The evolution of multicellularity in animals required the production of extracellular matrices that serve to spatially organize cells according to function. In corals, three matrices are involved in spatial organization: (i) an organic ECM, which facilitates cell-cell and cell-substrate adhesion; (ii) a skeletal organic matrix (SOM), which facilitates controlled deposition of a calcium carbonate skeleton; and (iii) the calcium carbonate skeleton itself, which provides the structural support for the 3D organization of coral colonies. In this report, we examine the production of these three matrices by using an in vitro culturing system for coral cells. In this system, which significantly facilitates studies of coral cell physiology, we demonstrate in vitro excretion of ECM by primary (nondividing) tissue cultures of both soft (Xenia elongata) and hard (Montipora digitata) corals. There are structural differences between the ECM produced by X. elongata cell cultures and that of M. digitata, and ascorbic acid, a critical cofactor for proline hydroxylation, significantly increased the production of collagen in the ECM of the latter species. We further demonstrate in vitro production of SOM and extracellular mineralized particles in cell cultures of M. digitata. Inductively coupled plasma mass spectrometry analysis of Sr/Ca ratios revealed the particles to be aragonite. De novo calcification was confirmed by following the incorporation of 45 Ca into acid labile macromolecules. Our results demonstrate the ability of isolated, differentiated coral cells to undergo fundamental processes required for multicellular organization.aragonite ͉ cell culture ͉ cnidaria ͉ calcification ͉ C orals (class, Anthozoa) are the most basal cnidarians and the first animal phylum with an organized neural system and complex active behavior (1). The embryonic gastrula develops to form an outer ectoderm and an inner endoderm separated by the mesoglea, a noncellular fibrous jelly-like material (2). The two germ layers are spatially structured by an ECM in which embedded, interstitial (stem) cells give rise to nematocysts, mucous glands, and sensory or nerve cells (2, 3). Many corals also precipitate calcium carbonate in the form of aragonite on a skeletal organic matrix (SOM) template (4, 5). The precipitation pattern is highly controlled between colonies, giving rise to morphological structures that are used as primary phenotypic markers of species in extant reefs and fossil samples.The basic cellular processes responsible for the production of ECM, SOM, and calcium carbonate skeleton remain largely unknown. Molecular, genetic, and physiological analyses of cellular processes in corals have been elusive mainly because it is difficult to grow corals under controlled conditions in the laboratory and because of the genetic and physiological complexities inherent in associations of the animals with symbionts and parasites. All zooxanthellate corals harbor intracellular symbiotic dinoflagellates (zooxanthellae) within their endoderm cells; the al...