This change is apparently the largest increase of atmospheric 14C known from late glacial and Holocene records (Goslar et al., 1995). Hajdas et al. (1998) used this sharp increase of atmospheric 14C at the onset of the YD as a tool for time correlation between sites. What are the possible causes for this large increase in atmospheric 14C? Geomagnetic variations are not a likely cause, since these generally act on a much longer time scale (i.e. millennia). Amongst others, Bjorck et al. (1996) and Goslar et al. (1999) postulate that the increase in 14C at the start of the YD is caused by a decrease of the CO2 exchange between the atmosphere and ocean, because of stagnation in ocean circulation (i.e. 14C changes as an effect of climate change). If the deep-water formation would weaken or even cease, this would reduce the atmosphere ocean exchange of CO2, thus effectively increasing the atmospheric 14C content.
My comments:
1) In the last 5 years there are multiple papers that provide evidence of abrupt changes to the geomagnetic field. An abrupt drop in the geomagnetic field for a thousand years would explain the Younger Dryas cooling.
2) C14 could be explained by changes in ocean currents hypothesis has been disproved Recent detailed analysis of ocean circulation indicates the North Atlantic Drift current is not reduced during the Younger Dryas. In addition, there are other periods where the North Atlantic Drift current is reduced and there is no increase in C14.