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dc.contributor.authorSetty, M.G.A.P.
dc.contributor.authorAmbre, N.V.
dc.date.accessioned2002-08-08T09:56:34Z
dc.date.accessioned2017-09-29T13:47:16Z
dc.date.available2002-08-08T09:56:34Z
dc.date.available2017-09-29T13:47:16Z
dc.date.issued1973
dc.identifier.citationRecent researches in geology, Vol. 9. Delhi:Hindustan Pub. Co; 1973; 349-356
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/5773
dc.description.abstractThe organic carbon/matter distribution pattern in the shallow restricted marine environment of the Gulf indicates very low values but it is found to rise as the particle size of the sediment decreases; however it appears to be erratic. The foraminiferal number (TFN) and the species diversity (TSN) seem to fluctuate with the variation in the sediment pattern. It is highest in the fine clays chiefly with embryonic or meiofaunal in size, thin-walled and hyaline, whereas it is large, thick-walled, and also porcellaneous in silts and sands. The agglutinated species being uncommon, the planktonic forms are characteristically rare. The relationship between organic carbon content, the substrate, and the number of foreminifers is not consistent at all stations, since organic carbon percentages are very low to monitor the sharp changes
dc.languageen
dc.publisherDelhi: Hindustan Pub. Co
dc.relation.isreferencedbyNON-SCI
dc.titleOrganic carbon pattern and foraminiferal assemblage in the sediments of Gulf of Kutch
dc.typeBook Chapter
dc.affiliation.authorCSIR-National Institute of Oceanography, Dona Paula, Goa, India


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