杨生超，中国科学院南京地质古生物研究所副研究员，主要从事地球化学与石油地质学研究，关注早古生代重大生物事件的环境背景、生物与环境之间的相互作用，以及含油气盆地烃源岩成因机理等领域。目前以第一或通讯作者身份在Earth and Planetary Science Letters、Earth-Science Reviews、Global and Planetary Change等国内外期刊上发表论文13篇。担任Science Advances、Communications Earth & Environment、Earth-Science Reviews、Marine and Petroleum Geology、Palaeogeography, Palaeoclimatology, Palaeoecology等学术期刊审稿人。
工作经历
2024.12-至今，中国科学院南京地质古生物研究所，副研究员
2021.01-2024.11，南京大学地球科学与工程学院，博士后
教育经历
2016.09-2020.12，南京大学地球科学与工程学院，地质学，理学博士
2013.09-2016.06，中国石油大学（华东）地球科学与技术学院，地质学，理学硕士
2009.09-2013.06，长江大学地球科学学院，地质学，理学学士
国家自然科学基金面上项目，2025.01-2028.12，主持
国家自然科学基金青年科学基金项目，2022.01-2024.12，主持
中国博士后科学基金第71批面上资助，2022.06-2024.11，主持
南京大学关键地球物质循环前沿科学中心“科技人才团队”培育项目，2022.05-2022.12，主持
南京大学优秀博士研究生创新能力提升计划A类项目，2019.07-2020.06，主持
国家自然科学基金重大研究计划集成项目，2023.01-2026.12，参与
代表论著：
Yang, S.C.*, Fan, J.X.*, 2025. Decreased marine organic carbon burial during the Hirnantian glaciation. Earth and Planetary Science Letters, 654, 119240. https://doi.org/10.1016/j.epsl.2025.119240
Yang, S.C., Hu, W.X.*, Wang, X.L., Jiang, B.Y., Yao, S.P., Sun, F.N., Huang, Z.C., Zhu, F., 2019. Duration, evolution, and implications of volcanic activity across the Ordovician–Silurian transition in the Lower Yangtze region, South China. Earth and Planetary Science Letters, 518, 13–25. https://doi.org/10.1016/j.epsl.2019.04.020
Yang, S.C., Fan, J.X.*, Algeo, T.J., Shields, G.A., Zhou, Y., Li, C.*, Chen, J.T., Li, W.Q., Li, N., Cao, J., Zhang, L.N., Sun, Z.Y., Shen, S.Z., 2024. Steep oceanic DIC δ13C depth gradient during the Hirnantian Glaciation. Earth-Science Reviews, 255, 104840. https://doi.org/10.1016/j.earscirev.2024.104840
Yang, S.C., Hu, W.X.*, Fan, J.X., Deng, Y.Y., 2022. New geochemical identification fingerprints of volcanism during the Ordovician-Silurian transition and its implications for biological and environmental evolution. Earth-Science Reviews, 228, 104016. https://doi.org/10.1016/j.earscirev.2022.104016
Yang, S.C., Hu, W.X.*, Wang, X.L., Fan, J.X., 2021. Nitrogen isotope evidence for a redox-stratified ocean and eustatic fall driven environmental evolution during the Ordovician–Silurian transition. Global and Planetary Change, 207, 103682. https://doi.org/10.1016/j.gloplacha.2021.103682
Yang, S.C., Hu, W.X.*, Wang, X.L., 2021. Evidences, mechanism and implications of widespread upwelling during the Late Ordovician to early Silurian in the Yangtze region, South China. Chemical Geology, 565, 120074. https://doi.org/10.1016/j.chemgeo.2021.120074
Yang, S.C., Hu, W.X.*, Yao, S.P., Wang, X.L., He, W.H., Wang, Y., Zhu, F., Sun, F.N., 2020. Constraints on the accumulation of organic matter in Upper Ordovician-Lower Silurian black shales from the Lower Yangtze region, South China. Marine and Petroleum Geology, 120, 104544. https://doi.org/10.1016/j.marpetgeo.2020.104544
Yang, S.C., Fan, J.X.*, Rasmussen, C.M.Ø., Wang, X-L., Sun, Z.Y., Deng, Y.Y., 2024. Globally synchronous meteorite rain during the Middle Ordovician. Palaeogeography, Palaeoclimatology, Palaeoecology, 655, 112550. https://doi.org/10.1016/j.palaeo.2024.112550
Deng, Y.Y.1, Fan, J.X.*, Yang, S.C.1 (共同一作), Shi, Y.K., Lu, Z.B., Xu, H.Q., Sun, Z.Y., Zhao, F.Q., Hou, Z.S., 2023. No Furongian Biodiversity Gap: Evidence from South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 618, 111492. https://doi.org/10.1016/j.palaeo.2023.111492
Qiu, L.W.*, Yang, S.C.* (共同通讯), Qu, C.S., Xu, N.N., Gao, Q.S., Zhang, X.J., Liu, X.G., Wang, D.H., 2017. A Comprehensive Porosity Prediction Model for the Upper Paleozoic Tight Sandstone Reservoir in the Daniudi Gas Field, Ordos Basin. Journal of Earth Science, 28, 1086–1096. https://doi.org/10.1007/s12583-016-0935-2
杨生超, 邱隆伟*, 刘魁元, 韩霄, 姜嘉诚, 单宝杰, 刘连启. 渤海湾盆地济阳坳陷邵家洼陷沙四段湖相碳酸盐岩储层特征与分类评价[J]. 天然气地球科学, 2016, 27(4): 628–638.
杨生超, 邱隆伟*, 刘魁元, 徐宁宁, 杨勇强, 韩霄, 姜嘉诚. 邵家洼陷沙四段湖相碳酸盐岩岩性测井解释模型[J]. 新疆石油地质, 2015, 12(6): 708–713.
连丽霞, 王剑, 马聪, 杨召, 罗正江, 杨生超*, 张文杰, 胡文瑄. 准噶尔盆地西北缘沸石发育特征及成储机理初探—以玛南地区二叠系乌尔禾组为例[J]. 高校地质学报, 2021, 27(1): 102–110.