“…For example, relict oyster beds, barnacle and tubeworm deposits have been used to constrain the elevation and duration of the mid-Holocene highstand along the east and west coasts of Australia (Beaman et al, 1994;Baker and Haworth, 1997, 2000a, 2000bBaker et al, 2001aBaker et al, , 2001bBaker et al, , 2005Lewis et al, 2008Lewis et al, , 2015. A detailed review of the use of FBIs as proxies for sea-level reconstructions is provided in Sloss et al (2007) and Lewis et al (2008Lewis et al ( , 2013Lewis et al ( , 2015 In the Wellesley Islands, the encrusting oyster Striostrea (Parastriostrea) mytiloides (common name black-lipped/blackedged oyster), commonly occur on elevated beach-rock deposits, wave-cut benches, and as mono-specific bioherm accumulations on exposed mudflats (Rosendahl et al, 2015). S. mytiloides is an intertidal species that commonly inhabits water levels from midtide to upper-tidal limits (HWNT) attached to rocks and mangrove roots.…”