<?xml version="1.0"?>
<?xml-stylesheet type="text/xsl" href="https://ontobee.org/ontology/view/MICRO?iri=http://purl.obolibrary.org/obo/ENVO_01000079"?>
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    <AnnotationProperty rdf:about="http://www.geneontology.org/formats/oboInOwl#creation_date"/>
    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000412"/>
    <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 rdf:datatype="http://www.w3.org/2001/XMLSchema#string">marine lysocline</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_01000261"/>
        <oboInOwl:creation_date rdf:datatype="http://www.w3.org/2001/XMLSchema#string">2010-03-16T12:16:11Z</oboInOwl:creation_date>
        <oboInOwl:hasOBONamespace rdf:datatype="http://www.w3.org/2001/XMLSchema#string">ENVO</oboInOwl:hasOBONamespace>
        <oboInOwl:id rdf:datatype="http://www.w3.org/2001/XMLSchema#string">ENVO:01000079</oboInOwl:id>
        <oboInOwl:created_by rdf:datatype="http://www.w3.org/2001/XMLSchema#string">ORCID:0000-0002-4366-3088</oboInOwl:created_by>
        <ns2:IAO_0000115 rdf:datatype="http://www.w3.org/2001/XMLSchema#string">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.</ns2:IAO_0000115>
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    <!-- http://purl.obolibrary.org/obo/ENVO_01000261 -->

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        <rdfs:label rdf:datatype="http://www.w3.org/2001/XMLSchema#string">lysocline</rdfs:label>
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<!-- Generated by the OWL API (version 3.2.4.1806) http://owlapi.sourceforge.net -->



