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                <text>&lt;h2&gt;&lt;strong&gt;TF0613&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Cheirurus hydei&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Cheirurus hydei&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;Ordovician 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: Arthropoda&lt;br /&gt;Class: Trilobita&lt;br /&gt;Order: Phacopida&lt;br /&gt;Family: Cheiruridae&lt;br /&gt;Genus: Cheirurus&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Pygidium&lt;br /&gt;Thorax&lt;br /&gt;Cephalon&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;External mould (manmade cast)&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0612&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ogygiocarella debuchi&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Ogygiocarella debuchi&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician&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: Arthropoda&lt;br /&gt;Class: Trilobita&lt;br /&gt;Order: Asaphida&lt;br /&gt;Genus: Ogygiocarella&lt;/div&gt;
&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Cephalon&lt;br /&gt;Thorax&lt;br /&gt;Pygidium&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 (manmade)&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0611&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Trinucleid&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician to Silurian&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: Arthropoda&lt;br /&gt;Class: Trilobita&lt;br /&gt;Order: Asaphida&lt;br /&gt;Family: Trinucleidae&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;Cephalon&lt;br /&gt;Thorax&lt;br /&gt;Pygidium&lt;br /&gt;Large fringe at front of cephalon&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 (manmade)&lt;/div&gt;
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&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;Trinucleids were fast moving low level epifaunal suspension feeders. The large fringe at the front of the cephalon may have been for food gathering, and their large cephalon size may have been an antipredatory adaptation. Some exceptionally preserved specimens have been found with sediment in the guts of the animals, perhaps supporting the suspension-feeding hypothesis.&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0603&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Paradoxides bohemicus&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Jince Formation, Bohemia&lt;/div&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Paradoxides bohemicus&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Cambrian&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: Arthropoda&lt;br /&gt;Class: Trilobita&lt;br /&gt;Order: Redlichiida&lt;br /&gt;Genus: Paradoxides&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Cephalon&lt;br /&gt;Thorax&lt;br /&gt;Pygidium&lt;br /&gt;Glabella&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;External mould (manmade cast)&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0602&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ogygopsis&lt;/h2&gt;</text>
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&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Mount Stephen, Brisith Columbia, Canada&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Cambrian&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: Arthropoda&lt;br /&gt;Class: Trilobita&lt;br /&gt;Order: Corynexochida&lt;br /&gt;Genus: Ogygopsis&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;Glabella&lt;br /&gt;Eye ridges&lt;br /&gt;Cephalon&lt;br /&gt;Thorax&lt;br /&gt;Pygidium&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 (manmade cast)&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0601&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ellipsocephalus hoffi&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Ellipsocephalus hoffi&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;Cambrian&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: Arthropoda&lt;br /&gt;Class: Trilobita&lt;br /&gt;Order: Ptychopariida&lt;br /&gt;Genus: Ellipsocephalus&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;Cephalon&lt;br /&gt;Thorax&lt;br /&gt;Pygidium&lt;br /&gt;No eyes&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 of a mould (manmade)&lt;br /&gt;External moulds of trilobite hard parts&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;&lt;em&gt;Ellipsocephalus hoffi&lt;/em&gt;&lt;span&gt; &lt;/span&gt;was a blind species of trilobite. It likely lived in deep, poorly lit, aphotic environments.&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0512&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Straight nautiloid&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Cambrian 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: Mollusca&lt;br /&gt;Class: Cephalopoda&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;Straight&lt;br /&gt;Chambers&lt;br /&gt;Septa&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;Manmade internal cast&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;Nautiloids originated in the Cambrian and radiated during the Ordovician. Straight nautiloids went extinct in the Permian, but planispirally coiled nautiloids, for example the nautilus, live in the sea today.&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;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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&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;
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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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            <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;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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            <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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            <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>
            <elementTextContainer>
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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;
&lt;/div&gt;</text>
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