DISTRIBUTION, MIGRATION AND ABUNDANCE OF NORWEGIAN SPRING SPAWNING HERRING IN RELATION TO THE TEMPERATURE AND ZOOPLANKTON BIOMASS IN THE NORWEGIAN SEA AS RECORDED BY COORDINATED SURVEYS IN SPRING AND SUMMER 1996

Citation
Oa. Misund et al., DISTRIBUTION, MIGRATION AND ABUNDANCE OF NORWEGIAN SPRING SPAWNING HERRING IN RELATION TO THE TEMPERATURE AND ZOOPLANKTON BIOMASS IN THE NORWEGIAN SEA AS RECORDED BY COORDINATED SURVEYS IN SPRING AND SUMMER 1996, Sarsia, 83(2), 1998, pp. 117-127
Citations number
16
Categorie Soggetti
Ecology,"Marine & Freshwater Biology
Journal title
SarsiaACNP
ISSN journal
00364827
Volume
83
Issue
2
Year of publication
1998
Pages
117 - 127
Database
ISI
SICI code
0036-4827(1998)83:2<117:DMAAON>2.0.ZU;2-V
Abstract
The distribution and migration of Norwegian spring spawning herring (C lupea harengus) in the Norwegian Sea in spring and summer 1996 were ma pped during 13 coordinated surveys carried out by Faroese, Icelandic, Norwegian and Russian research vessels. After spawning at the banks of the Norwegian Coast in February-March, most of the spent herring migr ated out in the Norwegian Sea through a corridor between 67 degrees N and 68 degrees N. In May, 4 and 5 year old herring, which form the you nger part of the spawning stock, were distributed in small schools or scattered layers at 25-100 m depth over large areas of the central Nor wegian Sea. Older and larger herring formed large schools, generally a t 250-400 m depth near the cold front along the eastern part of the Ic elandic Exclusive Economic Zone (EEZ). The total abundance of herring in the Norwegian Sea was estimated to be about 47 billion individuals or about 8 million tonnes. In June, the older and larger herring had m igrated northwards into the Jan Mayen zone, while the younger herring remained in the southern and central Norwegian Sea. In July, the young er herring had migrated back to the area off Vesteralen, northern Norw ay. In July/August, the larger herring were found in small schools nea r the surface in the northern Norwegian Sea. Relationships between the temperature distribution, zooplankton abundance and herring distribut ion and migration are considered. In May, the lowest zooplankton bioma ss was observed in the central and southern Norwegian Sea. At that tim e, there were high zooplankton concentrations in the westernmost part of the Norwegian Sea, within the domain of the East Icelandic Current. The herring did not enter this body of cold water with temperatures o f 1-2 degrees C in the uppermost 300 m, but migrated to the north and north-east in search of food.