邮箱： hudp08@mail.ustc.edu.cn

科研领域： 综合应用稳定同位素(d13C、d15N、d18O-D17O、d34S-D33S-D36S、d202Hg-D199Hg-D200Hg、d238U、d98Mo等)以及元素地球化学，探究地史时期环境气候变化及其对生命演化的影响




个人简介
中国科学技术大学，地球和空间科学学院，特任副研究员。
2012年6月本科毕业于兰州大学，同年9月直博进入中国科学技术大学，研究方向为环境生物地球化学，于2017年12月获博士学位。
近几年以第一作者及合作者身份在Nature communications, PNAS, Geology等国际一流期刊发表多篇学术论文。



教育经历
2012-9至2017-12, 中国科学技术大学, 博士
2008-9至2012-6, 兰州大学, 学士



科研与学术工作经历
2020-2至现在, 中国科学技术大学, 地球和空间科学学院, 特任副研究员
2017-12至2020-2, 中国科学技术大学, 博士后
2019-9至2020-1, 美国亚利桑那州立大学, 地球和空间探索学院, 访问****
2018-8至2019-1, 美国加州大学圣地亚哥分校, 化学与生物化学系, 访问****
2017-8至2017-10, 台湾中央研究院, 环境变迁研究中心, 访问****
2015-5至2015-11, 美国马里兰大学, 地质系, 访问****




发表学术论文
Li, M., Grasby, S.E., Wang, S.-J., Zhang, X., Wasylenki, L.E., Xu, Y., Sun, M., Beauchamp, B., Hu, D., Shen, Y., 2021. Nickel isotopes link Siberian Traps aerosol particles to the end-Permian mass extinction. Nature Communications 12: 2024.
Hu, D., Li, M., Chen, J., Luo, Q., Grasby, S. E., Zhang, T., Yuan, S., Xu, Y., Finney, S. C., Sun, L., Shen, Y., 2021. Major volcanic eruptions linked to the Late Ordovician mass extinction: Evidence from mercury enrichment and Hg isotopes. Global and Planetary Change 196, 103374.
Hu, D.,Li, M., Zhang, X., Turchyn, A. V., Gong, Y., Shen, Y., 2020. Large mass-independent sulphur isotope anomalies link stratospheric volcanism to the Late Ordovician mass extinction. Nature Communications 11, 2297.
Chen, K., Hu, D., Zhang, X., Zhu, H., Sun, L., Li, M., Shen, Y., 2020. Minor Δ³³S anomalies coincide with biotic turnover events during the Great Ordovician Biodiversification Event (GOBE) in South China. Global and Planetary Change 184, 103069.
Zhang, X., Zhou, X., Hu, D., 2020. High-resolution paired carbon isotopic records from the Meishucun section in South China: Implications for carbon cycling and environmental changes during the Ediacaran-Cambrian transition. Precambrian Research 337, 105561.
Li,D., Zhang,X., Hu,D.,Li,D.,Zhang,G., Zhang,X., Ling,H.,Xu,Y., Shen,Y., 2019. Multiple S-isotopic constraints on paleo-redox and sulfate concentrationsacross the Neoproterozoic-Cambrian transition in South China. Precambrian Research,105500.
Li,D., Zhang,X., Hu, D.,Chen,X., Huang,W., Zhang,X., Li,M., Qin,L., Peng,S., Shen,Y., 2018. Evidence ofa large δ¹³C_carb and δ¹³C_org depth gradientfor deep-water anoxia during the late Cambrian SPICE event. Geology 46, 631-634.
Zhang, X., Gao, Y., Chen, X., Hu, D., Li, M., Wang, C., Shen, Y., 2018. Nitrogen isotopic composition of sediments from the eastern Tethys during Oceanic Anoxic Event 2. Palaeogeography, Palaeoclimatology, Palaeoecology 515, 123-133.
Hu, D., Zhang, X., Zhou, L., Finney, S. C., Liu, Y., Shen, D., Shen, M., Huang, W., Shen, Y., 2017. ⁸⁷Sr/⁸⁶Sr evidence from the epeiric Martin Ridge Basin for enhanced carbonate weathering during the Hirnantian. Scientific Reports 7, 11348 .
Zhang, G., Zhang, X., Hu, D., Li, D., Algeo, T. J., Farquhar, J., Henderson, C. M., Qin, L., Shen, M., Shen, D., Schoepfer, S. D., Chen, K., Shen, Y., 2017. Redox chemistry changes in the Panthalassic Ocean linked to the end-Permian mass extinction and delayed Early Triassic biotic recovery. Proceedings of the National Academy of Sciences of the United States of America 114, 1806-1810.
Zhang, X., Chen, K., Hu, D., Sha, J., 2016. Mid-Cretaceous carbon cycle perturbations and Oceanic Anoxic Events recorded in southern Tibet. Scientific Reports 6, 39643.