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        <gco:CharacterString>Methane and sulfate concentration profiles - sediment cores from  White Oak River estuary Station H, October 2012 Dataset Description: &amp;lt;p&amp;gt;This dataset resulted from a graduate student project called &amp;quot;Culture independent genomic comparisons reveal environmental adaptations for Altiarchaeales&amp;quot;. The data is associated with a manuscript submitted to Frontier in Microbiology. The samples are from the White Oak River estuary, North Carolina, Station H to a sediment depth of 75 cm. The project was partially funded by OCE grants.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;Related reference:&amp;lt;/strong&amp;gt;&amp;amp;nbsp;Environmental evidence for net methane production and oxidation in putative ANaerobic MEthanotrophic (ANME) archaea (2011) by Karen G. Lloyd, Marc J. Alperin, Andreas Teske. Contains detailed methods that were nearly identical to the methods used here and similar data from the same location.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;The cores were&amp;amp;nbsp;sequentially cut into 3 cm section from the topmost to bottommost depth. For methane measurements, 3 ml of sediments were taken via cut-off syringe immediately after each section was sliced and quickly added to 60 ml serum vials containing 1 ml of 0.1 M KOH, which were stoppered and crimp-sealed with butyl rubber stoppers to minimize gas loss. After being shaken for 1 min to release methane from sediments (&amp;amp;gt; 99.5% of the methane equilibrated in the headspace), a 5 ml headspace aliquot was displaced with an equal volume of anaerobic distilled water, injected into a 1 ml sample loop, and then analyzed on an Agilent 7890a gas chromatograph&amp;amp;nbsp; equipped with flame ionization detector. For sulfate measurements, plastic 15 ml tubes filled completely with sediment were centrifuged and the resulting porewater was filtered at 0.2 µm, acidified with 10% HCl and measured using a 2010i Dionex ion chromatograph.&amp;lt;/p&amp;gt;</gco:CharacterString>
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C-DEBI's scientific goals are pursued with a combination of approaches:
(1) coordinate, integrate, support, and extend the research associated with four major programs—Juan de Fuca Ridge flank (JdF), South Pacific Gyre (SPG), North Pond (NP), and Dorado Outcrop (DO)—and other field sites;
(2) make substantial investments of resources to support field, laboratory, analytical, and modeling studies of the deep subseafloor ecosystems;
(3) facilitate and encourage synthesis and thematic understanding of submarine microbiological processes, through funding of scientific and technical activities, coordination and hosting of meetings and workshops, and support of (mostly junior) researchers and graduate students; and
(4) entrain, educate, inspire, and mentor an interdisciplinary community of researchers and educators, with an emphasis on undergraduate and graduate students and early-career scientists.
Note: Katrina Edwards was a former PI of C-DEBI; James Cowen is a former co-PI.
Data Management:
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The U.S. National Science Foundation (NSF) 
Japan's Ministry of Education, Culture, Sports, Science and Technology (MEXT) 
The European Consortium for Ocean Research Drilling (ECORD)

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                            <gco:CharacterString>&lt;p&gt;Marine sediments contain a microbial population large enough to rival that of Earth's oceans, but much about this vast community is unknown. Innovations in total cell counting methods have refined estimates of cell concentrations, but tell us nothing about specific taxa. Isotopic data provides evidence that a majority of subsurface microorganisms survive by breaking down organic matter, yet measurable links between specific microbial taxa and their organic matter substrates are untested. The proposed work overcomes these limitations, with a particular focus on the degradation of proteins and carbohydrates, which comprise the bulk of classifiable sedimentary organic matter. The project will link specific taxa to potential extracellular enzyme activity in the genomes of single microbial cells, apply newly-identified, optimal methods for counting viable cells belonging to specific taxa using catalyzed reporter deposition fluorescent in situ hybridization (CARD-FISH), and measure the potential activity of their enzymes in situ. The resulting data will provide key evidence about the strategies subsurface life uses to overcome extreme energy limitation and contribute to the long-term carbon cycle.&lt;/p&gt;
&lt;p&gt;The Principal Investigators are employing novel,improved methods to quantify cells of specific taxa in the marine subsurface and to determine the biogeochemical functions of those uncultured taxa, including:&lt;br /&gt;
1) Determine the pathway of organic carbon degradation in single cell genomes of uncultured, numerically dominant subsurface microorganisms.&lt;br /&gt;
2) Quantify viable bacteria and archaea in the deep subsurface using an improvement on the existing technology of CARD-FISH.&lt;br /&gt;
3 )Measure the potential activities (Vmax values) of enzymes in deep Baltic Sea sediments, and use the abundances of enzyme-producing microorganisms to calculate depth profiles of cell-specific Vmax values.&lt;/p&gt;
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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>WHOI MS#36</gco:CharacterString>
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				    <gco:CharacterString>Woods Hole</gco:CharacterString>
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				  <gmd:administrativeArea>
				    <gco:CharacterString>MA</gco:CharacterString>
				  </gmd:administrativeArea>
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				    <gco:CharacterString>02543</gco:CharacterString>
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				  <gmd:country>
				    <gco:CharacterString>USA</gco:CharacterString>
				  </gmd:country>
				  <gmd:electronicMailAddress>
				    <gco:CharacterString>info@bco-dmo.org</gco:CharacterString>
				  </gmd:electronicMailAddress>
		    </gmd:CI_Address>
		  </gmd:address>
      <gmd:onlineResource>
          <gmd:CI_OnlineResource>
            <gmd:linkage>
              <gmd:URL>http://www.bco-dmo.org</gmd:URL>
            </gmd:linkage>
          </gmd:CI_OnlineResource>
        </gmd:onlineResource>
		  <gmd:hoursOfService>
        <gco:CharacterString>Monday - Friday 8:00am - 5:00pm</gco:CharacterString>
      </gmd:hoursOfService>
		  <gmd:contactInstructions>
		    <gco:CharacterString>For questions regarding this resource, please contact BCO-DMO via the email address provided.</gco:CharacterString>
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    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="pointOfContact"  codeSpace="007">pointOfContact</gmd:CI_RoleCode>
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              <gco:Real>2868</gco:Real>
            </gmd:transferSize><gmd:onLine>
            <gmd:CI_OnlineResource>
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                  <gco:CharacterString>Primary data file for dataset ID 649751</gco:CharacterString>
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              <gmd:transferOptions>
        <gmd:MD_DigitalTransferOptions>
        <gmd:onLine>
            <gmd:CI_OnlineResource>
              <gmd:linkage>
                <gmd:URL>https://osprey.bco-dmo.org/dataset/649751/data/download</gmd:URL>
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        <gmd:DQ_Scope>
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          <gmd:processStep xlink:title="Methods and Sampling">
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                <gco:CharacterString>&amp;lt;p&amp;gt;The cores were&amp;amp;nbsp;sequentially cut into 3 cm section from the topmost to bottommost depth. For methane measurements, 3 ml of sediments were taken via cut-off syringe immediately after each section was sliced and quickly added to 60 ml serum vials containing 1 ml of 0.1 M KOH, which were stoppered and crimp-sealed with butyl rubber stoppers to minimize gas loss. After being shaken for 1 min to release methane from sediments (&amp;amp;gt; 99.5% of the methane equilibrated in the headspace), a 5 ml headspace aliquot was displaced with an equal volume of anaerobic distilled water, injected into a 1 ml sample loop, and then analyzed on an Agilent 7890a gas chromatograph&amp;amp;nbsp; equipped with flame ionization detector. For sulfate measurements, plastic 15 ml tubes filled completely with sediment were centrifuged and the resulting porewater was filtered at 0.2 µm, acidified with 10% HCl and measured using a 2010i Dionex ion chromatograph.&amp;lt;/p&amp;gt;</gco:CharacterString>
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              <gmd:description>
                <gco:CharacterString>&amp;lt;p&amp;gt;Methane concentrations (mmol per litre of porewater) were calculated using the following equation:&amp;lt;br /&amp;gt;
[CH&amp;lt;sub&amp;gt;4&amp;lt;/sub&amp;gt;] = (ρ(CH&amp;lt;sub&amp;gt;4&amp;lt;/sub&amp;gt;)V&amp;lt;sub&amp;gt;headspace&amp;lt;/sub&amp;gt;)/(RTφV&amp;lt;sub&amp;gt;sed&amp;lt;/sub&amp;gt;1000)&amp;lt;br /&amp;gt;
where p(CH4) is the partial pressure of methane (in ppmv), Vheadspace is the volume of the serum vial headspace (ml) after the sediment and KOH are added, R is the universal gas constant, T is the temperature at time of measurement in Kelvin and Vsed is the volume (ml) of whole sediment added to the serum vial.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Porosity, φ, was calculated using the formula:&amp;lt;br /&amp;gt;
φ = (m&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt;/ ρ&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt;)/(m&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt;/ρ&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt;+((m&amp;lt;sub&amp;gt;d&amp;lt;/sub&amp;gt;-S*m&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt;/1000)/ρ&amp;lt;sub&amp;gt;ds&amp;lt;/sub&amp;gt;))&amp;lt;br /&amp;gt;
where m&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt; is the mass of the water lost on drying, m&amp;lt;sub&amp;gt;d&amp;lt;/sub&amp;gt; is the mass of the dried sediment, ρ&amp;lt;sub&amp;gt;w&amp;lt;/sub&amp;gt; is the density of pure water, ρ&amp;lt;sub&amp;gt;ds&amp;lt;/sub&amp;gt; is the density of dry sediment (assumed to be 2.5 g cm−3), and S is salinity in grams per kilogram (assumed to be 19 grams per kilogram for all samples).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Standards at sulfate concentrations 0, 0.1, 0.5, 1, 5, 10 mM measure prior to samples from each core and sample peak areas were converted to sulfate concentrations using the standard curves after accounting for the dilution ((peak area * slope + intercept) * 0.7 / 0.6) by the 10% HCl.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;No samples have been flagged as below the detection limit.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;strong&amp;gt;BCO-DMO Processing:&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;- added conventional header with dataset name, PI name, version date&amp;lt;br /&amp;gt;
- renamed parameters to BCO-DMO and BODC standards&amp;lt;br /&amp;gt;
- replaced NaN with nd&amp;lt;br /&amp;gt;
- removed CH4_mod data&amp;lt;/p&amp;gt;</gco:CharacterString>
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              <gmd:source>
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                  <gmd:sourceCitation>
                    <gmd:CI_Citation>
                      <gmd:title>
                        <gco:CharacterString>Specified by the Principal Investigator(s)</gco:CharacterString>
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                      <gmd:date gco:nilReason="unknown"/>
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      </gmd:lineage>
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      <gmd:maintenanceNote>
        <gco:CharacterString>7.x-1.1</gco:CharacterString>
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      <gmd:contact>
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  <gmd:organisationName>
    <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>
  </gmd:organisationName>
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    <gmd:CI_Contact>
		  <gmd:phone>
		    <gmd:CI_Telephone>
				  <gmd:voice>
				    <gco:CharacterString>Unavailable</gco:CharacterString>
				  </gmd:voice>
				  <gmd:facsimile>
				    <gco:CharacterString>508-289-2009</gco:CharacterString>
				  </gmd:facsimile>
				</gmd:CI_Telephone>
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		  <gmd:address>
		    <gmd:CI_Address>
				  <gmd:deliveryPoint>
				    <gco:CharacterString>WHOI MS#36</gco:CharacterString>
				  </gmd:deliveryPoint>
				  <gmd:city>
				    <gco:CharacterString>Woods Hole</gco:CharacterString>
				  </gmd:city>
				  <gmd:administrativeArea>
				    <gco:CharacterString>MA</gco:CharacterString>
				  </gmd:administrativeArea>
				  <gmd:postalCode>
				    <gco:CharacterString>02543</gco:CharacterString>
				  </gmd:postalCode>
				  <gmd:country>
				    <gco:CharacterString>USA</gco:CharacterString>
				  </gmd:country>
				  <gmd:electronicMailAddress>
				    <gco:CharacterString>info@bco-dmo.org</gco:CharacterString>
				  </gmd:electronicMailAddress>
		    </gmd:CI_Address>
		  </gmd:address>
      <gmd:onlineResource>
          <gmd:CI_OnlineResource>
            <gmd:linkage>
              <gmd:URL>http://www.bco-dmo.org</gmd:URL>
            </gmd:linkage>
          </gmd:CI_OnlineResource>
        </gmd:onlineResource>
		  <gmd:hoursOfService>
        <gco:CharacterString>Monday - Friday 8:00am - 5:00pm</gco:CharacterString>
      </gmd:hoursOfService>
		  <gmd:contactInstructions>
		    <gco:CharacterString>For questions regarding this resource, please contact BCO-DMO via the email address provided.</gco:CharacterString>
		  </gmd:contactInstructions>
		</gmd:CI_Contact>
  </gmd:contactInfo>
  <gmd:role>
    <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="pointOfContact"  codeSpace="007">pointOfContact</gmd:CI_RoleCode>
  </gmd:role>
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      </gmd:contact>
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  <gmi:acquisitionInformation>
    <gmi:MI_AcquisitionInformation>
    <gmi:instrument>
        <gmi:MI_Instrument>
          <gmi:identifier>
            <gmd:MD_Identifier>
              <gmd:code>
                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/instrument/661.rdf" xlink:title="Gas Chromatograph" xlink:actuate="onRequest"></gmx:Anchor>
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            </gmd:MD_Identifier>
          </gmi:identifier>
          <gmi:type>
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          <gmi:description>
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      <gmi:instrument>
        <gmi:MI_Instrument>
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              <gmd:code>
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          <gmi:type>
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          <gmi:description>
            <gco:CharacterString>PI Supplied Instrument Name:  PI Supplied Instrument Description:2010i Dionex ion chromatograph Instrument Name: Ion Chromatograph Instrument Short Name:Ion Chromatograph   Instrument Description: Ion chromatography is a form of liquid chromatography that measures concentrations of ionic species by separating them based on their interaction with a resin. Ionic species separate differently depending on species type and size. Ion chromatographs are able to measure concentrations of major anions, such as fluoride, chloride, nitrate, nitrite, and sulfate, as well as major cations such as lithium, sodium, ammonium, potassium, calcium, and magnesium in the parts-per-billion (ppb) range. (from http://serc.carleton.edu/microbelife/research_methods/biogeochemical/ic.html)</gco:CharacterString>
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        </gmi:MI_Instrument>
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      <gmi:operation>
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              <gco:CharacterString>Cruise: White_Oak_River</gco:CharacterString>
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            <gmi:identifier>
              <gmd:MD_Identifier>
                <gmd:code>
                  <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/deployment/649762.rdf" xlink:title="Cruise" xlink:actuate="onRequest">White_Oak_River</gmx:Anchor>
                </gmd:code>
              </gmd:MD_Identifier>
            </gmi:identifier>
            <gmi:status>
              <gmd:MD_ProgressCode codeList="https://data.noaa.gov/resources/iso19139/schema/resources/Codelist/gmxCodelists.xml#MD_ProgressCode" codeListValue="completed"/>
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            <gmi:type>
              <gmi:MI_OperationTypeCode codeList="https://data.noaa.gov/resources/iso19139/schema/resources/Codelist/gmxCodelists.xml#MI_OperationTypeCode" codeListValue="real"/>
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            <gmi:parentOperation gco:nilReason="inapplicable"/>
            <gmi:platform>
  <gmi:MI_Platform>
    <gmi:identifier>
      <gmd:MD_Identifier>
        <gmd:code>
          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54155.rdf"
           xlink:actuate="onRequest">Unknown Vessel</gmx:Anchor>
        </gmd:code>
      </gmd:MD_Identifier>
    </gmi:identifier>
    <gmi:description>
      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54155.rdf" xlink:title="Unknown Vessel" xlink:actuate="onRequest">vessel</gmx:Anchor>
    </gmi:description>
    <gmi:instrument gco:nilReason="unknown"/>
  </gmi:MI_Platform>
</gmi:platform>
            <gmi:plan>
              <gmi:MI_Plan>
                <gmi:status>
                  <gmd:MD_ProgressCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#MD_ProgressCode" codeListValue="completed"/>
                </gmi:status>
                <gmi:citation>
                  <gmd:CI_Citation>
                    <gmd:title>
                      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/deployment/649762.rdf" xlink:title="Cruise" xlink:actuate="onRequest">White_Oak_River</gmx:Anchor>
                    </gmd:title>
                    <gmd:date gco:nilReason="unknown"/>
                    <gmd:citedResponsibleParty>
                      <gmd:CI_ResponsibleParty>
                      <gmd:individualName>
                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/639420.rdf" xlink:actuate="onRequest">Karen G. Lloyd</gmx:Anchor>
                        </gmd:individualName>
                        <gmd:organisationName>
                          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/226.rdf" xlink:title="Affiliation" xlink:actuate="onRequest">University of Tennessee Knoxville</gmx:Anchor>
                        </gmd:organisationName>
                        <gmd:role>
                        <gmd:CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="principalInvestigator"/>
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                      </gmd:CI_ResponsibleParty>
                    </gmd:citedResponsibleParty>
                   </gmd:CI_Citation>
                </gmi:citation>
              </gmi:MI_Plan>
            </gmi:plan>
            </gmi:MI_Operation>
      </gmi:operation><gmi:platform>
  <gmi:MI_Platform>
    <gmi:identifier>
      <gmd:MD_Identifier>
        <gmd:code>
          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54155.rdf"
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        </gmd:code>
      </gmd:MD_Identifier>
    </gmi:identifier>
    <gmi:description>
      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54155.rdf" xlink:title="Unknown Vessel" xlink:actuate="onRequest">vessel</gmx:Anchor>
    </gmi:description>
    <gmi:instrument gco:nilReason="unknown"/>
  </gmi:MI_Platform>
</gmi:platform>
          </gmi:MI_AcquisitionInformation>
  </gmi:acquisitionInformation>
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