Structure and composition of the boundary zone between aragonitic crossed lamellar and calcitic prism layers in the shell of Concholepas concholepas (Mollusca, Gastropoda)

Author:

Dauphin Yannicke1,Cuif Jean-Pierre2,Cotte Marine3,Salomé Murielle3

Affiliation:

1. Micropaleontology, Paris VI University; 75252; Paris; France

2. Geosciences, Paris Sud University; 91405; Orsay; France

3. European Synchrotron Radiation Facility; 38043; Grenoble; France

Publisher

Wiley

Subject

Animal Science and Zoology

Reference25 articles.

1. Méthode d'identification localisée de la diagenèse des aragonites d'origine biologique à l’échelle du microscope électronique à balayage;Dauphin;Paläont. Z.,1992

2. Soluble organic matrices of the calcitic prismatic shell layers of two pteriomorphid bivalves: Pinna nobilis and Pinctada margaritifera;Dauphin;J. Biol. Chem.,2003

3. The nanostructural unity of mollusc shells;Dauphin;Mineral. Mag.,2008

4. Mineralogy, chemistry and ultrastructure of the external shell layer in ten species of Haliotis with reference to Haliotis tuberculata (Mollusca: Archaeogastropoda);Dauphin;Bull. Geol. Inst. Univ. Uppsala, N.S.,1989

5. Microstructure, nanostructure and composition of the shell of Concholepas concholepas (Gastropoda, Muricidae);Dauphin;Aquat. Living Resour.,2003

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