4.4 Article Proceedings Paper

Isolation of Calcospherulites from the Mineralization Front of Bone

Journal

CELLS TISSUES ORGANS
Volume 189, Issue 1-4, Pages 75-79

Publisher

KARGER
DOI: 10.1159/000152914

Keywords

Bone formation; Mineralization front; Calcospherulites; Biomineralization; Bone matrix proteins

Funding

  1. NATIONAL INSTITUTE OF ARTHRITIS AND MUSCULOSKELETAL AND SKIN DISEASES [R01AR052775, R01AR045171] Funding Source: NIH RePORTER
  2. NIAMS NIH HHS [R01 AR045171, R01 AR052775, R01 AR052775-04] Funding Source: Medline

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Calcium-containing spherical bodies (calcospherulites) exist along the mineralization front of bone and are thought to play a role in bone formation. Existing methods to isolate calcospherulites involve harsh treatments that remove much of their organic matter. This study sought to isolate them using a less destructive approach to better preserve their organic components. Juvenile rats were injected with a low dose of calcein to label the newly formed mineral at the mineralization front of bone in vivo. Periosteum was completely dissected from the tibial diaphysis and unmineralized osteoid matrix was removed by collagenase in order to expose calcospherulites. Calcein-labeled calcospherulites of approximately 0.5 mu m average diameter were observed all along the mineralization front and they exhibited a Ca/P ratio of 1.3 in situ. Calcospherulites were released from the mineralization front by a short dispase digestion and isolated via fluorescence flow sorting. X-ray diffraction revealed they contained apatite crystals (c-axis length of 17.5 +/- 0.2 nm) and their Ca/P ratio was preserved during isolation. Calcospherulites treated with ice-cold ethanol exhibited a Ca/P ratio of 1.6, suggesting the presence of some extractable phospholipids. Proteins extracted from isolated calcospherulites were resolved by SDS-PAGE into more than 20 distinct bands. Western blot analyses showed the presence of matrix proteins in these preparations. These results indicate that calcospherulites can be isolated from the mineralization front of bone in a form that can be used to study their proteome and lipid composition. Copyright (C) 2008 S. Karger AG, Basel

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