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Uptake of nitrogenous nutrients by microplankton off the Washington and Oregon coasts was measured during the 1985 upwelling period. Nitrogen uptake rates in low‐NO3− waters (<5 µM) were 0.020–0.258 µmol N liter−1 h−1 and were primarily supported by regenerated nitrogen (71% of total uptake). Nitrogen uptake rates in high‐NO3 waters(≥20 µM) were 0.281–1.480 µmol N liter−1 h−1 and new (NO3−) nitrogen supported 83% of total uptake. Phytoplankton N was estimated by assuming a constant Chl a : PN for phytoplankton and was used to calculate phytoplankton‐specific uptake rates. Despite differences in nutrient concentrations, PN and Chl a at three upwelling sites (Oregon, Benguela, and Peru), NO3 uptake normalized to Chl a, and estimates of NO3−‐supported phytoplankton growth rates are remarkably similar. Nitrate uptake supports growth rates on the order of 1–2 d−1. Estimates of phytoplankton growth from rates of NH4+ + NO3− uptake range from 1.36 to 4.79 d−1 and are negatively correlated with concentrations of NO3− and phytoplankton N. The apparent increase in phytoplankton growth rates for waters with lower nitrogen availability may result from heterotrophic bacterial utilization of NH4+ nitrogen.
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Kokkinakis et al. (1987) studied this question.
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