{"refrec":{"BRefID":28419,"RR":"<b>Lubny-Gertzyk, E.A.</b> (1968). Distribution of zooplankton in the region where different water masses interact. <i>Sarsia 34(1)</i>: 273-276. <a href=\"https://dx.doi.org/10.1080/00364827.1968.10413390\" target=\"_blank\">https://dx.doi.org/10.1080/00364827.1968.10413390</a>","BEntID":28419,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>Sarsia 34(1)</i>: 273-276. <a href=\"https://dx.doi.org/10.1080/00364827.1968.10413390\" target=\"_blank\">https://dx.doi.org/10.1080/00364827.1968.10413390</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Lubny-Gertzyk, E.A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Lubny-Gertzyk, E.A.","Englishabstract":"In the north-western part of the Pacific Ocean where waters of subarctic and subtropical origin meet and interact the distribution of zooplankton has the following pattern.:In May 1955 the southern limit of the boreal species in the uppermost 50 m was found at 37° N, but at 35° N in the 50–100 m layer. 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