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  <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?tags=Cretaceous&amp;output=atom</id>
  <title><![CDATA[1A Collections]]></title>
  <subtitle><![CDATA[Rocks, minerals and fossils collections for Part 1A students]]></subtitle>
  <author>
    <name><![CDATA[Department of Earth Sciences]]></name>
  </author>
  <updated>2024-04-09T21:15:52+01:00</updated>
  <generator>Omeka</generator>
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  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/82</id>
    <title><![CDATA[<h2><strong>TF0402<br /></strong></h2>
<h2>Belemnite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida<br /><br />Set 1:<br />Group: Cylindroteuthis<br />Set 2:<br />Group: unknown</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard with radial calcite crystals<br />Crushed conical hole where phragmocone used to be<br />Long, near cylindrical shape</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Dissolution of phragmocone<br />Sediment infill of conical cavity where phragmocone used to be<br />Crushing of infilled phragmocone area</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:28+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/82"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/d334c4736d6513fda605078c572ddbf5.png" type="image/png" length="1069067"/>
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    <category term="Carboniferous"/>
    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <category term="Permian"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0402<br /></strong></h2>
<h2>Belemnite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida<br /><br />Set 1:<br />Group: Cylindroteuthis<br />Set 2:<br />Group: unknown</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard with radial calcite crystals<br />Crushed conical hole where phragmocone used to be<br />Long, near cylindrical shape</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Dissolution of phragmocone<br />Sediment infill of conical cavity where phragmocone used to be<br />Crushing of infilled phragmocone area</div>
</div></div>
            </div><!-- end element -->
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  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/81</id>
    <title><![CDATA[<h2><strong>TF0401<br /></strong></h2>
<h2>Belemnite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard of radial calcite crystals<br />Conical cavity where phragmocone used to be</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Aragonitic phragmocone dissolved<br />Sediment infil of conical cavity where phragmocone used to be (set 1 only)</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:27+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/81"/>
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    <category term="Carboniferous"/>
    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <category term="Permian"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0401<br /></strong></h2>
<h2>Belemnite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous to Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Guard of radial calcite crystals<br />Conical cavity where phragmocone used to be</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Aragonitic phragmocone dissolved<br />Sediment infil of conical cavity where phragmocone used to be (set 1 only)</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/80</id>
    <title><![CDATA[<h2>Belemnite</h2>]]></title>
    <summary><![CDATA[<div>
<div class="element-set">
<div class="element">
<div class="element-text">
<h2>Taxonomy<span><br /></span></h2>
<p>Phylum: Mollusca</p>
<p>Class: Cephalopoda</p>
<p>Subclass: Coleoidea</p>
<p>Cohort: Belemnoidea</p>
<h2>Diagnostic Features</h2>
<p>Diagram with labelled features of belemnites</p>
<p>'Bullet' shape</p>
<p>Phragmocone: chambers divided by aragonitic septa (often preserved as conical cavity)</p>
<p>Radial calcite crystals form the guard</p>
<h2>Way of life</h2>
<p>Nektonic</p>
<p>Predatory</p>
<p>Marine</p>
<h2>Advanced notes</h2>
<p>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.</p>
<p>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.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/belemnites" target="_blank" rel="noreferrer noopener">Browse belemnites</a></p>
<h2>External Links</h2>
<p><a href="http://www.conchsoc.org/MolluscWorld20/7">Mollusc World</a></p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
</div>
</div>
</div>
</div>]]></summary>
    <updated>2019-08-06T10:53:04+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/80"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/6009607451cd8aaf8df0774b2bdfdcde.png" type="image/png" length="103420"/>
    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Belemnite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div>
<div class="element-set">
<div class="element">
<div class="element-text">
<h2>Taxonomy<span><br /></span></h2>
<p>Phylum: Mollusca</p>
<p>Class: Cephalopoda</p>
<p>Subclass: Coleoidea</p>
<p>Cohort: Belemnoidea</p>
<h2>Diagnostic Features</h2>
<p>Diagram with labelled features of belemnites</p>
<p>'Bullet' shape</p>
<p>Phragmocone: chambers divided by aragonitic septa (often preserved as conical cavity)</p>
<p>Radial calcite crystals form the guard</p>
<h2>Way of life</h2>
<p>Nektonic</p>
<p>Predatory</p>
<p>Marine</p>
<h2>Advanced notes</h2>
<p>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.</p>
<p>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.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/belemnites" target="_blank" rel="noreferrer noopener">Browse belemnites</a></p>
<h2>External Links</h2>
<p><a href="http://www.conchsoc.org/MolluscWorld20/7">Mollusc World</a></p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
</div>
</div>
</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/79</id>
    <title><![CDATA[<h2>Ammonoid</h2>]]></title>
    <summary><![CDATA[<h2>Taxonomy</h2>
<p>Phylum: Mollusca</p>
<p>Class: Cephalopoda</p>
<p>Subclass: Ammonoidea</p>
<h2>Diagnostic features</h2>
<p>[See labelled diagram above]</p>
<p>Aragonite shell</p>
<p>Septa</p>
<p>Suture (different for goniatites, ceratites and ammonites, see second diagram above)</p>
<p>Chambers</p>
<p>Siphuncle</p>
<p>Planispiral shape, involute or evolute (see third diagram on right hand side)</p>
<h2>Stratigraphic range</h2>
<p>Devonian to Cretaceous</p>
<h2>Way of life</h2>
<p>Nektonic (jet propelled)</p>
<p>Predatory</p>
<p>Marine</p>
<h2>Common preservation</h2>
<p>Internal mould</p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
<h2>Advanced notes</h2>
<p>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.</p>
<p>Ammonoids are extremely good index fossils on account of their diverse morphologies, good preservation potentials and widespread fossil locations.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/ammonoids" target="_blank" rel="noreferrer noopener">Browse ammonoids</a></p>
<h2>External links</h2>
<p><a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener">Telling planispiral fossils apart</a></p>]]></summary>
    <updated>2019-08-06T10:44:34+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/79"/>
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    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/28a1fb886f7368006421315c7a409b82.png" type="image/png" length="54029"/>
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    <category term="Carboniferous"/>
    <category term="Cretaceous"/>
    <category term="Devonian"/>
    <category term="Jurassic"/>
    <category term="Permian"/>
    <category term="Triassic"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Ammonoid</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><h2>Taxonomy</h2>
<p>Phylum: Mollusca</p>
<p>Class: Cephalopoda</p>
<p>Subclass: Ammonoidea</p>
<h2>Diagnostic features</h2>
<p>[See labelled diagram above]</p>
<p>Aragonite shell</p>
<p>Septa</p>
<p>Suture (different for goniatites, ceratites and ammonites, see second diagram above)</p>
<p>Chambers</p>
<p>Siphuncle</p>
<p>Planispiral shape, involute or evolute (see third diagram on right hand side)</p>
<h2>Stratigraphic range</h2>
<p>Devonian to Cretaceous</p>
<h2>Way of life</h2>
<p>Nektonic (jet propelled)</p>
<p>Predatory</p>
<p>Marine</p>
<h2>Common preservation</h2>
<p>Internal mould</p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
<h2>Advanced notes</h2>
<p>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.</p>
<p>Ammonoids are extremely good index fossils on account of their diverse morphologies, good preservation potentials and widespread fossil locations.</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/ammonoids" target="_blank" rel="noreferrer noopener">Browse ammonoids</a></p>
<h2>External links</h2>
<p><a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener">Telling planispiral fossils apart</a></p></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/71</id>
    <title><![CDATA[<h2><strong>TF0325<br /></strong></h2>
<h2>Ammonite</h2>]]></title>
    <summary><![CDATA[<h3>Species</h3>
<div class="element-set">
<div class="element">
<div class="element-text">Deshayesites</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ammonitida<br /><br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Planispiral<br />Ammonitic suture pattern<br />Evolute<br />Ribs<br />Aperture</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould, with aperture partially crushed</div>
</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:24+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/71"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/1dd5d1b6aafd5e06176f0ceef151d20c.png" type="image/png" length="2541510"/>
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    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <category term="suture"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0325<br /></strong></h2>
<h2>Ammonite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><h3>Species</h3>
<div class="element-set">
<div class="element">
<div class="element-text">Deshayesites</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ammonitida<br /><br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Planispiral<br />Ammonitic suture pattern<br />Evolute<br />Ribs<br />Aperture</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould, with aperture partially crushed</div>
</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/70</id>
    <title><![CDATA[<h2><strong>TF0326<br /></strong></h2>
<h2>Ammonite</h2>]]></title>
    <summary><![CDATA[<div class="element"></div>
<div class="element">
<div class="element">
<h3>Species</h3>
<div class="element-text">Anahoplites splendens</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ammonitida<br /><br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Planispiral<br />Involute<br />Ammonitic suture pattern<br />Ribs</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould, pyritised</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">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.</div>
</div>
<div class="element-text"></div>
</div>]]></summary>
    <updated>2019-07-04T09:52:24+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/70"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/b003b76d4dfb95997069968d69a4cc20.png" type="image/png" length="1248244"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/a13515476842a5be081676dfcd2b8b68.png" type="image/png" length="145668"/>
    <category term="ammonite"/>
    <category term="Cretaceous"/>
    <category term="Jurassic"/>
    <category term="suture"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0326<br /></strong></h2>
<h2>Ammonite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element"></div>
<div class="element">
<div class="element">
<h3>Species</h3>
<div class="element-text">Anahoplites splendens</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ammonitida<br /><br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Planispiral<br />Involute<br />Ammonitic suture pattern<br />Ribs</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould, pyritised</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">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.</div>
</div>
<div class="element-text"></div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/69</id>
    <title><![CDATA[<h2><strong>TF0327<br /></strong></h2>
<h2>Heteromorphic ammonite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Species</h3>
<div class="element-text">Scaphites</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ammonitida<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">'g' shaped coiled shell<br />Ribs<br />Involute<br />Ammonitic suture lines</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">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.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:24+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/69"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/544be5dfa4507d24e71d16f1869a917f.png" type="image/png" length="1081687"/>
    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/5c2a07c0b21f88a97bec78216944a106.png" type="image/png" length="102834"/>
    <category term="Cretaceous"/>
    <category term="suture"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0327<br /></strong></h2>
<h2>Heteromorphic ammonite</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><div class="element">
<h3>Species</h3>
<div class="element-text">Scaphites</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Mollusca<br />Class: Cephalopoda<br />Subclass: Ammonoidea<br />Order: Ammonitida<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">'g' shaped coiled shell<br />Ribs<br />Involute<br />Ammonitic suture lines</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Internal mould</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">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.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
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