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【English】 行星科学与前沿技术重点实验室地球与行星物理学科中心 地球与行星磁场及宜居性学科组 ResearchGate
简历:
陈妍,特聘副研究员。主要从事天体生物学、沉积学、沉积地球化学和生物地球化学方面的研究。在埃迪卡拉纪-寒武纪和奥陶纪-志留纪转折时期海洋环境-生物协同演化、柴达木盆地类火星极端环境的生命信号及保存、地外生命探索等领域开展了较系统的工作。
2023.12-今:中国科学院地质与地球物理研究所,特聘副研究员
2019.09-2023.12:中国科学院地质与地球物理研究所,从事天体生物学工作,博士后
2015.10-2016.10:加州大学河滨分校,沉积地球化学专业,联合培养博士研究生
2012.09-2019.07:中国科学院地质与地球物理研究所,矿物学、岩石学、矿床学专业,博士
2008.09-2012.07:中山大学,地球信息科学与技术专业,学士
学科类别:
行星科学,天体生物学,地质学
研究方向:
- 地球重大环境转型期海洋环境-生物演化
- 类火星极端环境生命信号及保存
- 地外生命探索
承担科研项目情况:
- 国家自然科学基金青年科学基金项目,2022.01-2024.12,负责人。
- 国家自然科学基金重大项目课题,2023.01-2027.12,骨干。
- 国家重点研发计划项目子课题,2022.12-2027.11,骨干。
- 中国科学院重点部署项目课题,2022.1-2024.12,骨干。
代表论著:
2024:
- Chen,Y., Yin,Z.,Lin,W.,2024. Taphonomy of biosignatures in carbonate nodules from the Mars-analog Qaidam Basin: constraints from microscopic,spectroscopic,and geochemical analyses. Frontiers in Astronomy and Space Sciences 11.
- Shen,J.,Liu,L., Chen,Y.,Lin,W.,2024. A suite of spectroscopic devices as a potential tool to discriminate biotic and abiotic materials with an igneous rock. Icarus 407,115804.
- 郭雪,申建勋,刘立,黄诚祥, 陈妍,林红磊,林巍,2024. 柴达木盆地典型类火星地貌表层土壤的矿物与元素多谱学表征. 地球科学,1-18.
2023:
- Chen,Y.,Liu,L.,Zhang,H.,Guo,X.,Zhang,W.,Zhang,C.,Lin,W.,2023. Shallow subsurface habitats across the Mars-analog Qaidam Basin. SCIENCE CHINA Earth Sciences 66,2487-2496.
- 陈妍,刘立,张慧卿,郭雪,张文斯,张春霞,林巍 (2023). 柴达木盆地类火星区域的地下浅层微生物生境,中国科学:地球科学,53,11,2531-2540.
- Chen,Y.,Sun,Y.,Liu,L.,Shen,J.,Qu,Y.,Pan,Y.,Lin,W.,2023. Biosignatures preserved in carbonate nodules from the western Qaidam Basin,NW China: Implications for life detection on Mars. Astrobiology 23,172-182.(封面文章)
- Liu,L., Chen,Y.,Shen,J.,Pan,Y.,Lin,W.,2023. Metabolic versatility of soil microbial communities below the rocks of the hyperarid Dalangtan Playa. Applied and Environmental Microbiology 0,e01072-23.
- Yang,X.,Wu,S.,Shang,S., Chen,Y.,2023. Hydrodynamic variations and human activities have influenced sediment fluxes in the pearl river delta since the late holocene. Frontiers in Earth Science 10.
2022:
- Chen,Y.,Shen,J.,Liu,L.,Sun,Y.,Pan,Y.,Lin,W.,2022. Preservation of organic matter in aqueous deposits and soils across the Mars-analog Qaidam Basin,NW China: Implications for biosignature detection on Mars. Journal of Geophysical Research: Planets 127,e2022JE007418.(封面文章)
- Liu,L.,Liu,H.,Zhang,W., Chen,Y.,Shen,J.,Li,Y.,Pan,Y.,Lin,W.,2022. Microbial diversity and adaptive strategies in the Mars-like Qaidam Basin,North Tibetan Plateau,China. Environmental Microbiology Reports 14,873-885.
- Shen,J.,Liu,L., Chen,Y.,Sun,Y.,Lin,W.,2022. Geochemical and Biological Profiles of a Quartz Stone in the Qaidam Mars Analog Using LIBS: Implications for the Search for Biosignatures on Mars. ACS Earth and Space Chemistry 6,2595-2608.
- Shen,J., Chen,Y.,Sun,Y.,Liu,L.,Pan,Y.,Lin,W.,2022. Detection of biosignatures in terrestrial analogs of Martian regions: Strategical and technical assessments. Earth and Planetary Physics 6,431-450.
2021:
- Chen,Y.,Cai,C.,Qiu,Z.,Lin,W.,2021. Evolution of nitrogen cycling and primary productivity in the tropics during the Late Ordovician mass extinction. Chemical Geology 559,119926.
2019:
- Chen,Y.,Diamond,C.W.,Stüeken,E.E.,Cai,C.,Gill,B.C.,Zhang,F.,Bates,S.M.,Chu,X.,Ding,Y.,Lyons,T.W.,2019. Coupled evolution of nitrogen cycling and redoxcline dynamics on the Yangtze Block across the Ediacaran-Cambrian transition. Geochimica et Cosmochimica Acta 257,243-265.
2015:
- Cai,C.,Xiang,L.,Yuan,Y.,He,X.,Chu,X., Chen,Y.,Xu,C.,2015. Marine C,S and N biogeochemical processes in the redox-stratified early Cambrian Yangtze ocean. Journal of the Geological Society 172,390-406.
- Jiang,L.,Pan,W.,Cai,C.,Jia,L.,Pan,L.,Wang,T.,Li,H.,Chen,S., Chen,Y.,2015. Fluid mixing induced by hydrothermal activity in the ordovician carbonates in Tarim Basin,China. Geofluids 15,483-498.
2014:
- Yuan,Y.,Cai,C.,Wang,T.,Xiang,L.,Jia,L., Chen,Y.,2014. Redox condition during Ediacaran-Cambrian transition in the Lower Yangtze deep water basin,South China: constraints from iron speciation and δ13Corg in the Diben section,Zhejiang. Science Bulletin 59,3638-3649.
- 袁余洋,蔡春芳,汪天凯,向雷,贾连奇, 陈妍,2014. 埃迪卡拉纪-寒武纪过渡时期下扬子深水盆地氧化还原性质:来自浙西底本剖面铁组分及有机碳同位素的约束. 科学通报 59,2278.