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        <gco:CharacterString>Cellular trace elements collected on cruise RR1604 (GO-SHIP transect IO9N) in the Eastern Indian Ocean from March to April 2016 Dataset Description: &amp;lt;p&amp;gt;Cellular trace elements collected on cruise RR1604 (GO-SHIP transect IO9N) in the Eastern Indian Ocean from March to April 2016.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Samples were collected from 5 L Teflon-coated Niskin-X bottles hung on non-metal line, and clean techniques were followed throughout (Bruland et al., 1979). Niskin-X bottles were transferred to a clean lab immediately after retrieval. At most stations a single sample was collected from 20 m. Four-depth profiles extending to 200 m were collected at 6 stations along the transect.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;A small aliquot of unfiltered seawater was reserved from the surface-most Niskin-X bottle to collect phytoplankton cells for synchrotron X-ray fluorescence (SXRF) analysis. SXRF samples were collected following protocols described in Twining et al. (2015). Cellular metals were analyzed with the 2-ID-E microprobe beamline at the Advanced Photon Source, Argonne National Laboratory. Incident beam energy was 10 keV to enable the excitation of K&amp;lt;sub&amp;gt;α&amp;lt;/sub&amp;gt; fluorescence for elements ranging in atomic number from Si (14) to Zn (30). Approximately 15 cells were analyzed at each station. Flagellated autotrophs with diameters ranging from 1.65 - 6.6 µm were analyzed using 2D raster scans with 0.5 μm pixel step sizes and detector dwell times from 10-20 sec/pixel.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Element quantification was performed by averaging the spectra from pixels representing the cells of interest. Spectra were also extracted from a background area close to each cell. The spectra were then fit with MAPS, a custom fitting software package (Vogt, 2003).&amp;amp;nbsp; Concentrations were calculated based on conversion factors obtained by running the thin-film standards NBS 1832, NBS 1833, and custom Si, P, and Fe standards made by Micromatter XRF. Cell volume was calculated based on measurements taken from bright field images of the cells and using the equations of Hillebrand et al. (1999). Cellular C was then calculated from the volumes using the equations described in Menden-Deuer and Lessard (2000).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/628978.rdf" xlink:title="OCE-1559021" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1559021 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1559021</gmx:Anchor>
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