“…Indeed, as early as 1938, Irving Langmuir reported that aqueous clay suspensions can form a birefringent phase where the nanosheets have orientational order, in addition to the usual isotropic phase (Figure a) and in contrast with it . Some 60 years later, the nature of this orientational order was compared to that of lyotropic liquid crystals (LC), but the observation of an LC phase, at thermodynamic equilibrium, in suspensions of synthetic laponite and natural montmorillonite clays, was hampered by their strong tendency to form gels. , The clear-cut discovery of a nematic LC phase (Figure b) was only reported in 2006 when it was observed in aqueous suspensions of natural nontronite clays, a little later with beidellite clay, and more recently with synthetic hectorite and the microporous layered silicate ilerite. − Meanwhile, the smectic (i.e., lamellar) LC phase was reported for aqueous suspensions of other kinds of mineral compounds: synthetic phosphatoantimonate, niobate, and titanate nanosheets (Figure c). − Interestingly, the stability of the lamellar phase in these systems extends to very low concentrations, resulting in lamellar periods comparable to the wavelengths of visible light and therefore leading to photonic properties. ,,, However, LC phases more ordered than the nematic phase, such as the lamellar or columnar LC phases, have never been clearly evidenced in clay suspensions.…”