Dissolution of granules in the Malpighian tubules of Musca autumnalis degeer, during mineralization of the puparium

Abstract The dissolution of mineralized granules stored in the larval Malpighian tubules of the face fly, Musca autumnalis DeGeer, was studied both in situ and with isolated granules in vitro . The release of calcium, phosphorus, and magnesium from granules increased exponentially as the pH of the bathing medium was decreased. The pH measured in the distal region of the Malpighian tubules was 8.08 while that of the proximal region was 7.35. Thus, the decrease in pH of lumen contents from distal to proximal regions of the tubules appears to be a major effector of granule dissolution. Loss of structural integrity of the granules accompanied mineral release and also increased as pH of the bathing medium was lowered in vitro . This structural disintegration was similar to that observed in naturally dissolving granules isolated from the proximal region of the Malpighian tubules. The larval tubules, therefore, appear to have regional specialization in that granules are formed and stored in the distal lumen and dissolution takes place as granules move into the more acidic proximal region. No granules were found in the larval hindgut contents also indicating that dissolution and transport take place in the proximal region of the tubules. However, granules of similar composition were found in the meconium and in the most distal regions of adult Malpighian tubules.