ANTARCTIC climate during the Pliocene has been the subject of consider
able debate. One view holds that, during part of the Pliocene, East An
tarctica was largely free of glacier ice and that vegetation survived
on the coastal mountains(1-4). An alternative viewpoint argues for the
development of a stable polar ice sheet by the middle Miocene, which
has persisted since then(5-10). Here we report the discovery of buried
glacier ice in Beacon valley, East Antarctica, which appears to have
survived for at least 8.1 million years. We have dated the ice by Ar-4
0/Ar-39 analysis of volcanic ash in the thin, overlying glacial till w
hich, we argue, has undergone little (if any) reworking. Isotope and c
rystal fabric analyses of the ice show that it was derived from an ice
sheet. We suggest that stable polar conditions must have persisted in
this region for at least 8.1 million years for this ice to have avoid
ed sublimation.