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  <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>2024-04-09T21:16:05+01:00</updated>
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  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/149</id>
    <title><![CDATA[<h2><strong>TF1003<br /></strong></h2>
<h2>Didymograptus</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Ordovician</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Hemichordata<br />Class: Graptolithina<br />Genus: Didymograptus</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Stipes (2)<br />Thecae<br />Rhabdosome<br />Nema<br />'sawtooth'</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Flattened<br />Carbon film<br />Pale colourisation from chlorine inclusion into the fossil</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">The 'sawtooth' faces are facing each other. This is therefore a relatively old two stiped graptolite from the Ordovician. One specimen shows two graptolites with nemas overlapping. At first glance this could be mistaken for a four stiped graptolite, such as<span> </span><em>Tetrapgraptus</em>, but close examination reveals that there are two animals, squashed on top of each other.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:51+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/149"/>
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    <category term="branching"/>
    <category term="colonial"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF1003<br /></strong></h2>
<h2>Didymograptus</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Specimen Age</h3>
<div class="element-text">Ordovician<br /><br /><h3>Location</h3>
<div class="element-text">Llandeilo, Abereiddy Bay, Wales</div>
</div></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">Ordovician</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Hemichordata<br />Class: Graptolithina<br />Genus: Didymograptus</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Stipes (2)<br />Thecae<br />Rhabdosome<br />Nema<br />'sawtooth'</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Flattened<br />Carbon film<br />Pale colourisation from chlorine inclusion into the fossil</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">The 'sawtooth' faces are facing each other. This is therefore a relatively old two stiped graptolite from the Ordovician. One specimen shows two graptolites with nemas overlapping. At first glance this could be mistaken for a four stiped graptolite, such as<span> </span><em>Tetrapgraptus</em>, but close examination reveals that there are two animals, squashed on top of each other.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/148</id>
    <title><![CDATA[<h2><strong>TF1002<br /></strong></h2>
<h2>Graptoloid graptolite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Ordovician</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Hemichordata<br />Class: Graptolithina<br />Order: Graptoloidea</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Thecae<br />Stipes<br />Rhabdosome<br />Nema</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Flattened<br />Carbon film<br />Red colour from iron in sediment seeping into fossil</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">The number of stipes decreased over time, from 4 to 3 to 2. This specimen has 3 stipes, placing it between four stiped animals such as<span> </span><em>Tetragraptus</em><span> </span>and two stiped animals such as<span> </span><em>Didymograptus</em><span> </span>in time.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:50+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/148"/>
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    <category term="colonial"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF1002<br /></strong></h2>
<h2>Graptoloid graptolite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Specimen Age</h3>
<div class="element-text">Ordovician<br /><br /><h3>Location</h3>
<div class="element-text">Australia</div>
</div></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">Ordovician</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Hemichordata<br />Class: Graptolithina<br />Order: Graptoloidea</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Thecae<br />Stipes<br />Rhabdosome<br />Nema</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Flattened<br />Carbon film<br />Red colour from iron in sediment seeping into fossil</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">The number of stipes decreased over time, from 4 to 3 to 2. This specimen has 3 stipes, placing it between four stiped animals such as<span> </span><em>Tetragraptus</em><span> </span>and two stiped animals such as<span> </span><em>Didymograptus</em><span> </span>in time.</div>
</div></div>
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  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/146</id>
    <title><![CDATA[<h2><strong>TF1001<br /></strong></h2>
<h2>Dendroid graptolites</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cambrian to Carboniferous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Hemichordata<br />Class: Graptolithina<br />Order: Dendroidea</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Numerous branching stipes<br />Colonial<br />Thecae</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Flattened</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">In this specimen we cannot see the size of a potential holdfast. Because of this we cannot say if this is a planktonic or benthic animal.<br /><br />Dendroid graptolites began as benthic organisms attaching to the seafloor with a holdfast, but some diversified as planktonic animals, with a reduced holdfast.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:50+01:00</updated>
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    <category term="branching"/>
    <category term="colonial"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF1001<br /></strong></h2>
<h2>Dendroid graptolites</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">Cambrian to Carboniferous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Hemichordata<br />Class: Graptolithina<br />Order: Dendroidea</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Numerous branching stipes<br />Colonial<br />Thecae</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Flattened</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">In this specimen we cannot see the size of a potential holdfast. Because of this we cannot say if this is a planktonic or benthic animal.<br /><br />Dendroid graptolites began as benthic organisms attaching to the seafloor with a holdfast, but some diversified as planktonic animals, with a reduced holdfast.</div>
</div></div>
            </div><!-- end element -->
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