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<front>
<journal-meta>
<journal-id journal-id-type="publisher">JM</journal-id>
<journal-title-group>
<journal-title>Journal of Micropalaeontology</journal-title>
<abbrev-journal-title abbrev-type="publisher">JM</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">J. Micropalaeontol.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2041-4978</issn>
<publisher><publisher-name>GSL Publishing</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.1144/jm.14.2.135</article-id>
<title-group>
<article-title>Pliocene–Pleistocene radiolarian and diatom biostratigraphy of ODP Hole 709C (equatorial Indian Ocean)</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Haslett</surname>
<given-names>Simon K.</given-names>
</name>
<xref ref-type="aff" rid="aff0">
<sup>0</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kennington</surname>
<given-names>Kevin</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Funnell</surname>
<given-names>Brian M.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kersley</surname>
<given-names>Claire L.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff0">
<label>0</label>
<addr-line>Faculty of Applied Sciences, Bath College of Higher Education, Newton Park, Newton St. Loe, Bath BA2 9BN, UK</addr-line>
</aff>
<aff id="aff1">
<label>1</label>
<addr-line>School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Grafham Carbons, Grafham Water Works, Perry, Huntingdon PE18 OBW, UK</addr-line>
</aff>
<pub-date pub-type="epub">
<day>01</day>
<month>10</month>
<year>1995</year>
</pub-date>
<volume>14</volume>
<issue>2</issue>
<fpage>135</fpage>
<lpage>143</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 1995 Simon K. Haslett et al.</copyright-statement>
<copyright-year>1995</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://jm.copernicus.org/articles/14/135/1995/jm-14-135-1995.html">This article is available from https://jm.copernicus.org/articles/14/135/1995/jm-14-135-1995.html</self-uri>
<self-uri xlink:href="https://jm.copernicus.org/articles/14/135/1995/jm-14-135-1995.pdf">The full text article is available as a PDF file from https://jm.copernicus.org/articles/14/135/1995/jm-14-135-1995.pdf</self-uri>
<abstract>
<p>Ocean Drilling Program (ODP) Hole 709C was drilled on Madingley Rise in the equatorial Indian Ocean. Thirteen radiolarian and diatom events were identified in the Pliocene to Early Pleistocene section studied. Five radiolarian zones could be recognized: &lt;i&gt;Anthocyrtidium angulare, Pterocanium prismatium, Anthocyrtidium jenghisi, Stichocorys peregrina&lt;/i&gt;, and &lt;i&gt;Phormostichoartus doliolum&lt;/i&gt; zones. The LAD of &lt;i&gt;P. prismatium&lt;/i&gt; was found to be an unreliable indicator of the base of the &lt;i&gt;A. angulare&lt;/i&gt; zone in Hole 709C and in other upwelling areas. Accordingly, the base of the &lt;i&gt;A. angulare&lt;/i&gt; zone is redefined here by the FAD of &lt;i&gt;A. angulare.&lt;/i&gt; The &lt;i&gt;Phormostichoartus fistula&lt;/i&gt; zone, which normally separates the 5. &lt;i&gt;peregrina&lt;/i&gt; and &lt;i&gt;P. doliolum&lt;/i&gt; zones, could not be identified due to the scarcity of &lt;i&gt;P. fistula.&lt;/i&gt; Standard tropical diatom Pliocene–Pleistocene zones and subzones were identified: &lt;i&gt;Nitzschia reinholdii, Rhizosolenia praebergonii&lt;/i&gt;, and &lt;i&gt;Nitzschia jouseae&lt;/i&gt; zones. The development of oxygen isotope calibrated dates enabled the dating of some radiolarian events: FAD &lt;i&gt;A. angulare&lt;/i&gt; 1.65 Ma, LAD &lt;i&gt;Theocorythium vetulum&lt;/i&gt; 2 Ma, LAD &lt;i&gt;A. jenghisi&lt;/i&gt; 2.21 Ma, FAD &lt;i&gt;Theocalyptra davisiana&lt;/i&gt; 2.33 Ma, FAD &lt;i&gt;Theocorythium trachelium&lt;/i&gt; 2.33 Ma, and FAD &lt;i&gt;Lamprocyrtis neoheteroporos&lt;/i&gt; 2.4 Ma.</p>
</abstract>
<counts><page-count count="9"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>