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            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1003&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Didymograptus&lt;/h2&gt;</text>
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            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Specimen Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician&lt;br /&gt;&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Llandeilo, Abereiddy Bay, Wales&lt;/div&gt;
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            <description>An account of the resource</description>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Hemichordata&lt;br /&gt;Class: Graptolithina&lt;br /&gt;Genus: Didymograptus&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Stipes (2)&lt;br /&gt;Thecae&lt;br /&gt;Rhabdosome&lt;br /&gt;Nema&lt;br /&gt;'sawtooth'&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Flattened&lt;br /&gt;Carbon film&lt;br /&gt;Pale colourisation from chlorine inclusion into the fossil&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;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&lt;span&gt; &lt;/span&gt;&lt;em&gt;Tetrapgraptus&lt;/em&gt;, but close examination reveals that there are two animals, squashed on top of each other.&lt;/div&gt;
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1002&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Graptoloid graptolite&lt;/h2&gt;</text>
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          <element elementId="49">
            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Specimen Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician&lt;br /&gt;&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Australia&lt;/div&gt;
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            <name>Description</name>
            <description>An account of the resource</description>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Hemichordata&lt;br /&gt;Class: Graptolithina&lt;br /&gt;Order: Graptoloidea&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Thecae&lt;br /&gt;Stipes&lt;br /&gt;Rhabdosome&lt;br /&gt;Nema&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Flattened&lt;br /&gt;Carbon film&lt;br /&gt;Red colour from iron in sediment seeping into fossil&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;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&lt;span&gt; &lt;/span&gt;&lt;em&gt;Tetragraptus&lt;/em&gt;&lt;span&gt; &lt;/span&gt;and two stiped animals such as&lt;span&gt; &lt;/span&gt;&lt;em&gt;Didymograptus&lt;/em&gt;&lt;span&gt; &lt;/span&gt;in time.&lt;/div&gt;
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1001&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Dendroid graptolites&lt;/h2&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Cambrian to Carboniferous&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Hemichordata&lt;br /&gt;Class: Graptolithina&lt;br /&gt;Order: Dendroidea&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Numerous branching stipes&lt;br /&gt;Colonial&lt;br /&gt;Thecae&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Flattened&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;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.&lt;br /&gt;&lt;br /&gt;Dendroid graptolites began as benthic organisms attaching to the seafloor with a holdfast, but some diversified as planktonic animals, with a reduced holdfast.&lt;/div&gt;
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