个人简历

工作经历
2011-今东华理工大学副教授
2018.8-2019.8 澳大利亚国立大学访问学者（合作老师：Andrew P. Roberts）
2013.3-2014.3 美国辛辛那提大学访问学者（合作老师：Thomas J. Algeo）
教育
2008-2011 中国科学院地质与地球物理研究所博士
2005-2008 中国石油大学（北京）硕士
2001-2005 东北石油大学本科

研究领域

1）二叠纪瓜德鲁普世古海洋缺氧事件、全球碳循环及其与生物灭绝事件的成因关系；2）黑色岩系中钙质结核的成因；3）黑色岩系有机质富集成因机理

近期论文

1. Hengye Wei*, Zhanwen Tang, Detian Yan, Maquzong Bai, 2019.Formation of large carbonate concretions in black cherts in the Gufeng Formation (Guadalupian) at Enshi, South China. Geobiology. doi:10.1111/gbi.12362.
2. Hengye Wei*, Xingchao Jiang, 2019. Early Cretaceous ferruginous and its control on the lacustrine organic matter accumulation: Constrained by multiple proxies from the Bayingebi Formation in the Bayingebi Basin, inner Mongolia, NW China. Journal of Petroleum Science and Engineering. 178, 162-179.
3. 许涛，唐瞻文，张璇，耿梓傲，汪建国，韦恒叶*. 2019. 中二叠世茅口组热液交代硅质岩：贵州桑树湾剖面角砾硅质岩元素及硅同位素证据. 石油学报. （接收待刊）
4. 耿梓傲，韦恒叶*. 2019. 下扬子巢湖地区中二叠统孤峰组富有机质硅质岩有机地球化学特征. 高校地质学报. （接收待刊）
5. 唐瞻文，韦恒叶*. 2019. 巢湖地区二叠系瓜德鲁普统孤峰组古环境演化. 现代地质. （接收待刊）
6. 白玛曲宗，韦恒叶，江增光，邱振，2018. 江西东岭剖面P-T界线碳同位素变化与沉积物输入的关系。沉积学报，36（2）：267-279.
7. Caineng Zou, Zhen Qiu*, Hengye Wei*, Dazhong Dong, Bin Lu, 2018. Euxinia caused the Late Ordovician extinction: Evidence from pyrite morphology and pyritic sulfur isotopic composition in the Yangtze area, South China. Palaeogeography, Palaeoclimatology, Palaeoecology. 511：1-11.
8. Hengye Wei*, Quzong Baima, Zhen Qiu*, Chaocheng Dai, 2018. Carbon isotope perturbations and faunal changeovers during the Guadalupian mass extinction in the middle Yangtze Platform, South China. Geological Magazine,155(8): 1667-1683.
9. 白玛曲宗，韦恒叶，韦雪梅，江增光，张璇，耿梓傲，2017. 恩施剖面G-L界线自生石膏与钠长石成因. 东华理工大学学报（自然科学版），40（4）：212-218.
10. 韦雪梅，韦恒叶*，邱振，江增光，白玛曲宗，2017. 广西来宾蓬莱滩剖面G-L界线草莓状黄铁矿微晶粒径特征及其氧化还原意义. 地质科学，52（1）：230-241.
11. 江增光，韦恒叶*，邱振，于永善，2017. 恩施剖面栖霞组下部贫氧—缺氧环境成因模式. 地质科学，52（1）：218-229.
12. 韦雪梅，江增光，白玛曲宗，韦恒叶，2016. 广西来宾蓬莱滩剖面瓜德鲁普统—乐平统（G-L）界线生境型及其意义.东华理工大学学报（自然科学版），39（4）：331-340.
13. Hengye Wei*, Xuemei Wei, Zhen Qiu, Huyue Song, Guo Shi, 2016. Redox conditions across the G-L boundary in South China: Evidence from pyrite morphology and sulfur isotopic compositions. Chemical Geology, 440, 1-14.
14. Zhen Qiu, Shu Sun, Hengye Wei*, Qingchen Wang, Caineng Zou, Yijie Zhang. 2016. SIMS zircon U-Pb dating from bentonites in the Penglaitan Global stratotype Section for the Guadalupian-Lopingian boundary (GLB), South China. Geological Journal, 51, 811-816.
15. Chuan Guo*, Guorong Li, Hengye Wei, Feiyong Xia, Fachuan Xie, 2016. Stratigraphic architecture and platform evolution of the Changxing Formation (Upper Permian) in the Yuanba Gas Field, northeastern Sichuan Basin, China. Ara. J. Geosci., 9: 359.
16. 韦雪梅，韦恒叶*，邱振，2016年. 瓜德鲁普末期生物灭绝是由峨眉山LIP引起的吗？沉积学报。第34卷第3期，71-86页。
17. Hengye Wei*, Jun Shen, Shane D. Schoepfer, Leo Krystyn, Sylvain Richoz, Thomas J. Algeo*. 2015. Environmental controls on marine ecosystem recovery following mass extinctions, with an example from the Early Triassic. Earth-Science Reviews. Volume 149, pp. 108-135.
18. Hengye Wei*, Thomas J. Algeo*, Hao Yu, Jianguo Wang, Chuan Guo, Guo Shi. 2015. Episodic euxinia in the Changhsingian (late Permian) of South China: Evidence from framboidal pyrite and geochemical data. Sedimentary Geology, volume 319, pp.78-97.
19. Hengye Wei*, Hao Yu, Jianguo Wang, Zhen Qiu, Lei Xiang, Guo Shi. 2015. Carbon isotopic shift and its cause at the Wuchiapingian-Changhsingian boundary in the Upper Permian at the Zhaojiaba section, South China: Evidences from multiple geochemical proxies. Journal of Asian Earth Sciences, volume 105, pp.270-285.
20. Hao Yu, Hengye Wei*. 2015. A Kungurian oceanic upwelling on Yangtze platform: Evidenced by δ13Corg and authigenic silica in the Lower Chihsia Formation of Enshi Section in South China. Journal of Earth Science, vol. 26, pp. 211-218.