1984
DOI: 10.1093/icesjms/41.3.304
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Continuous Plankton Records: a possible reversal in the downward trend in the abundance of the plankton of the North Sea and the Northeast Atlantic

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Cited by 35 publications
(8 citation statements)
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“…We suggest a possible explanation for the downward trend in shark catches at Achill Island was that progressively fewer basking sharks occurred there between 1956 and 75 because fewer copepods occurred near the surface off west Ireland over the same period. A long‐term decline in zooplankton abundance in the north‐east Atlantic between 1950 and 1980 has been documented (Colebrook et al ., 1984). Therefore, the decline in basking sharks observed at Achill Island could be the result of a distributional shift of sharks to more productive areas rather than a population response to over‐exploitation.…”
Section: Discussionmentioning
confidence: 99%
“…We suggest a possible explanation for the downward trend in shark catches at Achill Island was that progressively fewer basking sharks occurred there between 1956 and 75 because fewer copepods occurred near the surface off west Ireland over the same period. A long‐term decline in zooplankton abundance in the north‐east Atlantic between 1950 and 1980 has been documented (Colebrook et al ., 1984). Therefore, the decline in basking sharks observed at Achill Island could be the result of a distributional shift of sharks to more productive areas rather than a population response to over‐exploitation.…”
Section: Discussionmentioning
confidence: 99%
“…Further, Heath & al. (1999) compared model results and observations in the field of the abundance and distribution of C. finm arch icus in the North Sea and concluded that advection of spawning individuals from the Norwegian Sea Deep Water, mainly via the Norwegian Trench, is an important source for replenishing the stock of C. finmarchicus and long-term changes in this current might be one of the important ~ it Sundby -Recruitment of Atlantic cod stocks 289 causes of the similar long-term changes observed in the abundance of C. finmarchicus in the North Sea (Colebrook & al. 1984).…”
Section: The Influence Of Temperature and Advection On Zooplankton Abmentioning
confidence: 99%
“…Trends have been detected in the prevalence of northerly winds (Dickson et al, 1988a), westerly winds (Aebischer et al, 1990;Corten, 1986;Turrell, 1992), windstress and winter cooling (Svendsen and Magnusson, 1992). The Continuous Plankton Recorder data show medium to long-term changes in the abundance of phytoplankton and zooplankton (Colebrook et al, 1984;Lindley et al, 1995).…”
Section: Possible Causesmentioning
confidence: 99%