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                <text>&lt;h2&gt;&lt;strong&gt;TF0103&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Trigonia&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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            <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;Jurassic 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: Trigoniida&lt;br /&gt;Family: Trigoniidae&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;Dentition, hinge&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;Set 1:&lt;br /&gt;Mineral replacement of shell (aragonite to calcite)&lt;br /&gt;Set 2:&lt;br /&gt;Disarticulation of valves&lt;br /&gt;Sediment infil (oolitic ironstone, which gives the reddy colour to the specimen)&lt;br /&gt;Mineral replacement of shell (aragonite to calcite)&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;Strong ribs are present on the anterior part of the shell - perhaps to discourage predators or as a response to a high energy environment?&lt;/div&gt;
&lt;/div&gt;</text>
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            <name>Title</name>
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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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            <description>An account of the resource</description>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Liostrea&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;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;
&lt;/div&gt;
&lt;/div&gt;</text>
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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;
&lt;/div&gt;</text>
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                  <text>Fossils</text>
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              <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;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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                <text>&lt;h2&gt;&lt;strong&gt;TF0404&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite Peel&lt;/h2&gt;</text>
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                <text>&lt;div class="element"&gt;
&lt;h3&gt;Taxonomy&lt;/h3&gt;
&lt;div class="element-text"&gt;Phylum: Mollusca&lt;br /&gt;Class: Cephalopoda&lt;br /&gt;Order: Belemnitida&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;'Bullet' shape&lt;br /&gt;Conical hole where phragmocone used to be&lt;br /&gt;Radial crystals (here in cross section)&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Peel of a cross section through a belemnite (manmade)&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;Have a look at this specimen under a microscope. The peel allows us to see very fine details.&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF0403&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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&lt;h3&gt;Location&lt;/h3&gt;
&lt;div class="element-text"&gt;Oxford Clay, Warboys Pit, St Ives&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;&lt;/h3&gt;
&lt;/div&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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&lt;h3&gt;Species&lt;/h3&gt;
&lt;div class="element-text"&gt;Hastatus&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;/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: Cephalopoda&lt;br /&gt;Order: Belemnitida&lt;br /&gt;Genus: Hibolites&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;'Bullet' shape&lt;br /&gt;Guard with radial crystals&lt;br /&gt;Hollow phragmocone area&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Mineral replacement of calcitic guard&lt;br /&gt;Dissolution of aragonitic phragmocone&lt;br /&gt;Sediment infil of phragmocone area&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;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.&lt;/div&gt;
&lt;/div&gt;</text>
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        <name>Jurassic</name>
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&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Carboniferous 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: Cephalopoda&lt;br /&gt;Order: Belemnitida&lt;br /&gt;&lt;br /&gt;Set 1:&lt;br /&gt;Group: Cylindroteuthis&lt;br /&gt;Set 2:&lt;br /&gt;Group: unknown&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;Guard with radial calcite crystals&lt;br /&gt;Crushed conical hole where phragmocone used to be&lt;br /&gt;Long, near cylindrical shape&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Dissolution of phragmocone&lt;br /&gt;Sediment infill of conical cavity where phragmocone used to be&lt;br /&gt;Crushing of infilled phragmocone area&lt;/div&gt;
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        <name>Jurassic</name>
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&lt;h2&gt;Belemnite&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Carboniferous 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: Cephalopoda&lt;br /&gt;Order: Belemnitida&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;Guard of radial calcite crystals&lt;br /&gt;Conical cavity where phragmocone used to be&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;Aragonitic phragmocone dissolved&lt;br /&gt;Sediment infil of conical cavity where phragmocone used to be (set 1 only)&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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&lt;div class="element-set"&gt;
&lt;div class="element"&gt;
&lt;div class="element-text"&gt;
&lt;h2&gt;Taxonomy&lt;span&gt;&lt;br /&gt;&lt;/span&gt;&lt;/h2&gt;
&lt;p&gt;Phylum: Mollusca&lt;/p&gt;
&lt;p&gt;Class: Cephalopoda&lt;/p&gt;
&lt;p&gt;Subclass: Coleoidea&lt;/p&gt;
&lt;p&gt;Cohort: Belemnoidea&lt;/p&gt;
&lt;h2&gt;Diagnostic Features&lt;/h2&gt;
&lt;p&gt;Diagram with labelled features of belemnites&lt;/p&gt;
&lt;p&gt;'Bullet' shape&lt;/p&gt;
&lt;p&gt;Phragmocone: chambers divided by aragonitic septa (often preserved as conical cavity)&lt;/p&gt;
&lt;p&gt;Radial calcite crystals form the guard&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Nektonic&lt;/p&gt;
&lt;p&gt;Predatory&lt;/p&gt;
&lt;p&gt;Marine&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Exceptional preservation of belemnites showing soft parts has shown them to be very similar to squid in shape. The guard and phragmocone were held inside the soft parts of the animals, acting as a kind of backbone.&lt;/p&gt;
&lt;p&gt;Because the phragmocone is made of aragonite it is often not preserved. In contrast the calcitic guard is very often preserved. This means that a common preservation of belemnites is of the guard with a conical hole where the phragmocone once was. This empty conical chamber is often crushed.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/belemnites" target="_blank" rel="noreferrer noopener"&gt;Browse belemnites&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;External Links&lt;/h2&gt;
&lt;p&gt;&lt;a href="http://www.conchsoc.org/MolluscWorld20/7"&gt;Mollusc World&lt;/a&gt;&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;/div&gt;
&lt;/div&gt;
&lt;/div&gt;
&lt;/div&gt;</text>
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&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;Ammonoid&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;p&gt;Subclass: Ammonoidea&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;[See labelled diagram above]&lt;/p&gt;
&lt;p&gt;Aragonite shell&lt;/p&gt;
&lt;p&gt;Septa&lt;/p&gt;
&lt;p&gt;Suture (different for goniatites, ceratites and ammonites, see second diagram above)&lt;/p&gt;
&lt;p&gt;Chambers&lt;/p&gt;
&lt;p&gt;Siphuncle&lt;/p&gt;
&lt;p&gt;Planispiral shape, involute or evolute (see third diagram on right hand side)&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Devonian to Cretaceous&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Nektonic (jet propelled)&lt;/p&gt;
&lt;p&gt;Predatory&lt;/p&gt;
&lt;p&gt;Marine&lt;/p&gt;
&lt;h2&gt;Common preservation&lt;/h2&gt;
&lt;p&gt;Internal mould&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;Ammonoids could passively remove or add water to chambers via the siphuncle. This allowed them to change their density, and maintain neutral buoyancy with the surrounding seawater. This meant that they were able to swim as efficiently as possible.&lt;/p&gt;
&lt;p&gt;Ammonoids are extremely good index fossils on account of their diverse morphologies, good preservation potentials and widespread fossil locations.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/ammonoids" target="_blank" rel="noreferrer noopener"&gt;Browse ammonoids&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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        <name>Carboniferous</name>
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        <name>Cretaceous</name>
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        <name>Devonian</name>
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        <name>Jurassic</name>
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        <name>Permian</name>
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      <tag tagId="95">
        <name>Triassic</name>
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