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Elasmoid scales from the common carp (and other teleostean fishes) appear to be an exciting new model in the research of mineralized tissues. The presence of alkaline phosphatase (ALP), a marker of mineralization, on both sides of the scale was demonstrated by means of enzyme histochemistry. Tartrate-resistant acid phosphatase, a marker for mineral degradation and osteoclasts, was observed along the radii, at the same location as the ALP activity on the episquamal side. This points towards an active mineral metabolism, were scale cells are involved in both formation and degradation of the mineralized matrix. Cathepsin K staining revealed the presence of multinuclear osteoclasts along the grooves of the scale. Interestingly, the scales were taken from growing control fish; they were not induced to resorb their matrix. Presence of these enzymes in scale cells, together with the demineralized regions in the centre of the scale suggest a more dynamic mineral metabolism in cyprinid scales then previously observed in other species. Scales are derived from odontode tissues, their formation relies on many the same underlying mechanisms and genes as other mineralized tissues. Moreover, a single scale offers the possibility to culture scale-forming and -degrading cells together on their original matrix. All of the these unique properties substantiate the potential of scales to yield new insights on osteoclasts and regulation of tissue mineralization. [ABSTRACT FROM AUTHOR]