主要研究方向：

金属稳定同位素示踪大陆风化状态、古海洋环境演变与低温成矿过程

简历：

2024.08至今 中国科学院地球化学研究所  助理研究员

2021.07-2023.07 中国科学院广州地化所  地质学博士后

2018.09-2021.07 中国科学院广州地化所  地球化学专业博士

2013.08-2018.07 乌江能源集团贵州天然气能投公司  项目经理

2010.09-2013.07 中国石油大学（北京）   矿产普查与勘探专业硕士

2006.09-2010.07 长江大学  资源勘查工程专业学士,石油地质学方向

承担科研项目情况：

1、国家自然科学青年基金，热液活动对上扬子下寒武统页岩氮元素富集与赋存的影响，2023/01-2025/12，主持

2、中国科学院地球化学研究所青年创新人才项目，2025/01-2028/12，主持

3、国家重点研发计划项目，晚奥陶—早志留世全球大规模有机质堆积对地球宜居性的影响，2023/12-2028/11，子课题负责人

代表论著：

1、Wu,Y.,Tian,H.,Yin,R.,Chen,D.,Grasby,S.E.,Shen,J.,Li,T.,Ji,S.,Peng,P.A.,2022. Highly fractionated Hg isotopes evidence for dynamic euxinia in shallow waters of the Mesoproterozoic ocean. Earth and Planetary Science Letters 616. 118211.

2、Wu,Y.,Tian,H.,Liu,Z.,Liu,S.,Li,T.,Ji,S.,Peng,P.A.,2022. Interpretation of abnormally negative carbon isotope excursions in Eifelian–Givetian (Middle Devonian) sediments of South China and implications for paleo-environmental variation. Palaeogeography,Palaeoclimatology,Palaeoecology 604,111225.

3、Wu,Y.,Yin,R.,Li,C.,Chen,D.,Grasby,S.E.,Li,T.,Ji,S.,Tian,H.,Peng,P. A.,2022. Global Hg cycle over Ediacaran–Cambrian transition and its implications for environmental and biological evolution. Earth and Planetary Science Letters 587,117551.

4、Wu,Y.,Tian,H.,Jia,W.,Li,J.,Li,T.,Zhou,Q.,Xie,L.,Peng,P. A.,2022. Nitrogen isotopes evidence for stratified ocean redox structure during the late Ediacaran to Cambrian Stage 3 in the Yangtze Block of South China. Chemical Geology 589,120679.

5、Wu,Y.,Tian,H.,Li,J.,Li,T.,Ji,S.,2021. Reconstruction of oceanic redox structures during the Ediacaran-Cambrian transition in the Yangtze Block of South China: Implications from Mo isotopes and trace elements. Precambrian Research 359,106181.

6、Wu,Y.,Tian,H.,Li,T.,Ji,S.,Liu,Z.,Xiao,X.,Xie,L.,2021. Enhanced terrestrial organic matter burial in the marine shales of Yangtze platform during the early Carboniferous interglacial interval. Marine and Petroleum Geology 129,105064.

7、Wu,Y.,Tian,H.,Gong,D.,Li,T.,Zhou,Q.,2020. Paleo-environmental variation and its control on organic matter enrichment of black shales from shallow shelf to slope regions on the Upper Yangtze Platform during Cambrian Stage 3. Palaeogeography,Palaeoclimatology,Palaeoecology 545,109653.