{"refrec":{"BRefID":38599,"RR":"<b>Witbaard, R.; Jansma, E.; Klaassen, U.S.</b> (2003). Copepods link quahog growth to climate. <i>J. Sea Res. 50(1)</i>: 77-83. <a href=\"http://dx.doi.org/10.1016/s1385-1101(03)00040-6\" target=\"_blank\">http://dx.doi.org/10.1016/s1385-1101(03)00040-6</a>","BEntID":38599,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>J. Sea Res. 50(1)</i>: 77-83. <a href=\"https://dx.doi.org/10.1016/s1385-1101(03)00040-6\" target=\"_blank\">https://dx.doi.org/10.1016/s1385-1101(03)00040-6</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Witbaard, R.; Jansma, E.; Klaassen, U.S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Witbaard, R. <i>et al.</i>","Englishabstract":"From samples collected in 1983, 1991 and 2000, a long-term growth record for the bivalve <i>Arctica islandica</i> from the northern North Sea was constructed with methods derived from dendrochronology. Subsequent response-function analyses demonstrated that shell growth was mainly influenced by the abundance of copepods as recorded by the CPR survey. In years with dense copepod populations a major part of the downward flux of food particles is intercepted by the copepods before it reaches the seafloor. 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