Abstract
Waulsortian buildups are dominated by lime mud, and conspicuously lack frame-building organisms such as corals, calcareous algae and stromatoporoids. They were first described by Dupont (1863) from the Dinantian (Lower Carboniferous) of the Waulsort area in Belgium. Dupont had already described certain sparry masses (“Stromatactis”) from Devonian mud mounds as stromatoporoids. In 1883, he recognized similar structures in the Waulsortian limestones, and considered these massive buildups to be reefs of stromatoporoids and fenestellid bryozoans. Nowadays, the sparry fabrics are considered to be diagenetic features. Lacking a skeletal framework, Waulsortian buildups are best regarded as carbonate banks rather than true reefs (Lees 1964).
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Miller, J. (1986). Facies Relationships and Diagenesis in Waulsortian Mudmounds from the Lower Carboniferous of Ireland and N. England. In: Schroeder, J.H., Purser, B.H. (eds) Reef Diagenesis. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-82812-6_16
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DOI: https://doi.org/10.1007/978-3-642-82812-6_16
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