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

Dang Haowen


Haowen Dang  Associate Researcher

Office Ocean   building 413


Email:   hwdang@tongji.edu.cn


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


2010.09-2015.03Tongji UniversityMarine GeologyPh.D

2007.09-2010.03Tongji UniversityMarine GeologyM.Sc

2003.09-2007.07Peking UniversityGeochemistryB.Sc


2019.09-2022.09Tongji UniversityAssociate Research Professor

2017.06-2019.08Tongji UniversityAssistant Research Professor

2016.01-2017.01LSCE, CNRS, France, Postdoctor

2015.06-2017.06Tongji UniversityPostdoctor

Research interests



3. 太平洋深部环流和碳储库的长尺度演化

4. 冷水珊瑚的生态系特征和古环境再造

1. Upper-ocean structural and hydro-climatic changes of the tropical Indo-Pacific

2. Provenance, transportation, and bio-geochemistry of the terrigenous matters in the West Equatorial Pacific

3. Long-term evolution of the circulation and carbon reservoir of the Pacific deep waters

4. Ecologic systems and paleoceanography reconstruction of Cold Water Corals


1. Long-term evolution of the tropical western Pacific carbon cycle in the Plio-Pleistocene (41606049)2016.1-2019.12200 kYoung Scholars Fund from the National Natural Science Foundation of ChinaPrincipal Investigator;

2. Evolution of the deep respiratory carbon reservoir of the tropical western Pacific and its linkage to the glacial-cycle of atmospheric pCO2 in the Plio-Pleistocene (91858106)2019.1-2022.12700 kCultivation Project of the Major Research Plan from the National Natural Science Foundation of ChinaParticipating Investigator

3. Late Quaternary thermocline change in the Indo-Pacific Warm Pool (2015M581658)2015.9-2017.950 kGeneral Project, National Science Foundation for Post-doctoral ScientistsPrincipal Investigator

4. Changes and dominant factors of the tropical sea-air CO2 exchange during the Late Quaternary glacial cycle (41630965)2016.1-2020.123 MState Key Program of the National Natural Science Foundation of ChinaParticipating Investigator

5. Paleoceanographic and Paleogeographic evolution of the Asian continental margin (GASI-GEOGE-04)2016.1-2020.123 MSpecial Project of “Global Change and Sea-Air Interaction” from the State Ocean AdministrationParticipating Investigator



[1] Dang, H., Z. Jian, T. Wang, P. Qiao, and F. Bassinot (2019). The B/Ca and Cd/Ca of a subsurface-dwelling foraminifera Pulleniatina obliquiloculata in tropical Indo-Pacific: implications for the sub-surface carbonate chemistry estimation. Acta Oceanologica Sinica, 38: 138-150.

[2] Dang, H., Z. Jian, J. Wu, F. Bassinot, T. Wang, C. Kissel (2018). The calcification depth and Mg/Ca thermometry of Pulleniatina obliquiloculata in the tropical Indo-Pacific: A core-top study. Marine Micropaleontology, 145: 28-40.

[3] Dang, H., Z. Jian, C. Kissel, and F. Bassinot (2015), Precessional changes in the western equatorial Pacific hydroclimate: A 240 kyr marine record from the Halmahera Sea, East Indonesia, Geochemistry Geophysics Geosystems, 16, doi: 10.1002/2014GC005550.

[4] Dang, H., Z. Jian, F. Bassinot, P. Qiao, and X. Cheng (2012), Decoupled Holocene variability in surface and thermocline watertemperatures of the Indo-Pacific Warm Pool, Geophysical Research Letters, 39, doi:10.1029/2011GL050154.

[5] Li, C., Z. Jian, G. Jia, H. Dang, J. Wang (2019). Nitrogen fixation changes regulated by upperwater structure in the South China Sea during the last two glacial cycles. Global Biogeochemical Cycles, doi: 10.1029/2019GB006262.

[6] Wang, Y., Z. Jian, P. Zhao, K. Xu, H. Dang, Z. Liu, D. Xiao, J. Chen (2019). Precessional forced zonal triple-pole anomalies in the tropical Pacific annual cycle. Journal of Climate, doi: 10.1175/JCLI-D-1118-0668.1171.

[7] Fan, W., Z. Jian, Z. Chu, H. Dang, Y. Wang, F. Bassinot, X. Han, Y. Bian (2018). Variability of the Indonesian Throughflow in the Makassar Strait over the Last 30 ka. Scientific Reports, 8, DOI:10.1038/s41598-41018-24055-41591.

[8] Wan, S., Z. Jian, H. Dang (2018). Deep Hydrography of the South China Sea and Deep Water Circulation in the Pacific Since the Last Glacial Maximum. Geochemistry Geophysics Geosystems, doi: 10.1029/2017GC007377.

[9] Wang, X., Z. Jian, A. Lückge, Y. Wang, H. Dang, M. Mohtadi (2018). Precession-paced thermocline water temperature changes in response to upwelling conditions off southern Sumatra over the past 300,000 years. Quaternary Science Reviews, 192: 123-134.

[10] Wang, T., A. C. Ravelo, H. Ren, H. Dang, H. Jin, J. Liu, Z. Jian (2018). Nitrogen Isotope Variations in the Northern South China Sea Since Marine Isotopic Stage 3: Reconstructed From Foraminifera-Bound and Bulk Sedimentary Nitrogen. Paleoceanography and Paleoclimatology, 33: 594-605.

[11] Wang, P., Q. Li, J. Tian, J. He, Z. Jian, W. Ma, H. Dang (2016). Monsoon influence on planktic d18O records from the South China Sea, Quaternary Science Reviews, 142, 26-39, doi: 10.1016/j.quascirev.2016.04.009.

[12] Wang Y., Jian Z., Zhao P., Dang H., Dong X., 2013. Solar forced transient evolution of Pacific upper water thermal structure during the Holocene in an earth system model of intermediate complexity, Chinese Science Bulletin, 58: doi: 10.1007/s11434-11012-15576-11432.

[13] 殷雅倩, 党皓文, 王跃, 乔培军, 翦知湣 (2019). 末次冰消期西太平洋暖池上层海水温度的千-百年尺度变化. 科学通报, 64(20): 2151-2162.

[14] 王海粟, 党皓文, 翦知湣 (2019). 中更新世转型时期南海北部上层水体结构演化特征——ODP1146站浮游有孔虫稳定同位素记录. 第四纪研究, 39(2): 316-327.

[15] 翦知湣, 党皓文 (2017). 解读过去、预告未来: IODP气候与海洋变化钻探研究进展与展望. 地球科学进展, 32(12): 1267-1276.

[16] 翦知湣, 金海燕, 万随, 党皓文 (2013), 古大洋环流重建方法, : 丁仲礼, 固体地球科学研究方法, pp. 66-81, 科学出版社, 北京.

[17] 党皓文, 翦知湣, F. Bassinot (2009). 西菲律宾海末次冰期以来的浊流沉积及其古环境意义. 第四纪研究, 29: 1078 - 1085.

[18] 党皓文, 刘建波, 袁鑫鹏 (2009). 湖北兴山中寒武统覃家庙群微生物岩及其古环境意义. 北京大学学报 (自然科学版), 45: 289-298.

[19] 袁鑫鹏, 袁金良, 刘建波, 党皓文 (2009). 湖北兴山寒武系覃家庙群底部三叶虫化石的地层学意义. 地层学杂志, 33: 48-55.


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