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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/868714.rdf" xlink:actuate="onRequest">Gross oxygen production and total daytime oxygen consumption derived from in vitro incubations deployed in situ at different depths at Station ALOHA during June 2019 (cruise ID KM1910)</gmx:Anchor>
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        <gco:CharacterString>Gross oxygen production Dataset Description: &amp;lt;p&amp;gt;Rates of gross oxygen production rates and total daytime oxygen consumption were measured using the &amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O-water in vitro method and membrane inlet mass spectrometry as described by Ferrón et al. (2016).&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Seawater samples for the incubations were collected in triplicate before dawn at six different depths (5, 25, 45, 75, 100, and 125m) with 12-L Niskin® bottles attached to a CTD rosette. Subsamples were taken from the Niskin bottles in acid-washed volume- calibrated 150-mLquartz glass bottles with ground-glass stoppers. The bottles were first rinsed with the seawater sample, and then filled from bottom to top using acid- washed silicon tubing, allowing the water to overflow at least twice the volume of the bottles. Before closing, the incubation bottles were spiked with 650 µL of &amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O-H&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O (97.2% &amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O, Medical Isotopes) for the surface samples (5-45 m) and 1,000 µL for deeper samples (75-125 m). The samples were deployed in situ at the corresponding depths before dawn using a free-drifting array, and incubated until dawn. After recovery, the incubated samples were poisoned with saturated mercuric chloride solution to inhibit biological activity. Time-zero samples were also collected pre-dawn and poisoned at the time of the deployment.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/805880.rdf" xlink:title="OCE-1911990" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1911990 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1911990</gmx:Anchor>
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&amp;lt;p&amp;gt;GOP = [R(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;)&amp;lt;sub&amp;gt;final&amp;lt;/sub&amp;gt; - R(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;)&amp;lt;sub&amp;gt;initial&amp;lt;/sub&amp;gt; / R(H&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O) - R(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;)&amp;lt;sub&amp;gt;initial&amp;lt;/sub&amp;gt; ] x [O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;]&amp;lt;sub&amp;gt;initial&amp;lt;/sub&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;where &amp;lt;em&amp;gt;R(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;)&amp;lt;sub&amp;gt;initia&amp;lt;/sub&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;sub&amp;gt;l&amp;lt;/sub&amp;gt; and &amp;lt;em&amp;gt;R(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;)&amp;lt;sub&amp;gt;final &amp;lt;/sub&amp;gt;&amp;lt;/em&amp;gt;are the initial and final isotope ratios (&amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O/&amp;lt;sup&amp;gt;16&amp;lt;/sup&amp;gt;O) for dissolved oxygen, respectively, &amp;lt;em&amp;gt;[O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;]&amp;lt;sub&amp;gt;initial&amp;lt;/sub&amp;gt;&amp;lt;/em&amp;gt; is the initial dissolved oxygen concentration, and &amp;lt;em&amp;gt;R(H&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;O)&amp;lt;/em&amp;gt; is the &amp;lt;sup&amp;gt;18&amp;lt;/sup&amp;gt;O isotope ratio of the incubation water.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The net oxygen change during the incubation is simultaneously determined from the net change in oxygen to argon molar ratios:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;NOC = [ ((O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;/Ar)&amp;lt;em&amp;gt;&amp;lt;sub&amp;gt;final&amp;lt;/sub&amp;gt;&amp;lt;/em&amp;gt; / (O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;/Ar)&amp;lt;sub&amp;gt;initial&amp;lt;/sub&amp;gt;) - 1 ] x [O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;]&amp;lt;sub&amp;gt;initial&amp;lt;/sub&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;where &amp;lt;em&amp;gt;(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;/Ar)&amp;lt;sub&amp;gt;final&amp;lt;/sub&amp;gt;&amp;lt;/em&amp;gt; and &amp;lt;em&amp;gt;(O&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;/Ar)&amp;lt;sub&amp;gt;initial &amp;lt;/sub&amp;gt;&amp;lt;/em&amp;gt;are the final and initial oxygen to argon molar ratios, respectively.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The total daytime oxygen consumption is derived as the difference between GOP and NOC and extrapolated to 24 hours (Ferrón et al., 2016).&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;BCO-DMO Processing Notes:&amp;lt;br /&amp;gt;
* Adjusted column names to comply with database requirements&amp;lt;br /&amp;gt;
* Added ISO8601 format of date and times&amp;lt;/p&amp;gt;</gco:CharacterString>
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