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Abstract
Calcified deposits in the tunica media of the human aorta have been studied in 128
cases by light microscopy and by electron microscopy and analytical methods in selected
samples. Although dissolved and not visible in routine histology with alum hematoxylin
stains, such calcification can be clearly seen after methylene blue staining in the
form of unstained refractile particles of 1–2 μm size. These are found between the
elastic laminae chiefly in the inner two-thirds of the media and appear at about age
20. By X-ray diffraction supported by energy dispersive X-ray analysis, they have
been identified as whitlockite (Ca,Mg)3(PO4)2. Statistical analysis shows a significant increase in numbers with age and significant
differences in severity related to county of origin but no differences between sexes
or races and no correlation with deaths related to cardiovascular diseases. Among
various substructures of the aortic wall, no unique crystal precursor was identified.
Possible etiologic factors and clinicopathologic significance are considered.
Keywords
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Article info
Publication history
Accepted:
March 22,
1993
Received in revised form:
March 19,
1993
Received:
January 8,
1993
Identification
Copyright
© 1993 Published by Elsevier Inc.