Climate influenced deposition on a low latitude Sheinwoodian carbonate ramp, Gotland, Sweden
The Sheinwoodian succession of Gotland comprises the Högklint, Tofta and Hangvar Formations and most of the Slite Group. The succession consists of hierarchically ordered shallow marine depositional cycles, produced by orbitally forced climate changes. During warmer and wetter intervals (climate maxima) more carbonate was produced than during the cooler and dryer climate minima. Higher carbonate p
