Abstract

This chapter reviews hypocalcaemia and other abnormalities of mineral homeostasis during the neonatal period. It describes three types of neonatal hypocalcaemia based on their time of occurrence in life: early neonatal hypocalcaemia, late neonatal hypocalcaemia, and demineralization and late-late hypocalcaemia. Early neonatal hypocalcaemia is prevalent in premature infants, infants of diabetic mothers, and asphyxiated infants. An exaggeration of the calcitonin surge probably plays a major role in premature and asphyxiated infants, while the infants of diabetic mothers and premature infants may have a prolonged functional hypoparathyroidism. Late neonatal hypocalcaemia occurs in full-term, otherwise healthy infants and is most common in vitamin D-deficient populations. It is much less frequent than early neonatal hypocalcaemia; however, the infants are usually symptomatic often with seizures and the entity always requires treatment with additional calcium and often magnesium supplementation and/or phosphate restriction. Late-late neonatal hypocalcaemia is seen in very premature infants and is associated with severe osteopenia or rickets. Its etiology appears to be a combination of calcium and phosphorus deficiency and an effective vitamin D metabolite deficiency. Both high calcium-high phosphorus formulae and 25-hydroxycholecalciferol to normalize serum 25-hydroxyvitamin D (25-OHD) have improved mineralization and decreased hypocalcaemia. Severe demineralization occurs most frequently when a phosphorus deficiency is superimposed on 25-OHD deficiency. Human milk per se , when fed to the very small premature infant, often produces classical phosphate deficiency rickets.

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