“…The common view has been that the main function of foliar Si accretions in solid form (e.g., phytoliths) is to protect plant tissues from herbivory (Cooke et al, ; Epstein, ; Hartley & DeGabriel, ; Hartley, Fitt, McLarnon, & Wade, ), especially from being eaten by (mostly mammalian) vertebrates (Massey & Hartley, ; Massey, Massey, Ennos, & Hartley, ; Strömberg et al, ; Teaford, Lucas, Ungar, & Glander, ; Wieczorek, Zub, Szafrańska, Książek, & Konarzewski, ) or invertebrates (Garbuzov, Reidinger, & Hartley, ; Hunt, Dean, Webster, Johnson, & Ennos, ; Johnson et al, ; Massey & Hartley, ; Reynolds, Keeping, & Meyer, ; Ryalls, Hartley, & Johnson, ; Soininen, Bråthen, Jusdado, Reidinger, & Hartley, ), and to act as a potentially cheap alternative to cellulose or lignin (Cooke & Leishman, ; Raven, ; Schoelynck et al, ). Silicon is even thought to have played a central role in the co‐evolution of grasses and their mammalian grazers, which had to evolve teeth that could withstand chronic erosion by foliar phytoliths, although this role is still under active debate (Calandra, Zub, Szafrańska, Zalewski, & Merceron, ; Hartley & DeGabriel, ; Strömberg et al, ). However, horsetails (Equisetopsida), which generally have a very high tissue Si concentration ([Si]; in milligrams per gram dry weight; Hodson, White, Mead, & Broadley, ), are known to have been abundant as early as the Carboniferous (Trembath‐Reichert, Wilson, McGlynn, & Fischer, ), when herbivorous vertebrates had hardly evolved or not yet evolved (Sues, ).…”