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      <src>https://theses.otagogeology.org.nz/files/original/9a6c34dd733b2484533fb92a9806fdbe.pdf</src>
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        <name>Dublin Core</name>
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        <elementContainer>
          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
            <elementTextContainer>
              <elementText elementTextId="1">
                <text>Geology theses</text>
              </elementText>
            </elementTextContainer>
          </element>
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  <itemType itemTypeId="18">
    <name>OU Geology thesis</name>
    <description>Thesis or dissertation completed by University of Otago Geology students</description>
    <elementContainer>
      <element elementId="52">
        <name>Author last name</name>
        <description>Last name of the Author</description>
        <elementTextContainer>
          <elementText elementTextId="31722">
            <text>Pole</text>
          </elementText>
        </elementTextContainer>
      </element>
      <element elementId="53">
        <name>Project type</name>
        <description>Is it an MSc, PhD, BSc(Hons) or PGDipSci?</description>
        <elementTextContainer>
          <elementText elementTextId="31725">
            <text>BSc(Hons)</text>
          </elementText>
        </elementTextContainer>
      </element>
      <element elementId="54">
        <name>Advisers</name>
        <description>Who supervised/advised this student</description>
        <elementTextContainer>
          <elementText elementTextId="31727">
            <text>Fordyce, R.E.</text>
          </elementText>
        </elementTextContainer>
      </element>
      <element elementId="55">
        <name>Abstract</name>
        <description>The Abstract for this thesis</description>
        <elementTextContainer>
          <elementText elementTextId="31728">
            <text>A study of Miocene sediments (Manuherikia Group) at Bannockburn and the banks of the Kawarau River, Central Otago, reveals the existence of at least 18 pollen taxa, 44 plant mcrofossil parataxa and casuarina n. sp. At least 6 floral associations are inferred to have existed -
(1) a closed-canopy beech and conifer forest,
(2) an open-canopy sclerophyllous forest or woodland including
casuarina and possibly Eucalyptus,
(3) palmaceous swamp forest,
(4) dicotyledonous swamp forest,
(5) coniferous swamp forest, and
(6) a probable lateral zonation of semi-aquatic plants surrormding
lake and bay mrgins which included burr-reeds.
Climtic data are inconclusive but indicate temperate rather than tropical conditions.</text>
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      <element elementId="59">
        <name>Department</name>
        <description>The department where the student is studying primarily.</description>
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          <elementText elementTextId="31729">
            <text>Geology</text>
          </elementText>
        </elementTextContainer>
      </element>
      <element elementId="61">
        <name>Named locality</name>
        <description>Named locality describing the field area location.</description>
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          <elementText elementTextId="31730">
            <text>Bannockburn</text>
          </elementText>
        </elementTextContainer>
      </element>
      <element elementId="60">
        <name>Thesis description</name>
        <description>Number of pages, maps, CDs, etc.</description>
        <elementTextContainer>
          <elementText elementTextId="31733">
            <text>244 leaves. Illus. 30 cm.</text>
          </elementText>
        </elementTextContainer>
      </element>
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    <elementSet elementSetId="1">
      <name>Dublin Core</name>
      <description>The Dublin Core metadata element set is common to all Omeka records, including items, files, and collections. For more information see, http://dublincore.org/documents/dces/.</description>
      <elementContainer>
        <element elementId="43">
          <name>Identifier</name>
          <description>An unambiguous reference to the resource within a given context</description>
          <elementTextContainer>
            <elementText elementTextId="31721">
              <text>1983Pole</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="39">
          <name>Creator</name>
          <description>An entity primarily responsible for making the resource</description>
          <elementTextContainer>
            <elementText elementTextId="31723">
              <text>Pole, MS</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="40">
          <name>Date</name>
          <description>A point or period of time associated with an event in the lifecycle of the resource</description>
          <elementTextContainer>
            <elementText elementTextId="31724">
              <text>1983</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="50">
          <name>Title</name>
          <description>A name given to the resource</description>
          <elementTextContainer>
            <elementText elementTextId="31726">
              <text>Paleoecology and Stratigraphy of Miocene Floras, Bannockburn, Central Otago.</text>
            </elementText>
          </elementTextContainer>
        </element>
        <element elementId="49">
          <name>Subject</name>
          <description>The topic of the resource</description>
          <elementTextContainer>
            <elementText elementTextId="31731">
              <text>Paleobotany</text>
            </elementText>
            <elementText elementTextId="31732">
              <text> Cenozoic</text>
            </elementText>
          </elementTextContainer>
        </element>
      </elementContainer>
    </elementSet>
  </elementSetContainer>
  <tagContainer>
    <tag tagId="377">
      <name>Casuarina</name>
    </tag>
    <tag tagId="368">
      <name>palynology</name>
    </tag>
  </tagContainer>
</item>
