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 K-edge

被引:73
|
作者
Dauphin, Y
Cuif, JP
Doucet, J
Salomé, M
Susini, J
Williams, CT
机构
[1] Univ Paris 11, FRE2566 CNRS, Lab Paleontol, F-91405 Orsay, France
[2] Univ Paris 11, LURE, F-91898 Orsay, France
[3] European Synchrotron Radiat Facil, ID21, F-38043 Grenoble, France
[4] Nat Hist Museum, Dept Mineral, London SW7 5BD, England
关键词
D O I
10.1007/s00227-002-0950-2
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
The microstructure and composition, including chemical speciation of sulphur (S), of two mollusc shells were investigated using a combination of scanning electron microscopy, X-ray absorption near-edge structure spectroscopy (XANES) and electron probe microanalysis (EPMA). The shell of Pinna is composed of monocrystalline, and Pinctada, of polycrystalline, calcite prisms separated by organic-rich walls. Sulphur speciation information from XANES spectra using a scanning X-ray microscope showed that the protein S content of the interprismatic walls is higher than the SO4 content, whereas the reverse is true for the intraprismatic structures. High-spatial-resolution XANES maps for the different S species across adjacent calcite prisms confirm their distinctive distributions in the molluscan shells and illustrate the presence of narrow, submicron transverse growth features. On a larger scale, a series of wider growth zones, incorporating the submicron zones, are aligned parallel to each other and cross-cut many calcite prisms. EPMA element maps for magnesium (Mg) and S demonstrate that these growth increments are compositionally zoned, comprising alternating layers of high mineral (Mg-rich) and high organic (S-rich) components. Additionally, these maps confirm that the organic interprismatic walls have lower Mg and higher S than the intraprismatic structures.
引用
收藏
页码:299 / 304
页数:6
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