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dc.contributor.authorGuptha, M.V.S.
dc.date.accessioned1995-05-06T09:57:13Z
dc.date.accessioned2017-09-29T13:48:44Z
dc.date.available1995-05-06T09:57:13Z
dc.date.available2017-09-29T13:48:44Z
dc.date.issued1981
dc.identifier.citationIndian Journal of Marine Sciences, vol.10; 1981; 293-295
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6731
dc.description.abstractSixteen sediment samples have been investigated for the distribution of nannoplankton. Of the total 38 species encountered, 14 are modern and remaining 24 are reworked fossils ranging in age from Eocene to Pliocene. Majority of the reworked fossils indicates that they are of Miocene age. Modern nannoplankton reveals their affinity to the tropical conditions. It is concluded that the source of reworked fossil may mainly be the outcrops of Miocene occuring on the Andaman Sea floor and in part from the turbidites resulting from deposition of the sediment transported by river Irrawaddy.
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.otherpliocene
dc.subject.otherecocene
dc.subject.otherfossils
dc.subject.othersediment transport
dc.subject.othernannoplankton
dc.subject.othersediment samples
dc.subject.otherEmiliania annula
dc.subject.otherISW, Andaman Sea
dc.titleNannoplankton from Recent Sediments off the Andaman Islands
dc.typeJournal Article
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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