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Please use this identifier to cite or link to this item: http://hdl.handle.net/1956/412

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contributor.authorReid, P. C.en_US
contributor.authorEdwards, M.en_US
contributor.authorBeaugrand, G.en_US
contributor.authorSkogen, M.en_US
contributor.authorStevens, D.en_US
date.accessioned2004-07-30T09:29:38Zen_US
date.accessioned2004-08-03T12:57:52Zen_US
date.accessioned2004-08-26T11:58:40Z-
date.available2004-07-30T09:29:38Zen_US
date.available2004-08-03T12:57:52Zen_US
date.available2004-08-26T11:58:40Z-
date.issued2003en_US
identifier.issn1054-6006en_US
identifier.urihttp://hdl.handle.net/1956/412-
description.abstractOceanic inflow is estimated to contribute more than 90% of the nutrient input into the North Sea. Variability in the volume, chemical properties, biological content and source of the inflowing water is thus likely to have a considerable effect on North Sea ecosystems. Changes seen in the plankton, and in particularen_US
format.extent433173 bytesen_US
format.extent166 bytesen_US
format.extent433173 bytesen_US
format.extent42720 bytes-
format.extent433173 bytes-
format.extent166 bytes-
format.mimetypeapplication/pdfen_US
format.mimetypetext/plainen_US
format.mimetypeapplication/pdfen_US
format.mimetypetext/plain-
format.mimetypeapplication/pdf-
format.mimetypetext/plain-
language.isoenen_US
publisherBlackwell Publishing-
relation.ispartofseriesFisheries Oceanography; 12(4/5)en_US
titlePeriodic changes in the zooplankton of the North Sea during the twentieth century linked to oceanic inflowen_US
typeArticleen_US
Appears in Collections:Eprints by the Bjerknes Centre for Climate Research (BCCR)

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