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                <text>&lt;h2&gt;&lt;strong&gt;TF0208&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Littorina muricata&lt;/h2&gt;</text>
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                <text>&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;Coralline Oolite, Upware, Cambridgeshire&lt;/div&gt;
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Littorina muricata&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;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Mollusca&lt;br /&gt;Class: Gastropoda&lt;br /&gt;Genus: Littorina&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;Coiled shell (helical)&lt;br /&gt;Spire&lt;br /&gt;Body whorl&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 and external casts&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0301&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Goniatite&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Goniaites&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;Devonian to Permian&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Goniatitida&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;Planispiral shell&lt;br /&gt;Goniatitic suture lines&lt;br /&gt;Involute&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal mould&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0311&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ceratite&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Ceratites&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Triassic&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;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ceratitida&lt;br /&gt;&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;Planispiral&lt;br /&gt;Aperture&lt;br /&gt;Body chamber&lt;br /&gt;Ceratitic suture lines&lt;br /&gt;Evolute&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal 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;Set 1 specimen is a plaster cast&lt;/div&gt;
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        <name>suture</name>
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        <name>Triassic</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0321&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ammonite&lt;/h2&gt;</text>
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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;Dactylioceras commune&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&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;Ribs&lt;br /&gt;Imprint of inner whorls visible&lt;br /&gt;Curved shape (part of coil)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Pyritised shell replacement&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>Jurassic</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0322&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ammonite&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Hildoceras bifrons&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;
&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;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&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;Planispiral&lt;br /&gt;Evolute&lt;br /&gt;Ribs&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of shell (aragonite to silica)&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0323&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ammonite&lt;/h2&gt;</text>
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            <description>An account of the resource</description>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Parkinsonia parkinsonia&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&lt;br /&gt;&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;Planispiral&lt;br /&gt;Evolute&lt;br /&gt;Ribs&lt;br /&gt;Ammonitic suture lines&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Calcite has replaced aragonite in the 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;Beware! The specimen in set 2 has a dark circular hole, which you may be tempted to identify as a siphuncle. However remember that in ammonoids the siphuncle runs around the outer edge of the chambers, so this hole is in the wrong place. It is probably there due to eccentricities of the mineralisation process.&lt;br /&gt;&lt;br /&gt;Why is it a dark colour when the rest of the shell is white? Generations of Earth Scientists have made the same mistake, their pencil marks fooling others into making the same error.&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;Amoeboceras alternans&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&lt;br /&gt;&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;Planispiral&lt;br /&gt;Ammonitic suture lines visible on some moulds&lt;br /&gt;Ribs&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Most external moulds, few examples of internal moulds, pyritised&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>Jurassic</name>
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        <name>suture</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0325&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ammonite&lt;/h2&gt;</text>
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&lt;div class="element"&gt;
&lt;div class="element-text"&gt;Deshayesites&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&lt;br /&gt;&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;Planispiral&lt;br /&gt;Ammonitic suture pattern&lt;br /&gt;Evolute&lt;br /&gt;Ribs&lt;br /&gt;Aperture&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal mould, with aperture partially crushed&lt;/div&gt;
&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;TF0326&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ammonite&lt;/h2&gt;</text>
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            <name>Description</name>
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&lt;div class="element"&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Anahoplites splendens&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&lt;br /&gt;&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;Planispiral&lt;br /&gt;Involute&lt;br /&gt;Ammonitic suture pattern&lt;br /&gt;Ribs&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal mould, pyritised&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;For the specimen in set 1 only part of the whole shell is present. The rest has either broken off or not been preserved at all.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element-text"&gt;&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>ammonite</name>
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        <name>Cretaceous</name>
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        <name>Jurassic</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0327&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Heteromorphic ammonite&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Scaphites&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: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Subclass: Ammonoidea&lt;br /&gt;Order: Ammonitida&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;'g' shaped coiled shell&lt;br /&gt;Ribs&lt;br /&gt;Involute&lt;br /&gt;Ammonitic suture lines&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal 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;Heteromorphic ammonites (such as Scaphites) diversified during the late Cretaceous. They may have lived as planktonic or benthic organisms depending on where the centre of gravity lies in the shell, which is much dependent on the soft parts. Sadly these soft parts rarely preserve.&lt;/div&gt;
&lt;/div&gt;</text>
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