Characteristics of bone surfaces are discussed in relation to the uptake of bone-seeking isotopes. The alkaline earths are concentrated behind the osteoid border of active surfaces. Yttrium, americium, and plutonium are concentrated on quiescent and resorbing surfaces; traces only occur in and beneath the osteoid border. In view of evidence of mucoproteins at sites where the latter elements are found in concentration, a separation of the mucoproteins in cortical bone was undertaken. Mucosubstances have been isolated which give the same reaction with certain reagents as the bone surfaces in question. One of these, a sialoprotein, might be expected, in view of its acidic nature, to be capable of metal binding.
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Herring et al. (1962) studied this question.
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