摘要：The duration and timing of the Last I nterglacial (LIG) Global Mean Sea Level (GMSL) fluctuations are active areas of research, with distinct features of this sea level change increasingly being repro-duced in diverse datasets and syntheses (Dutton & Lambeck 2012; Kopp et al. 2009; Thompson et al. 2011). We review and dis-cuss these possible changes in LIG GMSL and, in particular, what we may infer from them in terms of changes to continental ice
