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    <pubDate>Tue, 09 Apr 2024 21:15:59 +0100</pubDate>
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      <title><![CDATA[Graptolite]]></title>
      <link>https://wserv3.esc.cam.ac.uk/p1acollections/items/show/114</link>
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        <h3>Title</h3>
                    <div class="element-text"><h2>Graptolite</h2></div>
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        <h3>Description</h3>
                    <div class="element-text"><h2>Taxonomy</h2>
<p>Phylum: Hemichordata</p>
<p>Class: Graptolithina</p>
<h2>Diagnostic features</h2>
<p>Stick-shape (often branched)</p>
<p>One or both edges may appear serrated</p>
<p>Thecae</p>
<p>Rhabdosome</p>
<p>Stipes</p>
<h2>Stratigraphic range</h2>
<p>Cambrian to Carboniferous (Dendroids)</p>
<p>Ordovician to Middle Devonian (Graptoloids)</p>
<h2>Way of life</h2>
<p>Colonial</p>
<p>Planktonic (mostly, although some dendroids were sessile benthonic)</p>
<p>Suspension feeders</p>
<h2>Typical preservation</h2>
<p>Flattened along bedding planes, normally in shales</p>
<p>Carbonization or pyritization of the animal</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>Graptolites, because of their abundance and variation in morphology are very good index fossils. At a very basic level the angle between the stipes and number of stipes can be used to give a rough age for the fossil, with Early Ordovician graptolites having two stipes with the 'sawtooth' facing each other (pendent), later Ordovician graptolites having a more open oblique or reflex angle between the 'sawtooth' faces, and Siluran graptolites having the 'sawtooth' faces back to back (scandent) or having lost one stipe altogether (for example monograptids).</p>
<h2>Specimens</h2>
<p><a href="/p1acollections/exhibits/show/graptolites">Browse graptolites</a></p></div>
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      <pubDate>Thu, 20 Jun 2019 13:10:22 +0100</pubDate>
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