“…These occurrences are recorded from the Lower Carboniferous to Cretaceous, mostly from the Northern Hemisphere (Seward, 1923(Seward, , 1924Rothwell & Scott, 1983;Scott & Taylor, 1983;Scott & Paterson, 1984;Rex & Galtier, 1986;Labandeira & Beall, 1990; Lesnikowska, 1990;Tidwell & Hebbert, 1992;Labandeira et al, 1997;Ash, 2000;Labandeira & Phillips, 2002;Rößler, 2000;D'Rozario et al, 2011). These occurrences were reported mostly in the stems of Psaronius Cotta, 1832 a marattialean tree fern (Rothwell & Scott, 1983;Labandeira & Beall, 1990;Lesnikowska, 1990;Labandeira & Phillips 1996a,b;Labandeira et al, 1997;Labandeira & Phillips, 2002;Rößler, 2000;D'Rozario et al, 2011) and Tempskya Corda, 1845 a probable fi licalean tree fern (Seward, 1923(Seward, , 1924Scott & Paterson, 1984;Tidwell & Hebbert, 1992). Less common occurrences of insect damage are galls (Labandeira & Phillips, 1996b;Labandeira & Phillips, 2002), piercing and sucking (Scott & Taylor, 1983;Labandeira & Phillips, 1996a) and marginal excisions (Ash, 1997;Labandeira, 2002b) which have been recorded from the Carboniferous to the Eocene of the USA.…”