Primary productivity measurements for the Hawaii Ocean Time-Series (HOT) program from October 1988 to December 2023 at Station ALOHA
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<p>The <sup>14</sup>C-radiotracer method is used to measure the assimilation of dissolved inorganic carbon (DIC) by phytoplankton as an estimate of the rate of photosynthetic production of organic matter in the euphotic zone. These data are from monthly measurements of primary production collection at Station ALOHA as part of the HOT TimeSeries program</p>
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2026-04-06
