Mono, PhyllisPhyllisMonoHoffmann, RenéRenéHoffmannJöns, NielsNielsJönsKlügel, AndreasAndreasKlügelStevens, KevinKevinStevensBrachert, Thomas C.Thomas C.BrachertImmenhauser, Adrian MarkAdrian MarkImmenhauser2025-02-242025-02-242025https://publica.fraunhofer.de/handle/publica/48419810.1007/s10347-024-00697-8The sedimentary environment and mechanisms of formation of giant ooids (>2 mm) are not well understood. Here, we use petrographical, mineralogical and geochemical data of giant ooids from the Lower Triassic Buntsandstein Formation of central Germany to develop a coherent formation model. Structural preservation of calcite crystallites in ooid cortices in combination with comparatively low strontium concentrations (<545 μg/g) and the absence of dolomite in the cortex suggest a primary low-Mg calcite composition. Shale-normalised rare earth elements plus yttrium (REE+Y) patterns lack a pronounced heavy REE over light REE enrichment and show a positive cerium anomaly (Ce/Ce*SN =1.9-3.9). Together with a missing yttrium anomaly and low Y/Ho ratios (<40), these data are largely consistent with ooid formation in a lacustrine environment. Positive cerium and lanthanum anomalies further point to formation and deposition in an alkaline to hypersaline playa-lake environment. Based on our fndings, a fve-stage formation model is proposed. We suggest nucleus formation by microbial spheres, followed by calcite crystal nucleation on bioflm templates at the sediment–water interface, and crystal/cortex growth inside the sediment pile. The spherical ooid form is achieved by wave-induced physical rolling motion after exhumation. Ooid growth ceases when the ooid reaches a critical size (here 4 mm), depending on local hydrodynamic properties. Inhomogeneous crystal growth and the inclusion of exogenous particles lead to structural and geochemical anomalies in the ooid cortex. Results presented here have far-reaching implications for the application of REE and other trace elements as environmental proxies in ancient carbonates.enGiant ooid formationLower TriassicCarbonate microstructuresCarbonate diagenesisCathodoluminescence microscopyLA-ICP-MSjournal article