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dc.contributor.authorGoswami, S.C.
dc.date.accessioned1995-05-11T10:00:56Z
dc.date.accessioned2017-09-29T13:48:38Z
dc.date.available1995-05-11T10:00:56Z
dc.date.available2017-09-29T13:48:38Z
dc.date.issued1983
dc.identifier.citationIndian Journal of Marine Sciences, vol.12; 1983; 118-119
dc.identifier.issn0379-5136
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6584
dc.description.abstractZooplankton in an abnormally high sea surface temperature (33.1 to 33.8 degrees C) and alternate bands of slick formation were studied in the Eastern Arabian Sea during 26 and 29 April 1981. The phenomenon which may be due to intense diurnal heating and internal waves may cause zooplankton abundance. Average biomass values in high sea surface temperature areas were higher (0.30 ml.m/3) than at the other stations (0.07 ml.m/3). Crustacean eggs, fish eggs and mysids clustered in pockets of abnormally high sea surface temperature areas
dc.languageen
dc.publisherCSIR-NISCAIR
dc.relation.ispartofIndian J Mar Sci
dc.relation.isreferencedbySCI
dc.subjectAquatic Communities
dc.subject.othersurface temperature
dc.subject.otherabundance
dc.subject.othergeographical distribution
dc.subject.otherzooplankton
dc.subject.otherISW, Arabian Sea
dc.titleZooplankton incidence in abnormally high sea surface temperature in the Eastern Arabian Sea
dc.typeJournal Article


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