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  <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?tags=bilateral&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>2024-04-09T21:15:57+01:00</updated>
  <generator>Omeka</generator>
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  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/135</id>
    <title><![CDATA[<h2><strong>TF0905<br /></strong></h2>
<h2>Irregular echinoid</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Upper Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Echinodea<br />Subclass: Irregularia<br />Order: Holasteroida<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Mouth and anus out of line<br />Five radial ambulacra<br />Interambulacra with plates</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Sediment infill<br />Mineral replacement of shell</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Set 1: Anus and mouth appear to have been drilled to emphasise their positions.<br />Set 2: Fracturing of shell around the anus which obscures it. This would be a weak part of the shell which diagenetic processes have crushed.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:47+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/135"/>
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    <category term="bilateral"/>
    <category term="pentaradial"/>
    <category term="symmetry"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0905<br /></strong></h2>
<h2>Irregular echinoid</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">Upper Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Echinodea<br />Subclass: Irregularia<br />Order: Holasteroida<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Mouth and anus out of line<br />Five radial ambulacra<br />Interambulacra with plates</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Sediment infill<br />Mineral replacement of shell</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Set 1: Anus and mouth appear to have been drilled to emphasise their positions.<br />Set 2: Fracturing of shell around the anus which obscures it. This would be a weak part of the shell which diagenetic processes have crushed.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/134</id>
    <title><![CDATA[<h2><strong>TF0904<br /></strong></h2>
<h2>Irregular echinoid</h2>]]></title>
    <summary><![CDATA[<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: Echinodermata<br />Class: Echinoidea<br />Subclass: Irregularia<br />Order: Echinoneoida<br />Genus: Conulus</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Five radial ambulacra<br />Interambulacra<br />Migrated periproct (opening for anus)<br />Peristome (opening for mouth)</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">This fossil was collected in Quaternary river gravel. Originally it was preserved in the Upper Chalk (Cretaceous). This was broken up into clasts by erosive processes, one of which was this irregular echinoid. The echinoid clast was carried by a river downstream and deposited in the river gravel unit during the Quaternary.</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Note how the anus has migrated, but the peristome is still in the position you would expect from a regular echinoid (not migrated). Notice also how the ambulacra bearing the tube feet continue onto the underside, a feature not seen in more streamlined and derived irregular echinoids.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:47+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/134"/>
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    <category term="bilateral"/>
    <category term="pentaradial"/>
    <category term="symmetry"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0904<br /></strong></h2>
<h2>Irregular echinoid</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Source</h3>
<div class="element-text"><span>Quaternary River Gravel, derived from Cretaceous chalk</span></div></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">Cretaceous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Echinoidea<br />Subclass: Irregularia<br />Order: Echinoneoida<br />Genus: Conulus</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Five radial ambulacra<br />Interambulacra<br />Migrated periproct (opening for anus)<br />Peristome (opening for mouth)</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">This fossil was collected in Quaternary river gravel. Originally it was preserved in the Upper Chalk (Cretaceous). This was broken up into clasts by erosive processes, one of which was this irregular echinoid. The echinoid clast was carried by a river downstream and deposited in the river gravel unit during the Quaternary.</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Note how the anus has migrated, but the peristome is still in the position you would expect from a regular echinoid (not migrated). Notice also how the ambulacra bearing the tube feet continue onto the underside, a feature not seen in more streamlined and derived irregular echinoids.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/133</id>
    <title><![CDATA[<h2><strong>TF0903<br /></strong></h2>
<h2>Irregular echinoid</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Species</h3>
<div class="element-text">Praecursor</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: Echinodermata<br />Class: Echinoidea<br />Subclass: Irregularia<br />Order: Spatangoida<br />Genus: Micraster<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Five radial ambulacra<br />Peristome (opening for mouth) and periproct (opening for anus) migrated<br />Spine attachment scars</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Sediment infil<br />Shell mineral replacement<br />Disarticulation of spines</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Note the streamlined shape for burrowing through the sediment, and how the ambulacra, which bear the tube feet, do not continue onto the underside of the animal where the mouth is.<br />This is because the tube feet are used for respiration but not for movement, for which small spines are used.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:46+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/133"/>
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    <category term="bilateral"/>
    <category term="burrow"/>
    <category term="movement"/>
    <category term="pentaradial"/>
    <category term="symmetry"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0903<br /></strong></h2>
<h2>Irregular echinoid</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Location</h3>
<div class="element-text"><span>Upper Chalk, Weston Colville, Cambridgeshire</span></div></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">Praecursor</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: Echinodermata<br />Class: Echinoidea<br />Subclass: Irregularia<br />Order: Spatangoida<br />Genus: Micraster<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Five radial ambulacra<br />Peristome (opening for mouth) and periproct (opening for anus) migrated<br />Spine attachment scars</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Sediment infil<br />Shell mineral replacement<br />Disarticulation of spines</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">Note the streamlined shape for burrowing through the sediment, and how the ambulacra, which bear the tube feet, do not continue onto the underside of the animal where the mouth is.<br />This is because the tube feet are used for respiration but not for movement, for which small spines are used.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/132</id>
    <title><![CDATA[<h2><strong>TF0902<br /></strong></h2>
<h2>Irregular echinoid</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Species</h3>
<div class="element-text">depressus Lestre</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Jurassic</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Echinoidea<br />Subclass: Irregularia<br />Order: Holectypoida<br />Genus: Holectypus<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Five radial ambulacra<br />Spine attachment scars (very small)<br />Peristome and anus out of line</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Shell mineral replacement<br />Sediment infil<br />Disarticulation of spines</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">This is a primitive irregular echinoid which would have had a functional jaw apparatus (not preserved) held within the peristome. The anus has migrated and the symmetry is bilateral, so this echinoid is clearly identifiable as irregular.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:46+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/132"/>
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    <category term="bilateral"/>
    <category term="movement"/>
    <category term="pentaradial"/>
    <category term="symmetry"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0902<br /></strong></h2>
<h2>Irregular echinoid</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><h3>Location</h3>
<div class="element-text"><span>Coralline Oolite, Upware, Cambridgeshire</span></div></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">depressus Lestre</div>
</div>
<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Jurassic</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Echinoidea<br />Subclass: Irregularia<br />Order: Holectypoida<br />Genus: Holectypus<br /><br /></div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Bilateral symmetry<br />Five radial ambulacra<br />Spine attachment scars (very small)<br />Peristome and anus out of line</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Shell mineral replacement<br />Sediment infil<br />Disarticulation of spines</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">This is a primitive irregular echinoid which would have had a functional jaw apparatus (not preserved) held within the peristome. The anus has migrated and the symmetry is bilateral, so this echinoid is clearly identifiable as irregular.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/118</id>
    <title><![CDATA[<h2>Echinoid</h2>]]></title>
    <summary><![CDATA[<h2>Taxonomy</h2>
<p>Phylum: Echinodermata</p>
<p>Class: Echinoidea</p>
<h2>Diagnostic features</h2>
<p>Ambulacra (tube feet)</p>
<p>Periproct (opening for anus)</p>
<p>Peristome (opening for mouth)</p>
<p>Pentaradial symmetry (regular echinoids)</p>
<p>Bilateral symmetry imposed upon pentaradial symmetry (irregular echinoids)</p>
<h2>Stratigraphic range</h2>
<p>Ordovician to Present (Irregular Echinoids from Jurassic to Present)</p>
<h2>Way of life</h2>
<h3>Regular echinoids:</h3>
<p>Grazers with functional jaw apparatus</p>
<p>Long spines for protection and movement</p>
<p>Epifaunal at a wide range of depths</p>
<p>Use tube feet for respiration and movement</p>
<h3>Irregular echinoids:</h3>
<p>Feed on organic matter in sediment, front shaped to funnel sediment into mouth</p>
<p>Use fine spines to move</p>
<p>Infaunal burrowers</p>
<p>Use tube feet for respiration</p>
<h2>Advanced notes</h2>
<p>Grazing echinoids leave a distinctive pentagonal feeding trace<span> </span><em>Gnathicnus pentax</em>.</p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/echinoids" target="_blank" rel="noreferrer noopener">Browse echinoids</a></p>]]></summary>
    <updated>2019-08-06T10:58:24+01:00</updated>
    <link rel="alternate" type="text/html" href="https://wserv3.esc.cam.ac.uk/p1acollections/items/show/118"/>
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    <link rel="enclosure" href="https://wserv3.esc.cam.ac.uk/p1acollections/files/original/d7eb9ad67662f54a626c0d85caf42278.png" type="image/png" length="99073"/>
    <category term="bilateral"/>
    <category term="pentaradial"/>
    <category term="spines"/>
    <category term="symmetry"/>
    <content type="html"><![CDATA[<div class="element-set">
            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2>Echinoid</h2></div>
            </div><!-- end element -->
        <div id="dublin-core-description" class="element">
        <h3>Description</h3>
                    <div class="element-text"><h2>Taxonomy</h2>
<p>Phylum: Echinodermata</p>
<p>Class: Echinoidea</p>
<h2>Diagnostic features</h2>
<p>Ambulacra (tube feet)</p>
<p>Periproct (opening for anus)</p>
<p>Peristome (opening for mouth)</p>
<p>Pentaradial symmetry (regular echinoids)</p>
<p>Bilateral symmetry imposed upon pentaradial symmetry (irregular echinoids)</p>
<h2>Stratigraphic range</h2>
<p>Ordovician to Present (Irregular Echinoids from Jurassic to Present)</p>
<h2>Way of life</h2>
<h3>Regular echinoids:</h3>
<p>Grazers with functional jaw apparatus</p>
<p>Long spines for protection and movement</p>
<p>Epifaunal at a wide range of depths</p>
<p>Use tube feet for respiration and movement</p>
<h3>Irregular echinoids:</h3>
<p>Feed on organic matter in sediment, front shaped to funnel sediment into mouth</p>
<p>Use fine spines to move</p>
<p>Infaunal burrowers</p>
<p>Use tube feet for respiration</p>
<h2>Advanced notes</h2>
<p>Grazing echinoids leave a distinctive pentagonal feeding trace<span> </span><em>Gnathicnus pentax</em>.</p>
<p><a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/">Learn about types of preservation</a></p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/echinoids" target="_blank" rel="noreferrer noopener">Browse echinoids</a></p></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
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