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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)