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                <text>&lt;h2&gt;&lt;strong&gt;TF0110&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Lithophaga inclusa&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;br /&gt;&lt;br /&gt;&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Coral Rag, Upware&lt;/div&gt;
&lt;/div&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Lithophaga inclusa&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;br /&gt;&lt;br /&gt;Lithophaga: Triassic to recent&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: Mollusca&lt;br /&gt;Class: Bivalvia&lt;br /&gt;Order: Mytilida&lt;br /&gt;Family: Mytilidae&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Dorsoventral symmetry&lt;br /&gt;Two valves&lt;br /&gt;Growth lines&lt;br /&gt;Umbo&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Set 1:&lt;br /&gt;Original shell material&lt;br /&gt;Set 2:&lt;br /&gt;Mould of boring in which the shell lived (can see the structure of the Coral Rag)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;&lt;em&gt;Lithophaga&lt;/em&gt;&lt;span&gt; &lt;/span&gt;bore into hard substrates, and often preserve as the specimen from Set 2 has, as moulds of the borings they make. They lived as suspension feeders.&lt;/p&gt;
&lt;p&gt;&lt;em&gt;Lithophaga &lt;/em&gt;bore into rocks by secreting a weak acid. This dissolves calcareous substances, sometimes including other bivalve shells, into which the animal bores.&lt;/p&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0108&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Inoceramus&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Cretaceous&lt;/div&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic to Cretaceous&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: Mollusca&lt;br /&gt;Class: Bivalvia&lt;br /&gt;Order: Praecardioida&lt;br /&gt;Family: Inoceramidae&lt;br /&gt;Genus: Inoceramus&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Ribs&lt;br /&gt;Umbo&lt;br /&gt;Two valves&lt;br /&gt;Near dorso-ventral symmetry&lt;/div&gt;
&lt;/div&gt;
&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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                <text>&lt;h2&gt;&lt;strong&gt;TF0102&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Liostrea&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Jurassic&lt;/div&gt;</text>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Liostrea&lt;/div&gt;
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Triassic to Eocene&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: Mollusca&lt;br /&gt;Class: Bivalvia&lt;br /&gt;Order: Gryphaeidae&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Growth lines&lt;br /&gt;Two articulating valves&lt;br /&gt;Adductor muscle scar&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Original shell material&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;
&lt;p&gt;Much like modern oysters&lt;span&gt; &lt;/span&gt;&lt;em&gt;Liostrea&lt;span&gt; &lt;/span&gt;&lt;/em&gt;lived as a stationary epifaunal suspension feeder, encrusting hard substrates, after an initially planktonic larval stage.&lt;/p&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF0101&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Dunbarella&lt;/h2&gt;</text>
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                <text>&lt;h3&gt;Age&lt;/h3&gt;
&lt;div class="element-text"&gt;Carboniferous&lt;/div&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Permian to Carboniferous&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: Mollusca&lt;br /&gt;Class: Bivalvia&lt;br /&gt;Order: Pectinida&lt;br /&gt;Family: Pterinopectinidae&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Distinctive Features&lt;/h3&gt;
&lt;div class="element-text"&gt;Ribs&lt;br /&gt;Umbo&lt;br /&gt;Growth lines&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Compression between mud layers&lt;br /&gt;Potentially carbonization, though could be simply an external mould&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Advanced notes&lt;/h3&gt;
&lt;div class="element-text"&gt;Because of the bilateral symmetry and preservation at first glance this could be mistakenly identified as a brachiopod. Other specimens, with different preservation, show that this is in fact a bivalve, and once you have seen enough of these you will know that &lt;em&gt;Dunbarella&lt;/em&gt; is a bivalve not a brachiopod.&lt;/div&gt;
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                  <text>Fossils</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;Bivalve&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: Bivalvia&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;Palial line/palial sinus&lt;/p&gt;
&lt;p&gt;Adductor muscle scars&lt;/p&gt;
&lt;p&gt;Growth lines&lt;/p&gt;
&lt;p&gt;Dorsoventral symmetry (some exceptions, for example&lt;span&gt; &lt;/span&gt;&lt;em&gt;Gryphaea&lt;/em&gt;)&lt;/p&gt;
&lt;p&gt;Two hinged valves&lt;/p&gt;
&lt;p&gt;Umbo&lt;/p&gt;
&lt;p&gt;Hinge&lt;/p&gt;
&lt;p&gt;Gills (rarely preserved)&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Cambrian to present&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Bivalves have occupied many environmental niches, living in a variety of ways:&lt;/p&gt;
&lt;p&gt;Epifaunal, infaunal, nektonic&lt;/p&gt;
&lt;p&gt;Marine, freshwater, brackish&lt;/p&gt;
&lt;p&gt;Filter feeders through gills&lt;/p&gt;
&lt;p&gt;Majority of bivalves begin life in a planktonic larval stage&lt;/p&gt;
&lt;p&gt;By looking at the shell shape and palial sinus of fossil bivalves it is possible to say something about its mode of life.&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Apparent increase in bivalve diversity over time (or is this just a preservational bias?)&lt;/p&gt;
&lt;p&gt;Bivalves makes their shells out of calite, aragonites, or both&lt;/p&gt;
&lt;p&gt;The adductor muscles are used to keep the shell of the bivalve closed. This means that when they are relaxed, the ligament between the valves pulls them apart, so the 'relaxed state' for bivalves is 'open'.&lt;/p&gt;
&lt;p&gt;The depth at which infaunal bivalves burrowed can be inferred from the palial sinus. The more prominent the palial sinus, the deeper the bivalve burrowed. This is because the size of the palial sinus is indicative of the size of siphon needed, which in turn depends on the depth of the burrow (deeper burrow, larger siphon).&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/bivalves" target="_blank" rel="noreferrer noopener"&gt;Browse bivalves&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;Links&lt;/h2&gt;
&lt;p&gt;&lt;a href="https://www.youtube.com/watch?v=H5O1XYZcDh8" target="_blank" rel="noreferrer noopener"&gt;youtube&lt;/a&gt;: scallops swimming&lt;/p&gt;
&lt;p&gt;&lt;a href="http://www.museum.zoo.cam.ac.uk/bivalve.molluscs/lifestyles.of.bivalve.molluscs/"&gt;Cambridge University Museum of Zoology&lt;/a&gt;: Lifestyles of bivalves&lt;/p&gt;
&lt;p&gt;&lt;a href="http://peabody.yale.edu/collections/blog/2011-11-07/brachiopods-versus-bivalves" target="_blank" rel="noreferrer noopener"&gt;Yale Peabody Museum of Natural History&lt;/a&gt;: differences between bivalves and brachiopods&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;Also&lt;/h2&gt;
&lt;p&gt;Go to the front of the 1A Lab. A display on the right hand side (by the window) shows a number of bivalves in life position. Have a look at how they have adapted their shape and other features to their way of life.&lt;/p&gt;</text>
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      <tag tagId="101">
        <name>symmetry</name>
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</itemContainer>
