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&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; Gas Array near station ALOHA deployed during KM1016 and KM1110.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Rates of &amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; fixation were assessed using the &amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N isotopic tracer technique.&amp;amp;nbsp; Whole seawater samples from six discrete depths (5, 25, 45, 75, 100, and 125 m) were withdrawn into acid-washed duplicate 4.3 L polycarbonate bottles and sealed with caps fitted with a silicone septa. Three mL of &amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt; gas (98 %; Isotech Laboratories ©) was injected into each polycarbonate bottle through the silicone septum using a gas-tight syringe fitted with a stainless steel needle. The bottles were attached to a free drifting array, deployed before dawn and incubated at in situ light and temperature for ~24 hours.&amp;amp;nbsp; After recovery of the array, the entire volume of each bottle was filtered onto pre-combusted glass microfiber (GF/F) filters (25 mm diameter) for whole seawater N&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;-fixation estimates.&amp;amp;nbsp; All GF/F filters were placed on combusted foil pieces in Petri dishes and stored frozen at -20 °C for transport.&amp;lt;/p&amp;gt;</gco:CharacterString>
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