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The dynamics of dissolved inorganic carbon (DIC) and processes controlling net community production (NCP) were investigated within a mature cyclonic eddy, Cyclone Opal, which formed in the lee of the main Hawaiian Islands in the subtropical North Pacific Gyre. Within the eddy core, physical and biogeochemical properties suggested that nutrient- and DIC-rich deep waters were uplifted by similar to 80 m relative to surrounding waters, enhancing biological production. A salt budget indicates that the eddy core was a mixture of deep water (68%) and surface water (32%). NCP was estimated from mass balances of DIC, nitrate+nitrite, total organic carbon, and dissolved organic nitrogen, making rational inferences about the unobserved initial conditions at the time of eddy formation. Results consistently suggest that NCP in the center of the eddy was substantially enhanced relative to the surrounding waters, ranging from 14.1 +/- 10.6 (0-110 m: within the euphotic zone) to 14.2 +/- 9.2 (0-50 m: within the mixed layer) to 18.5 +/- 10.7 (0-75 m: within the deep chlorophyll-maximum layer) mmol Cm-2 d(-1) depending on the depth of integration. NCP in the ambient waters outside the eddy averaged about 2.37 +/- 4.24 mmol Cm-2 d(-1) in the mixed layer (similar to 0-95 m). Most of the enhanced NCP inside the eddy appears to have accumulated as dissolved organic carbon (DOC) rather than exported as particulate organic carbon (POC) to the mesopelagic. Our results also suggest that the upper euphotic zone (0-75 m) above the deep chlorophyll maximum is characterized by positive NCP, while NCP in the lower layer ( > 75 m) is close to zero or negative. (C) 2008 Elsevier Ltd. All rights reserved.