Evolution of dissolved oxygen in the ocean under global warming in the Cenozoic era: insights from ocean drilling

Article source: Release time:2024-03-26 10:05 Author: Views:128 Automatic translation:yes
Reporter:常燎 研究员(北京大学地球与空间科学学院)
  
Time:2024年3月26日(星期二)10:00
  
Place:钟健报告厅(系楼218)
  
Description:
  

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 & Nbsp& Nbsp; Researcher and Associate Professor at Peking University, recipient of the National Natural Science Foundation's Outstanding Youth Program, and Boya Young Scholar. He obtained a bachelor's degree from Peking University in 2004 and a doctoral degree from the University of Southampton in the UK in 2009. He has since worked and conducted research visits at the National Oceanic Center in the UK, the University of Utrecht in the Netherlands, the National University of Australia, and the Kochi Ocean Core Research Center in Japan. I have been working in the fields of rock magnetism and environmental magnetism for a long time, relying on scientific programs such as ocean drilling. By analyzing the growth, distribution, transport, and magnetization mechanisms of magnetic minerals in the ocean, I aim to understand marine geological and geophysical processes such as climate and environmental changes, as well as hydrothermal cycles in mid ocean ridges. The current co chairman of the International Association for Geomagnetism and High Altitude Physics (IAGA), Chinese Youth Committee member of the International Committee on Oceanographic Research (SCOR), and member of the Paleomagnetism Professional Committee of the Chinese Geological Society. He has won awards such as the Newton Senior Scholar Award from the Royal Society of England, the National Youth Talent Program, and the Fu Chengyi Youth Science and Technology Award from the Chinese Geophysical Society. He has also led key, general, and international cooperation and exchange projects funded by the National Natural Science Foundation of China. Published over 70 SCI papers in journals such as NC, Geology, EPSL, GRL, and JGR: SE