Ice samples from Dronning Maud Land, Antarctica, were analyzed for (CO2)-C-
14 and (CO)-C-14 by accelerator mass spectrometry. Only a small amount (sim
ilar to2%) of in situ produced radiocarbon was detected. The calibrated rad
iocarbon ages, corrected for in situ produced C-14, are in fair agreement w
ith age estimates obtained from stratigraphical methods added to a gas incl
usion model. The ages of the entrapped air range from recent to ca. 1200 AD
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