Abstract

Nacre, or mother of pearl, is composed of aragonite tablets and is produced by some mollusks. Because of the highly organized internal structure, chemical complexity, mechanical properties and optical effects of nacre, its formation is among the best-studied examples of calcium carbonate biomineralization. The pearl oyster Pinctada margaritifera is harvested in French Polynesia for pearl farming. The quality of the pearl depends on the quality of the nacre on its surface and its iridescent colors are affected by the thickness of the layers. Here we report on an experimental study conducted to influence the shape and the thickness of nacre tablets by keeping pearl oysters at four different depths (7, 20, 30 and 39 m) for one week. Scanning electron microscopy was used to measure the thickness of the nacre tablets and to analyze their final shape. The shape of the tablets changed from hexagonal to rhomboid at a depth of 39 m. The change in shape led to a change in size. The thickness of the tablets was reduced by between 16 and 30% on average. We also measured the oxygen isotopic composition using Secondary Ion Mass Spectrometry. In this study, we demonstrated that depth can modify the size, shape and thickness of nacre tablets, but not the d18O. This environmental modification is important for the biomineralization of the shell of the pearl oyster Pinctada margaritifera.

Highlights

  • Nacre, or mother of pearl, is a calcium carbonate structure produced by bivalves, gastropods, and cephalopods as an internal shell coating

  • The combination of the highly organized internal structure, chemical complexity, mechanical properties and optical effects of this biomineral are responsible for its characteristic beautiful luster

  • Scanning electron microscopy was used to measure the thickness of nacre tablets and to analyze their final shape, which changed from hexagonal to rhomboid at a depth of 39 meters

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Summary

Introduction

Mother of pearl, is a calcium carbonate structure produced by bivalves, gastropods, and cephalopods as an internal shell coating. We checked if depth could have an influence on the oxygen isotopic composition of the shell, this composition being an important proxy in paleoclimatic reconstructions. Isotopic compositions in biocarbonates, and more oxygen isotopic compositions are used as proxy of temperature and sea level change. It is based on the relationship first described by Urey [5] linking the isotopic fractionation to the temperature. We report on an experimental study in which we tried to influence the shape and the thickness of nacre tablets by keeping pearl oysters at four different depths (7, 20, 29 and 39 m) for one week

Scanning Electron Microscopy Observations
Oxygen Isotope Measurements
Modifications in Thickness and Size
Experimental Testing
Scanning Electron Microscopy
Conclusions
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