李超
基本信息Personal Information
教授 博士生导师 硕士生导师
主要任职 : 教授
学术荣誉 : 新世纪优秀人才 , 国家杰出青年基金获得者 , 万人计划领军人才
曾获荣誉 : 2014年获中国矿物岩石地球化学学会“侯德封奖”;2016年荣获国务院政府特殊津贴专家称号;2018获教育部高等学校科学研究优秀成果奖-自然科学一等奖(排名第3)。
性别 : 男
毕业院校 : 中国科学院广州地球化学研究所
学历 : 博士研究生
学位 : 博士
在职信息 : 在职
所在单位 : 生物地质与环境地质国家重点实验室
入职时间 : 2011年04月01日
学科 : 地球化学 地质学
办公地点 : 中国地质大学(武汉)未来城校区生环国重大楼
联系方式 : 电话:027-67883606 电子邮件:chaoli@cug.edu.cn or ucrchaoli@gmail.com
Email :
扫描关注
- [1]Matthew S. Dodd.Development of carbonate-1 associated phosphate (CAP) as a proxy for reconstructing ancient ocean phosphate levels.Geochimica et Cosmochimica Acta.2021,301 :48-69
- [2]Na Li.Redox changes in the outer Yangtze Sea (South China) through the Hirnantian Glaciation and their implications for the end-Ordovician biocrisis.Earth-Science Reviews.2020,212 (DOI: 10.1016/j.earscirev.2020.103443)
- [3]Chao Li.The redox structure of Ediacaran and early Cambrian oceans and its controls.Science Bulletin.2020,65 (24):2141-2149
- [4]Biao Chang.Massive formation of early diagenetic dolomite in the Ediacaran ocean: Constraints on the “dolomite problem.”.Proceedings of the National Academy of Sciences of USA.2020,117 (25):14005-14014
- [5]Meng Cheng.Evidence for high organic carbon export to the early Cambrian seafloor.Geochimica et Cosmochimica Acta.2020,287 :125-140
- [6]Haiyang Wang.Spatiotemporal redox heterogeneity and transient marine shelf oxygenation in the Mesoproterozoic ocean.Geochimica et Cosmochimica Acta.2020,270 :201-217
- [7]Wei Shi.Sulfur isotope evidence for transient marine-shelf oxidation during the Ediacaran Shuram Excursion.Geology.2018,46 (3):267-270
- [8]Chao Li.Heterogeneous and dynamic marine shelf oxygenation and coupled early animal evolution.Emerging Topics in Life Sciences.2018,2 (2):279-288
- [9]Chao Li.Coupled oceanic oxygenation and metazoan diversification during the early–middle Cambrian?.Geology.2017,45 :743-746
- [10]Meng Cheng.Transient deep-water oxygenation in the early Cambrian Nanhua Basin.Geochimica et Cosmochimica Acta.2017,210 :42-58
- [11]Chao Li.Uncovering the spatial heterogeneity of Ediacaran carbon cycling.Geobiology.2017,15 :211-224
- [12]Meng Cheng.Marine Mo biogeochemistry in the context of dynamically euxinic mid-depth waters: A case study of the lower Cambrian Niutitang shales, South China.Geochimica et Cosmochimica Acta.2016,183 (79-93)
- [13]Chengsheng Jin.A highly redox-heterogeneous ocean in South China during the early Cambrian (~529-514 Ma): Implications for biota-environment co-evolution.Earth and Planetary Science Letters.2016,441 :38-51
- [14]Chao Li.Marine redox conditions in the middle Proterozoic ocean and isotopic constraints on authigenic carbonate formation: Insights from the Chuanlinggou Formation, Yanshan Basin, North China.Geochimica et Cosmochimica Acta.2015,150 :90-105
- [15]Chao Li.A theoretical prediction of chemical zonation in early oceans (>520 Ma).Science China Earth Sciences.2015,58 (12):2123-2133
- [16]Chao Li.Evidence for a redox stratified Cryogenian marine basin, Datangpo Formation, South China.Earth and Planetary Science Letters.2012,331 :246-256
- [17]Chao Li.A stratified redox model for the Ediacaran ocean.Science.2010,328 :80-83
- [18]Chao Li.Hydrogen-isotopic variability in lipids from Santa Barbara Basin sediments.Geochimica et Cosmochimica Acta.2009,73 :4803-4823
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