Sarah Shackleton, Valens Hishamunda, Lindsey Davidge, Edward J. Brook, Julia Marks Peterson, A. Carter, Sarah M. Aarons, Andrei V. Kurbatov, D. Introne, Yuzhen Yan, Ian Nesbitt, Christo Buizert, Eric J. Steig, Andrew J. Schauer, Jason Phipps Morgan, Peter D. Neff, Jenna Epifanio, Jeffrey P. Severinghaus, Michael L. Bender, John A. Higgins
Antarctic ice cores provide a unique archive of Earth’s atmosphere and its largest extant ice sheet. The oldest continuous ice core extends back 800 ky, though discontinuous ice cores from the Allan Hills blue ice area (BIA) have been shown to preserve snapshots of ice and air back to at least 2.7 million years ago (Ma). Here, we provide snapshots of putatively Miocene and Pliocene ice and air from shallow ice cores drilled in the Allan Hills BIA. The ice, dated using the deficit in 40 Ar in ancient air compared to the modern atmosphere, is stratigraphically complex. Nevertheless, surface temperatures inferred from water isotopes correlate with sample age and indicate 12 ± 2 °C of cooling in Antarctica between 6 Ma and the late Pleistocene. Basal ice is nearly devoid of gases and remains to be dated with existing methods. This undated ice is characterized by an isotopic temperature 5 ± 1 °C warmer than the oldest dated (6 million year old) sample. We speculate that this ice reflects surface snowpack or permafrost that was preserved by the growth of the East Antarctic ice sheet in the Middle to Late Miocene.