Signals of the change in monsoonal precipitation at around 2,000 years BP in a sediment core off central west coast of India

dc.contributor.author	Nigam, R.
dc.contributor.author	Khare, N.
dc.date.accessioned	1994-03-16T10:06:25Z
dc.date.accessioned	2017-09-30T01:56:26Z
dc.date.available	1994-03-16T10:06:25Z
dc.date.available	2017-09-30T01:56:26Z
dc.date.issued	1994
dc.identifier.citation	Current Science, vol.66(3); 1994; 226-229
dc.identifier.issn	0011-3891
dc.identifier.uri	http://drs.nio.org/drs/handle/2264/7430
dc.description.abstract	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 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.language	en
dc.publisher	Current Science Association
dc.relation.ispartof	Curr Sci India
dc.relation.isreferencedby	SCI
dc.subject	Oceanography and Limnology
dc.subject.other	palaeoclimate
dc.subject.other	monsoons
dc.subject.other	climatic changes
dc.subject.other	atmospheric precipitations
dc.subject.other	foraminifera
dc.subject.other	ISW, India, Karnataka, Karwar
dc.title	Signals of the change in monsoonal precipitation at around 2,000 years BP in a sediment core off central west coast of India
dc.type	Journal Article
dc.affiliation.author	CSIR-National Institute of Oceanography, Dona Paula, Goa, India