RESUMO
Mesocestoides corti (syn. vogae), similar to many other cestode platyhelminthes, contains abundant calcium carbonate structures called calcareous corpuscles. These concretions that may constitute as much as 40% of the dry weight of the body, and were proposed to form intracellularly in certain parenchymal cells. As an approach to elucidate the biological role of calcareous corpuscles in cestodes, our aim was to characterize more precisely the structure and topological composition of the corpuscles from M. corti. Employing a variety of high resolution technical approaches, we found that the calcareous corpuscles are spheroid or ovoid layered concretions. They are formed by topographically homogeneous but compositionally heterogeneous layers, suggesting a cyclic process of biomineralization. The layers are composite structures, with granules of tens of nanometers, each surrounded by a cortex of about eight nanometers.
Assuntos
Carbonato de Cálcio , Mesocestoides/anatomia & histologia , Animais , Microscopia de Força Atômica , Microscopia Eletrônica de VarreduraRESUMO
Mesocestoides corti (syn. vogae), as many other cestode platyhelminthes, contains abundant mineralized structures called calcareous corpuscles. These concretions may constitute as much as 40% of the dry weight of the organisms, but their function remains poorly understood. In this work, we reviewed the mineral composition of the calcareous corpuscles of M. corti. X-ray diffraction pattern showed that the major mineral component of the corpuscles is a hydrated form of calcium carbonate, monohydrocalcite, also confirmed by infrared spectrometry. The baseline shift of the X-ray diffraction spectra suggested the presence of amorphous calcium carbonate, accordingly to previous reports, and an organic matrix was confirmed by FTIR. Monohydrocalcite is a rare mineral unusually found in biominerals. Although the significance of monohydrocalcite in biominerals has not been determined, the knowledge of corpuscles composition is of relevance to establish their function and for the elucidation of the mechanisms involved in mineralization processes.