“…Such contrasting ice-mass distributions between successive glacial maxima highlight significant complexity in the processes that drive glaciation into different 'modes' (e.g., Liakka et al, 2016). The difference also has repercussions for glacioisostatic adjustment (GIA) studies of sea-level history during the LIG, which was about 1 C warmer than the Holocene (Clark and Huybers, 2009;Turney and Jones, 2010;McKay et al, 2011;Hoffman et al, 2017;Hansen et al, 2017), with sea levels that reached 4e10 m higher than today Dutton and Lambeck, 2012;Grant et al, 2012;Stocker et al, 2013;Dutton et al, 2015aDutton et al, , 2015b. Dendy et al (2017) investigated the sensitivity of the predictions of the last interglacial highstand to uncertainties in the configuration of the major northern hemisphere ice sheets during MIS 6.…”