Growth of ferruginous oncoliths in the Bajocian (Middle Jurassic) of Europe

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Abstract
Limonitic oncoliths from the Bajocian of Europe, widely known as ‘snuff‐boxes’, grew by accretion of bundles of laminae on one side, followed by overturning and accretion of laminae on the other side. A diverse hard‐substrate encrusting fauna grew interleaved with the ferruginous laminations. The palaeoecological preferences of this fauna indicate that its growth, and hence the accumulation of the laminations, took place on the gloomy undersides of the oncoliths. This upsidedown growth is supported by characteristics of the lamination bundles themselves, and by the predominant present‐day orientations of the snuff‐boxes. The abundance of the associated fauna and the lack of carbonate‐dissolving macroborers cutting the laminae suggest an original ferric composition. Precipitation was probably under the control of non‐photosynthetic microorganisms that inhabited the microenvironments represented by the oncoliths' lower surfaces.