ABSTRACT. Fossil CO 2 emissions have been diluting the global 14 C/C ratio of atmospheric CO 2 (Suess effect). We estimated the 14 CO 2 amount in the atmosphere (and its trend) utilizing the calculated 14 CO 2 activity concentration in the atmosphere (a acn , reported in mBq m -3 ). This parameter, calculated from 14 CO 2 and the CO 2 mixing ratio (reported in micromoles of CO 2 per mole of air), is connected with the 14 CO 2 quantity in the volume or mass unit of air, which is not influenced by the Suess effect. This parameter can only be influenced by processes linked to 14 CO 2 emissions/uptake, e.g. associated with atmosphere-biosphere or atmosphere-ocean CO 2 exchange as well as by anthropogenic emissions of 14 CO 2 . Results obtained from measurements at Schauinsland station, Germany, indicate a stable amount of 14 CO 2 in the atmosphere since the early 1990s.