Central American Sub D–O/Heinrich Incident and its Formation Mechanism in Northern Hemisphere

Central American Sub D–O/Heinrich Incident and its Formation Mechanism in Northern Hemisphere: The Core Technology of Accelerator Mass Spectrometry for C14

Speaker: Wang Hong, Institute of natural resources, University of
Illinois Urbana-Champaign
Time: Thursday, May 10, 2018-4:00pm to 5:30pm
Location: 4th Floor Conference Hall in Geological Building
Sponsor: College of Environment and Planning, Henan University
Host: Prof. Feng Zhaodong
Brief introduction to the speaker: Wang Hong, Professor. In 1993 and 1996, he received a master's degree in literature and a PhD in Philosophy from the University of Illinois at Urbana-Champaign. He has been in charge of C14 and Photoneutic Geochronology laboratory in University of Illinois at Urbana-Champaign for 26 years, which operated and managed C14 and photometric laboratory for 12 years, and  managed stable isotope laboratories for 20 years. He has undertaken 9 fund totaling $1 million successively and has over 100 SCI papers in Geology、Geoderma、Quaternary Science Reviews、Geophysical Research Letters、Proceedings of the National Academy of Science. He focused in reconstructing the atmospheric evolution law of Northern Hemisphere by carbon isotope , measuring archaeological sites in Northern Hemisphere by C14 , and using high temperature   cracking accelerator. His research has drawn attention and highly respect in the field of global stable isotopic geochemistry and archaeology.

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