It has been known for a long time (1)(2)(3)(4), that mother-of-pearl, forming the innermost layer of various shells, consists of numerous mineral leaves or lamellae, disposed parallel to the inner surface of the shell, and piled upon each other horizontally. Each leaf or lamella is composed of microscopical crystals of aragonite (1) in which calcium carbonate is crystallized in a rhombic lattice t. The crystals, which have a long axis weakly developed (1-4) and therefore a tabular shape, are disposed side by side in a single layer within each leaf, and appear, in tangential view of a lamella, as polygonal slabs in a flagging.The organic components of mother-of-pearl (so called conchiolin) are traditionally described (26,25,13,24,23,(1)(2)(3)(4) as consisting of extremely thin parallel sheets, which alternate with the mineral lamellae in the horizontally stratified nacreous configuration. These parallel sheets are united by transverse bridges of the same organic substance, which cross the lamellae at right angles between the crystals of aragonite. The whole system appears in the figures recorded by light microscopy as an extremely thin linear network, resembling the concrete in a brick wall (22), but without any other detail of structure (1).Mter decalcification of mother-of-pearl, the organic residue consists of soft transparent stratified membranes. As shown previously (5, 6), ultrasonic vibrations may be used to cleave and break the organic membranes of decalcified mother-of-pearl into thinner pellicles and fragments of leaflets. In the electron microscope, these pellicles, collapsed by desiccation on to a formvar background, appear perforated by openings, the size, shape, and distribution of which vary with the groups and species of molluscs investigated. These details of structure were measured in twenty-seven species of Pelecypods and fifteen species of Gastropods. The results suggested that the differences recorded in the patterns of the leaflets were statistically characteristic at a high level (class) of the taxonomic hierarchy. Within the same class, the differences in the patterns were not, or were questionably significant at a lower level (genus, species). 1 In the inner layer of the shells, in which calcium carbonate is crystallized in a rhombohedric lattice, there is no mother-of-pearl. The results of a study of this so called subnacreous layer, or calcitostracum, will be reported later. 797