Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38871
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dc.contributor.authorGoswami, S C-
dc.date.accessioned2016-12-19T08:54:18Z-
dc.date.available2016-12-19T08:54:18Z-
dc.date.issued1983-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38871-
dc.description118-119en_US
dc.description.abstractZooplankton in an abnormally high sea surface temperature (33.1 to 33.8 ᵒ 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.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.12(2) [June 1983]en_US
dc.titleZooplankton incidence in abnormally high sea surface temperature in the Eastern Arabian Seaen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.12(2) [June 1983]

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