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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/995970.rdf" xlink:actuate="onRequest">Dissolved iron and iron isotopes for SGD well, river, and estuary samples collected between November 2022 and March 2024 along the West Florida Shelf</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Conway, T. M., Hunt, H. (2026) Dissolved iron and iron isotopes for SGD well, river, and estuary samples collected between November 2022 and March 2024 along the West Florida Shelf. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2026-04-06 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.995970.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>STING river, estuary, and SGD well Fe and Fe isotopes Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sample Collection&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;SGD Wells&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Submarine groundwater samples were collected by U.S. Geological survey (USGS) small boat from three offshore well transects, each with three well location. Samples were taken from well head (GWd) and from surface (SB) and bottom waters (BW). Divers, using acid-cleaned Teflon tubing attached to a trace metal clean diaphragm pump. First, bottom waters were collected, then the well uncapped, adequately purged, and sampled. All samples were filtered through 0.2 um Acropak Supor Cartridges (Pall, USA) into acid-cleaned LDPE bottles. NC5, NC10, NC15 = Nature Coast Transect, IRB25, IRB30, IRB35 = Indian Rocks Transect, VH45, VH50, VH55 = Venice Headlands Transect. More details are provided in Hunt (2025).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;Rivers and Estuaries&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;River Sample sites were located on land and samples were collected from five rivers (Hillsborough, Alafia, Manatee, Peace, and Caloosahatchee), using trace metal clean protocols. Estuary samples were collected in collaboration with Mote Marine Laboratory via small boat (RV Eugenie Clark), also using trace metal clean protocols. All water samples for dissolved Fe and d56Fe were syringe filtered using acid-cleaned 50 mL Henke Jet HDPE syringes and 0.2 um PVDF membrane Titan3 syringe filters into acid-cleaned LDPE bottles. AR1-2 = Alafia River, HB1-2 = Hillsborough, MR1-2 = Manatee, PR1 = Peace River, CR1 = Caloosahatchee, CS and E= Estuary sample locations. More details are provided in Hunt (2025).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sample Processing&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples were acidified back on shore at the University of South Florida (USF) using 2.4 mL 10 M Teflon-distilled HCl per liter of sample and stored for at least 6 months before processing.&amp;amp;nbsp;Samples were then processed for dissolved Fe isotope and concentration analysis at the University of South Florida following Sieber et al. (2019), modified from Conway et al (2013). Briefly, an Fe double-spike was added prior to batch extraction using Nobias PA-1 chelating resin, followed by purification by anion-exchange chromatography using AG-MP1 resin. Concentration and isotope analyses were performed on a Thermo Neptune Plus MC-ICPMS (Multicollecter Inductively Coupled Plasma Mass Spectrometer)&amp;amp;nbsp;in the Tampa Bay Plasma Facility at the University of South Florida using the double spike technique via a ~100 uL min&amp;lt;sup&amp;gt;-1&amp;lt;/sup&amp;gt;&amp;amp;nbsp;PFA nebulizer and Apex Ω introduction system, Pt Jet Sampler cone and an Al X skimmer cone.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sample Analysis&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Dissolved Fe stable isotope ratios are expressed in delta notation (δ&amp;lt;sup&amp;gt;56&amp;lt;/sup&amp;gt;Fe) relative to the IRMM-014 standard. A secondary Fe standard, NIST-3126, was analyzed over 56 sessions to provide an estimate of long-term instrumental precision. We obtain a value of +0.36 ± 0.06‰ (2SD, n = 772; runs = 56), in agreement with consensus values (Hunt 2025; Conway et al., 2013). Therefore, we consider a 2SD uncertainty of 0.06‰ as an estimate of analytical precision, and have applied it to all samples, except for low concentration samples where the larger internal error is considered a more conservative estimate of uncertainty. Dissolved Fe concentrations were calculated using the isotope dilution technique based on on-peak blank, interference and mass-bias corrected&amp;amp;nbsp;&amp;lt;sup&amp;gt;57&amp;lt;/sup&amp;gt;Fe/&amp;lt;sup&amp;gt;56&amp;lt;/sup&amp;gt;Fe ratios measured simultaneously with isotope analysis. We express uncertainty (1SD) on Fe concentrations as 2%, based on Conway et al. (2013).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/880515.rdf" xlink:title="OCE-2148836" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-2148836 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=2148836</gmx:Anchor>
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This project will investigate how groundwater discharge delivers important nutrients to the coastal ecosystems of the West Florida Shelf. Preliminary studies indicate that groundwater may supply both dissolved organic nitrogen (DON) and iron in this region. In coastal ecosystems like the West Florida Shelf that have very low nitrate and ammonium concentrations, DON is the main form of nitrogen available to organisms. Nitrogen cycling is strongly affected by iron availability because iron is essential for both photosynthesis and for nitrogen fixation. This study will investigate the sources and composition of DON and iron, and their influence on the coastal ecosystem. The team will sample offshore groundwater wells, river and estuarine waters, and conduct two expeditions across the West Florida Shelf in winter and summer. Investigators will participate in K-12 and outreach activities to increase awareness of the project and related science. The project will fund the work of six graduate and eight undergraduate students across five institutions, furthering NSF’s goals of education and training.&lt;/p&gt;
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&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;SGD Wells&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Submarine groundwater samples were collected by U.S. Geological survey (USGS) small boat from three offshore well transects, each with three well location. Samples were taken from well head (GWd) and from surface (SB) and bottom waters (BW). Divers, using acid-cleaned Teflon tubing attached to a trace metal clean diaphragm pump. First, bottom waters were collected, then the well uncapped, adequately purged, and sampled. All samples were filtered through 0.2 um Acropak Supor Cartridges (Pall, USA) into acid-cleaned LDPE bottles. NC5, NC10, NC15 = Nature Coast Transect, IRB25, IRB30, IRB35 = Indian Rocks Transect, VH45, VH50, VH55 = Venice Headlands Transect. More details are provided in Hunt (2025).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;Rivers and Estuaries&amp;lt;/em&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;River Sample sites were located on land and samples were collected from five rivers (Hillsborough, Alafia, Manatee, Peace, and Caloosahatchee), using trace metal clean protocols. Estuary samples were collected in collaboration with Mote Marine Laboratory via small boat (RV Eugenie Clark), also using trace metal clean protocols. All water samples for dissolved Fe and d56Fe were syringe filtered using acid-cleaned 50 mL Henke Jet HDPE syringes and 0.2 um PVDF membrane Titan3 syringe filters into acid-cleaned LDPE bottles. AR1-2 = Alafia River, HB1-2 = Hillsborough, MR1-2 = Manatee, PR1 = Peace River, CR1 = Caloosahatchee, CS and E= Estuary sample locations. More details are provided in Hunt (2025).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sample Processing&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples were acidified back on shore at the University of South Florida (USF) using 2.4 mL 10 M Teflon-distilled HCl per liter of sample and stored for at least 6 months before processing.&amp;amp;nbsp;Samples were then processed for dissolved Fe isotope and concentration analysis at the University of South Florida following Sieber et al. (2019), modified from Conway et al (2013). Briefly, an Fe double-spike was added prior to batch extraction using Nobias PA-1 chelating resin, followed by purification by anion-exchange chromatography using AG-MP1 resin. Concentration and isotope analyses were performed on a Thermo Neptune Plus MC-ICPMS (Multicollecter Inductively Coupled Plasma Mass Spectrometer)&amp;amp;nbsp;in the Tampa Bay Plasma Facility at the University of South Florida using the double spike technique via a ~100 uL min&amp;lt;sup&amp;gt;-1&amp;lt;/sup&amp;gt;&amp;amp;nbsp;PFA nebulizer and Apex Ω introduction system, Pt Jet Sampler cone and an Al X skimmer cone.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sample Analysis&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Dissolved Fe stable isotope ratios are expressed in delta notation (δ&amp;lt;sup&amp;gt;56&amp;lt;/sup&amp;gt;Fe) relative to the IRMM-014 standard. A secondary Fe standard, NIST-3126, was analyzed over 56 sessions to provide an estimate of long-term instrumental precision. We obtain a value of +0.36 ± 0.06‰ (2SD, n = 772; runs = 56), in agreement with consensus values (Hunt 2025; Conway et al., 2013). Therefore, we consider a 2SD uncertainty of 0.06‰ as an estimate of analytical precision, and have applied it to all samples, except for low concentration samples where the larger internal error is considered a more conservative estimate of uncertainty. Dissolved Fe concentrations were calculated using the isotope dilution technique based on on-peak blank, interference and mass-bias corrected&amp;amp;nbsp;&amp;lt;sup&amp;gt;57&amp;lt;/sup&amp;gt;Fe/&amp;lt;sup&amp;gt;56&amp;lt;/sup&amp;gt;Fe ratios measured simultaneously with isotope analysis. We express uncertainty (1SD) on Fe concentrations as 2%, based on Conway et al. (2013).&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;Data was processed in Microsoft Excel using an in-house double spike reduction scheme from Sieber et al (2021), based on Siebert et al (2001).&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gmd:description>
                  <gco:CharacterString>- Loaded sheet 1 from &amp;quot;BCO-DMO_STING_Rivers_Estuaries_Wells_Conway V1.0.xlsx&amp;quot; (xlsx format) using filename as resource name; missing values treated as empty string, &amp;quot;nd&amp;quot;, and &amp;quot;NaN&amp;quot;; duplicate headers deduplicated
- Converted DateTime field from &amp;quot;%m/%d/%y %H:%M&amp;quot; to &amp;quot;%Y-%m-%dT%H:%M&amp;quot; datetime format, stored back to DateTime field
- Edited row 57: set Longitude to &amp;quot;-81.97959&amp;quot; from &amp;quot;81.97959&amp;quot;
- Renamed deduplicated fields: &amp;quot;n (1)&amp;quot; to &amp;quot;n_dFe&amp;quot;, &amp;quot;n (2)&amp;quot; to &amp;quot;n_d56Fe&amp;quot;, &amp;quot;DateTime&amp;quot; to &amp;quot;DateTime_Local&amp;quot;, &amp;quot;2SD&amp;quot; to &amp;quot;SD_2&amp;quot;, to comply with BCO-DMO naming conventions (parameter should not start with number)
- Converted DateTime_Local from &amp;quot;%Y-%m-%dT%H:%M&amp;quot; (America/New_York) to &amp;quot;%Y-%m-%dT%H:%MZ&amp;quot; (UTC), stored in new field DateTime_UTC
- Exported file to &amp;quot;995970_v1_sting_fe_and_fe_isotopes.csv&amp;quot;</gco:CharacterString>
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				    <gco:CharacterString>WHOI MS#36</gco:CharacterString>
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				    <gco:CharacterString>Woods Hole</gco:CharacterString>
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				    <gco:CharacterString>02543</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/645675.rdf" xlink:title="Diving Mask and Snorkel" xlink:actuate="onRequest">Diver</gmx:Anchor>
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            <gco:CharacterString>PI Supplied Instrument Name: Diver PI Supplied Instrument Description:Divers, using acid-cleaned teflon tubing attached to a trace metal clean diaphragm pump.  Instrument Name: Diving Mask and Snorkel Instrument Short Name:   Instrument Description: A diving mask (also half mask, dive mask or scuba mask) is an item of diving equipment that allows underwater divers, including, scuba divers, free-divers, and snorkelers to see clearly underwater.

Snorkel: A breathing apparatus for swimmers and surface divers that allows swimming or continuous use of a face mask without lifting the head to breathe, consisting of a tube that curves out of the mouth and extends above the surface of the water.</gco:CharacterString>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/530.rdf" xlink:title="Inductively Coupled Plasma Mass Spectrometer" xlink:actuate="onRequest">Thermo Neptune Multicollecter Inductively Coupled Plasma Mass Spectrometer</gmx:Anchor>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/726.rdf" xlink:title="Pump" xlink:actuate="onRequest">Trace metal clean diaphragm pump</gmx:Anchor>
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