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dc.contributor.authorNigam, R.
dc.date.accessioned2009-05-06T10:47:11Z
dc.date.available2009-05-06T10:47:11Z
dc.date.issued1993
dc.identifier.citationCurrent Science, Vol.64(11-12); 935-937p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2857
dc.description.abstractThe 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
dc.language.isoen
dc.publisherCurrent Science Association, Bangalore, India
dc.rightsCopyright [1993]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectpalaeoclimatology
dc.subjectclimatic changes
dc.subjectmonsoons
dc.subjectatmospheric precipitations
dc.subjectforaminifera
dc.titleForaminifera and changing pattern of monsoon rainfall
dc.typeJournal Article


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