本人隶属于大陆边缘沉积学团队，依托同济大学海洋地质全国重点实验室开展相关科学研究，目前该实验室拥有齐全的矿物学、岩石学和地球化学分析仪器，包括：XRD分析仪、蔡司偏光显微镜、场发射扫描电镜和电子探针（JEOL JXA-8230）、多接收等离子体质谱仪（Neptune Plus）、无机元素分析仪器（ICP-OES、ICP-MS、XRF、XRF Core Scanner）、气体同位素比质谱仪（MAT252、MAT253、IRMS）。

1.镁-钾同位素耦合示踪长江口-东海反风化过程与镁循环，2024.01-2027.12，54万，国家自然科学基金面上项目，主持，在研；

2. 用岛礁白云岩Mg同位素制约新近纪以来海洋镁-钙循环，2022.1-2024.12，30万，国家自然科学青年基金，主持，结题；

3. 新近系岛礁白云岩镁同位素组成对海洋Mg/Ca变化的指示，2021.10-2022.12，8万，中国博士后基金面上项目二等资助，主持，结题；

4. 晚新生代亚洲大陆风化过程、沉积记录及碳汇效应，2023.01-2027.12，国家重点研发项目，参与，在研；

5. 长江口-东海陆架-冲绳海槽断面的反风化作用与关键元素循环，2023.01-2027.12，国家自然科学基金重点项目，参与，在研.

1.镁-钾同位素耦合示踪长江口-东海反风化过程与镁循环，2024.01-2027.12，54万，国家自然科学基金面上项目，主持，在研；

2. 用岛礁白云岩Mg同位素制约新近纪以来海洋镁-钙循环，2022.1-2024.12，30万，国家自然科学青年基金，主持，结题；

3. 新近系岛礁白云岩镁同位素组成对海洋Mg/Ca变化的指示，2021.10-2022.12，8万，中国博士后基金面上项目二等资助，主持，结题；

4. 晚新生代亚洲大陆风化过程、沉积记录及碳汇效应，2023.01-2027.12，国家重点研发项目，参与，在研；

5. 长江口-东海陆架-冲绳海槽断面的反风化作用与关键元素循环，2023.01-2027.12，国家自然科学基金重点项目，参与，在研.

[1] Hu, Z*., Weynell, M., Su, N., Hohl, S.V., Han, Z., Wen, Y., Yang, S*., 2025. Evidence from Mg isotopes indicating reverse weathering as a significant Mg sink in Tibetan Plateau lakes. Quaternary Science Reviews 349, 109138.

[2] Hu, Z*., Li, W., Hohl, S.V., Meister, P., Yang, S., Zhang, B., Xia, Z., Liu, C., 2024b. Evaporite sequences as archives for Mg isotope compositions of seawater - Evidence from a Tethys marginal shelf basin in the Anisian. Chemical Geology 668, 122346.

[3] Hu, Z*., Han, Z., Ma, A., Xia, Z., Wang, L., Li, W., 2024a. The covariation between Mg-C isotopes and trace elements in dolostones: Implications for reconstructing the seawater chemistry. Sedimentary Geology 459, 106552.

[4] Hu, Z., Hohl, S.V*., Viehmann, S., Meister, P., Tepe, N., 2023a. No biological effect on magnesium isotope fractionation during stromatolite growth. Geochimica et Cosmochimica Acta 358, 1-11.

[5] Hu, Z*., Yang, S*., Yang, C., Guo, Y., Xu, J., Zhang, C., 2023b. Mg isotopes of siliciclastic sediments on continental marginal sea: Insights for the potential to trace silicate weathering. Global and Planetary Change 231, 104307.

[6] Hu, Z., Shi, Z., Li, G., Xia, Z., Yi, L., Liu, C., Li, W*., 2022. The Cenozoic Seawater Conundrum: New constraints from Mg isotopes in island dolostones. Earth and Planetary Science Letters 595, 117755.

[7] Hu, Z., Bialik, O.M*., Hohl, S.V., Xia, Z., Waldmann, N.D., Liu, C., Li, W*., 2021a. Response of Mg isotopes to dolomitization during fluctuations in sea level: Constraints on the hydrological conditions of massive dolomitization systems. Sedimentary Geology 420, 105922.

[8] Hu, Z*., Hu, W*., Liao, Z., Sun, F., 2021b. Facies-dependent early diagenesis and hydrothermal reworking in dolostones: a case study on upper Permian and lower Triassic in northeast Sichuan Basin. Carbonates and Evaporites 36.

[9] Hu, Z., Li, W*., Zhang, H*., Krainer, K., Zheng, Q.-F., Xia, Z., Hu, W., Shen, S.-Z., 2021c. Mg isotope evidence for restriction events within the Paleotethys ocean around the Permian-Triassic transition. Earth and Planetary Science Letters 556, 116704.

[10] Hu, Z., Hu, W*., Liu, C., Sun, F., Liu, Y., Li, W*., 2019. Conservative behavior of Mg isotopes in massive dolostones: From diagenesis to hydrothermal reworking. Sedimentary Geology 381, 65-75.

[11]Hu, Z., Hu, W*., Wang, X., Lu, Y., Wang, L., Liao, Z., Li, W*., 2017. Resetting of Mg isotopes between calcite and dolomite during burial metamorphism: Outlook of Mg isotopes as geothermometer and seawater proxy. Geochimica et Cosmochimica Acta 208, 24-40.