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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/841583.rdf" xlink:actuate="onRequest">Element quotas of individual plankton cells collected during IRNBRU (MV1405) and June 2015 Line P cruises</gmx:Anchor>
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        <gco:CharacterString>Cellular trace elements from IRNBRU and Line P cruises Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;em&amp;gt;R/V Melville&amp;lt;/em&amp;gt;&amp;amp;nbsp;1405 took place in the North Pacific Ocean along the California coast from 32°S to 43°N and extending from -117°E to -127°E. The Line P cruise on CCGS John P. Tully was in the North Pacific Ocean off the coast British Columbia from Vancouver (48°N, 123°W) to Ocean Station Papa (50°N, 145°W).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples were collected with trace-metal clean bottles or trace-metal clean pump. A small aliquot of unfiltered seawater was 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). 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;

&amp;lt;p&amp;gt;Complete methodology is published in Twining et al. (2020).&amp;lt;/p&amp;gt;</gco:CharacterString>
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Diatoms are responsible for a significant fraction of primary production in the ocean. They are associated with enhanced carbon export and usually dominate the response of phytoplankton to additions of the micronutrient iron in high-nutrient, low-chlorophyll (HNLC) regions. Diatoms, particularly those isolated from the open ocean, appear to have a significant capacity to store iron for later use, and in some groups of diatoms this ability is enabled by the iron storage protein ferritin. Such luxury uptake of iron has long been observed in laboratory cultures and hypothesized to provide diatoms with an ecological benefit in the low-iron waters that cover 40% of the global ocean. However iron storage has been difficult to observe in natural systems due to the methodological challenges of working with mixed plankton assemblages, and a physiological understanding of the impacts of iron on ocean diatoms is lacking. This project combines state-of-the-art high-throughput transcriptomic sequencing and single-cell element analysis with novel laboratory and field incubation experiments to quantify iron storage abilities of cultured and natural diatoms that either contain or lack ferritin and determine the ecological impacts of this process. The overall objective of this project is to examine the ecological importance of iron storage as a selective mechanism controlling the distributions of diatoms along iron gradients in marine ecosystems. The proposed research includes three specific objectives:&lt;/p&gt;
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&lt;p&gt;B. Examine whether iron storage capacities across diverse diatom taxa consistently provide a mechanistic explanation for continued growth in the absence of iron.&lt;/p&gt;
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