The Cryosphere, 13, 2935–2951, 2019 https://doi.org/10.5194/tc-13-2935-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. New Last Glacial Maximum ice thickness constraints for the Weddell Sea Embayment, Antarctica Keir A. Nichols1, Brent M. Goehring1, Greg Balco2, Joanne S. Johnson3, Andrew S. Hein4, and Claire Todd5 1Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA 2Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA 3British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK 4School of GeoSciences, University of Edinburgh, Drummund Street, Edinburgh, EH8 9XP, UK 5Department of Geosciences, Pacific Lutheran University, Tacoma, WA 98447, USA Correspondence: Keir A. Nichols (
[email protected]) Received: 27 March 2019 – Discussion started: 14 May 2019 Revised: 12 September 2019 – Accepted: 2 October 2019 – Published: 8 November 2019 Abstract. We describe new Last Glacial Maximum (LGM) surements indicate that the long-lived nuclide measurements ice thickness constraints for three locations spanning the of previous studies were influenced by cosmogenic nuclide Weddell Sea Embayment (WSE) of Antarctica. Samples col- inheritance. Our inferred LGM configuration, which is pri- lected from the Shackleton Range, Pensacola Mountains, and marily based on minimum ice thickness constraints and thus the Lassiter Coast constrain the LGM thickness of the Slessor does not constrain an upper limit, indicates a relatively mod- Glacier, Foundation Ice Stream, and grounded ice proximal est contribution to sea level rise since the LGM of < 4.6 m, to the modern Ronne Ice Shelf edge on the Antarctic Penin- and possibly as little as < 1.5 m.