Evidence of a Biological Control over Origin, Growth and End of the Calcite Prisms in the Shells of Pinctada margaritifera (Pelecypod, Pterioidea)

Type Article
Date 2014-12
Language English
Author(s) Cuif Jean-Pierre1, Burghammer Manfred2, Chamard Virginie3, Dauphin Yannicke1, Godard Pierre3, Le Moullac GillesORCID4, Nehrke Gernot5, Perez-Huerta Alberto6
Affiliation(s) 1 : Department of Earth Sciences, Paris-Sud University, Bt. 504, 91405 Orsay, France
2 : Department of Analytical Chemistry, Gent University, Krijgslaan 281 S12, 9000 Gent, Belgium
3 : Institut Fresnel UMR 7249, Aix-Marseille University, Centrale Marseille, 13013 Marseille, France
4 : Ecosystèmes insulaires océaniens UMR 241, Institut français de recherche pour l'exploitation de la mer (IFREMER) Centre du Pacifique, 98719 Taravao, Tahiti, French Polynesia
5 : Alfred Wegener Institute for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany
6 : Department of Geological Sciences, The University of Alabama, 2018 Bevill Building, Tuscaloosa, AL 35487, USA
Source Minerals (2075-163X), 2014-12 , Vol. 4 , N. 4 , P. 815-834
DOI 10.3390/min4040815
WOS© Times Cited 12
Keyword(s) biomineralization, bivalve shell, microstructure, calcite prisms
Abstract Consistently classified among the references for calcite simple prisms, the microstructural units that form the outer layer of the Pinctada margaritifera have been investigated through a series of morphological, crystallographical and biochemical characterizations. It is often said that the polygonal transverse shape of the prisms result from the competition for space between adjacent crystals. In contrast to this classical scheme the Pinctada prisms appear to be composed of four successive developmental stages from the concentrically growing disks on the internal side of the periostracum to the morphological, structural and compositional changes in both envelopes and mineral components at the end of the prisms. These latest structural and compositional changes predate nacre deposition, so that the end of prism growth is not caused by occurrence of nacre, but by metabolic changes in the secretory epithelium. This sequence makes obvious the permanent biological control exerted by the outer cell layer of the mantle in both organic envelopes and mineralizing organic phases.
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Cuif Jean-Pierre, Burghammer Manfred, Chamard Virginie, Dauphin Yannicke, Godard Pierre, Le Moullac Gilles, Nehrke Gernot, Perez-Huerta Alberto (2014). Evidence of a Biological Control over Origin, Growth and End of the Calcite Prisms in the Shells of Pinctada margaritifera (Pelecypod, Pterioidea). Minerals, 4(4), 815-834. Publisher's official version : https://doi.org/10.3390/min4040815 , Open Access version : https://archimer.ifremer.fr/doc/00249/36039/