“…Plicidentine, defined as infoldings of the dentine into the pulp cavity at the base of the tooth, has long been known in early tetrapods, being first documented in the temnospondyl Mastodonsaurus by Owen (1841) . It has since been found to be widespread throughout numerous temnospondyls (often referred to as ‘labyrinthine infoldings’ in older literature) but is also known in a variety of extinct and extant fishes (e.g., Schultze, 1969 ; Schultze, 1970 ; Long, 1989 ; Meunier et al, 2015 ). Although the classical model of dental evolution suggested a loss of plicidentine in amniotes (e.g., Laurin & Reisz, 1995 ), these infoldings occur in a broad number of amniote groups, including ichthyosaurs ( Maxwell, Caldwell & Lamoureux, 2011b ), choristoderes ( Gao & Fox, 1998 ), lepidosaurs (e.g., Kearney, Rieppel & Wood, 2006 ; Maxwell et al, 2011 ), captorhinids ( De Ricqlès & Bolt, 1983 ), parareptiles (e.g., Modesto & Reisz, 2008 ; MacDougall, LeBlanc & Reisz, 2014 ; MacDougall, Modesto & Reisz, 2016 ), and synapsids ( Brink, LeBlanc & Reisz, 2014 ).…”