Protein bodies in seeds are important for seedling growth because they provide necessary nitrogenous compounds. It is often overlooked that protein bodies also function as the subcellular location of much of a seed's reserves of macronutrients such as P, K, Ca, and Mg. Structural investigations of storage tissue from several cucurbit seeds have revealed that protein bodies often consist of proteinaceous matrix, protein crystalloid, soft globoid, and globoid crystal regions (2, 8, 9). The protein reserves are thought to be located primarily in the proteinaceous matrix and protein crystalloid regions. The mineral reserves usually occur in the electron-dense globoid crystals and are generally considered to be largely phytin, a cation (K, Mg, Ca) salt of inositol hexaphosphoric acid (3,4,(11)(12)(13).Recently, Lott et al. (7) published results of an energy-dispersive x-ray analysis study of globoid crystal composition in 10 different regions of Cucurbita maxima embryos. Although P, K, and Mg were commonly found in globoid crystals in all squash embryo regions, the Ca distribution showed definite differences between embryo regions. Ca was common in globoid crystals of the radicle and stem regions. In the cotyledon, Ca levels were on average much lower than those of the root-shoot regions. Most globoid crystals from spongy or palisade mesophyll cells lacked any detectable Ca. The bulk of the Ca values for the cotyledon samples thus came from a fraction of the globoid crystals present. In this paper we report the results of EDX2 analysis studies designed to discover where globoid crystals with relatively high Ca levels are located within Cucurbita cotyledons.