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            <gco:CharacterString>Cite this dataset as: Weber, L., Apprill, A., Kujawinski, E. (2022) Incubation experiments were conducted in St. John, US Virgin Islands to investigate the macronutrient drawdown response of reef seawater microbial communities to exudates released from the coral species Porites astreoides and Gorgonia ventalina. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2022-11-10 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.865193.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Exudate Uptake Incubations - Macronutrient Data Dataset Description: &amp;lt;p&amp;gt;Note:  The macronutrient concentrations in this dataset reflect the raw data and have not been normalized (as is presented in the manuscript Weber et al., 2022)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Other relevant files and publications:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The targeted and untargeted metabolomics data and metadata associated with this study are located on the MetaboLights database under accession numbers MTBLS2855 and MTBLS3286.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The 16S rRNA gene sequencing data and metadata associated with this study are located on the NCBI Sequence Read Archive (SRA) under BioProject PRJNA739882. BioSample accession numbers are not linked with the data submitted to BCO-DMO because samples for flow cytometry and macronutrients were not always collected at the same time as samples collected for microbial community analyses, meaning that only some of the samples collected for microbial community analyses have affiliated microbial abundances and nutrient concentrations.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Experiments were conducted to monitor responses of reef seawater microbial communities to concentrated exudates from &amp;lt;em&amp;gt;P. astreoides&amp;lt;/em&amp;gt; and &amp;lt;em&amp;gt;G. ventalina&amp;lt;/em&amp;gt;. After the organism incubations were conducted, excess filtrate (2 l) from 3 of the 6 colony/fragment incubations (selected randomly) were pooled into an acid-washed, 10 l carboy and mixed. Excess filtrate (~2 l) from the three control incubations were also pooled into a second, acid-washed, 10 l carboy and mixed.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For the &amp;lt;em&amp;gt;P. astreoides&amp;lt;/em&amp;gt; experiment, surface seawater was collected from the offshore site and coarsely filtered through a GF/A filter (1.6 µm nominal pore size) using peristalsis to remove larger cells and minimize heterotrophic grazing, but retain bacteria and archaea. Approximately 2.4 l of this inoculum was added separately to each of the 10 l carboys (pooled coral and control filtrate) to create a 5:2 ratio of filtrate: inoculum. After this addition, each carboy was mixed and a suite of samples were collected for different analyses including cell counts, inorganic and organic macronutrient quantification, and 16S rRNA gene sequencing. This collection marked the first timepoint (0 hours [hrs]) for the exudate uptake experiment. For the &amp;lt;em&amp;gt;G. ventalina&amp;lt;/em&amp;gt; experiment, reef seawater inoculum was collected from Tektite reef (Table S1).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For each experiment, coral metabolite or control filtrate seawater were transferred into separate 1 l acid-washed polycarbonate bottles (6 bottles per treatment). Within each treatment (coral and control), 3 of the 6 bottles were blackened to block light. The bottles were placed into a flow-through seawater table. PAR readings in the seawater table for the &amp;lt;em&amp;gt;P. astreoides&amp;lt;/em&amp;gt; and &amp;lt;em&amp;gt;G. ventalina&amp;lt;/em&amp;gt; experiments ranged from 250 – 1000 and 164 - 530 µmol quanta m -2s -1, respectively, with variation caused by shading and cloud cover. Over the course of 48 hours, samples were collected for cell counts (1 ml) at all timepoints (0, 12, 24, 36, and 48 hrs), macronutrient analyses (30 – 40 ml) at 0 and 48 hrs, and microbial community analyses (60 – 300 ml) at 0, 24, and 48 hrs.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples (40 ml) collected for total organic carbon (TOC) and total nitrogen (TN) analyses were aliquoted into combusted, borosilicate EPA vials and acidified using 75 µl of phosphoric acid. Samples were stored at room temperature for two weeks and then refrigerated at 4 °C until analysis.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For inorganic nutrient analyses, seawater (30 ml) was allocated into acid-washed, polypropylene bottles (Nalgene) and frozen at -20 °C.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/746195.rdf" xlink:title="OCE-1736288" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1736288 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1736288</gmx:Anchor>
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Coral reefs are some of the most diverse and productive ecosystems in the ocean. Globally, reefs have declined in stony (reef-building) coral abundance due to environmental variations, and in the Caribbean this decline has coincided with an increase in octocoral (soft coral) abundance. This phase shift occurring on Caribbean reefs may be impacting the interactions between the sea floor and water column and particularly between corals and picoplankton. Picoplankton are the microorganisms in the water column that utilize organic matter released from corals to support their growth. These coral-picoplankton interactions are relatively unstudied, but could have major implications for reef ecology and coral health. This project will take place in the U.S. territory of the Virgin Islands (USVI) and will produce the first detailed knowledge about the chemical diversity and composition of organic matter released from diverse stony coral and octocoral species. This project will advance our understanding of coral reef microbial ecology by allowing us to understand how different coral metabolites impact picoplankton growth and dynamics over time. The results from this project will be made publically accessible in a freely available online magazine, and USVI minority middle and high school students will be exposed to a lesson about chemical-biological interactions on coral reefs through established summer camps. This project will also contribute to the training of USVI minority undergraduates as well as a graduate student.&lt;/p&gt;
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&amp;lt;p&amp;gt;For the &amp;lt;em&amp;gt;P. astreoides&amp;lt;/em&amp;gt; experiment, surface seawater was collected from the offshore site and coarsely filtered through a GF/A filter (1.6 µm nominal pore size) using peristalsis to remove larger cells and minimize heterotrophic grazing, but retain bacteria and archaea. Approximately 2.4 l of this inoculum was added separately to each of the 10 l carboys (pooled coral and control filtrate) to create a 5:2 ratio of filtrate: inoculum. After this addition, each carboy was mixed and a suite of samples were collected for different analyses including cell counts, inorganic and organic macronutrient quantification, and 16S rRNA gene sequencing. This collection marked the first timepoint (0 hours [hrs]) for the exudate uptake experiment. For the &amp;lt;em&amp;gt;G. ventalina&amp;lt;/em&amp;gt; experiment, reef seawater inoculum was collected from Tektite reef (Table S1).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For each experiment, coral metabolite or control filtrate seawater were transferred into separate 1 l acid-washed polycarbonate bottles (6 bottles per treatment). Within each treatment (coral and control), 3 of the 6 bottles were blackened to block light. The bottles were placed into a flow-through seawater table. PAR readings in the seawater table for the &amp;lt;em&amp;gt;P. astreoides&amp;lt;/em&amp;gt; and &amp;lt;em&amp;gt;G. ventalina&amp;lt;/em&amp;gt; experiments ranged from 250 – 1000 and 164 - 530 µmol quanta m -2s -1, respectively, with variation caused by shading and cloud cover. Over the course of 48 hours, samples were collected for cell counts (1 ml) at all timepoints (0, 12, 24, 36, and 48 hrs), macronutrient analyses (30 – 40 ml) at 0 and 48 hrs, and microbial community analyses (60 – 300 ml) at 0, 24, and 48 hrs.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

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&amp;lt;p&amp;gt;Samples collected for inorganic nutrient analyses were shipped to Oregon State University and the concentrations of nitrite, nitrite + nitrate, ammonium, silicate, and phosphate were obtained using a continuous segmented flow system (described in 18). Total organic nitrogen concentrations were obtained by subtracting the sum of the inorganic nitrogen species (nitrite and nitrate + ammonium) from the total nitrogen concentrations. Values measured below the detection limits of the instruments (ammonium= 0.02 M, phosphate = 0.01 M, nitrite + nitrate = 0.07 M, nitrite = 0.01 M) were reported as zero.&amp;lt;/p&amp;gt;

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