Radiocarbon as a geochronometer and as a tracer in paleoclimatology, geophysics and astrophysics
- 4:00 PM
ESB 5104-06, Earth Sciences Building
2020 - 2207 Main Mall
An accurate chronometer that covers the past 50,000 years is of paramount importance in fields such as geophysics, geochemistry, and paleoclimatology. However, we now recognize that the atmospheric 14C/12C ratio varies with time, which affects the accuracy of this geochronometer. Fortunately, short and long-term 14C variations on Earth and provide invaluable insights on climatological, biogeochemical, geophysical and astrophysical processes.