The Structure and Calcification of the Crustacean Cuticle

The integument of decapod crustaceans consists of an outer epicuticle,an exocuticle, an endocuticle and an inner membranous layerunderlain by the hypodermis. The outer three layers of the cuticleare calcified. The mineral is in the form of calcite crystalsand amorphous calcium carbonate. In the epicuticle, mineralis in the form of spherulitic calcite islands surrounded bythe lipid-protein matrix. In the exo- and endocuticles the calcitecrystal aggregates are interspersed with chitin-protein fiberswhich are organized in lamellae. In some species, the organizationof the mineral mirrors that of the organic fibers, but suchis not the case in certain cuticular regions in the xanthidcrabs. Thus, control of crystal organization is a complex phenomenonunrelated to the gross morphology of the matrix. Since the cuticle is periodically molted to allow for growth,this necessitates a bidirectional movement of calcium into thecuticle during postmolt and out during premolt resorption ofthe cuticle. In two species of crabs studied to date, thesemovements are accomplished by active transport effected by aCa-ATPase and Na/Ca exchange mechanism. The epi- and exocuticular layers of the new cuticle are elaboratedduring premolt but do not calcify until the old cuticle is shed.This phenomenon also occurs in vitro in cuticle devoid of livingtissue and implies an alteration of the nucleating sites ofthe cuticle in the course of the molt.