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                <text>&lt;h2&gt;&lt;strong&gt;TF0703&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Atrypa&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Specimen Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Silurian&lt;/div&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Silurian to Devonian&lt;/div&gt;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Brachiopoda&lt;br /&gt;Class: Rhynchonellata&lt;br /&gt;Order: Spiriferida&lt;br /&gt;Genus: Atrypa&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Two valves&lt;br /&gt;Commissure&lt;br /&gt;Radial ribs&lt;br /&gt;Growth lines&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of shell&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0704&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Chonetes&lt;/h2&gt;</text>
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&lt;h3&gt;Specimen Age&lt;/h3&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician to Permian&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Brachiopoda&lt;br /&gt;Class: Strophomenata&lt;br /&gt;Order: Strophomenida&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Ribs&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;External moulds and internal moulds&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0705&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Spirifer verneuli&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Spirifer verneuli&lt;/div&gt;
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&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: Brachiopoda&lt;br /&gt;Class: Rhynchonellata&lt;br /&gt;Order: Spiriferida&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Two articulated valves&lt;br /&gt;Commissure&lt;br /&gt;Ribs&lt;br /&gt;Pedicle&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Internal mould&lt;/div&gt;
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&lt;h2&gt;Ornithella&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;/div&gt;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Brachiopoda&lt;br /&gt;Class: Rhynchonellata&lt;br /&gt;Order: Terebratulida&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Two articulated valves&lt;br /&gt;Commissure&lt;br /&gt;Growth lines&lt;br /&gt;Pedicle&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of shell&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0707&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Terebratula biplicata&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Terebratula biplicata&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Cretaceous&lt;/div&gt;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Brachiopoda&lt;br /&gt;Class: Rhynchonellata&lt;br /&gt;Order: Terebratulida&lt;br /&gt;Genus: Terebratula&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Two articulated valves&lt;br /&gt;Commissure&lt;br /&gt;Pedicle&lt;br /&gt;Growth lines&lt;/div&gt;
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&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of shell&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0708&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Terebratula maximes&lt;/h2&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Pliocene to Pleistocene&lt;/div&gt;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Brachiopoda&lt;br /&gt;Class: Rhynchonellata&lt;br /&gt;Order: Terebratulida&lt;br /&gt;Genus: Terebratula&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Two articulated valves&lt;br /&gt;Growth lines&lt;br /&gt;Pedicle&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Infil of valves with bioclastic matrix&lt;br /&gt;Original shell material (partially broken)&lt;/div&gt;
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&lt;h2&gt;Leptaena&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Ordovician to Carboniferous&lt;/div&gt;
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&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Brachiopoda&lt;br /&gt;Class: Strophomenata&lt;br /&gt;Order: Strophomenida&lt;br /&gt;Family: Rafinesquinidae&lt;br /&gt;Genus: Leptaena&lt;/div&gt;
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&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Bilateral symmetry&lt;br /&gt;Ribs&lt;br /&gt;Growth lines&lt;/div&gt;
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&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of shell&lt;/div&gt;
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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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                <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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                  <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;Nautiloid&lt;/h2&gt;</text>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Mollusca&lt;/p&gt;
&lt;p&gt;Class: Cephalopoda&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;Simple suture&lt;/p&gt;
&lt;p&gt;Chambers&lt;/p&gt;
&lt;p&gt;Central siphuncle&lt;/p&gt;
&lt;p&gt;Straight, curved or coiled shell&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Cambrian to recent&lt;/p&gt;
&lt;p&gt;Straight forms: Cambrian to Permian&lt;/p&gt;
&lt;p&gt;Coiled forms: Devonian to Present&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;span&gt;Nektonic (jet propulsion)&lt;/span&gt;&lt;br /&gt;&lt;p&gt;Predatory&lt;/p&gt;
&lt;p&gt;Buoyancy controlled by changing gas/liquid contents of chambers&lt;/p&gt;
&lt;p&gt;Marine&lt;/p&gt;
&lt;h2&gt;Preservation&lt;/h2&gt;
&lt;p&gt;Commonly preserved as internal moulds&lt;/p&gt;
&lt;p&gt;Modern&lt;span&gt; &lt;/span&gt;&lt;em&gt;&lt;/em&gt;nautiloids preserved with original shell material&lt;/p&gt;
&lt;p&gt;&lt;a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/"&gt;Learn about types of preservation&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Nautiloids originated in the Cambrian period, and radiated during the Ordovician. These early nautiloids had conical shaped shells. In the Silurian some nautiloids used curved shells, and by the Devonian some were coiled. The evolution of the coiled shell from the straight is thought to be driven, at least in part, by increased mobility of a coiled shell compared to a long straight one.&lt;/p&gt;
&lt;p&gt;Nautiloids could be confused with ammonoids. You can distinguish them by the location of the siphuncle and the complexity of the suture pattern. Nautiloids, unlike ammonoids, are not extinct, although only six species remain today (compared to thousands in the Palaeozoic). This means that if presented with modern shell material it is likely a nautiloid and not an ammonoid.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/nautiloids"&gt;Browse nautiloids&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;External links&lt;/h2&gt;
&lt;p&gt;&lt;a href="https://www.youtube.com/watch?v=2ilSDcZAXNM" target="_blank" rel="noreferrer noopener"&gt;Telling planispiral fossils apart&lt;/a&gt;&lt;/p&gt;</text>
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&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;Graptolite&lt;/h2&gt;</text>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Hemichordata&lt;/p&gt;
&lt;p&gt;Class: Graptolithina&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;Stick-shape (often branched)&lt;/p&gt;
&lt;p&gt;One or both edges may appear serrated&lt;/p&gt;
&lt;p&gt;Thecae&lt;/p&gt;
&lt;p&gt;Rhabdosome&lt;/p&gt;
&lt;p&gt;Stipes&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Cambrian to Carboniferous (Dendroids)&lt;/p&gt;
&lt;p&gt;Ordovician to Middle Devonian (Graptoloids)&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Colonial&lt;/p&gt;
&lt;p&gt;Planktonic (mostly, although some dendroids were sessile benthonic)&lt;/p&gt;
&lt;p&gt;Suspension feeders&lt;/p&gt;
&lt;h2&gt;Typical preservation&lt;/h2&gt;
&lt;p&gt;Flattened along bedding planes, normally in shales&lt;/p&gt;
&lt;p&gt;Carbonization or pyritization of the animal&lt;/p&gt;
&lt;p&gt;&lt;a href="https://www.digitalatlasofancientlife.org/learn/nature-fossil-record/types-of-fossil-preservation/"&gt;Learn about types of preservation&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;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).&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/graptolites"&gt;Browse graptolites&lt;/a&gt;&lt;/p&gt;</text>
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