gamma Irradiation of (CaCO3)-C-14, followed by aqueous dissolution of
the irradiated solid, produces carbon-14-labelled formic acid and smal
l quantities of oxalic, glyoxylic, glycolic and acetic acids. Traces o
f formaldehyde are seen only at the highest absorbed doses. The yields
of products from gamma irradiation are similar to those observed upon
self-irradiation of (CaCO3)-C-14 The higher yields of glycolic and ac
etic acids from gamma irradiation may result from the higher dose rate
employed. These simple compounds, produced by irradiation of carbonat
es, may have been a source of organic carbon on the Primitive Earth.