Abstract

Evidence is presented in support of the hypothesis that the reappearance of spawning Atlantic herring (Clupea harengus) on Aberdeen Bank in 1983, after an absence of 16 years, was related to an increased Atlantic inflow in the area. Two Atlantic copepod species, Metridia lucens and Candacia armata, showed a simultaneous increase in the years when spawning herring returned to Aberdeen Bank. During the late 1960s, both species declined at the time when the spawning population on Aberdeen Bank disappeared. Earlier work has demonstrated that an increased Atlantic inflow results in a southward displacement of plankton concentrations and feeding herring in the northwestern North Sea. I hypothesize that such a southern distribution of the herring stock, caused indirectly by the increased Atlantic inflow, influenced recruit spawners to choose the nearby Aberdeen Bank as their spawning ground in 1983. Fluctuations of the spawning populations in the northern North Sea during earlier decades are explained by switches of recruitment between the northern and southern population, as a result of variations in latitudinal distribution of the recruiting year-class.

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