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        <gco:CharacterString>Polymetallic nodules occur in abyssal plains (~4000 – 6000 mm water depth) of all major oceans as two-dimensional deposits, formed on or just below sediment-covered seafloor, rich in metals of economic interest such as manganese (Mn), nickel (Ni), copper (Cu), cobalt (Co), molybdenum (Mo), titanium (Ti), lithium (Li), and rare earth elements (REE). The nodules are generated in marine environments where the sedimentation rates are low, commonly less than 10 centimeters (cm) per thousand years. The nodules consist of micro-layers of Mn oxides and Fe oxy-hydroxides concentrically precipitated around a nucleus. Nodules are generally about golf ball sized, most commonly 1–12 cm in diameter, but can vary in diameter from millimeter-size (micronodules) to as large as 20 cm. The polymetallic nodules are formed by metals precipitation either from ambient seawater (hydrogenetic formation), from pore-waters in the sediments (diagenetic formation), from hydrothermal derived fluids (Bonatti and Nayudu, 1965; Bau et al., 2014; Kuhn et al., 2017) and the formation processes that represent a mix of these different end-member processes. The formation mechanisms control the general chemical composition of the nodules, e.g. the hydrogenetic precipitation leads to an enrichment of Co and REE while the diagenetic precipitation favours enrichment of Ni and Cu. Hydrogenetic nodules grow remarkably slow (1 to 5 mm per million years), whereas diagenetic nodules grow at rates up to 250 mm per million years.</gco:CharacterString>
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        <gmd:MD_DigitalTransferOptions>
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            <gmd:CI_OnlineResource>
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                <gmd:URL>https://geoera.eu/projects/mindesea2/</gmd:URL>
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                <gco:CharacterString>WWW:LINK-1.0-http--link</gco:CharacterString>
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                <gmd:URL>https://maps.europe-geology.eu/?mapname=geoera#baslay=baseMapGEUS&amp;layers=Nodules_Predictivity_Area,Nodules_Exploration_Potential,Nodules_Potential_Area,Polymetallic_Nodules</gmd:URL>
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                <gmx:Anchor xlink:href="https://services.cuzk.gov.cz/registry/codelist/OnlineResourceProtocolValue/WWW:LINK">WWW:LINK-1.0-http--link</gmx:Anchor>
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    <gmd:DQ_DataQuality>
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        <gmd:DQ_Scope>
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                    <gmx:Anchor xlink:href="http://data.europa.eu/eli/reg/2010/1089">COMMISSION REGULATION (EU) No 1089/2010 of 23 November 2010 implementing Directive 2007/2/EC of the European Parliament and of the Council as regards interoperability of spatial data sets and services</gmx:Anchor>
                  </gmd:title>
                  <gmd:date>
                    <gmd:CI_Date>
                      <gmd:date>
                        <gco:Date>2010-12-08</gco:Date>
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                <gco:Boolean>true</gco:Boolean>
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          </gmd:result>
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        <gmd:LI_Lineage>
          <gmd:statement>
            <gco:CharacterString>Data modeling used D2.8.III.21 Data Specification on Mineral resources - Technical Guidelines to generate data schema for Ferro-manganese Crusts data produced by EMODnet Geology WP7 Minerals and MINDeSEA WP8 Link to Information Plaform for MINDeSEA WP4 Ferro-manganese crusts, phosphorites and Critical Raw Materials. The INSPIRE MineralResourcesCore UML class diagam applied for the spatial data attributes includes the following feature types: MineralOccurrence, Mine, MiningActivity, MineralDepositModel. The MINDeSEA WP4 applies the following tables: Chemistry, economic, environment, metallogeny, other and phosphoritesCriticalRawMaterials as agreed by the WP4 and WP8 leaders.</gco:CharacterString>
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        </gmd:LI_Lineage>
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