Welcome to the School of Ocean and Earth Science, Tongji University

HUANG Xiangtong


   Xiangtong Huang    lecturer


Office Ocean   building 304


Email:   xiangtong@tongji.edu.cn


Mailing   AddressSchool of Ocean and Earth   Science, Tongji   University, 1239 Siping Road, Shanghai 200092, China


2003.9-2006.10Tongji Univ.Marine GeologyPh.D

2000.9-2003.6Jilin Univ.Marine GeologyM.Sc

1996.9-2000.6Jilin Univ.Petroleum and nature gas explorationB.Sc


2006.10-, Tongji University, lecturer

Research interests

Cosmogenic nuclides and its application in geosciences

Sediment source to sink processes from river to sea

Past climatic and environmental changes reconstruction by sediments

Detrital zircon U-Pb dating and LA-ICP-MS techniques



Aeolian record in the Aral Sea and its investigation on climatic and environmental changes since late Holocene, NFSC, 200,000 yuan


Detrital zircon U-Pb Chronology and heavy mineral in situ geochemistry in the Yangtze to East China Sea source to sink system. Natural Science Foundation of Shanghai, 200,000yuan.


[1]Huang, X., Oberh?nsli, H., von Suchodoletz, H., Prasad, S., Sorrel, P., Plessen, B., Mathis, M., Usubaliev, R., 2014. Hydrological changes in western Central Asia (Kyrgyzstan) during the Holocene as inferred from a palaeolimnological study in lake Son Kul. Quat. Sci. Rev. 103, 134–152. doi:10.1016/j.quascirev.2014.09.012

[2]Mathis, M., Sorrel, P., Klotz, S., Huang, X., Oberh?nsli, H., 2014. Regional vegetation patterns at lake Son Kul reveal Holocene climatic variability in central Tien Shan (Kyrgyzstan, Central Asia). Quat. Sci. Rev. 89, 169–185. doi:10.1016/j.quascirev.2014.01.023

[3]Qiang, M., Y. Liu, Y. Jin, L. Song, X. Huang, and F. Chen, 2014.Holocene record of eolian activity from Genggahai Lake, northeastern Qinghai-Tibetan Plateau, China. Geophys. Res. Lett., 41, 589-595. doi:10.1002/2013GL058806.

[4]He, M., Zheng, H., Huang, X., Jia, J., Li, L., 2013. Yangtze River sediments from source to sink traced with clay mineralogy. J. ASIAN EARTH Sci. 69, 60–69. doi:10.1016/j.jseaes.2012.10.001

[5]黄湘通,郑洪波, John Chappell,王平 . 长江流域河流沉积物宇宙成因核素10Be特征与侵蚀速率估算. 第四纪研究, 20134,671-683.

[6]Huang, X., Oberh?nsli, H., von Suchodoletz, H., Sorrel, P., 2011. Dust deposition in the Aral Sea: implications for changes in atmospheric circulation in central Asia during the past 2000 years. Quaternary Science Reviews 30, 3661-3674.

[7]黄湘通,郑洪波,杨守业等. 长江三角洲DY03孔沉积物元素地球化学及其物源示踪意义. 第四纪研究,2009292):299-307

[8]Prins, M.A., Zheng, H., Beets, K., Troelstra, S., Bacon, P., Kamerling, I., Wester, W., Konert, M., Huang, X., Ke, W., Vandenberghe, J., 2009. Dust supply from river floodplains: the case of the lower Huang He (Yellow River) recorded in a loess-palaeosol sequence from the Mangshan Plateau. J. Quat. Sci. 24, 75–84. doi:10.1002/jqs.1167

[9]黄湘通,郑洪波,杨守业等. 长江三角洲DY03孔磁性地层研究及其意义. 海洋地质与第四纪研究,2008,(6):87-93

[10]黄湘通, 郑洪波,John Chappell. 宇宙成因核素10Be,26Al:原理及其在地表过程中的应用. 亚搏在线登录入口学报(自然科学版),2005,(9) 1206-1212

[11]何梦颖,郑洪波,黄湘通,贾军涛,李玲, 2011.长江流域沉积物黏土矿物组合特征及物源指示意义. 沉积学报,153):544-551.

[12]Jia J., Zheng, H., Huang, X. et al., .Detrital zircon U-Pb ages of late Cenozoic Sediments from the Yangtze delta: Implication for the evolution of the Yangtze River. Chinese Science Bulletin, 2010, 15, 1520-1528

[13]Zheng, H., Huang, X., Ji, J., Liu, R., Zeng, Q. and Jiang, F. Ultra-high rates of loess sedimentation at Zhengzhou since Stage 7: Implication for the Yellow River running through the Sanmen Gorge. Geomorphology2007, 85(3-4):131-142

[14]Zheng, H., Huang, X., Butcher, K. Lithostratigraphy, petrography and facies analysis of the Late Cenozoic sediments in the foreland basin of the West Kunlun. Paleogeography, Paleoclimatology, Paleoecology, 2006, 41(1):61-78

[15]郑洪波, 黄湘通, 向芳, 朱利东. 宇宙成因核素10Be:估算长江流域侵蚀速率的新方法. 亚搏在线登录入口学报(自然科学版),2005,(9)1160-1165

[16]郑洪波, 黄湘通, 刘锐, 强小科. 晚中新世以来亚洲季风阶段性演化的海陆记录. 矿物岩石地球化学通报,2005,(2)103-109

[17]季军良, 郑洪波, 李盛华, 黄湘通. 山西平陆黄河阶地与古三门湖消亡、黄河贯通三门峡时代问题的探讨. 第四纪研究,2006,(4)665-672



 《Geological Integrated Practice (undergraduate course)

 《Modern Analytical techniques(postgraduate course)


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