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        <identifier>oai:figshare.com:article/34033272</identifier>
        <datestamp>2026-10-02T06:22:29Z</datestamp>
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          <dc:title>Data for "Contrasting associations of sea-ice meltwater and meteoric water with nitrogen uptake patterns in the summer Cosmonaut Sea, Antarctica"</dc:title>
          <dc:creator>Kun Zhang (108291)</dc:creator>
          <dc:creator>Qianyao Ma (21581852)</dc:creator>
          <dc:creator>Jun Zhao (59250)</dc:creator>
          <dc:creator>Qiang Hao (511575)</dc:creator>
          <dc:creator>Shunan Cao (3462737)</dc:creator>
          <dc:creator>Zifei Yang (25163085)</dc:creator>
          <dc:creator>Zhen Tang (2977569)</dc:creator>
          <dc:creator>Minfang Zheng (789885)</dc:creator>
          <dc:creator>Mengya Chen (6269318)</dc:creator>
          <dc:creator>Jianfeng He (287004)</dc:creator>
          <dc:creator>Min Chen (147733)</dc:creator>
          <dc:subject>Biological oceanography</dc:subject>
          <dc:subject>Chemical oceanography</dc:subject>
          <dc:subject>nitrogen uptake pattern</dc:subject>
          <dc:subject>sea-ice meltwater</dc:subject>
          <dc:subject>meteoric water</dc:subject>
          <dc:subject>Cosmonaut Sea</dc:subject>
          <dc:description>&lt;p dir="ltr"&gt;Nitrogen uptake by phytoplankton influences Southern Ocean productivity and carbon export, but how source-resolved meltwater is associated with nitrate and ammonium use remains unclear. Here, &lt;sup&gt;15&lt;/sup&gt;N tracer incubations and a &lt;i&gt;δ&lt;/i&gt;&lt;sup&gt;18&lt;/sup&gt;O-salinity mixing model were combined to examine nitrogen uptake in the early-summer Cosmonaut Sea. Depth-integrated nitrate (&lt;i&gt;ρ&lt;/i&gt;NO&lt;sub&gt;3&lt;/sub&gt;) and ammonium uptake (&lt;i&gt;ρ&lt;/i&gt;NH&lt;sub&gt;4&lt;/sub&gt;) rates averaged 8.0 and 1.3 mmol m&lt;sup&gt;‑2&lt;/sup&gt; d&lt;sup&gt;-1&lt;/sup&gt;, respectively, yielding a mean &lt;i&gt;f&lt;/i&gt;-ratio of 0.80. Meteoric water (MW) fractions were positively correlated with chlorophyll &lt;i&gt;a&lt;/i&gt; (Chl-a) concentration, the micro-sized (&gt;20 μm) Chl-&lt;i&gt;a&lt;/i&gt; fraction, and &lt;i&gt;ρ&lt;/i&gt;NO&lt;sub&gt;3&lt;/sub&gt;, suggesting that MW-influenced waters were associated with higher biomass, larger size structure, and enhanced nitrate uptake. Sea-ice meltwater (SIM) fractions were positively correlated with ambient NH&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;+&lt;/sup&gt; and &lt;i&gt;ρ&lt;/i&gt;NH&lt;sub&gt;4&lt;/sub&gt;, consistent with greater regenerated nitrogen availability following sea-ice retreat and post-bloom recycling. These source-specific associations highlight the need to consider meltwater timing and source when assessing nitrogen assimilation pathways and biological-pump potential in Antarctic coastal waters.&lt;/p&gt;</dc:description>
          <dc:date>2026-10-02T06:22:29Z</dc:date>
          <dc:type>Dataset</dc:type>
          <dc:type>Dataset</dc:type>
          <dc:identifier>10.6084/m9.figshare.34033272.v2</dc:identifier>
          <dc:relation>https://figshare.com/articles/dataset/Data_for_Contrasting_associations_of_sea-ice_meltwater_and_meteoric_water_with_nitrogen_uptake_patterns_in_the_summer_Cosmonaut_Sea_Antarctica_/34033272</dc:relation>
          <dc:rights>CC BY 4.0</dc:rights>
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