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The deep chlorophyll maxlmum (DCM) IS a widespread feature In the subtropical gyre of the North Paclflc In mid-August 1985 chlorophyll concentration increased In the DCM, then dechned over time at 95 to 110 m depth near 28"N 155"W During the higher chlorophyll perlod the DCM lay w~th in the top of the nitracline Later, as the chlorophyll concentratlon decllned and the DCM deepened, following the 24 9 slgma-t surface, the maxlmum was above the nitracllne The DCM was also a maxlmum In abundance of autotrophlc flagellates Particulate nltrogen was retained over time in the euphotic zone relative to particulate carbon and chlorophyll Phytoplankton growth rate at 90 to 110 m depth averaged 0 11 d' and phytoplankton carbon was about 10 pg I ' , about 50 % of the total paruculate carbon

Subsurface chlorophyll maximum in August-September 1985 in the CLIMAX area of the North Pacific