Nanoscale chemical tomography reveals organic and inorganic clusters in fossilised dinosaur tooth

Mineralized dental tissues are formed through biomineralization processes involving the growth and self-organisation of hydroxylapatite (HAP) nanoscale grains. There remain open questions regarding the way elements such as Mg or Na are incorporated in the organic matter between HAP grains or within the grain structure where they influence the nucleation and growth of HAP. Here, mapping the enamel structure and composition of a well-preserved ca. 150-million-year-old Giraffatitan brancai sauropod dinosaur tooth from millimeters down to the near-atomic scale, we reveal the nanoscale accumulation of Mg at HAP grain boundaries, alongside F arising from diagenesis. Within the HAP grains and at HAP grain boundaries organic matter forms clusters that we propose contribute to the fast growth rate of the tooth. Moreover, unexpected Cu3As particles are found across the entire enamel structure. These elements are not in the dentine, that exhibits empty tubules, which suggests that they were integrated during the tooth growth itself. Our multiscale analysis provides new information encouraging to reconsider aspects of the biomineralization and fossilization processes.