<?xml version="1.0"?>
<?xml-stylesheet type="text/xsl" href="https://ontobee.org/ontology/view/ENVO?iri=http://purl.obolibrary.org/obo/ENVO_01000079"?>
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     xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#"
     xmlns:owl="http://www.w3.org/2002/07/owl#"
     xmlns:oboInOwl="http://www.geneontology.org/formats/oboInOwl#"
     xmlns:xsd="http://www.w3.org/2001/XMLSchema#"
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     xmlns:dc="http://purl.org/dc/elements/1.1/"
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    <!-- 
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    <AnnotationProperty rdf:about="http://www.geneontology.org/formats/oboInOwl#created_by"/>
    <AnnotationProperty rdf:about="http://www.geneontology.org/formats/oboInOwl#creation_date"/>
    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
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    <!-- 
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    <!-- 
    ///////////////////////////////////////////////////////////////////////////////////////
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    <!-- http://purl.obolibrary.org/obo/ENVO_01000079 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01000079">
        <rdfs:label>marine lysocline</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_01001674"/>
        <ns3:IAO_0000115>The marine lysocline denotes the depth in the ocean below which the rate of dissolution of calcite increases dramatically. As water column depth and therefore pressure increases, the corresponding calcite saturation of seawater decreases and the calcite begins dissolve.</ns3:IAO_0000115>
        <oboInOwl:creation_date>2010-03-16T12:16:11Z</oboInOwl:creation_date>
        <oboInOwl:inSubset>envoPolar</oboInOwl:inSubset>
        <oboInOwl:created_by>ORCID:0000-0002-4366-3088</oboInOwl:created_by>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/ENVO_01001674 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01001674">
        <rdfs:label xml:lang="en">lysocline</rdfs:label>
    </Class>
</rdf:RDF>



<!-- Generated by the OWL API (version 3.2.4.1806) http://owlapi.sourceforge.net -->



