Interannual abundance patterns of copepods during an ENSO event in Icy Strait, southeastern Alaska

Abstract Interannual copepod abundance (number m−3) and sea surface temperatures (SST, 2-m depth) were examined from four stations in Icy Strait, southeastern Alaska, monthly from May to September, 1997–2002. SST was generally lowest in May (≅7°C), increased rapidly to a summer peak (≅12°C), and dec...

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Bibliographic Details
Published in:ICES Journal of Marine Science
Main Authors: Park, Wongyu, Sturdevant, Molly, Orsi, Joseph, Wertheimer, Alex, Fergusson, Emily, Heard, William, Shirley, Thomas
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2004
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Online Access:http://dx.doi.org/10.1016/j.icesjms.2004.03.017
http://academic.oup.com/icesjms/article-pdf/61/4/464/29122056/61-4-464.pdf
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Summary:Abstract Interannual copepod abundance (number m−3) and sea surface temperatures (SST, 2-m depth) were examined from four stations in Icy Strait, southeastern Alaska, monthly from May to September, 1997–2002. SST was generally lowest in May (≅7°C), increased rapidly to a summer peak (≅12°C), and declined again by September. SST was relatively high in the El Niño year, 1998, and was low during a regional cold event, 2002, compared to other years. Overall, copepods constituted 18.8% of the total biomass and 88.2% of zooplankton abundance, and included >34 species. The common copepod species were grouped into two size classes by total length (TL), those >2.5 mm (11.4% biomass, 24.2% abundance) and those <2.5 mm (7.4% biomass, 64.0% abundance). In order of dominance, large species included Metridia ochotensis, Calanus marshallae, M. pacificus, and Neocalanus spp. and small species included Pseudocalanus spp., Acartia longiremis, and Centropages abdominalis. Overall, the small species were more abundant than the large species. Densities of large copepods were relatively low compared to those of small copepods during El Niño (1998) and a cold year (2002), suggesting that large copepods with long lifespans are more sensitive to ocean climate fluctuation.