欢迎访问同济大学海洋与地球科学学院!

预聘副教授

hwdang @ tongji.edu.cn

  • 教育背景

    2010.09-2015.03:同济大学,海洋地质专业,博士研究生
    2007.09-2010.03:同济大学,海洋地质专业,硕士研究生
    2003.09-2007.07:北京大学,地球化学专业,本科

  • 工作经历

    2021.04至今:同济大学,副教授
    2019.09-2021.04:同济大学,副研究员
    2017.06-2019.08:同济大学,助理研究员
    2016.01-2017.01:法国国家科学院气候与环境实验室博士后
    2015.06-2017.06:同济大学,博士后

  • 教学与科研成果

    研究兴趣

    1.热带印度-太平洋的上层海水结构和水文循环变化

    2.赤道西太平洋陆源物质的来源、搬运动力、生物地球化学循环

    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


    科研项目

    1.上新世以来热带西太平洋碳循环的长时间尺度演化(41606049),2016.1-2019.12,20万,国家自然科学基金青年基金项目,负责人;

    2.上新世以来热带西太平洋深部呼吸碳库的演化及其与大气pCO2冰期旋回的关联(91858106),2019.1-2022.12,70万,国家自然科学基金重大研究计划培育项目,参与人;

    3.晚第四纪印度-太平洋暖池区温跃层变化(2015M581658),2015.9-2017.9,5万,中国博士后科学基金会面上项目,负责人;

    4.晚第四纪冰期旋回中热带海气CO2交换格局的变化及其控制因素(41630965),2016.1-2020.12,300万,国家自然科学基金重点项目,参与人;

    5.亚洲大陆边缘的古海洋与古地理演化(GASI-GEOGE-04),2016.1-2020.12,300万,国家海洋局“全球变化与海气相互作用”专项,参与人。


    研究成果

    论文

    [1] Dang, H., Z. Jian, Y. Wang, M. Mohtadi, Y. Rosenthal, L. Ye, F. Bassinot, W. Kuhnt (2020). Pacific warm pool subsurface heat sequestration modulated Walker circulation and ENSO activity during the Holocene. Science Advances, 6 (42): doi: 10.1126/sciadv.abc0402.

    [2] S. Wan, Z. Jian, X. Gong, H. Dang, J. Wu, P. Qiao (2020). Deep water [CO32-] and circulation in the South China Sea over the last glacial cycle. Quaternary Science Reviews, 243, doi: 10.1016/j.quascirev.2020.106499.

    [3] Dang, H., J. Wu, Z. Xiong, P. Qiao, T. Li, Z. Jian (2020). Orbital and sea-level changes regulate the iron-associated sediment supplies from Papua New Guinea to the equatorial Pacific. Quaternary Science Reviews, 239, doi: 10.1016/j.quascirev.2020.106361.

    [4] Dang, H., N. Peng, X. Ma, S. Wan, Z. Jian (2020). Possible linkage between the long-eccentricity marine carbon cycle and the deep-Pacific circulation: Western equatorial Pacific benthic foraminifera evidences of the last 4 Ma. Marine Micropaleontology, 155, doi: 10.1016/j.marmicro.2019.101797.

    [5] Jian, Z., Y. Wang, H. Dang, D. W. Lea, Z. Liu, H. Jin, Y. Yin (2020). Half-precessional cycle of thermocline temperature in the western equatorial Pacific and its bihemispheric dynamics. Proceedings of the National Academy of Sciences, 117(13): 7044-7051.

    [6] Dang, H., N. Peng, Z. Jian (2020). A dataset of the Plio-Pleistocene at IODP Site U1489: benthic foraminifera stable carbon and oxygen isotopes, coarse fraction, and selected benthic foraminifera abundances. Data in Brief, 28, doi: 10.1016/j.dib.2019.105020.

    [7] Yi, L., Z. Jian, … H. Dang, … (2020). The potential of marine ferromanganese nodules from Eastern Pacific as recorders of Earth's magnetic field changes during the past 4.7 Myr: a geochronological study by magnetic scanning and authigenic 10Be/9Be dating. Journal of Geophysical Research: Solid Earth, doi: 10.1029/2019JB018639.

    [8] Zhang, P., J. Xu, A. Holbourn, … H. Dang, … (2020). Indo‐Pacific hydroclimate in response to changes of the Intertropical Convergence Zone: Discrepancy on precession and obliquity bands over the last 410 kyr. Journal of Geophysical Research: Atmospheres, doi: 10.1029/2019JD032125.

    [9] Ma, X., H. Yan, H. Fei, … H. Dang (2020). A high-resolution δ18O record of modern Tridacna gigas bivalve and its paleoenvironmental implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 554: doi: 10.1016/j.palaeo.2020.109800.

    [10] 张娜, 党皓文, 翦知湣. (2020). 中-晚更新世南海北部上层水体结构的轨道尺度变化: IODP U1501站浮游有孔虫氧碳稳定同位素记录. 第四纪研究 40(3): 605-615.

    [11] 党皓文, 马小林, 杨策, 金海燕, 翦知湣. (2019). 重建高分辨率深海环境变化:冷水竹节珊瑚无机地球化学方法. 地球科学进展 34(12): 1262-1272.

    [12] 党皓文, 汪品先 (2019). “深水珊瑚研究进展”专题序言. 地球科学进展 34(12): 1221.

    [13] Li, C., Z. Jian, G. Jia, H. Dang, J. Wang (2019). Nitrogen fixation changes regulated by upper‐water structure in the South China Sea during the last two glacial cycles. Global Biogeochemical Cycles, 33, doi: 10.1029/2019GB006262.

    [14] Wang, Y., Z. Jian, P. Zhao, K. Xu, H. Dang, … (2019). Precessional forced zonal triple-pole anomalies in the tropical Pacific annual cycle. Journal of Climate, 32: 7369-7402.

    [15] 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.

    [16] 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.

    [17] 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.

    [18] Rosenthal, Y., A. E. Holbourn, D. K. Kulhanek… H. Dang… (2018). Western Pacific Warm Pool. Proceedings of the International Ocean Discovery Program, 363: College Station, TX (International Ocean Discovery Program). https://doi.org/10.14379/iodp.proc.363.2018.

    [19] 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.

    [20] Fan, W., Z. Jian, Z. Chu, H. Dang, et al. (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.

    [21] 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.

    [22] 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.

    [23] 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.

    [24] Rosenthal, Y., A. E. Holbourn, D. K. Kulhanek… H. Dang… (2017). Expedition 363 Preliminary Report: Western Pacific Warm Pool. International Ocean Discovery Program. http://dx.doi.org/10.14379/iodp.pr.363.2017.

    [25] 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.

    [25] 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.

    [27] 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.

    [28] Wang Y., Z. Jian, P. Zhao, H. Dang, X. Dong, (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.

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

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

    [31] 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.

    [32] 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.

    [33] 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.

     

    专利

    [1] 实用新型专利(专利授权公告号CN 209156516),万向调节装置

    [2] 实用新型专利(专利授权公告号CN 209156114),可编组泥沙颗粒自动清洗装置

    [3] 实用新型专利(专利授权公告号CN 209156114),滑杆夹持装置

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