Is there 1.5 million-year old ice near Dome C, Antarctica?

• Published in: The Cryosphere
• Main Authors: Parrenin, F, Cavitte, MGP, Blankenship, DD, Chappellaz, J, Fischer, H, Gagliardini, O, Masson-Delmotte, V, Passalacqua, O, Ritz, C, Siegert, MJ, Roberts, J, Young, DA
• Other Authors: British Council (UK)
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Copernicus Publications 2017
• Subjects: Science & Technology; Physical Sciences; Geography; Physical; Geosciences; Multidisciplinary; Physical Geography; Geology; CARBON-DIOXIDE CONCENTRATION; 100,000-YEAR GLACIAL CYCLES; PAST 800,000 YEARS; OLD ICE; MIDPLEISTOCENE TRANSITION; CHRONOLOGY AICC2012; MILLENNIAL-SCALE; SUBGLACIAL LAKES; EAST ANTARCTICA; VOLUME; 0405 Oceanography; 0406 Physical Geography And Environmental Geoscience; Meteorology & Atmospheric Sciences; East Antarctica; Antarc*; Antarctica; EPICA; ice core; Ice Sheet; The Cryosphere
• Online Access: http://hdl.handle.net/10044/1/53057; https://doi.org/10.5194/tc-11-2427-2017

Ice sheets provide exceptional archives of past changes in polar climate, regional environment and global atmospheric composition. The oldest dated deep ice core drilled in Antarctica has been retrieved at EPICA Dome C (EDC), reaching ∼ 800 000 years. Obtaining an older paleoclimatic record from Antarctica is one of the greatest challenges of the ice core community. Here, we use internal isochrones, identified from airborne radar coupled to ice-flow modelling to estimate the age of basal ice along transects in the Dome C area. Three glaciological properties are inferred from isochrones: surface accumulation rate, geothermal flux and the exponent of the Lliboutry velocity profile. We find that old ice (> 1.5 Myr, 1.5 million years) likely exists in two regions: one ∼ 40 km south-west of Dome C along the ice divide to Vostok, close to a secondary dome that we name Little Dome C (LDC), and a second region named North Patch (NP) located 10–30 km north-east of Dome C, in a region where the geothermal flux is apparently relatively low. Our work demonstrates the value of combining radar observations with ice flow modelling to accurately represent the true nature of ice flow, and understand the formation of ice-sheet architecture, in the centre of large ice sheets.