In: Journal of Paleolimnology, 1998, vol. 19, no. 1, p. 63-75
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In: Botanica Helvetica, 2005, vol. 115, no. 2, p. 137-154
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In: Geological Magazine, 2013, vol. 150, no. 5, p. 767-782
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In: Facies, 2007, vol. 53, no. 4, p. 535-552
Abundant lagoonal oncoids occur in the Late Oxfordian Hauptmumienbank Member of the Swiss Jura Mountains. Four oncoid types are observed in the studied sections and classified according to the oncoid surface morphology, the structure and composition of the cortex, and the texture and fauna of the encasing sediment. Micrite-dominated oncoids (types 1 and 2) have a smooth surface. Type 1 has a...
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