Geochemical and isotopic evidence for the escape of ice sheet fluids in an East Antarctic Ice Sheet outlet glacier, Taylor Valley, Antarctica 1 1 1 1 1 Michael G. Scudder , Graham H. Edwards , Gavin G. Piccione , Terrence Blackburn , Slawek Tulaczyk 1Earth & Planetary Science Department, University of California Santa Cruz, Santa Cruz, CA, USA 5 Correspondence to: Michael Scudder (
[email protected]) Abstract: The isotopic similarities between fluids beneath the East Antarctic Ice Sheet (EAIS) and the subglacial discharge found at the snout of Taylor glacier, one of the outlet glaciers located hundreds of kilometers away, implies that subglacial fluids may transit across this incredible distance. Such a model is consistent with the imaging, by airborne transient electromagnetic (ATE), of high salinity fluids at the 10 base of Taylor glacier to at least 5.75 km up-glacier from the snout, where ATE resolution fails (Mikucki et al., 2015). The transit of subglacial discharge could also be detected through the examination of basal ice, which has been hypothesized to form by subglacial freeze on of fluids at the ice-rock interface. We test these ice formation models as well search for direct evidence for the passage of subglacial discharge beneath Taylor glacier through examination of the elemental and U-Series isotopic compositions of basal 15 ice from Taylor Valley and compare with the compositions for regional lakes, streams, bedrock, and subglacial brines. For example, the basal ice from Suess Glacier, an alpine glacier draining a local accumulation zone in the Asgard Mountains, has 234U/238U and major element compositions nearly identical to surface waters and local silicates indicating mechanical entrainment of surface salts into basal ice by a cold-based formation mechanism.