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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/961706.rdf" xlink:actuate="onRequest">Stable isotope compositions (carbon, nitrogen, and sulfur) of muscle tissue in three species of fish from the Matagorda Bay region of Texas in the northwestern Gulf of Mexico from 2021 to 2023</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Walther, B., Oster, J. (2025) Stable isotope compositions (carbon, nitrogen, and sulfur) of muscle tissue in three species of fish from the Matagorda Bay region of Texas in the northwestern Gulf of Mexico from 2021 to 2023. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2025-05-14 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.961706.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Texas fish muscle stable isotopes Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;Fish collection locations and associated information are found in an accompanying dataset for this project: &amp;lt;a href=&amp;quot;https://www.bco-dmo.org/dataset/916418&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;https://www.bco-dmo.org/dataset/916418&amp;lt;/a&amp;gt;.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Fish carcasses were obtained from anglers at boat docks, fish cleaning stations, or other locations in the region. Fish were also obtained from bait shops where the proprietors verified the fish were sourced from the Matagorda Bay study region. These fish will be dissected to subsample white muscle tissue from each fish (skin and scales removed). Fish muscle tissue was dehydrated, pulverized to a fine powder, and packed into individual tin capsules for stable isotope analyses. All isotope analyses were conducted at the University of California, Davis Stable Isotope Facility. Analytical methods follow those described by Walther &amp;amp;amp; Torrance (2024) and Valenza et al. (2025).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Additional text describing methods below are from &amp;lt;a href=&amp;quot;https://stableisotopefacility.ucdavis.edu/&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;https://stableisotopefacility.ucdavis.edu/&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples were analyzed for 13C and 15N isotopes using a PDZ Europa ANCA-GSL elemental analyzer interfaced to a PDZ Europa 20-20 isotope ratio mass spectrometer (Sercon Ltd., Cheshire, UK). Samples are combusted at 1000 degrees Celsius (°C) in a reactor packed with chromium oxide and silvered copper oxide. Following combustion, oxides are removed in a reduction reactor (reduced copper at 650°C). The helium carrier then flows through a water trap (magnesium perchlorate and phosphorous pentoxide). N2 and CO2 are separated on a Carbosieve GC column (65°C, 65 milliliters per minute (mL/min)) before entering the IRMS. During analysis, samples are interspersed with several replicates of at least four different laboratory reference materials. The long-term standard deviation is 0.2 ‰ for 13C and 0.3 ‰ for 15N. The final delta values, delivered to the customer, are expressed relative to international standards VPDB (Vienna Pee Dee Belemnite) and Air for carbon and nitrogen, respectively.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Stable isotope ratios of 34S in solid samples are measured using an Elementar vario ISOTOPE cube interfaced to an Isoprime PrecisION IRMS (Cheadle Hume, Stockport, UK). Samples are combusted at 1000°C in a reactor packed with tungsten oxide and elemental copper. Immediately following combustion, sample gases are reduced with elemental copper at 900°C and subsequently pass through a buffering reactor filled with quartz chips held at 900°C. SO2 and CO2 are then separated by purge and trap, allowing for full separation and peak focusing. Following separation, the SO2 adsorption trap is heated and the sample SO2 passes directly to the IRMS for measurement.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;During analysis, samples are interspersed with replicates of several laboratory reference materials to monitor and allow for correction of any potential variation in drift and linearity. Final 34S delta values are obtained after adjusting the provisional measurements such that correct 34S delta values for laboratory quality assurance materials are obtained. The long-term reproducibility of this method is ± 0.4 ‰.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/780578.rdf" xlink:title="OCE-1924011" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1924011 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1924011</gmx:Anchor>
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                <gco:CharacterString>&amp;lt;p&amp;gt;Fish collection locations and associated information are found in an accompanying dataset for this project: &amp;lt;a href=&amp;quot;https://www.bco-dmo.org/dataset/916418&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;https://www.bco-dmo.org/dataset/916418&amp;lt;/a&amp;gt;.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Fish carcasses were obtained from anglers at boat docks, fish cleaning stations, or other locations in the region. Fish were also obtained from bait shops where the proprietors verified the fish were sourced from the Matagorda Bay study region. These fish will be dissected to subsample white muscle tissue from each fish (skin and scales removed). Fish muscle tissue was dehydrated, pulverized to a fine powder, and packed into individual tin capsules for stable isotope analyses. All isotope analyses were conducted at the University of California, Davis Stable Isotope Facility. Analytical methods follow those described by Walther &amp;amp;amp; Torrance (2024) and Valenza et al. (2025).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Additional text describing methods below are from &amp;lt;a href=&amp;quot;https://stableisotopefacility.ucdavis.edu/&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;https://stableisotopefacility.ucdavis.edu/&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples were analyzed for 13C and 15N isotopes using a PDZ Europa ANCA-GSL elemental analyzer interfaced to a PDZ Europa 20-20 isotope ratio mass spectrometer (Sercon Ltd., Cheshire, UK). Samples are combusted at 1000 degrees Celsius (°C) in a reactor packed with chromium oxide and silvered copper oxide. Following combustion, oxides are removed in a reduction reactor (reduced copper at 650°C). The helium carrier then flows through a water trap (magnesium perchlorate and phosphorous pentoxide). N2 and CO2 are separated on a Carbosieve GC column (65°C, 65 milliliters per minute (mL/min)) before entering the IRMS. During analysis, samples are interspersed with several replicates of at least four different laboratory reference materials. The long-term standard deviation is 0.2 ‰ for 13C and 0.3 ‰ for 15N. The final delta values, delivered to the customer, are expressed relative to international standards VPDB (Vienna Pee Dee Belemnite) and Air for carbon and nitrogen, respectively.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Stable isotope ratios of 34S in solid samples are measured using an Elementar vario ISOTOPE cube interfaced to an Isoprime PrecisION IRMS (Cheadle Hume, Stockport, UK). Samples are combusted at 1000°C in a reactor packed with tungsten oxide and elemental copper. Immediately following combustion, sample gases are reduced with elemental copper at 900°C and subsequently pass through a buffering reactor filled with quartz chips held at 900°C. SO2 and CO2 are then separated by purge and trap, allowing for full separation and peak focusing. Following separation, the SO2 adsorption trap is heated and the sample SO2 passes directly to the IRMS for measurement.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;During analysis, samples are interspersed with replicates of several laboratory reference materials to monitor and allow for correction of any potential variation in drift and linearity. Final 34S delta values are obtained after adjusting the provisional measurements such that correct 34S delta values for laboratory quality assurance materials are obtained. The long-term reproducibility of this method is ± 0.4 ‰.&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;Data are provided as reported by the analytical facility without additional processing. Duplicate samples from some fish were analyzed separately to assess within-fish variation. Those results are provided separately and indicated as duplicates within the dataset.&amp;lt;/p&amp;gt;</gco:CharacterString>
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          </gmd:processStep>
        <gmd:processStep xlink:title="BCO-DMO Data Processing Description">
              <gmd:LI_ProcessStep>
                <gmd:description>
                  <gco:CharacterString>- Imported fish collection location data (file &amp;quot;916418_v2_fish_collection_locations.csv&amp;quot;)
- Imported original file &amp;quot;SIA_Data_Upload.xlsx&amp;quot; into the BCO-DMO system.
- Flagged &amp;quot;NAN&amp;quot; as a missing data value (missing data are empty/blank in the final CSV file).
- Added the following columns from the fish collection location data file to this dataset by joining on Fish_ID: Station_Latitude, Station_Longitude, Date_Collected, Species.
- Saved the final file as &amp;quot;961706_v1_fish_muscle_stable_isotopes.csv&amp;quot;.</gco:CharacterString>
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                          <gco:CharacterString>Specified by BCO-DMO Data Managers</gco:CharacterString>
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                        <gmd:date gco:nilReason="unknown"/>
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    <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/191.rdf" xlink:actuate="onRequest">Biological and Chemical Oceanography Data Management Office (BCO-DMO)</gmx:Anchor>
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				    <gco:CharacterString>Woods Hole</gco:CharacterString>
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				    <gco:CharacterString>MA</gco:CharacterString>
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				    <gco:CharacterString>USA</gco:CharacterString>
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				    <gco:CharacterString>info@bco-dmo.org</gco:CharacterString>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/546339.rdf" xlink:title="Elemental Analyzer" xlink:actuate="onRequest">PDZ Europa ANCA-GSL elemental analyzer</gmx:Anchor>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/469.rdf" xlink:title="Isotope-ratio Mass Spectrometer" xlink:actuate="onRequest">Isoprime PrecisION IRMS</gmx:Anchor>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/956626.rdf" xlink:title="PDZ Europa 20-20 isotope ratio mass spectrometer" xlink:actuate="onRequest">PDZ Europa 20-20 isotope ratio mass spectrometer</gmx:Anchor>
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            <gco:CharacterString>PI Supplied Instrument Name: PDZ Europa 20-20 isotope ratio mass spectrometer Instrument Name: PDZ Europa 20-20 isotope ratio mass spectrometer Instrument Short Name:Europa 20-20 IRMS   Instrument Description: The PDZ Europa 20-20 is a dedicated continuous flow isotope ratio mass spectrometer for hyphenated stable isotope analyses able to measure 15N, 13C, 18O, and 34S in a host of applications. The analyzer has been purposely designed to measure 2H by continuous flow methodology and is also suitable to analyze the light stable isotopes in all the commonly measured gases: H2, N2, NO, N2O, O2, CO, CO2, SO, and SO2.</gco:CharacterString>
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