Abstract
Plankton metabolic rates, such as rates of gross, net community production and community respiration, were measured in the surface waters using triple oxygen isotopes and O2 : Ar ratios. The 17D anomaly showed clear coastal and offshore gradients that were consistent with the distribution of chlorophyll a and oxygen saturation. Gross primary production (GPP) rates in coastal regions were several times higher than offshore regions, and the net‐to‐gross production ratio (N : G) indicated that coastal regions were net autotrophic, whereas offshore regions were net heterotrophic. On a seasonal scale, about 73% of the phytoplankton‐produced carbon was respired. Based on floating‐sediment‐trap data, export production to the aphotic zone was about 12‐20% of the GPP; the rest accumulated as dissolved organic carbon (DOC) or was respired.
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