“…While investigating the movement of water through isolated cuticles, Schonherr (1976b) established a pore size near 0.9 nm, which can typically accommodate hydrated mineral ions. Although the outer layer of the cuticle is largely composed of a mixture of hydrophobic waxes (Tulloch, 1970), the inner layer, inherently more porous (Schonherr, 1976a), has a more complex chemistry, including dissociable acidic groups (Schonherr and Huber, 1977;Kolattukudy, 1980) that appear to be associated with the pores through which mineral acids pass (Hauser et al, 1993). The acid groups in the pores act as fixed buffers, "absorbing" protons for considerable periods before the pores become protonated and allow the free and rapid passage of protons through the cuticle to the inside.…”