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    Foraminifera and changing pattern of monsoon rainfall

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    Curr_Sci_64_935.pdf (576.3Kb)
    Date
    1993
    Author
    Nigam, R.
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    Abstract
    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 approximately at 420, 910 and 1680 years B.P. during the last 2000 years. A prominent association has also been observed between cyclicity (approx 77 years) in dry periods of monsoonal precipitation and Gleissberg cycle
    URI
    http://drs.nio.org/drs/handle/2264/2857
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