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     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#"
     xmlns:rdfs="http://www.w3.org/2000/01/rdf-schema#"
     xmlns:ns4="http://purl.obolibrary.org/obo/"
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    <!-- 
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    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/uberon/core#human_subset"/>
    <AnnotationProperty rdf:about="http://www.geneontology.org/formats/oboInOwl#hasExactSynonym"/>
    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/UBPROP_0000008"/>
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    <!-- http://purl.obolibrary.org/obo/RO_0002131 -->

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        <rdf:type rdf:resource="http://www.w3.org/2002/07/owl#SymmetricProperty"/>
        <rdfs:label>overlaps</rdfs:label>
        <rdfs:label xml:lang="en">overlaps</rdfs:label>
    </ObjectProperty>
    


    <!-- 
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    //
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    <!-- http://purl.obolibrary.org/obo/UBERON_0002412 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/UBERON_0002412">
        <rdfs:label>vertebra</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/UBERON_0035086 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/UBERON_0035086">
        <rdfs:label>plane of autotomy</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/UBERON_0035087 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/UBERON_0035087">
        <rdfs:label>fracture plane</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/UBERON_0035088 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/UBERON_0035088">
        <rdfs:label>vertebral fracture plane</rdfs:label>
        <equivalentClass>
            <Class>
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        <oboInOwl:hasExactSynonym>plane of autotomy bisecting vertebral bone</oboInOwl:hasExactSynonym>
        <ns4:UBPROP_0000008>Interestingly, zones of cartilage or connective tissue do not demarcate the fracture planes in A. carolinensis, as seen in other lizard taxa (Cox, 1969a; Hoffstetter and Gasc, 1969)[PMID:22753107]</ns4:UBPROP_0000008>
        <ns4:UBPROP_0000008>Many authors (e.g., Holder, 1960; Mufti and Hafiz, 1972; Bellairs and Bryant, 1985; Russell and Bauer, 1992) have referred to the more proximal caudal vertebrae that lack fracture planes as &#39;pygal vertebrae&#39; and the more distal caudal vertebrae that possess fracture planes as &#39;postpygal vertebrae&#39; However, many lizard taxa lack fracture planes in their caudal vertebrae altogether, making this classification difficult to apply in these cases (Etheridge, 1967; Bellairs and Bryant, 1985). Furthermore, in some species (including A. carolinensis) the most distal of the transverse process-bearing vertebrae may possess fracture planes and should technically be called postpygal vertebrae, despite the fact that they more closely resemble the more proximal, non-fracture plane-bearing vertebrae in overall morphology (Cox, 1969a)[PMID:22753107]</ns4:UBPROP_0000008>
        <oboInOwl:id>UBERON:0035088</oboInOwl:id>
        <ns4:IAO_0000115>A plane of autotomy that divides an appendage through a vertebral bone.</ns4:IAO_0000115>
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        <oboInOwl:inSubset rdf:resource="http://purl.obolibrary.org/obo/uberon/core#mouse_subset"/>
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