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dc.contributor.authorGuptha, M.V.S.
dc.date.accessioned1995-05-12T10:00:56Z
dc.date.accessioned2017-09-29T13:48:36Z
dc.date.available1995-05-12T10:00:56Z
dc.date.available2017-09-29T13:48:36Z
dc.date.issued1983
dc.identifier.citationJournal of the Geological Society of India, vol.24; 1983; 468-475
dc.identifier.issn0016-7622
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6541
dc.description.abstractA deep sea core RC9-156 collected in the Arabian Sea at a water depth of 4583 m was analysed for calcareous nannoplankton and dissolution studies. Twelve species of nannoplankton were identified and based on the assemblage, it is suggested that the age of the sediment is late Quaternary. The alternate fossiliferous and unfossiliferous bands encountered in the core is attributed to the fluctuations in the rate of sedimentation by the river Indus during glacial and interglacial periods
dc.languageen
dc.publisherGeological Society of India
dc.relation.ispartofJ Geol Soc India
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.othercorrelation analysis
dc.subject.otherglaciation
dc.subject.othersedimentation
dc.subject.otherquaternary
dc.subject.othersediments
dc.subject.otherplankton
dc.subject.othercores
dc.subject.otherdeep-sea drilling
dc.subject.otherISW, Arabian Sea
dc.titleNannoplankton from RC9-156 in the southeastern Arabian Sea
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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