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dc.contributor.authorNigam, R.
dc.contributor.authorKhare, N.
dc.date.accessioned1994-03-16T10:06:25Z
dc.date.accessioned2017-09-30T01:56:26Z
dc.date.available1994-03-16T10:06:25Z
dc.date.available2017-09-30T01:56:26Z
dc.date.issued1994
dc.identifier.citationCurrent Science, vol.66(3); 1994; 226-229
dc.identifier.issn0011-3891
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7430
dc.description.abstractA 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 which represents the last 4,500 years approximately (@u14@@C dates) revealed the evidences of a significant change in the intensity of the precipitation around 2,000 years BP
dc.languageen
dc.publisherCurrent Science Association
dc.relation.ispartofCurr Sci India
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.otherpalaeoclimate
dc.subject.othermonsoons
dc.subject.otherclimatic changes
dc.subject.otheratmospheric precipitations
dc.subject.otherforaminifera
dc.subject.otherISW, India, Karnataka, Karwar
dc.titleSignals of the change in monsoonal precipitation at around 2,000 years BP in a sediment core off central west coast of India
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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