“…This is also true at coral reef coasts, which have shallow, intertidal reef flats created by reef-building organisms (e.g., corals, calcareous algae, and foraminifera) and calcareous sand distributions on beaches and reef islands (Woodroffe, 2002). Previous studies have shown distinct zonal distributions of reef-dwelling organisms due to subaerial exposure, which is basically a function of surface morphology in intertidal areas (e.g., Stoddart, 1969;Yamano et al, 2001;Tanaka and Nakaoka, 2004). However, possible future rises in sea levels threaten to drown or inundate coral reefs and islands (Leatherman, 1997).…”