Origin of spherulitic and cone-in-cone concretions in Cambro-Ordovician black shales, St Lawrence Estuary, Quebec, Canada. (4th June 2019)

• Record Type: Journal Article
• Authors: Hesse, Reinhard; Fong, Christopher; Schumann, Dirk
• Is Part Of: Geological magazine. Volume 156:Number 10(2019)
• Page Start: 1793
• Page End: 1804
• Publication Date: 2019-06-04
• Subjects: concretions, -- spherulites, -- cone-in-cone structure, -- fibrous calcite-quartzine intergrowth, -- diagenesis, -- Cambro-Ordovician, -- Quebec; Geology -- Periodicals; 551.05
• DOI: 10.1017/S0016756819000128
• Languages: English
• ISSNs: 0016-7568

Abstract

Abstract: Spherulitic concretions are very rare among carbonate concretions that generally consist of micritic carbonate. The occurrence of spherulitic concretions in Cambro-Ordovician black shales of unknown stratigraphic age on a mid-channel island in the St Lawrence Estuary in Quebec is a new example in addition to only three hitherto reported occurrences of spherulitic carbonate concretions. Their origin is still poorly understood. These concretions occur in close association with, and show various transitions to, cone-in-cone structure. The spherules, measuring 0.5 to 12 mm in diameter, consist of intergrown fine fibres of ferroan calcite and quartzine, pointing to the formation of the concretions below the sulfate-reduction zone. A phenomenological theory of spherulitic crystallization relates the thickness δ of an impurity-rich layer in front of impurity-rejecting growing crystals to the impurity-diffusion coefficient D and the growth velocity G of the crystal by δ = D/G. In spherulite-forming environments, extremely small values of δ (in the order of <10 −4 cm) in conjunction with cellulation lead to spherulitic fibre growth. The theory of spherulitic crystallization is here applied to sedimentary deposits for the first time. The intimate association of calcite and quartzine in the concretions requires a chemical change from alkaline to acidic conditions, which occurs below the carbonate-reduction zone owing to the dissolution of sponge spicules or radiolarians. The transition from spherulite to the silica-free cone-in-cone structure occurs when the silica reservoir that acted as an impurity is exhausted in the crystallization process.