Electron spectroscopic imaging, a new technique that permits the quantitative detection of the spatial distributions of atomic elements at high resolution, has been applied to the epiphyseal zone of hypertrophy in the mouse for the visualization of calcium, phosphorus, and sulfur. Longitudinally sectioned epiphyseal growth plates reveal a developmental sequence in the longitudinal septum leading from a noncalcified matrix to a calcified matrix. During the early stages of this transition, matrix granules containing highly localized concentrations of P (200-400 atoms/nm2) are found spatially separate from Ca-containing sites.These Ca localizations displayed a concentration range of 20-350 atoms/nm2 and a complete spatial overlap with sulfur. At these sites, S levels range from 10 to 200 atoms/nm2. At a later stage, and therefore more proximal to the zone of provisional calcification, the usual scattered, irregularly shaped mineral deposits are found. These sites contain a virtual superposition of Ca with both P and S. The Ca/P and Ca/S ratios of these mineral deposits are predominantly 1.0 with only minor, locally varying ratios present.A fundamcntal problem in the study of calcifying tissues is the identification and characterization of the site of initial mineralization-the nucleation site. The organic matrices of cartilage, bone, and dentin possess common structural components although organized in different characteristic fashions. From ultrastructural and biochemical studies, various components of these calcifying matrices and their parenchyma have been implicated in the role of nucleation-e.g., collagen fibers (1), matrix vesicles (2-4), mitochondria (5), y-carboxyglutamic acid (6), lipids, and Ca-phospholipid-PO4 complexes (7,8). Of these components, various ones may interact in concert to initiate nucleation or to control it in some way. However, the exact mechanism of matrix-mediated mineralization remains controversial.In order to assist conventional microscopic imaging of the dynamic events of calcification, many techniques have been used: pyroantimonate staining for Ca (9, 10), electron probe x-ray microanalysis for detection of elements (2, 11), cationic dyes for staining proteoglycans (12), specific immunofluorescence to localize both monomer core protein and link proteins of proteoglycans (13), and ultracryomicrotomy for the increased preservation of matrix ground substance (2,14). These techniques have helped greatly in establishing the present state of knowledge. However, the techniques have limited the definition of a nucleation site to a Ca-containing mineral deposit with thousands of Ca atoms.In the work reported here, a new technique known as electron spectroscopic imaging was used to study the quantitative distribution of Ca, P, and S in the epiphyseal growth plate. This technique enables the direct visualization of elements in entire images with a spatial resolution as fine as 0.3-0.5 nm and with a minimum detection level as low as 2 X 10-21 g (or 50 atoms for P) (15, 16). Compared ...