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  <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/browse?tags=Calcite&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>2024-04-09T21:16:06+01:00</updated>
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    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/129</id>
    <title><![CDATA[<h2><strong>TF0804<br /></strong></h2>
<h2>Apiocrinites</h2>]]></title>
    <summary><![CDATA[<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: Crinoidea<br />Order: Millericrinida<br />Genus: Apiocrinites</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Pentaradial symmetry<br />Calyx<br />Attachment point for 'arms' of the animal</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Cast (manmade)</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:45+01:00</updated>
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    <category term="Calcite"/>
    <category term="pentaradial"/>
    <category term="symmetry"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0804<br /></strong></h2>
<h2>Apiocrinites</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">
<div class="element-set">
<div class="element">
<div class="element-text">Bradford Clay</div>
</div>
</div>
<div class="element-set">
<div class="element"></div>
</div>
</div></div>
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        <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">Jurassic</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Crinoidea<br />Order: Millericrinida<br />Genus: Apiocrinites</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Pentaradial symmetry<br />Calyx<br />Attachment point for 'arms' of the animal</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Cast (manmade)</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/127</id>
    <title><![CDATA[<h2><strong>TF0802<br /></strong></h2>
<h2>Actinocritus (stem segments)</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Stratigraphic Range</h3>
<div class="element-text">Carboniferous</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Crinoidea</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Ossicles (fused)<br />Stereome</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Mineral replacement<br />Sediment infill</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:45+01:00</updated>
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    <category term="Calcite"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0802<br /></strong></h2>
<h2>Actinocritus (stem segments)</h2></div>
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        <h3>Subject</h3>
                    <div class="element-text"><div class="element-set">
<div class="element">
<div class="element-text">
<h3>Location</h3>
Carboniferous limestone, Whatley</div>
</div>
</div>
<div class="element-set">
<div class="element"></div>
</div></div>
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        <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</div>
</div>
<div class="element">
<h3>Taxonomy</h3>
<div class="element-text">Phylum: Echinodermata<br />Class: Crinoidea</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">Ossicles (fused)<br />Stereome</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Mineral replacement<br />Sediment infill</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
  </entry>
  <entry>
    <id>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/83</id>
    <title><![CDATA[<h2><strong>TF0403<br /></strong></h2>
<h2>Belemnite</h2>]]></title>
    <summary><![CDATA[<div class="element">
<h3>Species</h3>
<div class="element-text">Hastatus</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: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida<br />Genus: Hibolites</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">'Bullet' shape<br />Guard with radial crystals<br />Hollow phragmocone area</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Mineral replacement of calcitic guard<br />Dissolution of aragonitic phragmocone<br />Sediment infil of phragmocone area</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">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.</div>
</div>]]></summary>
    <updated>2019-07-04T09:52:28+01:00</updated>
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    <category term="Calcite"/>
    <category term="Jurassic"/>
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            <div id="dublin-core-title" class="element">
        <h3>Title</h3>
                    <div class="element-text"><h2><strong>TF0403<br /></strong></h2>
<h2>Belemnite</h2></div>
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        <div id="dublin-core-subject" class="element">
        <h3>Subject</h3>
                    <div class="element-text"><div class="element">
<h3>Location</h3>
<div class="element-text">Oxford Clay, Warboys Pit, St Ives</div>
</div>
<div class="element">
<h3></h3>
</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">Hastatus</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: Mollusca<br />Class: Cephalopoda<br />Order: Belemnitida<br />Genus: Hibolites</div>
</div>
<div class="element">
<h3>Distinctive Features</h3>
<div class="element-text">'Bullet' shape<br />Guard with radial crystals<br />Hollow phragmocone area</div>
</div>
<div class="element">
<h3>Preservation</h3>
<div class="element-text">Mineral replacement of calcitic guard<br />Dissolution of aragonitic phragmocone<br />Sediment infil of phragmocone area</div>
</div>
<div class="element">
<h3>Advanced notes</h3>
<div class="element-text">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.</div>
</div></div>
            </div><!-- end element -->
    </div><!-- end element-set -->
]]></content>
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