Phytate, the main mineral nutrient storage compound in seeds, is stored inside protein bodies. Phytate is usually concentrated in dense bodies called globoid crystals. In 1985, Lott and co-workers proposed that the balance of (Mg + Ca):K may be important in controlling globoid crystal formation and provided some experimental evidence to support this proposal. To test this hypothesis further, developing Cucurbita fruits were injected with sterile K salt solutions. Squash cotyledons generally have large globoid crystals and a relatively high (Mg + Ca):K ratio. We hypothesized that experimental reduction of the ratio by the addition of K would result in the alteration of the size and number of globoid crystals. Developing seeds were remarkably resistant to attempts to alter the elements taken up for storage. The elemental content of embryo tissues was measured quantitatively with neutron activation analysis. Controls plus those few samples showing a distinct shift in the ratio owing to elevated K content were analyzed further. Energy dispersive X-ray analysis of cryogenically prepared samples was used to study the elemental content of globoid crystals and transmission electron microscopy was used to study the ultrastructure of the protein bodies. The results provide additional support for the hypothesis being tested. Key words: phytate, globoid crystals, Cucurbita, seeds, mineral nutrients, protein bodies.
Salinity-induced changes in the morphology and major mineral nutrient composition of purslane (Portulaca oleracea L.) accessions