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Foraminifera and changing pattern of monsoon rainfall
(Current Science Association, Bangalore, India, 1993)
The palaeomonsoonal history can be reconstructed utilizing climatically sensitive properties of marine microorganisms; foraminifera. The results show a major boundary at 3500 years B.P. and periods of rather low precipitation ...
Signals of the change in monsoonal precipitation at around 2,000 years BP in a sediment core off central west coast of India
(Current Science Association, 1994)
A 4.80 m long shallow water sediment core, collected from the inner shelf (at 22 m water depth) off Karwar near Kali River mouth is studied for foraminiferal tracers of palaeomonsoons. The climatic history of this core ...