Email: jiangsiliu@hhu.edu.cn
2015.09–2019.06, 博士, 中国地质大学（武汉）, 地球生物学
2009.09–2013.06, 学士, 中国地质大学（武汉）, 地质学（基地班）
工作经历：
2025.01-至今, 河海大学海洋学院, 讲师
2022.01- 2024.12, 中国科学院广州地球化学研究所, 博士后
2019.08 - 2021.12, 厦门大学海洋与地球学院, 博士后
古海洋碳-氮-硫生物地球化学循环
本科：地学通用软件与大数据
2023.01-2025.12, 国家自然科学基金(青年C), 右江盆地泥盆纪-石炭纪之交海洋氮循环的变化及其氮素来源重建, 主持
2023.09-2024.12, 博士后面上基金, 火山作用对早白垩世热河生物群演化的影响——来自湖相沉积物中陆地生态系统重建的证据, 主持，已结题
2019.09-2021.09, 博士后面上基金, 白垩纪-古近纪之交古海洋水化学条件变化, 主持，已结题
2021.01-2024.12, 国家自然科学基金重大研究计划, 西北太平洋真光层氮循环关键过程及其对氧化亚氮海气通量的贡献, 参与
Liu, J., Luo, G., Algeo, T.J., Qie, W., Yao, L., Huang, J., Xie, S., 2024. Marine sulfate sulfur isotopic evidence for enhanced terrestrial weathering and expansion of oceanic anoxia during the Devonian-Carboniferous transition. Global and Planetary Change 239, 104494
Liu, J., Algeo, T.J., 2020. Beyond redox: control of trace-metal enrichment in anoxic marine facies by watermass chemistry and sedimentation rate. Geochimica et Cosmochimica Acta, 287, 296-317.
Liu J., Luo, G., Lu Z., Lu, W., Qie, W., Zhang, F., Wang X., Xie, S., 2019. Intensified ocean deoxygenation during the end Devonian mass extinction, Geochemistry, Geophysical, Geosystems, 20, 6187– 6198.
Liu, J., Algeo, T.J., Jaminski, J., Kuhn, T., Joachimski, M.M., 2019. Evaluation of high-frequency paleoenvironmental variation using an optimized cyclostratigraphic framework: Example for C-S-Fe analysis of Devonian-Mississippian black shales (Central Appalachian Basin, USA). Chemical Geology 525, 303-320.
Liu, J., Algeo, T.J., Qie, W., Saltzman, M.R., 2019. Intensified oceanic circulation during Early Carboniferous cooling events: Evidence from carbon and nitrogen isotopes. Palaeogeography, Palaeoclimatology, Palaeoecology, 531, 108962.
Liu, J., Algeo, T.J., Yang, H., Pan, J., Tang, C., Huang, J., Xie, S., 2018. Changes in vegetation type on the Chinese Loess Plateau since 75 ka related to East Asian Summer Monsoon variation. Palaeogeography, Palaeoclimatology, Palaeoecology, 510: 124-139.
Liu, J., Qie, W., Algeo, T.J., Yao, L., Huang, J., Luo, G., 2016. Changes in marine nitrogen fixation and denitrification rates during the end-Devonian mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology, 448: 195-206.
Shen, J., Feng, Q., Algeo, T.J., Liu, J., Zhou, C., Wei, W., Liu, J., Them, T.R., Gill, B.C., Chen, J., 2020. Sedimentary host phases of mercury (Hg) and implications for use of Hg as a volcanic proxy. Earth and Planetary Science Letters 543, 116333.
Zhang, F., Dahl, T.W., Lenton, T.M., Luo, G., Shen, S.-z., Algeo, T.J., Planavsky, N., Liu, J., Cui, Y., Qie, W., Romaniello, S.J., Anbar, A.D., 2020. Extensive marine anoxia associated with the Late Devonian Hangenberg Crisis. Earth and Planetary Science Letters 533, 115976.
Algeo, T.J., Liu, J., 2020. A re-assessment of elemental proxies for paleoredox analysis. Chemical Geology 540, 119549.
Lu, J., Algeo, T.J., Zhuang, G., Yang, J., Xiao, G., Liu, J., Huang, J., Xie, S., 2020. The Early Pliocene global expansion of C4 grasslands: A new organic carbon-isotopic dataset from the north China plain. Palaeogeography, Palaeoclimatology, Palaeoecology 538, 109454.
Luo, G., Algeo, T.J., Zhan, R., Yan, D., Huang, J., Liu, J., Xie, S., 2016. Perturbation of the marine nitrogen cycle during the Late Ordovician glaciation and mass extinction. Palaeogeography, Palaeoclimatology, Palaeoecology, 448: 339-348.
Qie, W., Liu, J., Chen, J., Wang, X., Mii, H.-s., Zhang, X., Huang, X., Yao, L., Algeo, T.J., Luo, G., 2015. Local overprints on the global carbonate δ13C signal in Devonian–Carboniferous boundary successions of South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 418: 290-303.
Yao, L., Qie, W., Luo, G., Liu, J., Algeo, T.J., Bai, X., Yang, B., Wang, X., 2015. The TICE event: Perturbation of carbon–nitrogen cycles during the mid-Tournaisian (Early Carboniferous) greenhouse–icehouse transition. Chemical Geology, 401: 1-14.
Chen, B., Chen, J., Qie, W., Huang, P., He, T., Joachimski, M.M., Regelous, M., Pogge von Strandmann, P.A.E., Liu, J., Wang, X., Montañez, I.P., Algeo, T.J., 2021. Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants? Earth and Planetary Science Letters 565, 116953.
