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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/819975.rdf" xlink:actuate="onRequest">Silica and nitrogen analyses from incubation experiments conducted using seagrass cores from 1m depth in Grand Bay in 2017.</gmx:Anchor>
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        <gco:CharacterString>Methods and Sampling: &amp;lt;p&amp;gt;Three repeated experimental trials were done in summer months. Thirty-two cores (27 cm diameter, 14 cm depth) were collected from 50 m2 area of seagrass bed at 1 m depth on: June 28, July 12 and July 26, 2017 for trials 1-3, respectively. On each date, 16 cores were collected from seagrass habitat in pairs. Another 16 cores were collected from open sediment (OS) habitat. Extracted, paired cores were placed upright into an open-top plastic tub (49 x 33 x 42 cm) to produce eight tubs of each habitat.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Tubs were transported to Dauphin Island Sea Lab (~30-minute drive) filled with seawater (to core depth of 16 cm) pumped from Mobile Bay (20 km, east of site) and arranged in four blocks within an outdoor mesocosm. Each block contained two tubs of each habitat. After two days, a diatom-specific inhibitor (3 µM solution of germanic acid, i.e. Ge treatment) was randomly added to water, i.e. two tubs per block, one of each habitat type. Germanium (Ge) at high Ge/Si ratios (&amp;amp;gt; 0.01) prevents formation of siliceous cell wall (Azam and Chisholm 1976). We added 3 µM solution and allowed two days for Ge incorporation.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Metabolism measurements:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Two days after, we quantified productivity and respiration from changes in oxygen content within 2-3 hour incubations of chambers and bottles following methods in Anton et al. (2009).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Nitrogen and Silica:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;At end of incubation, 100 mL of water from each clear chamber was filtered through 47 mm Whatman glass fiber filter. Filtered water was analyzed for total dissolved nitrogen (TDN) and nitrate+nitrite (NO3-+NO2-) colorimetrically using Skalar autoanalyzer (Dzwonkowski et al. 2017), and for dissolved silicic acid (Si(OH)4) using a manual colorimetric method (Krause et al. 2009).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Statistical analyses:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;A series of two-way ANOVAs with trial and treatment as fixed factors were used to test for differences in environment in both habitats.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/712666.rdf" xlink:title="OCE-1558957" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1558957 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1558957</gmx:Anchor>
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The Louisiana Shelf system in the northern Gulf of Mexico is fed by the Mississippi River and its many tributaries which contribute large quantities of nutrients from agricultural fertilizer to the region. Input of these nutrients, especially nitrogen, has led to eutrophication. Eutrophication is the process wherein a body of water such as the Louisiana Shelf becomes enriched in dissolved nutrients that increase phytoplankton growth which eventually leads to decreased oxygen levels in bottom waters. This has certainly been observed in this area, and diatoms, a phytoplankton which represents the base of the food chain, have shown variable silicon/nitrogen (Si/N) ratios. Because diatoms create their shells from silicon, their growth is controlled not only by nitrogen inputs but the availability of silicon. Lower Si/N ratios are showing that silicon may be playing an increasingly important role in regulating diatom production in the system. For this reason, a scientist from the University of South Alabama will determine the biogeochemical processes controlling changes in Si/N ratios in the Louisiana Shelf system. One graduate student on their way to a doctorate degree and three undergraduate students will be supported and trained as part of this project. Also, four scholarships for low-income, high school students from Title 1 schools will get to participate in a month-long summer Marine Science course at the Dauphin Island Sea Laboratory and be included in the research project. The study has significant societal benefits given this is an area where $2.4 trillion gross domestic product revenue is tied up in coastal resources. Since diatoms are at the base of the food chain that is the biotic control on said coastal resources, the growth of diatoms in response to eutrophication is important to study.&lt;/p&gt;
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&amp;lt;p&amp;gt;Tubs were transported to Dauphin Island Sea Lab (~30-minute drive) filled with seawater (to core depth of 16 cm) pumped from Mobile Bay (20 km, east of site) and arranged in four blocks within an outdoor mesocosm. Each block contained two tubs of each habitat. After two days, a diatom-specific inhibitor (3 µM solution of germanic acid, i.e. Ge treatment) was randomly added to water, i.e. two tubs per block, one of each habitat type. Germanium (Ge) at high Ge/Si ratios (&amp;amp;gt; 0.01) prevents formation of siliceous cell wall (Azam and Chisholm 1976). We added 3 µM solution and allowed two days for Ge incorporation.&amp;lt;/p&amp;gt;

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&amp;lt;p&amp;gt;Two days after, we quantified productivity and respiration from changes in oxygen content within 2-3 hour incubations of chambers and bottles following methods in Anton et al. (2009).&amp;lt;/p&amp;gt;

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&amp;lt;p&amp;gt;BCO-DMO Data Manager Processing Notes:&amp;lt;br /&amp;gt;
* added a conventional header with dataset name, PI name, version date&amp;lt;br /&amp;gt;
* modified parameter names to conform with BCO-DMO naming conventions&amp;lt;br /&amp;gt;
* blank values in this dataset are displayed as &amp;quot;nd&amp;quot; for &amp;quot;no data.&amp;quot;&amp;amp;nbsp; nd is the default missing data identifier in the BCO-DMO system. Added ND as a missing data identifier.&amp;lt;br /&amp;gt;
* removed all spaces in headers and replaced with underscores&amp;lt;br /&amp;gt;
* removed all units from headers&amp;lt;br /&amp;gt;
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