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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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                <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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                <text>&lt;div class="element"&gt;
&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;
&lt;/div&gt;</text>
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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;TF1004&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Horizontal didymograptid&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;
&lt;/div&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;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Hemichordata&lt;br /&gt;Class: Graptolithina&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;Nema&lt;br /&gt;Horizontal&lt;br /&gt;Thecae&lt;br /&gt;Rhabdosome&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Compressed&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 position of the nema tells us that there are two horizontal stipes and not one stipe. This allows identification as a&lt;span&gt; &lt;/span&gt;&lt;em&gt;Didymograptid&lt;span&gt; &lt;/span&gt;&lt;/em&gt;and not as a&lt;span&gt; &lt;/span&gt;&lt;em&gt;Monograptid&lt;/em&gt;.&lt;/div&gt;
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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;TF1005&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Graptoloid graptolites&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;
&lt;/div&gt;</text>
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          <element elementId="41">
            <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;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;Stipes&lt;br /&gt;Rhabdosome&lt;br /&gt;Thecae&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;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;You can see a range of geometries on this specimen: scandent, horizontal and pendent.&lt;/div&gt;
&lt;/div&gt;</text>
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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;TF1006&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Spiral monograptids&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;Silurian to Devonian&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;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Spiral stipes&lt;br /&gt;Rhabdosome&lt;br /&gt;Thecae&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;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;You can see various preservational geometries in these slabs.&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>colonial</name>
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            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1101&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Halysites&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>Tabulate coral</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;Silurian&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: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Tabulata&lt;br /&gt;Genus: Halysites&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;Halysites is a so-called 'chain coral'. Unsurprisingly it can be identified as it has a distinctive 'chain' appearance, each 'link' in the chain is a separate animal, all part of a larger colony.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;External mould&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>chain</name>
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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;TF1102&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Isastraea explanata&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;span&gt;&lt;span&gt;Scleractinian coral&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;h3&gt;Specimen Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;br /&gt;&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Coral Rag, Upware, Cambridgeshire&lt;/div&gt;
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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Isastraea explanata (also Isastrea explanata)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&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: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Scleractinia&lt;br /&gt;Genus: Isastrea&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;Septa&lt;br /&gt;Weak columella&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;External mould (of the 'top' of the scleractinian coral hard parts)&lt;/div&gt;
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1103&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Rugose coral&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician to Permian&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: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Tabulata&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;Septa&lt;br /&gt;Colonial&lt;br /&gt;Columella&lt;br /&gt;Polyps&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of skeleton&lt;br /&gt;Precipitation of minerals in spaces&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 presence of columella (central support structures) and septa allow identification of this fossil as a colonial rugose specimen. Columella are not present in tabulate corals as these are always colonial, and do not need the extra support.&lt;br /&gt;Solitary rugose corals developed columella as an internal support structure, and it was retained for some colonial forms, such as this one.&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF1104&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Tabulate coral&lt;/h2&gt;</text>
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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 to Permian&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: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Tabulata&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;Tabulae&lt;br /&gt;Colonial&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of skeleton&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;Due to the way that this specimen has been cut and polished, the tabulae are not immediately obvious. They are visible on parts of the slab, allowing for this to be identified as a tabulate coral.&lt;br /&gt;&lt;br /&gt;You may recognise this specimen from the coffee table in the common room on the ground floor of the Earth Sciences Department. Have a go at identifying the other fossils in the table on your next coffee break!&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1120&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Solitary rugose coral&lt;/h2&gt;</text>
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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 to Permian&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: Cnidaria&lt;br /&gt;&lt;br /&gt;Class: Anthozoa&lt;br /&gt;&lt;br /&gt;Order: Rugosa&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;Septa&lt;br /&gt;Growth lines&lt;br /&gt;'Horn' shape&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>radial</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1122&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Scleractinian coral (modern)&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Triassic to present&lt;/div&gt;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Scleractinia&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Branching structure&lt;br /&gt;Polyps&lt;br /&gt;Septa&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Original skeleton material&lt;/div&gt;
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