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During periods of stratification of the upper water column, the temperature at the chlorophyll maximum may differ from the sea surface temperature by 10°C in the western North Atlantic.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380011144764623872","@type":"Researcher","foaf:name":[{"@value":"Richard G. Fairbanks"}],"jpcoar:affiliationName":[{"@value":"Lamont-Doherty Geological Observatory of Columbia University, Palisades. New York 10964"}]},{"@id":"https://cir.nii.ac.jp/crid/1380011144764623873","@type":"Researcher","foaf:name":[{"@value":"Peter H. 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