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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/840678.rdf" xlink:actuate="onRequest">Water column data from samples collected on R/V Hugh Sharp cruise HRS1709 in the Chesapeake Bay in August 2017</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Luther, G. W., Tebo, B. M. (2021) Water column data from samples collected on R/V Hugh Sharp cruise HRS1709 in the Chesapeake Bay in August 2017. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2021-02-17 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.840678.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Water column Chesapeake Bay 2017 Dataset Description:  Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;In situ &amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;strong&amp;gt;pump profiler cast&amp;lt;/strong&amp;gt; refers to profiling with a pump profiler for O₂ and H₂S using solid state gold-amalgam electrodes for voltammetry (Luther et al, 2008; Analytical Instrument Systems DLK-60). Water was pumped aboard to make measurements on discrete samples for Mn and Fe speciation as well. See Hudson et al (2019) for more information.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples for Mn and Fe parameters were filtered through 0.20 um filters. Whatman track etched polycarbonate filters were soaked in 1M HCl for 1 week before rinsing and storage in DI.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;C parameters&amp;lt;/strong&amp;gt; performed by Dr. Wei-Jun Cai's group for:&amp;lt;br /&amp;gt;
TA - Open cell Gran titration with semi-automatic AS-ALK2 Apollo Scitech titrator;&amp;lt;br /&amp;gt;
pH - glass electrode, NBS buffers;&amp;lt;br /&amp;gt;
DIC - infrared CO₂ analyzer (AS-C3, Apollo Scitech).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Uses Dickson CRM for calibration. DIC/TA samples were filtered (0.45um) and fixed with 100 ul of saturated mercury bichloride. Uses the methods of Gran (1952) and Huang, et al. (2012).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Dissolved Mn parameters:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
The porphyrin spectrophotometric method of Madison et al (2011, 2013) measures dissolved Mn(II), Mn(III) bound to weaker ligands and total Mn. Method includes calibration and intercomparison of totals with other instrumentation (ICP, AA). Detection limit is 0.050 micromolar. Detection limit (DL) is 50 micromolar with a 1 cm path length cell.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Modification of Madison et al for Mn(III) bound to strong ligands by adding a reducing agent to a separate subsample with the porphyrin to obtain total Mn (Oldham 2015, 2017; Thibault de Chanvalon and Luther, 2019). Mn(III) bound to strong ligand complexes is determined by difference. Typically, triplicate measurements performed. Detection limit can be extended to 3.0 nanomolar with a 1m path length cell.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Modification of Madison et al. for water column samples by adding higher Cd(II) so that cadmium-chloride complex formation would not inhibit cadmium-porphyrin formation and thus incorporation of Mn into the porphyrin by Cd replacement (Thibault de Chanvalon and Luther, 2019, this work). This modification enhanced the kinetics of the reaction progress for both Mn(II) and weak Mn(III)-L complexes.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;MnO&amp;lt;/strong&amp;gt;ₓ&amp;lt;strong&amp;gt; on unfiltered samples&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
The leucoberbelein blue method is that of Jones et al (2019, this work) in 1 cm cells, but can be modified for longer path length cells.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;H₂&amp;lt;/strong&amp;gt;&amp;lt;strong&amp;gt;S&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
O₂ and H₂S by the voltammetry method of Luther et al (2008) and Hudson et al (2019) using a flow cell. O₂ also from CTD sensor.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Fe parameters&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
The method of Stookey (1972) is used to determine dissolved Fe(II) and on addition if hydroxylamine Fe total. Fe(III) is determined by difference. Modified and calibrated by many including Lewis et al (2007). Typically, triplicate measurements performed.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Nitrite&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Nitrite as determined by the method of Grasshoff (1983).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Dissolved Mn speciation references:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Madison et al. (2011)&amp;lt;br /&amp;gt;
Madison et al. (2013)&amp;lt;br /&amp;gt;
Oldham et al. (2015)&amp;lt;br /&amp;gt;
Oldham et al. (2017) - Here, we modified the method of Madison et al. (2011) for water column samples to achieve a detection limit of 3.0 nM (3 times the standard deviation of a blank) by using a 100-cm liquid waveguide capillary cell and the addition of a heating step as well as a strong reducing agent for Mn. Speciation [Mn³⁺ = Mn&amp;lt;sub&amp;gt;T&amp;lt;/sub&amp;gt; – Mn²⁺]. As weak Mn(III)-L complexes could not be measured in our previous work (Oldham et al, 2015; paper above), this method was used throughout this cruise.&amp;lt;br /&amp;gt;
Thibault de Chanvalon &amp;amp;amp; Luther (2019) - Here, we modified the method of Madison et al. (2011) for water column samples by adding higher Cd(II) so that cadmium-chloride complex formation would not inhibit cadmium-porphyrin formation and thus incorporation of Mn into the porphyrin by Cd replacement. This modification enhanced the kinetics of the reaction progress for both Mn(II) and weak Mn(III)-L complexes.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Dissolved Fe speciation references:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Stookey (1970)&amp;lt;br /&amp;gt;
Lewis et al. (2007)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;H2S (in situ voltammetry)– water column:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Luther et al. (2008)&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
&amp;lt;strong&amp;gt;H2S (UV-Vis spectrophotometry) – sedimentary porewater samples:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Luther et al. (2011)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;MnOₓ&amp;lt;strong&amp;gt; &amp;lt;/strong&amp;gt;solids:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Jones et al. (2019)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;pH and inorganic carbon parameters:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Gran (1952)&amp;lt;br /&amp;gt;
Huang et al. (2012)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Nitrite:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Determination of nitrite, nitrate, oxygen, thiosulphate in Grasshoff et al. (1983)&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/715476.rdf" xlink:title="OCE-1558738" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1558738 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1558738</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/715486.rdf" xlink:title="OCE-1558692" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1558692 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1558692</gmx:Anchor>
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Manganese (Mn) is an important trace nutrient for biological growth in marine organisms. In the past, all Mn dissolved in seawater was thought to exist in only one chemical form: Mn(II). Recent work in waters and sediments with little or no oxygen has shown that Mn(III) can be the dominant form of dissolved Mn and can even be present in oxygenated water if attached to specific organic molecules called ligands. This research will further investigate these discoveries, aiming to quantify the chemical and microbiological processes responsible for Mn(III) cycling under varying oxygen concentrations. The research will compare field sites in the Broadkill River wetland, the Chesapeake Bay, and the Lower St. Lawrence Estuary; measuring the water column and sediments known to have strong oxygen gradients and different organic carbon sources that could change the availability and binding strength of ligands that would stabilize dissolved Mn(III). In some chemical forms, Mn tends to act like iron, so this research may have broader implications by helping marine chemists to understand more about iron cycling in similar oxygen gradients. With growing concerns over diminished oxygen concentrations (hypoxia) in the ocean, and particularly in coastal regions, understanding the reactions of Mn(III) with organic ligands across oxygen gradients could become important for understanding Mn availability to organisms. The project includes support for the participation and mentoring of one graduate student and two postdoctoral researchers, and there will be a U.S.-Canada collaboration. A variety of public outreach activities are planned with a K-12 teacher to be selected as a participant on a research cruise.&lt;/p&gt;
&lt;p&gt;Mn(III) has only recently been recognized as an important redox state for Mn in seawater. Previously, it was widely accepted that all Mn that passes through a 0.2 or 0.4 µm filter is dissolved Mn(II) while the retained portion is solid Mn(III, IV) oxide. Research in the Black Sea, the Baltic Sea, and the Chesapeake Bay has shown that soluble Mn(III) can be up to 100% of the dissolved Mn in the water column. Also, Mn(III) can exist as complexes with organic ligands in oxygenated seawater. This project will quantify and constrain the mechanisms surrounding weak and strong Mn(III) ligand transformations across vertical and horizontal oxygen gradients. Field sites to be studied include systems with a variety of organic carbon sources and oxygen dynamics: the Lower St. Lawrence Estuary, Chesapeake Bay, and Broadkill River wetland estuary. This research will continue to inform the fundamental shift that is taking place in our current understanding of Mn biogeochemistry in coastal systems. The results should also be applicable to redox processes involving Fe(III) ligand transformations, since Mn and Fe tend to exhibit similar redox chemistry under similar environmental conditions.&lt;/p&gt;</gco:CharacterString>
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	Name: Region
	Units: unitless
	Description: &lt;p&gt;Sampling location&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840884.rdf
	Name: cruise
	Units: unitless
	Description: &lt;p&gt;Cruise identifier&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840885.rdf
	Name: cast
	Units: unitless
	Description: &lt;p&gt;Cast number&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840886.rdf
	Name: sample
	Units: unitless
	Description: &lt;p&gt;Bottle number or pump-profiler number&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840887.rdf
	Name: date
	Units: unitless
	Description: &lt;p&gt;Date of sample collection; format: YYYY-MM-DD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840888.rdf
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	Description: &lt;p&gt;Time of sample collection in the local time zone (US Eastern Daylight); format: hh:mm&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840889.rdf
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	Units: unitless
	Description: &lt;p&gt;Date and time of sample collection (UTC/GMT) formatted to ISO8601 standard: YYYY-mm-ddTHH:MMZ&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840890.rdf
	Name: Latitude
	Units: degrees North
	Description: &lt;p&gt;Latitude in decimal degrees; positive values = North&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840891.rdf
	Name: Longitude
	Units: degrees East
	Description: &lt;p&gt;Longitude in decimal degrees; negative value = West&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840892.rdf
	Name: depth
	Units: meters (m)
	Description: &lt;p&gt;Sample depth&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840893.rdf
	Name: temperature
	Units: degrees Celsius
	Description: &lt;p&gt;Water temperature from CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840894.rdf
	Name: salinity
	Units: PSU
	Description: &lt;p&gt;Salinity from CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840895.rdf
	Name: CTD_O2
	Units: micromolar (uM)
	Description: &lt;p&gt;O2 from CTD&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840896.rdf
	Name: O2_100_pcnt_sat_at_T
	Units: micromolar (uM)
	Description: &lt;p&gt;100% O2 sat at T&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840897.rdf
	Name: pcnt_O2_sat
	Units: unitless (percent)
	Description: &lt;p&gt;Percent O2 saturation&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840898.rdf
	Name: fluor_voltage
	Units: volts
	Description: &lt;p&gt;Fluorescence (chl) voltage&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840899.rdf
	Name: transmiss_voltage
	Units: volts
	Description: &lt;p&gt;Transmissometry voltage&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840900.rdf
	Name: H2S
	Units: micromolar (uM)
	Description: &lt;p&gt;H2S&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840901.rdf
	Name: TA
	Units: micromoles per kilogram (umol/kg)
	Description: &lt;p&gt;TA&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840902.rdf
	Name: DIC
	Units: micromoles per kilogram (umol/kg)
	Description: &lt;p&gt;DIC&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840903.rdf
	Name: pH_NBS
	Units: unitless
	Description: &lt;p&gt;pH, NBS scale at 25 degrees C&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840904.rdf
	Name: pMnOx
	Units: micromolar (uM)
	Description: &lt;p&gt;Particulate MnOx; particulate on the 0.20 micrometer filter; single measurement; detection limit = 0.01 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840905.rdf
	Name: dMn2plus
	Units: micromolar (uM)
	Description: &lt;p&gt;Dissolved Mn2+;  filtered through 0.20 micrometer filters; detection limit = 0.05 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840906.rdf
	Name: dMn2plus_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of dMn2plus&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840907.rdf
	Name: dMn3plus
	Units: micromolar (uM)
	Description: &lt;p&gt;Dissolved Mn3+ by difference; Mn3+ = [MnT - Mn2+]; detection limit = 0.05 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840908.rdf
	Name: dMn3plus_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of dMn3plus&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840909.rdf
	Name: dMnTotal
	Units: micromolar (uM)
	Description: &lt;p&gt;Mn total; filtered through 0.20 micrometer filters; detection limit = 0.05 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840910.rdf
	Name: dMnTotal_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of dMnTotal&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840911.rdf
	Name: dFe2plus
	Units: micromolar (uM)
	Description: &lt;p&gt;Dissolved Fe2+; filtered through 0.20 micrometer filters; detection limit = 0.02 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840912.rdf
	Name: dFe2plus_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of dFe2plus&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840913.rdf
	Name: pFe2plus
	Units: micromolar (uM)
	Description: &lt;p&gt;Particulate Fe2+; no filtering of water; detection limit = 0.02 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840914.rdf
	Name: pFe2plus_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of pFe2plus&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840915.rdf
	Name: dFeTotal
	Units: micromolar (uM)
	Description: &lt;p&gt;Dissolved Fe total =  FeT = [Fe2+] + [Fe3+]; filtered through 0.20 micrometer filters; detection limit = 0.02 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840916.rdf
	Name: dFeTotal_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of dFeTotal&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840917.rdf
	Name: pFeTotal
	Units: micromolar (uM)
	Description: &lt;p&gt;Particulate Fe total =  FeT = [Fe2+] + [Fe3+]; no filtering of water; detection limit = 0.02 uM&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840918.rdf
	Name: pFeTotal_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of pFeTotal&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840919.rdf
	Name: dFe3plus
	Units: micromolar (uM)
	Description: &lt;p&gt;Dissolved Fe3+ by difference; Fe3+ = [FeT - Fe2+]&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840920.rdf
	Name: dFe3plus_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of dFe3plus&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840921.rdf
	Name: pFe3plus
	Units: micromolar (uM)
	Description: &lt;p&gt;Particulate Fe3+ by difference; Fe3+ =  [FeT - Fe2+]&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840922.rdf
	Name: pFe3plus_stdev
	Units: micromolar (uM)
	Description: &lt;p&gt;Standard deviation of pFe3plus&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840923.rdf
	Name: Nitrite
	Units: micromolar (uM)
	Description: &lt;p&gt;Nitrite; single measurement; dissolved, filtered through 0.20 micrometer filters&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/840924.rdf
	Name: Comments
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	Description: &lt;p&gt;Notes/comments about the sampling events&lt;/p&gt; 
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&amp;lt;p&amp;gt;Samples for Mn and Fe parameters were filtered through 0.20 um filters. Whatman track etched polycarbonate filters were soaked in 1M HCl for 1 week before rinsing and storage in DI.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;C parameters&amp;lt;/strong&amp;gt; performed by Dr. Wei-Jun Cai's group for:&amp;lt;br /&amp;gt;
TA - Open cell Gran titration with semi-automatic AS-ALK2 Apollo Scitech titrator;&amp;lt;br /&amp;gt;
pH - glass electrode, NBS buffers;&amp;lt;br /&amp;gt;
DIC - infrared CO₂ analyzer (AS-C3, Apollo Scitech).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Uses Dickson CRM for calibration. DIC/TA samples were filtered (0.45um) and fixed with 100 ul of saturated mercury bichloride. Uses the methods of Gran (1952) and Huang, et al. (2012).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Dissolved Mn parameters:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
The porphyrin spectrophotometric method of Madison et al (2011, 2013) measures dissolved Mn(II), Mn(III) bound to weaker ligands and total Mn. Method includes calibration and intercomparison of totals with other instrumentation (ICP, AA). Detection limit is 0.050 micromolar. Detection limit (DL) is 50 micromolar with a 1 cm path length cell.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Modification of Madison et al for Mn(III) bound to strong ligands by adding a reducing agent to a separate subsample with the porphyrin to obtain total Mn (Oldham 2015, 2017; Thibault de Chanvalon and Luther, 2019). Mn(III) bound to strong ligand complexes is determined by difference. Typically, triplicate measurements performed. Detection limit can be extended to 3.0 nanomolar with a 1m path length cell.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Modification of Madison et al. for water column samples by adding higher Cd(II) so that cadmium-chloride complex formation would not inhibit cadmium-porphyrin formation and thus incorporation of Mn into the porphyrin by Cd replacement (Thibault de Chanvalon and Luther, 2019, this work). This modification enhanced the kinetics of the reaction progress for both Mn(II) and weak Mn(III)-L complexes.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;MnO&amp;lt;/strong&amp;gt;ₓ&amp;lt;strong&amp;gt; on unfiltered samples&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
The leucoberbelein blue method is that of Jones et al (2019, this work) in 1 cm cells, but can be modified for longer path length cells.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;H₂&amp;lt;/strong&amp;gt;&amp;lt;strong&amp;gt;S&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
O₂ and H₂S by the voltammetry method of Luther et al (2008) and Hudson et al (2019) using a flow cell. O₂ also from CTD sensor.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Fe parameters&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
The method of Stookey (1972) is used to determine dissolved Fe(II) and on addition if hydroxylamine Fe total. Fe(III) is determined by difference. Modified and calibrated by many including Lewis et al (2007). Typically, triplicate measurements performed.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Nitrite&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Nitrite as determined by the method of Grasshoff (1983).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Dissolved Mn speciation references:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Madison et al. (2011)&amp;lt;br /&amp;gt;
Madison et al. (2013)&amp;lt;br /&amp;gt;
Oldham et al. (2015)&amp;lt;br /&amp;gt;
Oldham et al. (2017) - Here, we modified the method of Madison et al. (2011) for water column samples to achieve a detection limit of 3.0 nM (3 times the standard deviation of a blank) by using a 100-cm liquid waveguide capillary cell and the addition of a heating step as well as a strong reducing agent for Mn. Speciation [Mn³⁺ = Mn&amp;lt;sub&amp;gt;T&amp;lt;/sub&amp;gt; – Mn²⁺]. As weak Mn(III)-L complexes could not be measured in our previous work (Oldham et al, 2015; paper above), this method was used throughout this cruise.&amp;lt;br /&amp;gt;
Thibault de Chanvalon &amp;amp;amp; Luther (2019) - Here, we modified the method of Madison et al. (2011) for water column samples by adding higher Cd(II) so that cadmium-chloride complex formation would not inhibit cadmium-porphyrin formation and thus incorporation of Mn into the porphyrin by Cd replacement. This modification enhanced the kinetics of the reaction progress for both Mn(II) and weak Mn(III)-L complexes.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Dissolved Fe speciation references:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Stookey (1970)&amp;lt;br /&amp;gt;
Lewis et al. (2007)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;H2S (in situ voltammetry)– water column:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Luther et al. (2008)&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
&amp;lt;strong&amp;gt;H2S (UV-Vis spectrophotometry) – sedimentary porewater samples:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Luther et al. (2011)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;MnOₓ&amp;lt;strong&amp;gt; &amp;lt;/strong&amp;gt;solids:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Jones et al. (2019)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;pH and inorganic carbon parameters:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Gran (1952)&amp;lt;br /&amp;gt;
Huang et al. (2012)&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Nitrite:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Determination of nitrite, nitrate, oxygen, thiosulphate in Grasshoff et al. (1983)&amp;lt;/p&amp;gt;</gco:CharacterString>
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&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;BCO-DMO Processing:&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
- converted date field to YYYY-MM-DD format;&amp;lt;br /&amp;gt;
- added date/time column in ISO8601 format (UTC/GMT);&amp;lt;br /&amp;gt;
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