Hostname: page-component-848d4c4894-2xdlg Total loading time: 0 Render date: 2024-06-28T23:09:17.909Z Has data issue: false hasContentIssue false

Crystallization of biogenic Ca-carbonate within organo-mineral micro-domains. Structure of the calcite prisms of the Pelecypod Pinctada margaritifera (Mollusca) at the submicron to nanometre ranges

Published online by Cambridge University Press:  05 July 2018

A. Baronnet
Affiliation:
Université Paul Cézanne and CRMCN-CNRS, UPR 7251, Campus Luminy, Case 913, 13288- Marseilles cedex 9, France
J. P. Cuif*
Affiliation:
UMR 8148 IDES, Bat. 504, Université Paris XI, 91405 Orsay cedex, France
Y. Dauphin
Affiliation:
UMR 8148 IDES, Bat. 504, Université Paris XI, 91405 Orsay cedex, France
B. Farre
Affiliation:
UMR 8148 IDES, Bat. 504, Université Paris XI, 91405 Orsay cedex, France
J. Nouet
Affiliation:
UMR 8148 IDES, Bat. 504, Université Paris XI, 91405 Orsay cedex, France

Abstract

Atomic force microscopy (AFM) and transmission electron microscopy (TEM) were used to investigate the fine structure of the calcite prisms from the pearl-oyster shell Pinctada margaritifera. The AFM analysis shows that the prisms are made of densely packed circular micro-domains (in the 0.1 μm range) surrounded by a dense cortex. The TEM images and diffraction patterns allow the internal structure of the micro-domains to be described. Each of them is enriched in Ca-carbonate. Hosted in distinct regions of each prism, some are fully amorphous, and some others fully crystallized as subunits of a large calcite single crystal. At the border separating the two regions, micro-domains display a crystallized core and an amorphous rim. Such a border probably marks out an arrested crystallization front having propagated through a previously bio-controlled architecture of the piling of amorphous micro-domains. Compared to recent data concerning the stepping mode of growth of the calcite prisms and the resulting layered organization at the μm-scale, these results give unexpected views regarding the modalities of biocrystallization.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 2008

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Addadi, L., Moradian, L, Shay, E., Maroudas, N.G. and Werner, S. (1987) A chemical model for the cooperation of sulfates and carboxylates in calcite crystal nucleation: relevance to biomineralization. Proceedings of the National Academy of Science USA, 84, 27322736.CrossRefGoogle ScholarPubMed
Adkins, J.F., Boyle, E.A., Curry, W.B. and Lutringer, A. (2003) Stable isotopes in deep-sea corals and a new mechanism for ‘vital effects'. Geochimica et Cosmochimica Ada, 67, 11291143.CrossRefGoogle Scholar
Beniash, E., Aizenberg, J., Addadi, L. and Weiner, S. (1997) Amorphous calcium carbonate transforms into calcite during sea urchin larval spicule growth. Proceedings of the Royal Society of London, 264, 461465.CrossRefGoogle Scholar
Boggild, O.B. (1930) The shell structure of the molluscs. Det Kongelige Danske Videnskabernes Selskabs Skrifter, Naturvidenskabelig og Mathematisk Afdeling, Kebenhavn, 9—2, 231326.Google Scholar
Bowerbank, J.S. (1844) On the structure of the shells of molluscan and conchyferous animals. Transactions of the Microscopical Society of London, 1, 123 — 152.CrossRefGoogle Scholar
Carpenter, W. (1845) On the microscopic studies of shells. British Association for Advancement of Science, 14, 1 -24.Google Scholar
Crenshaw, M.A. (1980) Mechanisms of shell formation and dissolution. Pp. 115128 in: Skeletal Growth of Aquatic Organisms (Rhoads, D.C. and Lutz, R.A., editors). Plenum Press.CrossRefGoogle Scholar
Cuif, J.P. and Dauphin, Y. (1998) Microstructural and physico-chemical characterizations of the ‘centers of calcification’ in the septa of some recent Scleractinian corals. Palaontologische Zeitschrifi, 72, 257270.CrossRefGoogle Scholar
Cuif, J.P. and Dauphin, Y. (2005a) The environmental recording unit in coral skeletons — a synthesis of structural and chemical evidences for a biochemically driven, stepping-growth process in fibres. Biogeosciences, 2, 6173.CrossRefGoogle Scholar
Cuif, J.P. and Dauphin, Y. (2005) The two-step mode of growth in the scleractinian coral skeletons from the micrometre to the overall scale. Journal of Structural Biology, 150, 319331.CrossRefGoogle ScholarPubMed
Cuif, J.P., Dauphin, Y., Doucet, J., Salome, M. and Susini, J. (2003) XANES mapping of organic sulphate in three scleractinian coral skeletons. Geochimica et Cosmochimica Ada, 67, 7583.CrossRefGoogle Scholar
Cuif, J.P., Dauphin, Y., Berthet, P. and Jegoudez, J. (2004) Associated water and organic compounds in coral skeletons: quantitative thermogravimetry coupled to infrared absorption spectrometry. Geochemistry, Geophysics, Geosystems, 5, doi: 10.2004GC000783.CrossRefGoogle Scholar
Dauphin, Y. and Dufour, E. (2007) Nanostructures of the aragonitic otolith of cod (Gadus morhua). Micron, doi:10.1016/j.micron.2007.11.007.CrossRefGoogle Scholar
Dauphin, Y., Cuif, J.P., Doucet, J., Salome, M., Susini, J. and Williams, C.T. (2003) In situ mapping of growth lines in the calcitic prismatic layers of mollusc shells using X-ray absorption near-edge structure (XANES) spectroscopy at the sulphur edge. Marine Biology, 142, 299304.CrossRefGoogle Scholar
Duffy, D.M. and Harding, J.H. (2004) Simulation of organic monolayers as templates for the nucleation of calcite crystals. Langmuir, 20, 76307636.CrossRefGoogle ScholarPubMed
Erben, H.K. and Watabe, N. (1974) Crystal formation and growth in bivalve nacre. Nature, 248, 128130.CrossRefGoogle Scholar
Fremy, E. (1855) Recherches chimiques sur les os. Annales de Chimie Paris, 43, 47107.Google Scholar
Hatchett, C. (1799) Experiments and observations on shell and bone. Philosophical Transactions of the Royal Society of London, 89, 315334.Google Scholar
McCrea, J.M. (1950) On the isotopie chemistry of carbonates and a paleotemperature scale. Journal of Chemical Physics, 18, 417426.CrossRefGoogle Scholar
Schlossenberger, J.E. (1856) Erster Versuch einer Allgemeiner und Vergleichenden Thier-Chemie. Winter, Leipzig.Google Scholar
Schmidt, WJ.(1924) Die Bausteine des Tierkorpers in polarisiertem Lichte. Cohen publishers, Bonn, Germany.Google Scholar
Taylor, J.D., Kennedy, WJ. and Hall, A. (1969) The shell structure and mineralogy of the Bivalvia. I. Introduction. Nuculacae—Trigonacae. Bulletin of the British Museum of Natural history, Zoology, 3, 1125.Google Scholar
Taylor, J.D., Kennedy, WJ. and Hall, A. (1973) The shell structure and mineralogy of the Bivalvia. II. Lucinacea—Clavagellacea. Conclusions. Bulletin of the British Museum of Natural history, Zoology, 22, 253294.Google Scholar
Urey, H.C. (1947) The thermodynamic properties of isotopie substances. Journal of the Chemical Society, 82, 562581.CrossRefGoogle Scholar
Urey, H.C, Lowenstam, H.A., Epstein, S. and McKinney, C.R. (1951) Measurements of paleotem-peratures and temperatures of the Upper Cretaceous of England, Denmark, and the southeastern United States. Bulletin of the Geological Society of America, 62, 399416.CrossRefGoogle Scholar
Weiner, S. and Addadi, L. (1991) Acidic macromole-cules of mineralized tissues: the controllers of crystal formation. Trends in Biochemical Sciences (TIBS), 16, 252256.CrossRefGoogle ScholarPubMed
Weiner, S., Levi-Kalisman, Y., Raz, S. and Addadi, L. (2003) Biologically formed amorphous calcium carbonate. Connective Tissue Research, 44, 214218.CrossRefGoogle ScholarPubMed
Weiss, I.M., Tuross, N., Addadi, L. and Weiner, S. (2002) Mollusc larval shell formation: amorphous calcium carbonate is a precursor phase for aragonite. Journal of Experimental Zoology, A293, 478491.CrossRefGoogle Scholar