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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0806&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Crinoid (cast)&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;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Echinodermata&lt;br /&gt;Class: Crinoidea&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;Stem&lt;br /&gt;Calyx&lt;br /&gt;Crown&lt;br /&gt;Ossicles (fused)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Cast (manmade)&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;TF0901&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Regular echinoid spine&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Coral Rag, Upware, Cambridgeshire&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;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Florigemma&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: Echinodermata&lt;br /&gt;Class: Echinoidea&lt;br /&gt;Order: Cidaroida&lt;br /&gt;Genus: Cidaris&lt;br /&gt;&lt;br /&gt;&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;'Club' shaped&lt;br /&gt;Thorns&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 (calcite)&lt;br /&gt;Disarticulated from body shell&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;This is a spine from a regular echinoid. You can tell this by the shape and thickness of the spine.&lt;br /&gt;Irregular echinoids live under the sediment in burrows, using their spines for movement, not for protection, and hence the spines are fine and able to be manipulated.&lt;br /&gt;Regular echinoids live epifaunally, and so are a target for predators. These spines are needed to prevent attack of the shell containing the soft parts of the animal, and the 'club' like shape decreases access opportunities for predators. Other regular echinoid spines are long and thin, pointed, offering a more 'offensive defence' than spines such as this one.&lt;/div&gt;
&lt;/div&gt;</text>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0902&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Irregular echinoid&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;&lt;span&gt;Coralline Oolite, Upware, Cambridgeshire&lt;/span&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;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;depressus Lestre&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: Echinodermata&lt;br /&gt;Class: Echinoidea&lt;br /&gt;Subclass: Irregularia&lt;br /&gt;Order: Holectypoida&lt;br /&gt;Genus: Holectypus&lt;br /&gt;&lt;br /&gt;&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;Bilateral symmetry&lt;br /&gt;Five radial ambulacra&lt;br /&gt;Spine attachment scars (very small)&lt;br /&gt;Peristome and anus out of line&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Shell mineral replacement&lt;br /&gt;Sediment infil&lt;br /&gt;Disarticulation of spines&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;This is a primitive irregular echinoid which would have had a functional jaw apparatus (not preserved) held within the peristome. The anus has migrated and the symmetry is bilateral, so this echinoid is clearly identifiable as irregular.&lt;/div&gt;
&lt;/div&gt;</text>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0903&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Irregular echinoid&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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                <text>&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;&lt;span&gt;Upper Chalk, Weston Colville, Cambridgeshire&lt;/span&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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              <elementText elementTextId="362">
                <text>&lt;div class="element"&gt;
&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Praecursor&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;Cretaceous&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: Echinodermata&lt;br /&gt;Class: Echinoidea&lt;br /&gt;Subclass: Irregularia&lt;br /&gt;Order: Spatangoida&lt;br /&gt;Genus: Micraster&lt;br /&gt;&lt;br /&gt;&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;Bilateral symmetry&lt;br /&gt;Five radial ambulacra&lt;br /&gt;Peristome (opening for mouth) and periproct (opening for anus) migrated&lt;br /&gt;Spine attachment scars&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Sediment infil&lt;br /&gt;Shell mineral replacement&lt;br /&gt;Disarticulation of spines&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;Note the streamlined shape for burrowing through the sediment, and how the ambulacra, which bear the tube feet, do not continue onto the underside of the animal where the mouth is.&lt;br /&gt;This is because the tube feet are used for respiration but not for movement, for which small spines are used.&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;TF0904&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Irregular echinoid&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;Source&lt;/h3&gt;
&lt;div class="element-text"&gt;&lt;span&gt;Quaternary River Gravel, derived from Cretaceous chalk&lt;/span&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;Cretaceous&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: Echinodermata&lt;br /&gt;Class: Echinoidea&lt;br /&gt;Subclass: Irregularia&lt;br /&gt;Order: Echinoneoida&lt;br /&gt;Genus: Conulus&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;Bilateral symmetry&lt;br /&gt;Five radial ambulacra&lt;br /&gt;Interambulacra&lt;br /&gt;Migrated periproct (opening for anus)&lt;br /&gt;Peristome (opening for mouth)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;This fossil was collected in Quaternary river gravel. Originally it was preserved in the Upper Chalk (Cretaceous). This was broken up into clasts by erosive processes, one of which was this irregular echinoid. The echinoid clast was carried by a river downstream and deposited in the river gravel unit during the Quaternary.&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;Note how the anus has migrated, but the peristome is still in the position you would expect from a regular echinoid (not migrated). Notice also how the ambulacra bearing the tube feet continue onto the underside, a feature not seen in more streamlined and derived irregular echinoids.&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>bilateral</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;TF0905&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Irregular echinoid&lt;/h2&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;Upper Cretaceous&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: Echinodermata&lt;br /&gt;Class: Echinodea&lt;br /&gt;Subclass: Irregularia&lt;br /&gt;Order: Holasteroida&lt;br /&gt;&lt;br /&gt;&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;Bilateral symmetry&lt;br /&gt;Mouth and anus out of line&lt;br /&gt;Five radial ambulacra&lt;br /&gt;Interambulacra with plates&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Sediment infill&lt;br /&gt;Mineral replacement of shell&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;Set 1: Anus and mouth appear to have been drilled to emphasise their positions.&lt;br /&gt;Set 2: Fracturing of shell around the anus which obscures it. This would be a weak part of the shell which diagenetic processes have crushed.&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>pentaradial</name>
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      <name>Physical Object</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0906&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Regular echinoid (cast)&lt;/h2&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;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Echinodermata&lt;br /&gt;Class: Echinoidea&lt;br /&gt;Subclass: Regularia&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;Pentaradial symmetry&lt;br /&gt;Anus and peristome lie in line&lt;br /&gt;Spine attachments&lt;br /&gt;Five sets of ambulacra&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Cast (internal mould of an external mould)&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;Spine attachments very much larger than for irregular echinoids as they have to hold much larger spines. Spines on regular echinoids are for defence and preventing predation, unlike for irregular echinoids where the spines are for movement in burrows. Watch a video of regular echinoids moving:&lt;span&gt; &lt;/span&gt;&lt;a href="https://www.youtube.com/watch?v=D3W4OCnHyCs"&gt;BBC Wildlife Army of Sea Urchins&lt;/a&gt;&lt;/div&gt;
&lt;/div&gt;</text>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0907&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Regular echinoid&lt;/h2&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;Modern&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: Echinodermata&lt;br /&gt;Class: Echinoidea&lt;br /&gt;Subclass: Regularia&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;Pentaradial symmetry&lt;br /&gt;Anus and peristome in line&lt;br /&gt;Spine attachments&lt;br /&gt;Ambulacra&lt;br /&gt;Attachments for the jaw apparatus visible on the inside of the peristome&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Original shell material&lt;br /&gt;Jaw apparatus disarticulated&lt;br /&gt;Soft parts removed&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;Look at the colour of the shell and compare it to the permineralised specimens. Colour is almost always lost in the fossilisation process, even when the preservation looks to be near-perfect.&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>symmetry</name>
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        <name>urchin</name>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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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;
&lt;/div&gt;</text>
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        <name>branching</name>
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      <tag tagId="120">
        <name>colonial</name>
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          <element elementId="50">
            <name>Title</name>
            <description>A name given to the resource</description>
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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;
&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;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;
&lt;/div&gt;</text>
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      <tag tagId="120">
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