“…Strongly plicate margins in marine bivalves are almost all restricted to epifaunal and shallowly infaunal species, including members of the Pectinidae, Plicatulidae, Anomiidae (Placunanomia), Ostreoidea, Pinnidae, Mytilidae (the Miocene North Pacific Plicatomytilus), Carditidae, Donacidae (Tridonax), Chamidae (Arcinella), post-Triassic Trigonioidea and Mesozoic Inoceramidae (Yoshida, 1998;Savazzi & Sa¨lgeback, 2004;Huber, 2010). Whether the folded margin itself functions in these bivalves is unclear, but the external sculptural elements generated by it serve to stiffen the valves against bending (Reif, 1978;Pennington & Currey, 1984;Alexander, 1990a, b;Savazzi & Sa¨lgeback, 2004). Similar stiffening, but then without marginal deviations, occurs in concentrically corrugated, thin-shelled, slow-burrowing mactrids such as Harvella, Mactrinula, Raeta and Raetellops (see also Morton, 2010;Signorelli, 2013) as well as in some thraciids, inoceramids and the Middle Permian genus Kolymia (Checa & Crampton, 2002;Biakov, 2012).…”