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Science 28 November 1969:
Vol. 166. no. 3909, pp. 1147 - 1150
DOI: 10.1126/science.166.3909.1147
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Articles

X-ray Diffraction Studies of Echinoderm Plates

Gabrielle Donnay 1 and David L. Pawson 2

1 Geophysical Laboratory, Carnegie Institution of Washington, Washington, D.C. 20008
2 National Museum of Natural History, Smithsonian Institution, Washington, D.C. 20560

X-ray diffraction studies confirm that, with few exceptions, each skeletal element of echtinoderms is a single crystal of magnesium-rich calcite and that a relation exists between the shape of the element and the crystallographic a- and c-axes. The exceptions incluide the teeth of echinoids, and the calcareous ring as well as the anal teeth of holothurians. The tubercles of an echinoid plate begin their growth as parts of the single crystal of the plate; under the mechanical action of the spines that are attached to them, they become partly polycrystalline, as shown by scanning electron microscopy and by x-ray powder diffraction. The interface between inorganic crystalline and organic amorphous matter in the skeletal element appears to be the first example reported in nature of a periodic mninimal suirface.


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