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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/892576.rdf" xlink:actuate="onRequest">Benthic microalgal photopigment concentrations from nearshore shelf waters off Charleston, SC from June 2018 to August 2021</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Pinckney, J. L. (2023) Benthic microalgal photopigment concentrations from nearshore shelf waters off Charleston, SC from June 2018 to August 2021. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2023-04-10 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.892576.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Methods and Sampling: &amp;lt;p&amp;gt;Samples for Benthic microalgal photopigment analysis were collected by SCUBA divers from the R/V &amp;lt;em&amp;gt;Trinity&amp;lt;/em&amp;gt; in nearshore waters of Charleston, SC using 1 square centimeter x 10 centimeter (cm) plastic core tubes gently pushed into the sediment to minimize disruption of the surface layers. Tubes were capped and carefully removed from the sediment. Ten cores were obtained randomly within a 1 square meter area at select locations for each sample date. The upper 1 centimeter of the core was extruded, frozen at -80 degrees Celsius, and analyzed within 30 days after collection. Sediments were dried and sieved for grain size analysis.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;High-performance liquid chromatography (HPLC) was used to determine chemosystematic photosynthetic pigments. Samples were lyophilized for 24 hours at -50 degrees Celsius, placed in 90 percent acetone (1 milliliter), sonicated on ice for 30 seconds, and extracted at -20 degrees Celsius for 18 to 20 hours. Filtered extracts: 0.45 micrometers, 250 microliters were injected into a Shimadzu 10AD HPLC equipped with a monomeric (Rainin Microsorb-MV, 0.46 x 10 centimeters, 3 micrometers) and a polymeric (Vydac 201TP54, 0.46 x 25 centimeters, 5 micrometers) reverse-phase C18 column in series. A nonlinear binary gradient of 80&amp;amp;nbsp;percent methanol: 20&amp;amp;nbsp;percent 0.50 M ammonium acetate and 80 percent methanol:20&amp;amp;nbsp;percent acetone was the mobile phase (Pinckney et al. 1996, 2001). Absorption spectra and chromatograms (440 ± 4 nanometers) were acquired using a Shimadzu SPD-M10av photodiode array detector. Pigment peaks were identified by comparison of retention times and absorption spectra with pure carotenal and chlorophyll standards (DHI, Denmark). The synthetic carotenoid β-apo-8'-carotenal (Sigma) was used as an internal standard.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;</gco:CharacterString>
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Continental shelves are highly productive, with both ecological and economic importance. Benthic microalgae (BMA) are key primary producers in these location. As much as 6x the water column biomass of primary producers is compressed into a layer only a few mm thick on the sediment surface. The source(s) of fixed nitrogen (N) supporting such highly concentrated BMA biomass is currently unknown. Recent studies of sub-seafloor groundwater flow at the University of South Carolina have demonstrated that upwelling saline groundwater likely supplies high concentrations of nutrients in the ridge-swale habitats in the South Atlantic Bight (SAB). The investigators suggest that groundwater input of fixed N into surficial sediments is the primary source of N supporting BMA biomass and production in the mid-shelf region of the SAB. The purpose of this project is to determine the primary source of fixed N supporting BMA biomass in the surface sediments of the shallow shelf waters (&amp;lt;30 m), using the SAB as a field area. A secondary objective is to apply novel and innovative methods to directly quantify groundwater inputs of N into surficial sediments. Research results will fully document the spatio-temporal distributions of BMA and phytoplankton biomass and community structure in the mid-shelf region of the SAB and relate the observed patterns to groundwater inputs of fixed N sources as well as hydrographic and climatic conditions. This research will provide full support and tuition for 2 graduate students, summer support for undergraduate assistants, and involve upper level undergraduates as lab interns. The study team will also work with the Baruch Institute and other partners to develop an &quot;Ocean Schoolyard&quot; program to meet the needs of teachers, students, and community audiences. The project will also provide partial support for Girls Go for I.T., a coding summer camp designed to attract middle-school-aged girls to careers in I.T. and STEM fields.&lt;/p&gt;
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&amp;lt;p&amp;gt;High-performance liquid chromatography (HPLC) was used to determine chemosystematic photosynthetic pigments. Samples were lyophilized for 24 hours at -50 degrees Celsius, placed in 90 percent acetone (1 milliliter), sonicated on ice for 30 seconds, and extracted at -20 degrees Celsius for 18 to 20 hours. Filtered extracts: 0.45 micrometers, 250 microliters were injected into a Shimadzu 10AD HPLC equipped with a monomeric (Rainin Microsorb-MV, 0.46 x 10 centimeters, 3 micrometers) and a polymeric (Vydac 201TP54, 0.46 x 25 centimeters, 5 micrometers) reverse-phase C18 column in series. A nonlinear binary gradient of 80&amp;amp;nbsp;percent methanol: 20&amp;amp;nbsp;percent 0.50 M ammonium acetate and 80 percent methanol:20&amp;amp;nbsp;percent acetone was the mobile phase (Pinckney et al. 1996, 2001). Absorption spectra and chromatograms (440 ± 4 nanometers) were acquired using a Shimadzu SPD-M10av photodiode array detector. Pigment peaks were identified by comparison of retention times and absorption spectra with pure carotenal and chlorophyll standards (DHI, Denmark). The synthetic carotenoid β-apo-8'-carotenal (Sigma) was used as an internal standard.&amp;lt;/p&amp;gt;

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- Longitude values were converted to decimal degrees where negative values denote the Southern hemisphere&amp;lt;/p&amp;gt;

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