Summary
Mantle-derived carbonate and carbon bearing rocks are direct indicators of the Earth’s solid carbon cycle, whose periodic energetic activity transfer elements from the mantle to the crust, and releases CO2 into the atmosphere. The network will focus on multi-disciplinary studies of carbon reservoirs and bring together the research expertise of all aspects of the visible carbon cycle. More
Duration
3 years, from 2000 to 2003.
For current status, see News
