Miocene and Pliocene ice and air from the Allan Hills blue ice area, East Antarctica

S S. Shackleton (Department of Geosciences, Princeton University) V V. Hishamunda (Department of Geosciences, Princeton University) L L. Davidge (Department of Earth & Space Sciences, University of Washington) E E. Brook (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University) J J. Marks Peterson (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University) A A. Carter S S. Aarons (Scripps Institution of Oceanography, University of California San Diego) A A. Kurbatov (Climate Change Institute, University of Maine) D D. Introne (Climate Change Institute, University of Maine) Y Y. Yan (State Key Laboratory of Marine Geology, Tongji University) I I. M. Nesbitt (Climate Change Institute, University of Maine) C C. Buizert (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University) E E. J. Steig (Department of Earth & Space Sciences, University of Washington) A A. J. Schauer (Department of Earth & Space Sciences, University of Washington) J J. Morgan (Scripps Institution of Oceanography, University of California San Diego) P P. D. Neff (Department of Soil, Water, and Climate, University of Minnesota) J J. A. Epifanio (College of Earth, Ocean, and Atmospheric Sciences, Oregon State University) J J. Severinghaus (Scripps Institution of Oceanography, University of California San Diego) M M. Bender (Department of Geosciences, Princeton University) J J. A. Higgins (Department of Geosciences, Princeton University)

Abstract

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.

Article Details

Volume / Issue Vol. 122, Issue 44
Published November 04, 2025
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (20)

S

S. Shackleton

Department of Geosciences, Princeton University

V

V. Hishamunda

Department of Geosciences, Princeton University

L

L. Davidge

Department of Earth & Space Sciences, University of Washington

E

E. Brook

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University

J

J. Marks Peterson

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University

A

A. Carter

S

S. Aarons

Scripps Institution of Oceanography, University of California San Diego

A

A. Kurbatov

Climate Change Institute, University of Maine

D

D. Introne

Climate Change Institute, University of Maine

Y

Y. Yan

State Key Laboratory of Marine Geology, Tongji University

I

I. M. Nesbitt

Climate Change Institute, University of Maine

C

C. Buizert

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University

E

E. J. Steig

Department of Earth & Space Sciences, University of Washington

A

A. J. Schauer

Department of Earth & Space Sciences, University of Washington

J

J. Morgan

Scripps Institution of Oceanography, University of California San Diego

P

P. D. Neff

Department of Soil, Water, and Climate, University of Minnesota

J

J. A. Epifanio

College of Earth, Ocean, and Atmospheric Sciences, Oregon State University

J

J. Severinghaus

Scripps Institution of Oceanography, University of California San Diego

M

M. Bender

Department of Geosciences, Princeton University

J

J. A. Higgins

Department of Geosciences, Princeton University