ye X Y, Zhang J, Song C H, Li J J, 2020. Sources and transport wind evolution of eolian sediments on XSZ planation surface in the NE Tibetan Plateau since 6.7 Ma. Geochemistry, Geophysics, Geosystems, in press. [3] Ma Z H, Li X M, Peng T J*, Zhang J*, Dou L F, Yu H, Liu J, Ye X Y, Feng Z T, Li M, Guo B H, Song C H, Zhao Z J, Li J J, 2020. Landscape evolution of the Dabanshan planation surface: implications for uplift of the eastern tip of the Qilian Mountains since the Late Miocene. Geomorphology, https://doi.org/10.1016/j.geomorph.2020.107091. [4] Ma Z H, Feng Z T, Peng T J*, Liu S P, Li M, Guo B H, Li X M, Song C H, Zhao Z J, Li J J, 2020. Quaternary drainage evolution of the Datong River, Qilian Mountains, northeastern Tibetan Plateau, China. Geomorphology, 353: 107021. [5] Ma Z H, Peng T J*, Feng Z T, Li M, Li X M, Guo B H, Li J J, Song C H, 2019. Asymmetrical river valleys and their tectonic significance in the Maxianshan area, NE Tibetan Plateau. Geomorphology, 329: 70-80. [6] Guo B H, Peng T J*, Feng Z T, Li X M, Li M, Ma Z H, Li J J, Song C H, Zhang J, Hui Z C, Zhang S D, 2019. The pedogenic component of loess deposits of the Lanzhou Basin and its paleoclimatic implications over the past 2.2 Ma. Journal of Asian Earth Sciences, 170: 128-137. [7] Li, J J, Ma Z H, Li X M, Peng T J*, Guo B H, Zhang J, Song C H, Liu J J, Hui Z C, Yu H, Ye X Y, Liu S P, Wang X X, 2017. Late Miocene-Pliocene geomorphological evolution of the Xiaoshuizi peneplain in the Maxian Mountains and its tectonic significance for NE Tibetan Plateau. Geomorphology, 295: 393-405. [8] Peng T J*, Li J J, Song C H, Guo B H, Zhao Z J, Zhang J, Liu J, 2016. An integrated biomarker perspective on Neogene-Quaternary climatic evolution in NE Tibetan Plateau: Implications for the permanent aridification. Quaternary International, 399: 174-182. [9] Peng T J, Li J J, Zhao Z J*, Song C H, Zhang J, 2013. Biomarkers aid paleoenvironment studies of Asian aridification. Eos, Transactions American Geophysical Union, 94:173-174. [10] Peng T J, Li J J*, Song C H, Zhao Z J, Zhang J, Hui Z C, King J W, 2012. Biomarkers challenge early Miocene loess and inferred Asian desertification. Geophysical Research Letters, 39, L06702, doi:10.1029/2012GL050934. (AGU Research Spotlight) [11] Yu H, Peng T J*, Li M, Yu F X, Ye X Y, Guo B H, Zhang J, Li J J, 2018. Magnetic susceptibility enhancement model and its driving mechanism of Lanzhou loess on the Western Loess Plateau. Marine Geology & Quaternary Geology. 38: 165-174. (in Chinese with English abstract) [12] Ye X Y, Feng Z T, Peng T J*, Yu F X, Li M, Yu H, 2018. Preliminary clay minerals on the loess-paleosol sequence in the Xijin core, Lanzhou. Journal of Lanzhou University: Natural Sciences, 54: 75-81. (in Chinese with English abstract)