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    Foraminifera and changing pattern of monsoon rainfall 

    Nigam, R. (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 ...
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    Significance of correspondence between river discharge and proloculus size of benthic foraminifera in paleomonsoonal studies 

    Nigam, R.; Khare, N. (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 ...
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    Signals of the change in monsoonal precipitation at around 2,000 years BP in a sediment core off central west coast of India 

    Nigam, R.; Khare, N. (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 ...

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    Nigam, R. (3)
    Khare, N. (2)Subjectforaminifera (3)
    monsoons (3)
    atmospheric precipitations (2)climatic changes (2)benthos (1)ISW, India, Karnataka, Karwar (1)Oceanography and Limnology (1)palaeo studies (1)palaeoclimate (1)palaeoclimatology (1)... View MoreDate Issued1993 (1)1994 (1)1995 (1)Has File(s)Yes (3)

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