Stratigraphic information concerning the retreat of the Antarctic ice sheet from the continental shelf after the Last Glacial Maximum is reviewed and compared with new results from a shelf valley off Mac. Robertson Land, East Antarctica. Radiocarbon dates and detailed lithostratigraphic logs indicate that the onset of open-marine conditions over shallow shelf banks (<200 m water depth) was achieved prior to 7000 yr BP and over deep (� 1000 m) middle to outer shelf valleys, open-marine conditions were achieved prior to 5400 yr BP. Radiocarbon dating ofbulk-organic carbon in some diatom oozes by the AMS method demonstrates problems of contamination.Jurassic pollen, spores and organic maner have been eroded and incorporated into Holocene diarom ooze, causing anomalously old 14 C dates (e. g. one surface age of7084 ± 86 yr BP was determined). This problem may arise at other locations around East Antarctica where older strata outcrop on the seafloor.
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