Fig. 5From: Two times lowering of lake water at around 48 and 38 ka, caused by possible earthquakes, recorded in the Paleo-Kathmandu lake, central Nepal HimalayaPhotomicrograph of micro-fossils obtained from cores of the lacustrine Kalimati Formation. a charcoal grain, b sponge spicule, c Pediastrum, d phytoliths and diatom. Arrow shows Bambusoideae. A scale bar is 100 μmBack to article page