Planktonic foraminifera from a quaternary deep sea core from the southern Arabian Sea

dc.contributor.author	Naidu, P.D.
dc.contributor.author	Rao, P.S.
dc.contributor.author	Pattan, J.N.
dc.date.accessioned	1997-12-01T10:01:55Z
dc.date.accessioned	2017-09-30T01:29:58Z
dc.date.available	1997-12-01T10:01:55Z
dc.date.available	2017-09-30T01:29:58Z
dc.date.issued	1989
dc.identifier.citation	Journal of the Geological Society of India, vol.34(4); 1989; 393-397
dc.identifier.issn	0016-7622
dc.identifier.uri	http://drs.nio.org/drs/handle/2264/7262
dc.description.abstract	An investigation on planktonic foraminifera and calcium carbonate content of a box core collected at a depth of 2556 m from the southern part of the Arabian sea indicates faunal changes depicting Quaternary climatic fluctuations. Based on the study the Last Glacial maxima (LGM) boundary is placed at65 cm and below LGM. Three warm and two cold episodes are identified
dc.language	en
dc.publisher	Geological Society of India
dc.relation.ispartof	J Geol Soc India
dc.relation.isreferencedby	SCI
dc.subject	Geology and Geophysics
dc.subject.other	plankton
dc.subject.other	foraminifera
dc.subject.other	cores
dc.subject.other	quaternary
dc.subject.other	calcium carbonates
dc.subject.other	palaeoclimatology
dc.subject.other	ISW, Andaman Sea
dc.title	Planktonic foraminifera from a quaternary deep sea core from the southern Arabian Sea
dc.type	Journal Article
dc.affiliation.author	CSIR-National Institute of Oceanography, Dona Paula, Goa, India