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            <gco:CharacterString>Cite this dataset as: Knapp, A. N., Liang, Z. (2025) Total dissolved nitrogen (TDN) concentrations and δ15N measurements from samples collected on R/V Nathaniel B. Palmer GO-SHIP cruises NBP1706 and NBP1707 in the South Pacific from Jul 3 to Sep 30, 2017. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2025-11-25 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.986627.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>2017 GO-SHIP P06 transect TDN d15N Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;Total dissolved nitrogen (TDN) samples were collected from Niskin bottles deployed on a CTD rosette. All samples were filtered through a PES filter with 0.2 µm nominal pore size and frozen at -20 ˚C until analysis in the lab at Florida State University. We used the persulfate oxidation approach adapted from Knapp et al., 2005 to convert all TDN to nitrate, and the resulting nitrate concentration was determined using a chemiluminescent method, which quantitatively reduces NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; to NO gas in a heated, acidic vanadium (III) solution (Braman &amp;amp;amp; Hendrix, 1989). DON concentrations were computed by the difference between TDN and NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; concentrations, with NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; concentrations measured at sea using colorimetric methods (Armstrong et al., 1967) and reported at CCHDO Hydrographic Data Office (2023).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;After TDN concentration analysis, each TDN sample was acidified to a pH = ~4, and the TDN δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N was measured by the “denitrifier” method (Sigman et al., 2001; Casciotti et al., 2002; McIlvin &amp;amp;amp; Casciotti, 2011; Weigand et al., 2016). In samples with measurable NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; concentration, the δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N of DON can be calculated by mass balance by subtracting the concentration and δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N of NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; from the TDN concentration and TDN δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N measurements (Knapp et al., 2005).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/820042.rdf" xlink:title="OCE-1829797" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1829797 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1829797</gmx:Anchor>
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Phytoplankton play an important role in the Earth's elemental cycles of carbon and nitrogen. In addition to sunlight, phytoplankton living in the surface waters of the oceans require the elements nitrogen and phosphorus for growth. Much of these nutrients are supplied in their inorganic forms from mixing of deep waters towards the surface during the winter months when vertical stability of the water column breaks down. However much of the low latitude oceans, 45degS45degN, suffer from limited nutrient input to sunlit surface waters due to strong thermal stratification (vertical stability) of the upper water column. As a consequence, tropical and subtropical phytoplankton have devised alternative ways of acquiring nitrogen and phosphorus. Marine nitrogen fixation is a process by which specialized microbes utilize the abundant nitrogen gas from the atmosphere to convert elemental nitrogen into the bioavailable form ammonia. These nitrogen fixing phytoplankton and many others also use organic forms of phosphorus in the low latitude ocean where inorganic nutrients are often scarce. This project will significantly increase the number of dissolved organic nitrogen and dissolved organic phosphorus concentration measurements, especially from the currently under-sampled Pacific and Indian Oceans. Changes in the concentration of organic nutrients across the surface ocean will be used to infer rates of organic nutrient use by phytoplankton in numerical models. Specifically, the role for the biological uptake of dissolved organic phosphorus to stimulate the processes of marine nitrogen fixation and photosynthesis in the low latitude ocean will be quantified from the combined data and model output. The project will train one graduate student and several undergraduate students in both laboratory chemical analysis techniques and numerical simulation of ocean biological and chemical processes. New scientific knowledge will be shared with the public via a social media campaign and will inform the development of the next generation of global climate models.&lt;/p&gt;
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&amp;lt;p&amp;gt;After TDN concentration analysis, each TDN sample was acidified to a pH = ~4, and the TDN δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N was measured by the “denitrifier” method (Sigman et al., 2001; Casciotti et al., 2002; McIlvin &amp;amp;amp; Casciotti, 2011; Weigand et al., 2016). In samples with measurable NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; concentration, the δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N of DON can be calculated by mass balance by subtracting the concentration and δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N of NO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt;+NO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;&amp;lt;sup&amp;gt;-&amp;lt;/sup&amp;gt; from the TDN concentration and TDN δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N measurements (Knapp et al., 2005).&amp;lt;/p&amp;gt;</gco:CharacterString>
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