Fig. 8From: Geologic evidence for coseismic uplift at ~ AD 400 in coastal lowland deposits on the Shimizu Plain, central JapanStratigraphic distributions of the dominant species of mollusk fossils, total sulfur content (TS), ratio of total organic carbon to TS (i.e., the C/S ratio), and foraminifera in cored deposits at sites 1 and 2. See Fig. 5 for legendBack to article page