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dc.contributor.authorNigam, R.
dc.contributor.authorHashimi, N.H.
dc.contributor.authorMenezes, E.T.
dc.contributor.authorWagh, A.B.
dc.date.accessioned2009-05-08T11:56:19Z
dc.date.available2009-05-08T11:56:19Z
dc.date.issued1992
dc.identifier.citationCurrent Science, Vol.62; 309-311p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/3038
dc.description.abstractA 26.5-metre-long core collected from the outer-shelf area off Bombay (India) at 75 m water depth showed ooids and shallow-water benthic foraminifera all along the core. The presence of these well-known indicators of shallow-water environment of deposition shows that sea level had transgressed considerably prior to 10,000 years before present (super(14) C age of the surface sediment). By comparison with global events, we infer that the sea level was at 101.5 m below the present level at about 14,500 years BP. We further observe that this rise occurred with two minor pauses (or minor reversals) at 13,000 and 11,500 years BP
dc.language.isoen
dc.publisherCurrent Science Association, Bangalore, India
dc.rightsCopyright [1992]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.titleFluctuating sea levels off Bombay (India) between 14,500 and 10,000 years before present
dc.typeJournal Article


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