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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/915912.rdf" xlink:actuate="onRequest">Sediment core porewater and particulate measurements from three sites on the Louisiana Shelf sampled during R/V Pelican cruises from December 2021 through August 2022</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Lemke, L. R., Roseburrough, R., Rahman, S., Krause, J. W. (2023) Sediment core porewater and particulate measurements from three sites on the Louisiana Shelf sampled during R/V Pelican cruises from December 2021 through August 2022. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2023-12-11 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/915912 [access date]</gco:CharacterString>
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        <gco:CharacterString>Sediment porewater and particulates on Louisiana Shelf Dec 2021-Aug 2022 Dataset Description: &amp;lt;p&amp;gt;This dataset&amp;amp;nbsp;provides information on silica cycling in coastal sediments from the Louisiana shelf region after an extreme storm event. When Hurricane Ida made landfall on August 29th, 2021, this Category 4 storm disrupted&amp;amp;nbsp;sediments of the proximal coastal zone and possibly altered redox and diagenetic conditions. As part of a multi-proxy approach, this data can help inform how an extreme event altered biogenic silica burial over the 10 to 12 months following the storm. Sampling for initial conditions occurred 13 days prior to the storm event from topset delta sediment. Data from this companion project can be viewed here: https://www.bco-dmo.org/dataset/945927.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;I. Field sampling&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Sample collection took place during R/V Pelican cruises on the Louisiana Shelf in the northern part of the Gulf of Mexico.&amp;amp;nbsp;At each site, an 8-spot&amp;amp;nbsp;Ocean Instruments Multi-corer&amp;amp;nbsp;collected sediment that was sectioned in 2 cm intervals and placed into 50mL metal clean, acid washed tubes, pre-weighed and labeled microcentrifuge tubes for porosity, and freezer-safe Ziploc bags. Tubes were centrifuged at 3500 rpm for 10 minutes to extract and filter supernatant. The filtered supernatant was placed into a metal clean/acid washed tube and frozen for later analysis of metal and dissolved silica. The 50mL tube of sediment was frozen at -20°C for further analysis.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;II. Porewater Dissolved Constituents&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Where there was sufficient supernatant (porewater) from the centrifuged sediment sample, it was divided for three different analyses: dissolved silica analysis (DSi), nutrient analysis (Skalar), and metal concentrations (ICPMS).&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;1. &amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;DSi analysis&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;: 50uL of porewater was analyzed for dissolved Si(OH)&amp;lt;sub&amp;gt;4&amp;lt;/sub&amp;gt;&amp;amp;nbsp;concentration using a spectrophotometric molybdate-blue method (Brzezinski &amp;amp;amp; Nelson, 1986).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;2.&amp;amp;nbsp;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Skalar Analysis (N+N, NH4, PO4)&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;: Porewater was diluted with Milli‐Q (18.2 MΩ&amp;amp;nbsp;* cm) water and run through a Skalar Analyzer for Nitrate and Nitrite, Phosphorus, and Ammonia. For detection limits, please refer to the&amp;amp;nbsp;descriptions in the Parameters section below.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;3.&amp;amp;nbsp;&amp;lt;em&amp;gt;&amp;lt;strong&amp;gt;ICPMS (Metal Concentrations)&amp;lt;/strong&amp;gt;&amp;lt;/em&amp;gt;: Porewater was reconstituted in dilute HNO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;amp;nbsp;and diluted to minimize salt interferences before analysis on a Thermo Scientific Element XR High Resolution-ICP-MS housed at the University of Southern Mississippi at the Stennis Space Center. The following elements are reported in the data from the ICPMS analysis:&amp;amp;nbsp; magnesium (Mg), sulfur (S),&amp;amp;nbsp;calcium (Ca), manganese (Mn), iron (Fe), potassium (K), cesium (Cs), uranium (U), lithium (Li), vanadium (V), cobalt (Co), nickel (Ni), copper (Cu), strontium (Sr), molybdenum (Mo), barium (Ba), phosphorus (P), and aluminum (Al), along with phosphorus (P) and silica (Si).&amp;amp;nbsp; For each element's detection limit, please see the description in the Parameters section below.&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sediments&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Sediments were analyzed for physical properties, chemical properties, phases of silica, and isotopic composition. Each&amp;amp;nbsp;section below describes the specific methods in greater detail.&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;III. Sediment properties&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;em&amp;gt;&amp;lt;strong&amp;gt;Porosity&amp;lt;/strong&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;br /&amp;gt;
For porosity measurements, microcentrifuge tubes were placed in a drying oven at 60°C until the sediment was dry. Once dried, tubes were weighed. Porosity was calculated as in Comeaux et al. (2012).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;&amp;lt;strong&amp;gt;Loss on ignition (LOI)&amp;lt;/strong&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;br /&amp;gt;
For loss on ignition (LOI) analysis, dried sediment was ground into a fine consistency using a mortar and pestle. Then 1g of the ground sediment was weighed into pre-muffled and pre-weighed porcelain crucibles. To remove any carbon from the presence of calcium carbonate, samples were fumed by adding 1mL of mili-Q to each crucible and placing samples into a desiccator with 10 mL of 12M HCl for 6 hours (Harris et al. 2001,&amp;amp;nbsp;Ramnarine et al. 2011, Walthert et al. 2010). After 6 hours, samples were placed in a vacuum oven for roughly 16 hours, until dry (Ramnarine et al. 2011, Walthert et al. 2010). Once dry, samples were kept in the oven and weighed one at a time to keep moisture out of samples. If sample was still acidic (yellow in color), 1 mL of mili-Q was added and the sample was dried again. Sediment was ground again into a fine powder.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;After the above preparation, fumed and ground sediment was weighed (100 mg) in triplicate into pre-weighed and muffled liquid scintillation (LSC) vials. Samples were combusted at 550°C for 6 hours (Kemp et al. 2021). After combustion, weights were recorded, and loss of organic matter was calculated (Kemp et al. 2021).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;IV. Sediment Silica Pools&amp;lt;/strong&amp;gt;&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Sequential Extractions&amp;lt;/em&amp;gt;&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Frozen samples were thawed, homogenized, and 50 mg were weighed in triplicates (per depth) into pre-labeled 50 mL centrifuge tubes (Krause et al., 2017; Pickering et al., 2020). Samples with procedural blanks (in triplicate) then went through the sequential extraction process. The sequential extraction methodology separates silica into operationally defined pools based on kinetics, reaction conditions and reaction sequence (DeMaster, 1981; Michalopoulos and Aller, 2004; Rahman et al., 2016; Pickering et al., 2020).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Operational Definitions&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Based on prior studies, we use the following nomenclature:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;1. &amp;lt;strong&amp;gt;Si-HCl&amp;lt;/strong&amp;gt;: Mild acid-leachable pre-treatment; Highly reactive silica associated with authigenic clays and metal oxide coatings (Michalopoulos and Aller, 2004).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;2. &amp;lt;strong&amp;gt;Si-Alk&amp;lt;/strong&amp;gt;: Mild alkaline-leachable digestion completed after acid pretreatment; Frees reactive silica associated with the biogenic silica pool (Michalopoulos and Aller, 2004).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;3. &amp;lt;strong&amp;gt;Si-NaOH (Alk)&amp;lt;/strong&amp;gt;: Harsh NaOH digestion done after Si-HCl and Si-Alk (Rahman et al., 2016; Rahman et al., 2017); Associated with the reactive lithogenic Si (LSi) pool and the comparatively refractory “dark bSiO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;” (e.g. sponge spicules and Rhizaria).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;4.&amp;amp;nbsp;&amp;lt;strong&amp;gt;tbSi&amp;lt;/strong&amp;gt;: Following the traditional definition of biogenic silica (DeMaster, 1981), with no acid pre-treatment.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;5.&amp;amp;nbsp;&amp;lt;strong&amp;gt;Si-NaOH (TbSi)&amp;lt;/strong&amp;gt;: Harsh NaOH digestion done after T-bSi.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;strong&amp;gt;V. Sediment Organic matter&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Preparation&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Same preparation as that listed above for Loss on Ignition&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Particulate Organic Carbon and Nitrogen content and isotopes (δ&amp;lt;sup&amp;gt;13&amp;lt;/sup&amp;gt;C and δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N)&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
After fumigation (explained above), ~60 to 70 mg of sediment were packed in 5x9mm silver capsules, which were then packed in tin 5x9mm capsules in triplicate (UC Davis protocol recommendation). Samples were placed in a 96 well plate and kept in a desiccator until shipped to UC Davis for isotopic (δ13C and δ15N) analysis (Krause et al. 2017).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Results from UC Davis had an absolute accuracy for calibrated reference materials of&amp;amp;nbsp;±0.04 ‰ (±0.05 ‰ SD) for δ13C and ±0.05 ‰ (±0.05 ‰ SD) for δ15N. Core depth 24-26cm was the only sample below detection (9.7ug) for δ15N, which is represented as 0 on the data sheet.&amp;lt;/p&amp;gt;</gco:CharacterString>
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This project will take advantage of the passage of Hurricane Ida across the northern Gulf of Mexico shelf in August, 2021 to study important aspects of the cycling of silica in coastal sediments. In coastal systems, water column primary productivity is dominated by diatoms, a group of phytoplankton which produce a shell of amorphous biogenic silica. This biogenic silica can either be buried in its original unaltered form or undergo chemical reactions that convert it to aluminosilicate minerals (e.g. marine clays). This latter process is important in global chemical budgets for many elements, including carbon. One of the factors that influences whether silicon is buried as biogenic silica or converted to aluminosilicates may be the amount of oxygen in the sediments. Storms mix the ocean waters and can add oxygen to sediments in shallow water, potentially changing the silica balance. The investigators collected sediment samples in early August, 2021, two weeks before Hurricane Ida. Sampling through the year after the storm will allow them to test whether storms affect silica cycling. This project will support an early-career investigator and undergraduate student researchers.&lt;/p&gt;
&lt;p&gt;Tropical and subtropical coastal deposition systems sequester 25-40% of the global silica sink, a disproportionately large impact relative to their area. In the northern Gulf of Mexico seasonal water column stratification may impact how sedimentary biogenic silica is processed and preserved by limiting oxygen injections into the benthos, seasonally driving biogenic silica burial efficiency. Hurricane Ida moved through the Mississippi Delta and adjacent Louisiana shelf at the end of August 2021. Thirteen days prior to Hurricane Ida’s landfall in Port Fourchon, LA, in August 2021, the team collected sediment cores at 3 sites in the topset delta sediment between the Southwest Pass (major Mississippi River distributary) and Cocodrie, LA; all sites experienced Category 4 hurricane conditions from Ida with maximum sustained winds of 130 knots (67 m/s). Ida, a much stronger storm than either Hurricanes Harvey or Nate in 2017, likely introduced oxygen into the sediment of the proximal coastal zone, perhaps enough to turn most of the top meter or so of the sediment column oxic. The investigators hypothesize that the storm-induced change in redox and diagenetic conditions initially favored burial of biogenic silica rather than an authigenic aluminosilicate. Using a multi-proxy approach, this project will analyze how this major storm event altered biogenic silica burial over the course of ten months.&lt;/p&gt;
&lt;p&gt;This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.&lt;/p&gt;</gco:CharacterString>
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        <gmd:MD_TopicCategoryCode>oceans</gmd:MD_TopicCategoryCode>
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            <gco:CharacterString>BCO-DMO catalogue of parameters from Sediment core porewater and particulate measurements from three sites on the Louisiana Shelf sampled during R/V Pelican cruises from December 2021 through August 2022</gco:CharacterString>
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            http://lod.bco-dmo.org/id/dataset-parameter/916741.rdf
	Name: Cruise
	Units: unitless
	Description: &lt;p&gt;Cruise name&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916742.rdf
	Name: Cruise_ID
	Units: unitless
	Description: &lt;p&gt;Cruise ID&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916743.rdf
	Name: DateTime_Local
	Units: unitless
	Description: &lt;p&gt;Local datetime of event&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916744.rdf
	Name: Event_number
	Units: unitless
	Description: &lt;p&gt;Event number described by GMT date and time&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916745.rdf
	Name: Activity
	Units: unitless
	Description: &lt;p&gt;Sediment collection activity for event&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916746.rdf
	Name: Latitude
	Units: decimal degrees
	Description: &lt;p&gt;Latitude for event&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916747.rdf
	Name: Longitude
	Units: decimal degrees
	Description: &lt;p&gt;Longitude for event&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916748.rdf
	Name: Station_Number
	Units: unitless
	Description: &lt;p&gt;Station number of event&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916749.rdf
	Name: Bottom_Depth
	Units: meters (m)
	Description: &lt;p&gt;Station bottom depth&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916750.rdf
	Name: Core_Section_Depth
	Units: centimeter (cm)
	Description: &lt;p&gt;Core depth shallow and deep range for each sample collected&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916751.rdf
	Name: Core_Section_Mid_Depth
	Units: centimeter (cm)
	Description: &lt;p&gt;Core depth median for each sample collected&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916752.rdf
	Name: PW_orthosilicic_acid_avg_spec
	Units: micromoles per liter (umol/L)
	Description: &lt;p&gt;Average particulate dissolved silica in porewater using spectrophotometric method&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916753.rdf
	Name: PW_orthosilicic_acid_stdev_spec
	Units: micromoles per liter (umol/L)
	Description: &lt;p&gt;Standard deviation of particulate dissolved silica in porewater using spectrophotometric method&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916754.rdf
	Name: PW_Phosphate_AA
	Units: micromoles per liter (umol/L)
	Description: &lt;p&gt;Porewater nutrients: Phosphate measured using an autoanalyzer. Detection limit = 0.062 umol/L.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916755.rdf
	Name: PW_Nitrate_AA
	Units: micromoles per liter (umol/L)
	Description: &lt;p&gt;Porewater nutrients: Nitrate measured using an autoanalyzer. Below detection (0.857 umol/L) represented as 0.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916756.rdf
	Name: PW_Nitrite_AA
	Units: micromoles per liter (umol/L)
	Description: &lt;p&gt;Porewater nutrients: Nitrite measured using an autoanalyzer. Below detection (0.041 umol/L) represented as 0.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916757.rdf
	Name: PW_Ammonium_AA
	Units: micromoles per liter (umol/L)
	Description: &lt;p&gt;Porewater nutrients: Ammonium measured using an autoanalyzer. Below detection = 1.704 umol/L.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916758.rdf
	Name: PW_Mg_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Magnesium. Estimated detection limit = 625 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916759.rdf
	Name: PW_Si_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Silicon. Estimated detection limit = 2018 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916760.rdf
	Name: PW_S_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Sulfur. Estimated detection limit = 580 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916761.rdf
	Name: PW_Ca_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Calcium. Estimated detection limit = 297 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916762.rdf
	Name: PW_Mn_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Manganese. Estimated detection limit = 6 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916763.rdf
	Name: PW_Fe_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Iron. Estimated detection limit = 20 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916764.rdf
	Name: PW_K_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Potassium. Estimated detection limit = 207 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916765.rdf
	Name: PW_Cs_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Cesium. Estimated detection limit = 0.01 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916766.rdf
	Name: PW_U_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Uranium. Estimated detection limit = &amp;lt;0.01 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916767.rdf
	Name: PW_Li_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Lithium. Estimated detection limit = 1.1 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916768.rdf
	Name: PW_V_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Vanadium. Estimated detection limit = 0.2 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916769.rdf
	Name: PW_Co_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Cobalt. Estimated detection limit = 0.2 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916770.rdf
	Name: PW_Ni_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Nickel. Estimated detection limit = 0.3 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916771.rdf
	Name: PW_Cu_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Copper. Estimated detection limit = 0.2 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916772.rdf
	Name: PW_Sr_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Strontium. Estimated detection limit = 14 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916773.rdf
	Name: PW_Mo_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Molybdenum. Estimated detection limit = 0.1 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916774.rdf
	Name: PW_Ba_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Barium. Estimated detection limit = 1.9 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916775.rdf
	Name: PW_P_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Phosphorus. Estimated detection limit = 8.1 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916776.rdf
	Name: PW_Al_ICPMS
	Units: parts per billion (ppb)
	Description: &lt;p&gt;ICPMS derived Porewater concentration: Aluminum. Estimated detection limit = 27 ppb.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916777.rdf
	Name: Sediment_Porosity_pct
	Units: dimensionless
	Description: &lt;p&gt;Porosity of each core sediment sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916778.rdf
	Name: Partic_Si_HCl_avg
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Average particulate silica after HCl leach&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916779.rdf
	Name: Partic_Si_HCl_stdev
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Standard deviation of dissolved particulate silica after HCl leach&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916780.rdf
	Name: Partic_Si_Alk_avg
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate average of dissolved silica after Si-Alk leach&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916781.rdf
	Name: Partic_Si_Alk_stdev
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate standard deviation of dissolved silica after Si-Alk leach&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916782.rdf
	Name: Partic_tbSi_avg
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate average of dissolved silica after tbSi leach&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916783.rdf
	Name: Partic_tbSi_stdev
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate standard deviation of dissolved silica after tbSi leach&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916784.rdf
	Name: Partic_Si_NaOH_from_Si_Alk_avg
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate average of dissolved silica after Si-NaOH from Si-Alk leach material&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916785.rdf
	Name: Partic_Si_NaOH_from_Si_Alk_stdev
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate standard deviation of dissolved silica after Si-NaOH from Si-Alk leach material&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916786.rdf
	Name: Partic_Si_NaOH_from_tbSi_avg
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate average of dissolved silica after Si-NaOH from tbSi leach material&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916787.rdf
	Name: Partic_Si_NaOH_from_tbSi_stdev
	Units: micromoles per gram (umol/g)
	Description: &lt;p&gt;Particulate standard deviation of dissolved silica after Si-NaOH from tbSi leach material&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916788.rdf
	Name: POC_d13C_avg
	Units: parts per mil (‰)
	Description: &lt;p&gt;Average particulate organic carbon isotopic composition&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916789.rdf
	Name: POC_d13C_stdev
	Units: parts per mil (‰)
	Description: &lt;p&gt;Standard deviation of particulate organic carbon isotopic composition&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916790.rdf
	Name: POC_Total_C_pct_avg
	Units: percent (%)
	Description: &lt;p&gt;Average total of particulate organic carbon&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916791.rdf
	Name: POC_Total_C_pct_stdev
	Units: percent (%)
	Description: &lt;p&gt;Standard deviation of averaged total particulate organic carbon&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916792.rdf
	Name: POC_d15N_Air_avg
	Units: parts per mil (‰)
	Description: &lt;p&gt;Average particulate organic nitrogen isotopic composition. Below detection represented as 0 (Below detection = 9.7ug)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916793.rdf
	Name: POC_d15N_Air_stdev
	Units: parts per mil (‰)
	Description: &lt;p&gt;Standard deviation of particulate organic nitrogen isotopic composition&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916794.rdf
	Name: POC_Total_N_pct_avg
	Units: percent (%)
	Description: &lt;p&gt;Average total of particulate organic nitrogen&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916795.rdf
	Name: POC_Total_N_pct_stdev
	Units: percent (%)
	Description: &lt;p&gt;Standard deviation of averaged total particulate organic nitrogen&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916796.rdf
	Name: Particulate_Sediment_LOI_pct
	Units: percent (%)
	Description: &lt;p&gt;Amount of organic matter lost per sediment sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/916797.rdf
	Name: ISO_DateTime_UTC
	Units: unitless
	Description: &lt;p&gt;Datetime of event in UTC and ISO8601 format&lt;/p&gt; 
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            <gco:CharacterString>GB/NERC/BODC &gt; British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;I. Field sampling&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Sample collection took place during R/V Pelican cruises on the Louisiana Shelf in the northern part of the Gulf of Mexico.&amp;amp;nbsp;At each site, an 8-spot&amp;amp;nbsp;Ocean Instruments Multi-corer&amp;amp;nbsp;collected sediment that was sectioned in 2 cm intervals and placed into 50mL metal clean, acid washed tubes, pre-weighed and labeled microcentrifuge tubes for porosity, and freezer-safe Ziploc bags. Tubes were centrifuged at 3500 rpm for 10 minutes to extract and filter supernatant. The filtered supernatant was placed into a metal clean/acid washed tube and frozen for later analysis of metal and dissolved silica. The 50mL tube of sediment was frozen at -20°C for further analysis.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;II. Porewater Dissolved Constituents&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Where there was sufficient supernatant (porewater) from the centrifuged sediment sample, it was divided for three different analyses: dissolved silica analysis (DSi), nutrient analysis (Skalar), and metal concentrations (ICPMS).&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;1. &amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;DSi analysis&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;: 50uL of porewater was analyzed for dissolved Si(OH)&amp;lt;sub&amp;gt;4&amp;lt;/sub&amp;gt;&amp;amp;nbsp;concentration using a spectrophotometric molybdate-blue method (Brzezinski &amp;amp;amp; Nelson, 1986).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;2.&amp;amp;nbsp;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Skalar Analysis (N+N, NH4, PO4)&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;: Porewater was diluted with Milli‐Q (18.2 MΩ&amp;amp;nbsp;* cm) water and run through a Skalar Analyzer for Nitrate and Nitrite, Phosphorus, and Ammonia. For detection limits, please refer to the&amp;amp;nbsp;descriptions in the Parameters section below.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;3.&amp;amp;nbsp;&amp;lt;em&amp;gt;&amp;lt;strong&amp;gt;ICPMS (Metal Concentrations)&amp;lt;/strong&amp;gt;&amp;lt;/em&amp;gt;: Porewater was reconstituted in dilute HNO&amp;lt;sub&amp;gt;3&amp;lt;/sub&amp;gt;&amp;amp;nbsp;and diluted to minimize salt interferences before analysis on a Thermo Scientific Element XR High Resolution-ICP-MS housed at the University of Southern Mississippi at the Stennis Space Center. The following elements are reported in the data from the ICPMS analysis:&amp;amp;nbsp; magnesium (Mg), sulfur (S),&amp;amp;nbsp;calcium (Ca), manganese (Mn), iron (Fe), potassium (K), cesium (Cs), uranium (U), lithium (Li), vanadium (V), cobalt (Co), nickel (Ni), copper (Cu), strontium (Sr), molybdenum (Mo), barium (Ba), phosphorus (P), and aluminum (Al), along with phosphorus (P) and silica (Si).&amp;amp;nbsp; For each element's detection limit, please see the description in the Parameters section below.&amp;amp;nbsp;&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Sediments&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Sediments were analyzed for physical properties, chemical properties, phases of silica, and isotopic composition. Each&amp;amp;nbsp;section below describes the specific methods in greater detail.&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;III. Sediment properties&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;em&amp;gt;&amp;lt;strong&amp;gt;Porosity&amp;lt;/strong&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;br /&amp;gt;
For porosity measurements, microcentrifuge tubes were placed in a drying oven at 60°C until the sediment was dry. Once dried, tubes were weighed. Porosity was calculated as in Comeaux et al. (2012).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;&amp;lt;strong&amp;gt;Loss on ignition (LOI)&amp;lt;/strong&amp;gt;&amp;lt;/em&amp;gt;&amp;lt;br /&amp;gt;
For loss on ignition (LOI) analysis, dried sediment was ground into a fine consistency using a mortar and pestle. Then 1g of the ground sediment was weighed into pre-muffled and pre-weighed porcelain crucibles. To remove any carbon from the presence of calcium carbonate, samples were fumed by adding 1mL of mili-Q to each crucible and placing samples into a desiccator with 10 mL of 12M HCl for 6 hours (Harris et al. 2001,&amp;amp;nbsp;Ramnarine et al. 2011, Walthert et al. 2010). After 6 hours, samples were placed in a vacuum oven for roughly 16 hours, until dry (Ramnarine et al. 2011, Walthert et al. 2010). Once dry, samples were kept in the oven and weighed one at a time to keep moisture out of samples. If sample was still acidic (yellow in color), 1 mL of mili-Q was added and the sample was dried again. Sediment was ground again into a fine powder.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;After the above preparation, fumed and ground sediment was weighed (100 mg) in triplicate into pre-weighed and muffled liquid scintillation (LSC) vials. Samples were combusted at 550°C for 6 hours (Kemp et al. 2021). After combustion, weights were recorded, and loss of organic matter was calculated (Kemp et al. 2021).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;IV. Sediment Silica Pools&amp;lt;/strong&amp;gt;&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Sequential Extractions&amp;lt;/em&amp;gt;&amp;amp;nbsp;&amp;amp;nbsp;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Frozen samples were thawed, homogenized, and 50 mg were weighed in triplicates (per depth) into pre-labeled 50 mL centrifuge tubes (Krause et al., 2017; Pickering et al., 2020). Samples with procedural blanks (in triplicate) then went through the sequential extraction process. The sequential extraction methodology separates silica into operationally defined pools based on kinetics, reaction conditions and reaction sequence (DeMaster, 1981; Michalopoulos and Aller, 2004; Rahman et al., 2016; Pickering et al., 2020).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Operational Definitions&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Based on prior studies, we use the following nomenclature:&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;1. &amp;lt;strong&amp;gt;Si-HCl&amp;lt;/strong&amp;gt;: Mild acid-leachable pre-treatment; Highly reactive silica associated with authigenic clays and metal oxide coatings (Michalopoulos and Aller, 2004).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;2. &amp;lt;strong&amp;gt;Si-Alk&amp;lt;/strong&amp;gt;: Mild alkaline-leachable digestion completed after acid pretreatment; Frees reactive silica associated with the biogenic silica pool (Michalopoulos and Aller, 2004).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;3. &amp;lt;strong&amp;gt;Si-NaOH (Alk)&amp;lt;/strong&amp;gt;: Harsh NaOH digestion done after Si-HCl and Si-Alk (Rahman et al., 2016; Rahman et al., 2017); Associated with the reactive lithogenic Si (LSi) pool and the comparatively refractory “dark bSiO&amp;lt;sub&amp;gt;2&amp;lt;/sub&amp;gt;” (e.g. sponge spicules and Rhizaria).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;4.&amp;amp;nbsp;&amp;lt;strong&amp;gt;tbSi&amp;lt;/strong&amp;gt;: Following the traditional definition of biogenic silica (DeMaster, 1981), with no acid pre-treatment.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;5.&amp;amp;nbsp;&amp;lt;strong&amp;gt;Si-NaOH (TbSi)&amp;lt;/strong&amp;gt;: Harsh NaOH digestion done after T-bSi.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;br /&amp;gt;
&amp;lt;strong&amp;gt;V. Sediment Organic matter&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Preparation&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
Same preparation as that listed above for Loss on Ignition&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;&amp;lt;em&amp;gt;Particulate Organic Carbon and Nitrogen content and isotopes (δ&amp;lt;sup&amp;gt;13&amp;lt;/sup&amp;gt;C and δ&amp;lt;sup&amp;gt;15&amp;lt;/sup&amp;gt;N)&amp;lt;/em&amp;gt;&amp;lt;/strong&amp;gt;&amp;lt;br /&amp;gt;
After fumigation (explained above), ~60 to 70 mg of sediment were packed in 5x9mm silver capsules, which were then packed in tin 5x9mm capsules in triplicate (UC Davis protocol recommendation). Samples were placed in a 96 well plate and kept in a desiccator until shipped to UC Davis for isotopic (δ13C and δ15N) analysis (Krause et al. 2017).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Results from UC Davis had an absolute accuracy for calibrated reference materials of&amp;amp;nbsp;±0.04 ‰ (±0.05 ‰ SD) for δ13C and ±0.05 ‰ (±0.05 ‰ SD) for δ15N. Core depth 24-26cm was the only sample below detection (9.7ug) for δ15N, which is represented as 0 on the data sheet.&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gco:CharacterString>&amp;lt;p&amp;gt;Raw data were input into Microsoft Excel (Version 2302) to calculate final reported values.&amp;lt;/p&amp;gt;

&amp;lt;ul&amp;gt;
&amp;lt;li&amp;gt;Porosity was calculated as in Comeaux et al. (2012).&amp;lt;/li&amp;gt;
&amp;lt;li&amp;gt;Loss of organic matter was calculated as in Kemp et al. (2021).&amp;lt;/li&amp;gt;
&amp;lt;/ul&amp;gt;

&amp;lt;p&amp;gt;&amp;amp;nbsp;&amp;lt;/p&amp;gt;</gco:CharacterString>
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                <gmd:description>
                  <gco:CharacterString>- Imported data from source file &amp;quot;Extreme_Si_MASTER_BCODMO.xlsx&amp;quot; into the BCO-DMO data system. 
- Added R/V Pelican official cruise IDs corresponding to the submitted cruise name.
- Combined separate date and time columns into a single datetime column
- Kept local datetime but added a column for ISO8601 formatted UTC datetime 
- Removed percent (%) signs from the column values
- Modified parameter (column) names to conform with BCO-DMO naming conventions. The only allowed characters are A-Z,a-z,0-9, and underscores. Replaced spaces with underscores.</gco:CharacterString>
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                          <gco:CharacterString>Specified by BCO-DMO Data Managers</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>info@bco-dmo.org</gco:CharacterString>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/526.rdf" xlink:title="Box Corer" xlink:actuate="onRequest">Box core</gmx:Anchor>
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            <gco:CharacterString>PI Supplied Instrument Name: Box core PI Supplied Instrument Description:A box core was used on the December 2021 cruise to sample sediments Instrument Name: Box Corer Instrument Short Name:Box Corer   Instrument Description: General description of a box corer:

A box corer is a marine geological tool that recovers undisturbed soft surface sediments. It is designed for minimum disturbance of the sediment surface by bow wave effects. Traditionally, it consists of a weighted stem fitted to a square sampling box. The corer is lowered vertically until it impacts with the seabed. At this point the instrument is triggered by a trip as the main coring stem passes through its frame. While pulling the corer out of the sediment a spade swings underneath the sample to prevent loss. When hauled back on board, the spade is under the box. (definition from the SeaVox Device Catalog)

Box corers are one of the simplest and most commonly used types of sediment corers. The stainless steel sampling box can contain a surface sediment block as large as 50cm x 50cm x 75cm with negligible disturbance. Once the sediment is recovered onboard, the sediment box can be detached from the frame and taken to a laboratory for subsampling and further analysis. The core sample size is controlled by the speed at which the corer is lowered into the ocean bottom. When the bottom is firm, a higher speed is required to obtain a complete sample. A depth pinger or other depth indicator is generally used to determine when the box is completely filled with sediment. Once the core box is filled with sediment, the sample is secured by moving the spade-closing lever arm to lower the cutting edge of the spade into the sediment, until the spade completely covers the bottom of the sediment box. (definition from Woods Hole Oceanographic Institution). Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/51/</gco:CharacterString>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/629890.rdf" xlink:title="Centrifuge" xlink:actuate="onRequest">centrifuge</gmx:Anchor>
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            <gco:CharacterString>PI Supplied Instrument Name: centrifuge PI Supplied Instrument Description:Mulitcorer samples were placed into tubes and centrifuged at 3500 rpm for 10 minutes to extract and filter supernatant, which was later used for dissolved silica analysis.  Instrument Name: Centrifuge Instrument Short Name:   Instrument Description: A machine with a rapidly rotating container that applies centrifugal force to its contents, typically to separate fluids of different densities (e.g., cream from milk) or liquids from solids.</gco:CharacterString>
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              <gmd:code>
                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/661968.rdf" xlink:title="Continuous Flow Analyzer" xlink:actuate="onRequest">Skalar San++ Automated Wet Chemistry Analyzer</gmx:Anchor>
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         <gmx:Anchor xlink:href="http://www.lumcon.edu/Pelican/" xlink:actuate="onRequest">R/V Pelican</gmx:Anchor>
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              <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/authority/1.rdf" xlink:actuate="onRequest">International Council for the Exploration of the Sea</gmx:Anchor>
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          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54114.rdf"
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                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/905462.rdf" xlink:actuate="onRequest">Shaily Rahman</gmx:Anchor>
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         <gmx:Anchor xlink:href="http://www.lumcon.edu/Pelican/" xlink:actuate="onRequest">R/V Pelican</gmx:Anchor>
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          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54114.rdf"
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