范育新,教授、博士生导师,教育部新世纪优秀人才,中国海洋学会海底科学分会委员、中国地理学会地理测年技术分会委员、全国释光与电子自选共振测年学术讨论会学术委员会委员、中国第四纪研究会终身会员。
围绕我国西部干旱-半干旱地区沉积环境演变的历史与机制的关键科学问题,在阿拉善高原及周边地区系统开展了沙漠-湖泊环境演化、第四纪沉积物源区识别及源区演变、荒漠化历史与机制、晚第四纪高湖面的年代等研究;通过低温热年代学手段研究了金川及东昆仑等地区关键金属矿床的隆升剥露历史及机制。主持或参与包括国家自然科学基金面上项目、国家自然科学基金重点、基础研究发展计划、创新群体在内的20余个科研项目;国家自然科学基金通讯评议人、科技部国际科技合作专项会评专家、全国第四-五轮学科评估通讯评议人、教育部学位与研究生教育发展中心通讯评议人、留学基金委通讯评审专家;QSR等多个重要学术期刊审稿人;获第十届甘肃青年地质科技奖、甘肃省科技进步二等奖、中国地理学会学术年会青年优秀论文奖、兰州大学大学生创新创业行动计划“优秀指导教师”称号,曾享受甘肃省高层次专业技术人才津贴。2023年11月入职南京师范大学海洋科学与工程学院。
学术专长:物源示踪(U-Pb)、年代学(OSL、ESR、U-Th/He)
Email: yxfan@njnu.edu.cn
通讯地址:南京市栖霞区学林路2号南京师范大学海洋科学与工程学院,210023
学习经历
2004/09-2008/12,兰州大学资源环境学院地理系,博士,论文题目为“‘吉兰泰-河套’古大湖演化(侧重光释光测年)研究”,导师为陈发虎院士、赵晖研究员和Charles Oviatt教授
1998/09-2001/06,兰州大学资源环境学院地质系,硕士,论文题目为“北山地区镁铁-超镁铁岩构造环境与含矿性分析”,导师为汤中立院士
1994/09-1998/06,兰州大学资源环境学院地质系,学士
工作经历:
2023.11-今, 南京师范大学海洋科学与工程学院,教授
2015.05-2023.10,兰州大学地质科学与矿产资源学院,博士生导师
2013.05-2023.10,兰州大学地质科学与矿产资源学院,教授
2001.07-2013.05,兰州大学,教师
近期主要在研项目:
[1] 国家自然科学基金面上项目, 阿拉善高原东部第四纪碎屑沉积物源区时空变化及其驱动机制研究(42371157), 2024/01-2027/12,46万(直接经费),主持;
[2] 国家自然科学“战略性关键金属超常富集成矿动力学”重大研究计划”重点支持项目, 中国西部典型岩浆铂族元素和钴金属超常富集成矿动力学(91962212),2020/01-2023/12,311万(直接经费),本人承担低温年代学部分(60万),项目组成员,3/10。
[3] 第三次新疆综合科学考察项目(编号: 2021xjkk0302),塔里木河流域干旱与风沙灾害调查和风险评估专题,2021/11-2024/10,987万,项目组成员。
已完成/参与完成的主要科研项目
[4] 国家自然科学基金面上项目, 腾格里地区晚更新世晚期以来沙漠化的时空变化及机制研究(41772169),2018/01-2021/12,80万(直接经费),已结题,主持;
[5] 国家自然科学基金面上项目,腾格里沙漠覆盖区晚第四纪大湖期的多手段测年及高湖面成因研究(41371033),2014/01-2017/12,90万,已结题,主持;
[6] 国家自然科学基金面上项目,吉兰泰地区晚更新世大湖期存在的沉积地层及测年(41172163),2012/01-2015/12,74万,已结题,主持;
[7] 教育部新世纪优秀人才支持计划,干旱区环境变化与光释光年代学(NCET-12-0251),2013-2015,50万,已结题,主持;
[8] 国家自然科学基金青年基金项目,晚第四纪吉兰泰湖面波动与环境变化研究(40502016),2006/01-2008/12,28万,已结题,主持;
[9] 国家自然科学基金面上项目,乌兰布和沙漠演化历史及形成机制研究(40972116),2011/01-2013/12,46万,本人承担23万,已结题,项目组主要成员;
[10] 国家重点基础研究发展计划(973计划)项目,“末次盛冰期以来我国气候环境变化及干旱-半干旱区人类的影响与适应”之“西风区气候环境变化的特征与机制”(2010CB950202),2010/6-2014/12,753万,已结题,项目组成员;
[11] 国家自然科学基金面上项目,阿拉善高原-黄土高原全新世重大干旱事件(侧重于释光年代)研究(40401061),2005/01-2007/12,已结题,项目组成员;
[12] 国家自然科学基金西部计划重点项目,中国西部干旱区全新世气候变化的集成研究(90502008),2006/01-2009/12,已结题,项目组成员;
代表性成果 (*通讯作者):
[1] Sun X., Wang F., Fan Y.(共一), Li Z.J., Liu X., Zhao J., Li B.F., Xia D.S., 2023. Transformation of lakebed into a major soluble-salt-bearing dust source for Asia since the mid-pleistocene, Global and Planetary Change (2023), https://doi.org/10.1016/j.gloplacha.2023.104282.
[2] Cai Q.S., Fan Y.X.*, Yan X.Y., Wang Y., Gao M.M., Yang G.L., Zhang M.J., Zhang H.F., 2023. Paleozoic rapid denudation of the Proterozoic Jinchuan Ni-Cu-PGE sulfide deposit, NW China: insights from single-grain zircon (U-Th)/He thermochronology. Journal of Asian Earth Sciences 225. https://doi.org/10.1016/j.jseaes.2023.105762.
[3] Fan Y.X.*, Li Z.J., Cai Q.S., Yang G.L., Zhang Q.S., Zhao H., Chen F.H., Maghsoudi M., 2022. Dating of the late Quaternary high lake levels in the Jilantai area, northwestern China, using optical luminescence of quartz and K-feldspar. Journal of Asian Earth Sciences, 224, 105024, https://doi.org/10.1016/j.jseaes.2021.105024.
[4] Yang G.L., Fan Y.X.*, Cai Q.S., Wang F., Zhang Q.S., Yan X.Y., Gao M.M., Chen F.H., 2022. Provenance of Quaternary aeolian silts in western China and its spatial difference and its spatial difference with source of the Yellow River. Quaternary Science Reviews,196,https://doi.org/10.1016/j.quascirev.2022.107785.
[5] Niu Y.N., Fan Y.X.*, Qiao Y.S., Lü T.Y., Li C.Z., Qi L., Wang S, Peng S.S., Tan Y.L., 2022. Chronostratigraphy of a loess-paleosol sequence in the western Chinese Loess Plateau based on ESR dating and magnetostratigraphy. Quaternary International, https://doi.org/10.1016/j.quaint.2022.08.005.
[6] Fan Y.X.*, Wang F., Yang G.L., Cai Q.S., Zhang Q.S., Li Z.J., Long X., Li X.H., Chen F.H., 2021. Decoupling of the detrital linkage between proximal dunefields and early and middle Pleistocene accumulation in the Chinese Loess Plateau: evidence from the Badain Jaran and Tengger sandy deserts. Quaternary Science Reviews, 264, 107026, https://doi.org/10.1016/j.quascirev.2021.107026.
[7] Li Z.J., Mou X.S., Fan Y.X.*, Zhang Q.S., Yang G.L., Zhao H., 2020. Establishing a common standardized growth curve for single aliquot OSL dating of quartz from sediments in the Jilantai area of North China. Geochronometria 47(1), 71-92. DOI: 10.2478/geochr-2020-0017.
[8] Fan Y.X.*, Li Z.J., Yang G.L., Yi S.W., Zhang Q.S., Liu W.H., Mou X.S., 2020. Sedimentary evidence and luminescence and ESR dating of Early Pleistocene high lake levels of Megalake Tengger, northwestern China. Journal of Quaternary Science 35(8): 994–1006. DOI: 10.1002/jqs.3246.
[9] Fan Y.X.*, Li Z.J., Wang F., Ma J., Mou X.S., Li X.H., Zhang Q.S., Zhao H., and Chen F.H., 2019. Provenance variations of the Tengger Desert since 2.35 Ma and its linkage with the Northern Tibetan Plateau: evidence from U-Pb age spectra of detrital zircons. Quaternary Science Reviews, doi: 10.1016/j.quascirev.2019.105916.
[10] Fan Y.X.*, Mou X.S., Wang Y.D., Liu C.Y., Zhao H., Wang F., Li Z.J., Mao X., Liu W.H., Ma J., Liu C.R., Zhang F., Zhang F., 2018. Quaternary paleoenvironmental evolution of the Tengger Desert and its implications for the provenance of the loess of the Chinese Loess Plateau. Quaternary Science Reviews, 197: 21–34, https://doi.org/10.1016/j.quascirev.2018.08.002.
[11] Fan Y.X.*, Wang Y.D., Mou X.S., Zhao H., Zhang F., Zhang F., Liu W.H., Hui Z.C., Huang X.Z., Ma J., 2017. Environmental status of the Jilantai Basin, North China, on the northwestern margin of the modern Asian summer monsoon domain during Marine Isotope Stage 3. Journal of Asian Earth Sciences, 147(2017): 178–192.
[12] Fan Y.X.*, Zhang F., Zhang F., Liu W.H., Chen X.L., Fan T.L., Wang Y.D., Chen F.H., Lai Z.P., 2016. History and mechanisms for the expansion of the Badain Jaran Desert, northern China since 20 ka: Geological and luminescence chronological evidence. The Holocene 26(4): 532–548.
[13] Fan Y.X.*, Chen X.L., Liu W.H., Zhang F., Zhang F., 2015. Formation of present desert landscape surrounding Salt Lake Jilantai in northern China based on OSL dating. Frontiers of Earth Sciences, 9(3): 497–508.
[14] Fan Y.X.*, Chen X.L., Fan T.L., Jin M., Liu J.B., Chen F.H., 2013. Sedimentary and OSL dating evidence for the development of the present Hobq desert landscape, northern China. Science China: Earth Sciences, 56(12): 2037–2044.
[15] Fan T.L., Fan Y.X.*, Zhao H., Chen F.H., Lai Z.P., 2013. Investigations on the degree of bleaching of quartz OSL signals using modern aeolian dust from western Loess Plateau, China. Geochronometria 40(3): 165–176.
[16] Fan Y.X.*, Chen F.H., Wei G.X., Madsen D.B., Oviatt C., Zhao H., Chun X., Yang L.P., Fan T.L., Li G.Q., 2010. Potential water sources for Late Quaternary Megalake Jilantai-Hetao, China, inferred from mollusk shell 87Sr/ 86Sr ratios. Journal of Paleolimnology 43(3), 577–587.
[17] Fan Y.X.*, Chen F.H., Fan T.L., Zhao H., Yang L.P, 2010. Sedimentary and Optically Stimulated Luminescence (OSL) dating for formation of the present northern Ulan Buh Desert landform in northern China. Science China Earth Sciences 53 (11): 1675–1682.
[18] Fan Y.X., Zhao H.*, Chen F.H., 2010. The equivalent dose of different grain size quartz fractions from lakeshore sediments in the arid region of north China. Quaternary Geochronology 5(2): 205–211.