“…Palaeoenvironmental data can provide a detailed understanding of these changes and inform the range of potential options for management and/or restoration, in effect "learning from the past" (Anderson et al, 2006;Dearing, 2006;Dearing et al, 2006;McCarroll, 2010;Newman et al, 2010). While there are unlikely to be any exact analogues for a future warmer world, Quaternary palaeoenvironmental records, in particular, are important in understanding how climate, physical processes, sea level and habitats have changed in the past and enabling informed evaluation of scenarios of future change over different temporal and spatial scales (Willis and Birks, 2006;Willis et al, 2007Willis et al, , 2010Froyd and Willis, 2008;Davies and Bunting, 2010). For example, comparison of UKCP09 relative sea-level rise rates with those for the mid-and late-Holocene allows a means of scaling potential future coastline changes (Gehrels, 2010;Rennie and Hansom, 2011), and changes in slope stability, sediment production, landform distributions and floodplain and wetland histories can provide pointers for future catchment responses (Higgitt and Lee, 2001;Lane et al, 2007;Macklin et al, 2010).…”