The two-step mode of growth in the scleractinian coral skeletons from the micrometre to the overall scale.
It has been known since the 19th century that coral skeletons are built of aragonite crystals with taxonomy-linked arrangements, but the way by which each coral species controls this crystallization process remains an unsolved question. The problem became still more intriguing when it was shown that isotopic compositions of coral aragonite were subject to taxonomy-linked influences (the "vital effect"). On the other hand, presence of an organic component in coral skeletons is also long known, but localization of these compounds is admittedly restricted to particular structures called "centres of calcifications." Fibres, the largely predominant part of the coral skeletons, are usually considered as purely mineral units. In this paper, it is shown that in both "centres of calcification" and fibres, organic compounds are associated with the mineral material at a deep structural level. A series of variously scaled observations and localized measurements allow recognition of the presence of an organic component at the nanometre scale. Far from being a freely operating process, crystallization of coral fibres is thus permanently controlled by the polyp basal ectoderm through a cyclic two-step process acting at the micrometre-scale. The biomineralization cycle begins by secretion of a proteoglycan matrix. As the composition of these sugars-proteins assemblages has been shown taxonomy dependent, the hypothesis can be made that multiple and long recognized specificities of coral skeletons are linked to this biochemically driven crystallization process. Additionally, this new concept of the biomineralization process in coral skeletons provides us with an access to the long term evolution of the Scleractinia. Remarkably, results of a skeleton-based approach using microstructural criteria (i.e., the spatial relationships of "centres of calcification" and the three-dimensional arrangements of fibres), are consistent with a molecular phylogenetic analysis carried out on the same species. Clearly, at the overall ontogenic level, the two-step growth mode of coral skeletons is also a valuable tool to reconstruct the evolutionary history of Scleractinia.
Cuif
Jean-Pierre
JP
UMR 8148 IDES, Geology, bat. 504, Université Paris XI-Orsay, F-91405 Orsay cedex, France. cuif@geophy.geol.u-psud.fr
Dauphin
Yannicke
Y
D000165:Acridine Orange / Q000494:pharmacology; D000825:Animal Structures; D000818:Animals; D037421:Anthozoa / Q000033:anatomy & histology* / Q000502:physiology*; D002113:Calcification, Physiologic; D002118:Calcium / Q000737:chemistry; D002119:Calcium Carbonate / Q000737:chemistry; D018360:Crystallography, X-Ray; D008855:Microscopy, Electron, Scanning; D011134:Polysaccharides / Q000737:chemistry; D013053:Spectrophotometry
D011134:Polysaccharides; D000165:Acridine Orange; D002119:Calcium Carbonate; D002118:Calcium