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dc.contributor.authorBorole, D.V.
dc.contributor.authorRao, K.K.
dc.contributor.authorKrishnamurthy, R.V.
dc.contributor.authorSomayajulu, B.L.K.
dc.date.accessioned1995-06-17T10:00:55Z
dc.date.accessioned2017-09-29T13:48:40Z
dc.date.available1995-06-17T10:00:55Z
dc.date.available2017-09-29T13:48:40Z
dc.date.issued1982
dc.identifier.citationQuaternary�Research, vol.18; 1982; 236-239
dc.identifier.issn0033-5894
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6628
dc.description.abstractCarbonate 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.languageen
dc.publisherElsevier
dc.relation.ispartofQuaternary Res
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.othergeochronometry
dc.subject.otherforaminifera
dc.subject.othermicroorganisms
dc.subject.otherpalaeoenvironments
dc.subject.otherquaternary
dc.subject.otherISW, Arabian Sea
dc.titleLate Quaternary faunal change in coastal Arabian sea sediments
dc.typeJournal Article


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