Late Quaternary Faunal Change in Coastal Arabian sea Sediments

dc.contributor.author	Borole, D.V.
dc.contributor.author	Rao, K.K.
dc.contributor.author	Krishnamurthy, R.V.
dc.contributor.author	Somayajulu, B.L.K.
dc.date.accessioned	1995-06-17T10:00:55Z
dc.date.accessioned	2017-09-29T13:48:40Z
dc.date.available	1995-06-17T10:00:55Z
dc.date.available	2017-09-29T13:48:40Z
dc.date.issued	1982
dc.identifier.citation	Quaternary Research, vol.18; 1982; 236-239
dc.identifier.issn	0033-5894
dc.identifier.uri	http://drs.nio.org/drs/handle/2264/6628
dc.description.abstract	Carbonate content and faunal composition of two gravity cores from the coastal Arabian Sea provide evidence of a major environmental change in surface ocean waters about 13,000 yr B.P. Radiocarbon dating indicates that deposition rates ranged from 1.8 to 9.8 cm/103 yr, with a major change in rate occurring in one core at about 7500 yr B.P.
dc.language	en
dc.publisher	Elsevier
dc.relation.ispartof	Quaternary Res
dc.relation.isreferencedby	SCI
dc.subject	Oceanography and Limnology
dc.subject.other	geochronometry
dc.subject.other	foraminifera
dc.subject.other	microorganisms
dc.subject.other	palaeoenvironments
dc.subject.other	quaternary
dc.subject.other	ISW, Arabian Sea
dc.title	Late Quaternary Faunal Change in Coastal Arabian sea Sediments
dc.type	Journal Article