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  <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?tags=Triassic&amp;output=atom</id>
  <title><![CDATA[1A Collections]]></title>
  <subtitle><![CDATA[Rocks, minerals and fossils collections for Part 1A students]]></subtitle>
  <author>
    <name><![CDATA[Department of Earth Sciences]]></name>
  </author>
  <updated>2024-04-09T21:16:30+01:00</updated>
  <generator>Omeka</generator>
  <link rel="self" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?tags=Triassic&amp;output=atom"/>
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    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/82</id>
    <title><![CDATA[<h2><strong>TF0402<br /></strong></h2>
<h2>Belemnite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida<br /><br />Set 1:<br />Group: Cylindroteuthis<br />Set 2:<br />Group: unknown</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard with radial calcite crystals<br />Crushed conical hole where phragmocone used to be<br />Long, near cylindrical shape</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Dissolution of phragmocone<br />Sediment infill of conical cavity where phragmocone used to be<br />Crushing of infilled phragmocone area</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:28+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/82"/>
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    <category term="Carboniferous"/>
    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <category term="Permian"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0402<br /></strong></h2>
<h2>Belemnite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida<br /><br />Set 1:<br />Group: Cylindroteuthis<br />Set 2:<br />Group: unknown</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard with radial calcite crystals<br />Crushed conical hole where phragmocone used to be<br />Long, near cylindrical shape</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Dissolution of phragmocone<br />Sediment infill of conical cavity where phragmocone used to be<br />Crushing of infilled phragmocone area</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/81</id>
    <title><![CDATA[<h2><strong>TF0401<br /></strong></h2>
<h2>Belemnite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard of radial calcite crystals<br />Conical cavity where phragmocone used to be</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Aragonitic phragmocone dissolved<br />Sediment infil of conical cavity where phragmocone used to be (set 1 only)</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:27+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/81"/>
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    <category term="Carboniferous"/>
    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <category term="Permian"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0401<br /></strong></h2>
<h2>Belemnite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard of radial calcite crystals<br />Conical cavity where phragmocone used to be</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Aragonitic phragmocone dissolved<br />Sediment infil of conical cavity where phragmocone used to be (set 1 only)</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/79</id>
    <title><![CDATA[<h2>Ammonoid</h2>]]></title>
    <summary><![CDATA[<h2>Taxonomy</h2>
<p>Phylum: Mollusca</p>
<p>Class: Cephalopoda</p>
<p>Subclass: Ammonoidea</p>
<h2>Diagnostic features</h2>
<p>[See labelled diagram above]</p>
<p>Aragonite shell</p>
<p>Septa</p>
<p>Suture (different for goniatites, ceratites and ammonites, see second diagram above)</p>
<p>Chambers</p>
<p>Siphuncle</p>
<p>Planispiral shape, involute or evolute (see third diagram on right hand side)</p>
<h2>Stratigraphic range</h2>
<p>Devonian to Cretaceous</p>
<h2>Way of life</h2>
<p>Nektonic (jet propelled)</p>
<p>Predatory</p>
<p>Marine</p>
<h2>Common preservation</h2>
<p>Internal mould</p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
<h2>Advanced notes</h2>
<p>Ammonoids could passively remove or add water to chambers via the siphuncle. This allowed them to change their density, and maintain neutral buoyancy with the surrounding seawater. This meant that they were able to swim as efficiently as possible.</p>
<p>Ammonoids are extremely good index fossils on account of their diverse morphologies, good preservation potentials and widespread fossil locations.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/ammonoids" target="_blank" rel="noreferrer noopener">Browse ammonoids</a></p>
<h2>External links</h2>
<p><a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener">Telling planispiral fossils apart</a></p>]]></summary>
    <updated>2019-08-06T10:44:34+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/79"/>
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    <category term="Carboniferous"/>
    <category term="Cretaceous"/>
    <category term="Devonian"/>
    <category term="Jurassic"/>
    <category term="Permian"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Ammonoid</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><h2>Taxonomy</h2>
<p>Phylum: Mollusca</p>
<p>Class: Cephalopoda</p>
<p>Subclass: Ammonoidea</p>
<h2>Diagnostic features</h2>
<p>[See labelled diagram above]</p>
<p>Aragonite shell</p>
<p>Septa</p>
<p>Suture (different for goniatites, ceratites and ammonites, see second diagram above)</p>
<p>Chambers</p>
<p>Siphuncle</p>
<p>Planispiral shape, involute or evolute (see third diagram on right hand side)</p>
<h2>Stratigraphic range</h2>
<p>Devonian to Cretaceous</p>
<h2>Way of life</h2>
<p>Nektonic (jet propelled)</p>
<p>Predatory</p>
<p>Marine</p>
<h2>Common preservation</h2>
<p>Internal mould</p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
<h2>Advanced notes</h2>
<p>Ammonoids could passively remove or add water to chambers via the siphuncle. This allowed them to change their density, and maintain neutral buoyancy with the surrounding seawater. This meant that they were able to swim as efficiently as possible.</p>
<p>Ammonoids are extremely good index fossils on account of their diverse morphologies, good preservation potentials and widespread fossil locations.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/ammonoids" target="_blank" rel="noreferrer noopener">Browse ammonoids</a></p>
<h2>External links</h2>
<p><a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener">Telling planispiral fossils apart</a></p></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/76</id>
    <title><![CDATA[<h2><strong>TF0311<br /></strong></h2>
<h2>Ceratite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Species</h3>
<div class="element-text">Ceratites</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Triassic</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ceratitida<br /><br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Planispiral<br />Aperture<br />Body chamber<br />Ceratitic suture lines<br />Evolute</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Set 1 specimen is a plaster cast</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:26+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/76"/>
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    <category term="suture"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0311<br /></strong></h2>
<h2>Ceratite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Species</h3>
<div class="element-text">Ceratites</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Triassic</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ceratitida<br /><br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Planispiral<br />Aperture<br />Body chamber<br />Ceratitic suture lines<br />Evolute</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Set 1 specimen is a plaster cast</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
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