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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;TF1120&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Solitary rugose coral&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;Ordovician 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: Cnidaria&lt;br /&gt;&lt;br /&gt;Class: Anthozoa&lt;br /&gt;&lt;br /&gt;Order: Rugosa&lt;/div&gt;
&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Septa&lt;br /&gt;Growth lines&lt;br /&gt;'Horn' shape&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>radial</name>
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                  <text>Fossils</text>
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              <name>Description</name>
              <description>An account of the resource</description>
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                  <text>&lt;p&gt;Welcome to the fossils section of the website. This is designed to help you learn the different characteristics of each major fossil group so that you are able to distinguish between them.&lt;/p&gt;
&lt;p&gt;First year students, please refer to the specimens housed in the first year teaching laboratory. There is no substitute for handling the specimens themselves; this website is just an accessory to help you along the way.&lt;/p&gt;
&lt;p&gt;Animals occupy different environments, have different life habits and lived through different periods in geological time. It is good to be aware of these differences in lifestyle and timing, within and between phyla, classes, orders and families.&lt;/p&gt;</text>
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                <text>&lt;h2&gt;Coral&lt;/h2&gt;</text>
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            <description>An account of the resource</description>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Cnidaria&lt;/p&gt;
&lt;p&gt;Class: Anthozoa&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;Radial or biradial symmetry&lt;/p&gt;
&lt;p&gt;External skeleton&lt;/p&gt;
&lt;p&gt;Septa&lt;/p&gt;
&lt;p&gt;Tabulae&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Ordovician to present&lt;/p&gt;
&lt;p&gt;Tabulate, rugose: Ordovician to Permian (extinct at P/T extinction)&lt;/p&gt;
&lt;p&gt;Scleractinian: Triassic to present&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Colonial or solitary&lt;/p&gt;
&lt;p&gt;Filter feeding&lt;/p&gt;
&lt;p&gt;Reef builders&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Remember, although the most well-known modern corals enjoy a symbiotic relationship with photosynthesising algae (Zooxanthellea) many modern corals do not. When thinking about Palaeozoic corals do not assume that they lived as well known corals do now.&lt;/p&gt;
&lt;p&gt;Corals built their skeletons out of aragonite (Ordovician to Permian) or calcite (Triassic to recent). They are often preserved as moulds, casts, intact or replaced.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/corals" target="_blank" rel="noreferrer noopener"&gt;Browse corals&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;External links&lt;/h2&gt;
&lt;p&gt;&lt;a href="http://paleosoc.org/wp-content/uploads/2015/08/Corals.pdf" target="_blank" rel="noreferrer noopener"&gt;Paleosoc coral info&lt;/a&gt;&lt;/p&gt;</text>
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