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[Calcifications in temporal arteries -- their morphogenesis in comparison to physiological osteogenesis]
1Abteilung Pathologie, Universität Ulm, Albert-Einstein-Allee 11, 89081 Ulm, Germany.
Summary
Vascular calcification begins with calcospherites, similar to bone development, but progresses differently. This biphasic process involves initial calcospherite formation followed by bone-like apatite, creating hardened vessels.
Area of Science:
- Vascular biology
- Biomineralization
- Histopathology
Background:
- Vascular calcification was traditionally viewed as a degenerative process.
- Recent interpretations suggest it is a biologically regulated, bone-like phenomenon.
- Temporal arteries offer a model for studying vascular calcification due to their accessibility.
Purpose of the Study:
- To investigate the morphogenesis of calcification in temporal arteries.
- To compare this process with the development of fetal bone.
- To elucidate the cellular and molecular mechanisms underlying vascular calcification.
Main Methods:
- Analysis of formaldehyde-fixed temporal artery sections using light, transmission, and scanning electron microscopy.
- X-ray microanalysis to determine the atomic composition of calcifications.
- Comparative analysis with formaldehyde-fixed fetal bone specimens.
Main Results:
- Early vascular calcification is characterized by granular mediacalcinosis and calcospherites, sometimes showing the Liesegang phenomenon.
- Advanced calcification involves sheet-like structures containing calcospherites, with a lower magnesium content than early calcifications.
- Ultrastructural differences were observed between vascular calcospherites and those in endochondral ossification, with the latter showing apatite crystals.
Conclusions:
- Vascular calcification in temporal arteries is a calcospherite-dependent process, similar to other vascular calcifications.
- The process is biphasic: initial calcospherite formation followed by a secondary phase with bone-like apatite.
- Vascular calcification is distinct from bone formation, characterized by calcospherites and secondary apatite deposition.