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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;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>
            <description>The topic of the resource</description>
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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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            <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;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>fingernail</name>
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        <name>Jurassic</name>
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        <name>smooth</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;TF0401&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite&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;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;
&lt;/div&gt;</text>
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        <name>Jurassic</name>
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        <name>Permian</name>
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      <tag tagId="95">
        <name>Triassic</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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            <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;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;
&lt;/div&gt;</text>
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        <name>Carboniferous</name>
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        <name>Cretaceous</name>
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        <name>Jurassic</name>
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        <name>Permian</name>
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      <tag tagId="95">
        <name>Triassic</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;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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                <text>&lt;div class="element"&gt;
&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;
&lt;/div&gt;</text>
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        <name>Calcite</name>
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      <tag tagId="94">
        <name>Jurassic</name>
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            <name>Title</name>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0404&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite Peel&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: 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;'Bullet' shape&lt;br /&gt;Conical hole where phragmocone used to be&lt;br /&gt;Radial crystals (here in cross section)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Peel of a cross section through a belemnite (manmade)&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;Have a look at this specimen under a microscope. The peel allows us to see very fine details.&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;TF0512&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Straight nautiloid&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 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;
&lt;/div&gt;
&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;
&lt;/div&gt;
&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;TF0601&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ellipsocephalus hoffi&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;Ellipsocephalus hoffi&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;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;
&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;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;TF0602&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Ogygopsis&lt;/h2&gt;</text>
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            <name>Subject</name>
            <description>The topic of the resource</description>
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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;
&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;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: Corynexochida&lt;br /&gt;Genus: Ogygopsis&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;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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            <name>Title</name>
            <description>A name given to the resource</description>
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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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            <name>Subject</name>
            <description>The topic of the resource</description>
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&lt;div class="element-text"&gt;Jince Formation, Bohemia&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;Paradoxides bohemicus&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;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: Redlichiida&lt;br /&gt;Genus: Paradoxides&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;Glabella&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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            <name>Title</name>
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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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            <name>Description</name>
            <description>An account of the resource</description>
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              <elementText elementTextId="430">
                <text>&lt;div class="element"&gt;
&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician to Silurian&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: 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;
&lt;/div&gt;
&lt;div class="element"&gt;
&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;
&lt;/div&gt;</text>
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