In reef-building corals, larval settlement and its rapid calcification
provides a unique opportunity to study the bio-calcium carbonate formation
mechanism involving skeleton morphological changes. Here we investigate the
mineral formation of primary polyps, just after settlement, in two taxa of the
pocilloporoid corals: Stylophora pistillata (Esper, 1797) and
Pocillopora acuta (Lamarck, 1816). We show that the initial
mineral phase is nascent Mg-Calcite, with rod-like morphology in P.
acuta, and dumbbell morphology in S. pistillata.
These structures constitute the first layer of the basal plate which is
comparable to Rapid Accretion Deposits (Centers of Calcification, CoC) in adult
coral skeleton. We found also that the rod-like/dumbbell Mg-Calcite structures
in subsequent growth step may merge into larger aggregates by deposition of
aragonite needles. Our results suggest that a biologically controlled
mineralization of initial skeletal deposits (CoC) occurs in three steps: first,
vesicles filled with divalent ions are formed intracellularly. These vesicles
are then transferred to the calcification site, forming nascent Mg-Calcite
rod/pristine dumbbell structures. During the third step, aragonite crystals may
develop between these structures forming spherulite-like aggregates.