Tidal facies in the Upper Silurian Oved-Ramsasa Group of Scania, Sweden: Linkages of radial and cerebroid ooids and evaporite tracers to subtidal, lagoonal environment
A sequence in the Upper Silurian Oved-Ramsasa Group in Scania, Sweden has been investigated sedimentologically and geochemically. This sequence represents a regressive marine succession. The sedimentary structures and the rapid vertical changes in lithologies and the lateral variability of beds indicate a tide-dominated sedimentation in a shallow epeiric sea, where even small oscillations in sea w