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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 ...
Significance of correspondence between river discharge and proloculus size of benthic foraminifera in paleomonsoonal studies
(Springer, 1995)
Variations in the mean proloculus size (MPS) of the benthic foraminiferal species Rotalidium annectens were studied in a core collected off Karwar (20 m water depth), on the west coast of India. Comparison of downcore ...
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 ...