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                <text>&lt;h2&gt;&lt;strong&gt;TF0403&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Oxford Clay, Warboys Pit, St Ives&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;&lt;/h3&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;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Hastatus&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;Order: Belemnitida&lt;br /&gt;Genus: Hibolites&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;'Bullet' shape&lt;br /&gt;Guard with radial crystals&lt;br /&gt;Hollow phragmocone area&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 calcitic guard&lt;br /&gt;Dissolution of aragonitic phragmocone&lt;br /&gt;Sediment infil of phragmocone area&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;Hibolites are not as bullet shaped as most belemnites, and at first glance could be confused with an Echinoid spine. However the radial arrangement of crystals and the presence of a hollow region where the phragmocone would once have been allows us to, after some examination, confirm these specimens as belemnites.&lt;/div&gt;
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        <name>Calcite</name>
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        <name>Jurassic</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0402&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Carboniferous to 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;Order: Belemnitida&lt;br /&gt;&lt;br /&gt;Set 1:&lt;br /&gt;Group: Cylindroteuthis&lt;br /&gt;Set 2:&lt;br /&gt;Group: unknown&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;Guard with radial calcite crystals&lt;br /&gt;Crushed conical hole where phragmocone used to be&lt;br /&gt;Long, near cylindrical 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;Dissolution of phragmocone&lt;br /&gt;Sediment infill of conical cavity where phragmocone used to be&lt;br /&gt;Crushing of infilled phragmocone area&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0401&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Carboniferous to 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;Order: Belemnitida&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;Guard of radial calcite crystals&lt;br /&gt;Conical cavity where phragmocone used to be&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Aragonitic phragmocone dissolved&lt;br /&gt;Sediment infil of conical cavity where phragmocone used to be (set 1 only)&lt;/div&gt;
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                  <text>&lt;p&gt;Welcome to the fossils section of the website. This is designed to help you learn the different characteristics of each major fossil group so that you are able to distinguish between them.&lt;/p&gt;
&lt;p&gt;First year students, please refer to the specimens housed in the first year teaching laboratory. There is no substitute for handling the specimens themselves; this website is just an accessory to help you along the way.&lt;/p&gt;
&lt;p&gt;Animals occupy different environments, have different life habits and lived through different periods in geological time. It is good to be aware of these differences in lifestyle and timing, within and between phyla, classes, orders and families.&lt;/p&gt;</text>
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                <text>&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h2&gt;Taxonomy&lt;span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/h2&gt;
&lt;p&gt;Phylum: Mollusca&lt;/p&gt;
&lt;p&gt;Class: Cephalopoda&lt;/p&gt;
&lt;p&gt;Subclass: Coleoidea&lt;/p&gt;
&lt;p&gt;Cohort: Belemnoidea&lt;/p&gt;
&lt;h2&gt;Diagnostic Features&lt;/h2&gt;
&lt;p&gt;Diagram with labelled features of belemnites&lt;/p&gt;
&lt;p&gt;'Bullet' shape&lt;/p&gt;
&lt;p&gt;Phragmocone: chambers divided by aragonitic septa (often preserved as conical cavity)&lt;/p&gt;
&lt;p&gt;Radial calcite crystals form the guard&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Nektonic&lt;/p&gt;
&lt;p&gt;Predatory&lt;/p&gt;
&lt;p&gt;Marine&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Exceptional preservation of belemnites showing soft parts has shown them to be very similar to squid in shape. The guard and phragmocone were held inside the soft parts of the animals, acting as a kind of backbone.&lt;/p&gt;
&lt;p&gt;Because the phragmocone is made of aragonite it is often not preserved. In contrast the calcitic guard is very often preserved. This means that a common preservation of belemnites is of the guard with a conical hole where the phragmocone once was. This empty conical chamber is often crushed.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/belemnites" target="_blank" rel="noreferrer noopener"&gt;Browse belemnites&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;External Links&lt;/h2&gt;
&lt;p&gt;&lt;a href="http://www.conchsoc.org/MolluscWorld20/7"&gt;Mollusc World&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;&lt;a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/"&gt;Learn about types of preservation&lt;/a&gt;&lt;/p&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>Cretaceous</name>
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        <name>Jurassic</name>
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                  <text>&lt;p&gt;Welcome to the fossils section of the website. This is designed to help you learn the different characteristics of each major fossil group so that you are able to distinguish between them.&lt;/p&gt;
&lt;p&gt;First year students, please refer to the specimens housed in the first year teaching laboratory. There is no substitute for handling the specimens themselves; this website is just an accessory to help you along the way.&lt;/p&gt;
&lt;p&gt;Animals occupy different environments, have different life habits and lived through different periods in geological time. It is good to be aware of these differences in lifestyle and timing, within and between phyla, classes, orders and families.&lt;/p&gt;</text>
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                <text>&lt;h2&gt;Ammonoid&lt;/h2&gt;</text>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Mollusca&lt;/p&gt;
&lt;p&gt;Class: Cephalopoda&lt;/p&gt;
&lt;p&gt;Subclass: Ammonoidea&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;[See labelled diagram above]&lt;/p&gt;
&lt;p&gt;Aragonite shell&lt;/p&gt;
&lt;p&gt;Septa&lt;/p&gt;
&lt;p&gt;Suture (different for goniatites, ceratites and ammonites, see second diagram above)&lt;/p&gt;
&lt;p&gt;Chambers&lt;/p&gt;
&lt;p&gt;Siphuncle&lt;/p&gt;
&lt;p&gt;Planispiral shape, involute or evolute (see third diagram on right hand side)&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Devonian to Cretaceous&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Nektonic (jet propelled)&lt;/p&gt;
&lt;p&gt;Predatory&lt;/p&gt;
&lt;p&gt;Marine&lt;/p&gt;
&lt;h2&gt;Common preservation&lt;/h2&gt;
&lt;p&gt;Internal mould&lt;/p&gt;
&lt;p&gt;&lt;a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/"&gt;Learn about types of preservation&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Ammonoids could passively remove or add water to chambers via the siphuncle. This allowed them to change their density, and maintain neutral buoyancy with the surrounding seawater. This meant that they were able to swim as efficiently as possible.&lt;/p&gt;
&lt;p&gt;Ammonoids are extremely good index fossils on account of their diverse morphologies, good preservation potentials and widespread fossil locations.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/ammonoids" target="_blank" rel="noreferrer noopener"&gt;Browse ammonoids&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;External links&lt;/h2&gt;
&lt;p&gt;&lt;a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener"&gt;Telling planispiral fossils apart&lt;/a&gt;&lt;/p&gt;</text>
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        <name>Carboniferous</name>
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      <tag tagId="92">
        <name>Cretaceous</name>
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      <tag tagId="96">
        <name>Devonian</name>
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      <tag tagId="94">
        <name>Jurassic</name>
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      <tag tagId="98">
        <name>Permian</name>
      </tag>
      <tag tagId="95">
        <name>Triassic</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0331&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ammonite Aptychus&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>&lt;h3&gt;Location&lt;/h3&gt;
&lt;span&gt;Kimmeridge Clay, Roslyn Pit, Ely&lt;/span&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;latus Parkinson&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;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Straight edge&lt;br /&gt;Growth lines&lt;br /&gt;Curved plate&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Calcite&lt;br /&gt;Disarticulated from ammonite 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;One could be forgiven for thinking, at first glance, that this was the valve of a bivalve mollusc. However further interrogation of the fossil: the shape, the fact that the growth lines are on one side of the shell but there is no sign of adductor muscle scars, palial sinuses or other characteristic bivalve signs, and the 'bobbled' texture on the plate, leads us to the conclusion that this is not from a bivalve.&lt;br /&gt;&lt;br /&gt;Rare examples of ammonite shells with aptychi preserved articulated have shown these plates to be located in the body chamber of ammonites. Upon death most pairs of aptychi disarticulate and hence they are found as single plates, such as this one.&lt;/div&gt;
&lt;/div&gt;</text>
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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;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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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Dactylioceras commune&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;/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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                <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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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Hildoceras bifrons&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;/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;/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 shell (aragonite to silica)&lt;/div&gt;
&lt;/div&gt;</text>
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&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;Parkinsonia parkinsonia&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;Evolute&lt;br /&gt;Ribs&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;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;
&lt;/div&gt;</text>
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&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;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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