Review article: Existing and potential evidence for Holocene grounding line retreat and readvance in Antarctica

• Published in: The Cryosphere
• Main Authors: Johnson, JS, Venturelli, RA, Balco, G, Allen, CS, Braddock, S, Campbell, S, Goehring, BM, Hall, BL, Neff, PD, Nichols, KA, Rood, DH, Thomas, ER, Woodward, J
• Other Authors: Natural Environment Research Council (NERC)
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2022
• Subjects: Science & Technology; Physical Sciences; Geography; Physical; Geosciences; Multidisciplinary; Physical Geography; Geology; ICE CORE; 0405 Oceanography; 0406 Physical Geography and Environmental Geoscience; Meteorology & Atmospheric Sciences; Antarctic; The Antarctic; Antarc*; Antarctica; ice core; Ice Sheet; The Cryosphere
• Online Access: http://hdl.handle.net/10044/1/96772; https://doi.org/10.5194/tc-16-1543-2022

Widespread existing geological records from above the modern ice sheet surface and outboard of the current ice margin show that the Antarctic Ice Sheet (AIS) was much more extensive at the Last Glacial Maximum (∼ 20 ka) than at present. However, whether it was ever smaller than present during the last few millennia, and (if so) by how much, is known only for a few locations because direct evidence lies within or beneath the ice sheet, which is challenging to access. Here, we describe how retreat and readvance (henceforth “readvance”) of AIS grounding lines during the Holocene could be detected and quantified using subglacial bedrock, subglacial sediments, marine sediment cores, relative sea-level (RSL) records, geodetic observations, radar data, and ice cores. Of these, only subglacial bedrock and subglacial sediments can provide direct evidence for readvance. Marine archives are of limited utility because readvance commonly covers evidence of earlier retreat. Nevertheless, stratigraphic transitions documenting change in environment may provide support for direct evidence from subglacial records, as can the presence of transgressions in RSL records, and isostatic subsidence. With independent age control, ice structure revealed by radar can be used to infer past changes in ice flow and geometry, and therefore potential readvance. Since ice cores capture changes in surface mass balance, elevation, and atmospheric and oceanic circulation that are known to drive grounding line migration, they also have potential for identifying readvance. A multidisciplinary approach is likely to provide the strongest evidence for or against a smaller-than-present AIS in the Holocene.