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                <text>&lt;h2&gt;&lt;strong&gt;TF1124&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Rugose coral (manmade cast)&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: 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;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Manmade cast&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0801&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Crinoid stem fragment&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Crinoids: Ordovician to recent&lt;/div&gt;
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&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;Ossicles (fused)&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal mould of stereome by haematite, slightly compressed&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0802&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Actinocritus (stem segments)&lt;/h2&gt;</text>
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h3&gt;Location&lt;/h3&gt;
Carboniferous limestone, Whatley&lt;/div&gt;
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&lt;div class="element"&gt;&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Carboniferous&lt;/div&gt;
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&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;Ossicles (fused)&lt;br /&gt;Stereome&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&lt;br /&gt;Sediment infill&lt;/div&gt;
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        <name>Calcite</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0803&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Encrinus Lilliformis&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;Brunswick, Germany&lt;/div&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Encrinus lilliformis&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Triassic&lt;/div&gt;
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&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;br /&gt;Order: Encrinida&lt;br /&gt;Family: Encrinidae&lt;br /&gt;Genus: Encrinus&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Ossicles (fused)&lt;br /&gt;Crown with individual arms&lt;br /&gt;Attachment point for calyx&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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                <text>&lt;h2&gt;&lt;strong&gt;TF0804&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Apiocrinites&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;Bradford Clay&lt;/div&gt;
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&lt;div class="element-set"&gt;
&lt;div class="element"&gt;&lt;/div&gt;
&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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&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: Crinoidea&lt;br /&gt;Order: Millericrinida&lt;br /&gt;Genus: Apiocrinites&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Pentaradial symmetry&lt;br /&gt;Calyx&lt;br /&gt;Attachment point for 'arms' of the animal&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;
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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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            <description>An account of the resource</description>
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&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;
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&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Cast (manmade)&lt;/div&gt;
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      <description>An inanimate, three-dimensional object or substance. Note that digital representations of, or surrogates for, these objects should use Moving Image, Still Image, Text or one of the other types.</description>
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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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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Florigemma&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;/div&gt;
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&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;
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&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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          <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;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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          <element elementId="49">
            <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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            <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;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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          <element elementId="50">
            <name>Title</name>
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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>
          <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>
            <elementTextContainer>
              <elementText elementTextId="365">
                <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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