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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;Trilobite&lt;/h2&gt;</text>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Arthropoda&lt;/p&gt;
&lt;p&gt;Class: Trilobita&lt;/p&gt;
&lt;h2&gt;Distinctive features&lt;/h2&gt;
&lt;p&gt;Pygidium (tail)&lt;/p&gt;
&lt;p&gt;Thorax (body)&lt;/p&gt;
&lt;p&gt;Cephalon (head)&lt;/p&gt;
&lt;p&gt;Paired appendages (not often preserved)&lt;/p&gt;
&lt;p&gt;Three lobed longitudinal division of body (2x pleural, 1x axial)&lt;/p&gt;
&lt;p&gt;Calcitic exoskeleton&lt;/p&gt;
&lt;p&gt;Segmented body&lt;/p&gt;
&lt;p&gt;Glabella&lt;/p&gt;
&lt;p&gt;Eyes (holochroal or schizochroal; only present in some groups)&lt;/p&gt;
&lt;p&gt;Eye ridges&lt;/p&gt;
&lt;p&gt;Occipital ring&lt;/p&gt;
&lt;p&gt;Axial rings&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Cambrian to Permian (most common Cambrian to Silurian)&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Trilobites lived as planktonic, nektonic, epifaunal and infaunal organisms in deep and shallow marine environments. They lived as predators, filter feeders, deposit feeders, particle feeders, scavengers and even symbiotically.&lt;/p&gt;
&lt;p&gt;By looking at the functional morphology of the trilobite in question you can be more specific about how it lived, by looking at body shape, size, legs, eyes and other characters.&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Trilobites were very abundant during the Palaeozoic. Their preservation potential was increased further as they moulted their exoskeletons periodically as they grew. This means that one trilobite left numerous hard skeletons or partial skeletons as it grew, each of which has the potential to fossilise.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/trilobites" target="_blank" rel="noreferrer noopener"&gt;Browse trilobites&lt;/a&gt;&lt;/p&gt;
&lt;h2&gt;Links&lt;/h2&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;</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;Gastropod&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: Gastropoda&lt;/p&gt;
&lt;h2&gt;Diagnostic Features&lt;/h2&gt;
&lt;p&gt;Coiled shell - planispiral or helical - consists of body whorl and spire&lt;/p&gt;
&lt;p&gt;Mostly aragonitic shell&lt;/p&gt;
&lt;p&gt;Shell consists of one large chamber (no septa)&lt;/p&gt;
&lt;p&gt;Aperture&lt;/p&gt;
&lt;p&gt;Siphonal notch&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Marine, non-marine, land-dwelling&lt;/p&gt;
&lt;p&gt;Carnivorous, scavenging, deposit feeding and more&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Because of their conservative shell shape it is difficult to use gastropods as environmental or stratigraphic indicators.&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/gastropods" target="_blank" rel="noreferrer noopener"&gt;Browse gastropods&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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                  <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;Crinoid&lt;/h2&gt;</text>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Echinodermata&lt;/p&gt;
&lt;p&gt;Class: Crinoidea&lt;/p&gt;
&lt;h2&gt;Diagnostic Features&lt;/h2&gt;
&lt;p&gt;Crown&lt;/p&gt;
&lt;p&gt;Stalk&lt;/p&gt;
&lt;p&gt;Pentaradial symmetry&lt;/p&gt;
&lt;p&gt;Ossicles&lt;/p&gt;
&lt;p&gt;Calyx&lt;/p&gt;
&lt;p&gt;Pinnule&lt;/p&gt;
&lt;p&gt;Holdfast&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;p&gt;Benthic (some pseudoplanktonic)&lt;/p&gt;
&lt;p&gt;Filter feeders&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Ordovician to present&lt;/p&gt;
&lt;h2&gt;Advanced Notes&lt;/h2&gt;
&lt;p&gt;The heyday of the crinoids was the Palaeozoic, where they dominated shallow marine environments. Modern crinoids are exclusively deep marine, and the diversity of forms is far less than it was during the Paleozoic.&lt;/p&gt;
&lt;p&gt;Were they victims of the increased grazing and predation pressure of the Mesozoic Marine Revolution?&lt;/p&gt;
&lt;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/crinoids" target="_blank" rel="noreferrer noopener"&gt;Browse crinoids&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=s1xfRc4SDsw" target="_blank" rel="noreferrer noopener"&gt;youtube&lt;/a&gt;: modern crinoid behaving pseudoplanktonically. You can see the pinnules, crown and multiple stalks.&lt;/p&gt;
&lt;p&gt;&lt;a href="https://www.flickr.com/search/?q=crinoid" target="_blank" rel="noreferrer noopener"&gt;flickr&lt;/a&gt;: beautiful photographs of both living and fossil crinoids. Compare the levels of detail you can see, admire the colours, and spot the distinctive features that make these crinoids identifiable.&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;</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;Echinoid&lt;/h2&gt;</text>
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                <text>&lt;h2&gt;Taxonomy&lt;/h2&gt;
&lt;p&gt;Phylum: Echinodermata&lt;/p&gt;
&lt;p&gt;Class: Echinoidea&lt;/p&gt;
&lt;h2&gt;Diagnostic features&lt;/h2&gt;
&lt;p&gt;Ambulacra (tube feet)&lt;/p&gt;
&lt;p&gt;Periproct (opening for anus)&lt;/p&gt;
&lt;p&gt;Peristome (opening for mouth)&lt;/p&gt;
&lt;p&gt;Pentaradial symmetry (regular echinoids)&lt;/p&gt;
&lt;p&gt;Bilateral symmetry imposed upon pentaradial symmetry (irregular echinoids)&lt;/p&gt;
&lt;h2&gt;Stratigraphic range&lt;/h2&gt;
&lt;p&gt;Ordovician to Present (Irregular Echinoids from Jurassic to Present)&lt;/p&gt;
&lt;h2&gt;Way of life&lt;/h2&gt;
&lt;h3&gt;Regular echinoids:&lt;/h3&gt;
&lt;p&gt;Grazers with functional jaw apparatus&lt;/p&gt;
&lt;p&gt;Long spines for protection and movement&lt;/p&gt;
&lt;p&gt;Epifaunal at a wide range of depths&lt;/p&gt;
&lt;p&gt;Use tube feet for respiration and movement&lt;/p&gt;
&lt;h3&gt;Irregular echinoids:&lt;/h3&gt;
&lt;p&gt;Feed on organic matter in sediment, front shaped to funnel sediment into mouth&lt;/p&gt;
&lt;p&gt;Use fine spines to move&lt;/p&gt;
&lt;p&gt;Infaunal burrowers&lt;/p&gt;
&lt;p&gt;Use tube feet for respiration&lt;/p&gt;
&lt;h2&gt;Advanced notes&lt;/h2&gt;
&lt;p&gt;Grazing echinoids leave a distinctive pentagonal feeding trace&lt;span&gt; &lt;/span&gt;&lt;em&gt;Gnathicnus pentax&lt;/em&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;h2&gt;Specimens&lt;/h2&gt;
&lt;p&gt;&lt;a href="/p1acollections/exhibits/show/echinoids" target="_blank" rel="noreferrer noopener"&gt;Browse echinoids&lt;/a&gt;&lt;/p&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1101&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Halysites&lt;/h2&gt;</text>
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            <name>Subject</name>
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                <text>Tabulate coral</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;Silurian&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;Class: Anthozoa&lt;br /&gt;Order: Tabulata&lt;br /&gt;Genus: Halysites&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;Halysites is a so-called 'chain coral'. Unsurprisingly it can be identified as it has a distinctive 'chain' appearance, each 'link' in the chain is a separate animal, all part of a larger colony.&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;External mould&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1102&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Isastraea explanata&lt;/h2&gt;</text>
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                <text>&lt;span&gt;&lt;span&gt;Scleractinian coral&lt;br /&gt;&lt;/span&gt;&lt;/span&gt;
&lt;h3&gt;Specimen 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, Cambridgeshire&lt;/div&gt;
&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;Isastraea explanata (also Isastrea explanata)&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: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Scleractinia&lt;br /&gt;Genus: Isastrea&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;Septa&lt;br /&gt;Weak columella&lt;/div&gt;
&lt;/div&gt;
&lt;div class="element"&gt;
&lt;h3&gt;Preservation&lt;/h3&gt;
&lt;div class="element-text"&gt;External mould (of the 'top' of the scleractinian coral hard parts)&lt;/div&gt;
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                <text>&lt;h2&gt;&lt;strong&gt;TF1103&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Rugose coral&lt;/h2&gt;</text>
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            <name>Description</name>
            <description>An account of the resource</description>
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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: Cnidaria&lt;br /&gt;Class: Anthozoa&lt;br /&gt;Order: Tabulata&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;Septa&lt;br /&gt;Colonial&lt;br /&gt;Columella&lt;br /&gt;Polyps&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 skeleton&lt;br /&gt;Precipitation of minerals in spaces&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;The presence of columella (central support structures) and septa allow identification of this fossil as a colonial rugose specimen. Columella are not present in tabulate corals as these are always colonial, and do not need the extra support.&lt;br /&gt;Solitary rugose corals developed columella as an internal support structure, and it was retained for some colonial forms, such as this one.&lt;/div&gt;
&lt;/div&gt;</text>
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                <text>&lt;h2&gt;&lt;strong&gt;TF1104&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Tabulate 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;Class: Anthozoa&lt;br /&gt;Order: Tabulata&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;Tabulae&lt;br /&gt;Colonial&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 skeleton&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;Due to the way that this specimen has been cut and polished, the tabulae are not immediately obvious. They are visible on parts of the slab, allowing for this to be identified as a tabulate coral.&lt;br /&gt;&lt;br /&gt;You may recognise this specimen from the coffee table in the common room on the ground floor of the Earth Sciences Department. Have a go at identifying the other fossils in the table on your next coffee break!&lt;/div&gt;
&lt;/div&gt;</text>
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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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            <description>An account of the resource</description>
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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: Cnidaria&lt;br /&gt;&lt;br /&gt;Class: Anthozoa&lt;br /&gt;&lt;br /&gt;Order: Rugosa&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;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>&lt;h2&gt;&lt;strong&gt;TF1122&lt;br /&gt;&lt;/strong&gt;&lt;/h2&gt;
&lt;h2&gt;Scleractinian coral (modern)&lt;/h2&gt;</text>
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&lt;h3&gt;Stratigraphic Range&lt;/h3&gt;
&lt;div class="element-text"&gt;Triassic to present&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;Class: Anthozoa&lt;br /&gt;Order: Scleractinia&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;Branching structure&lt;br /&gt;Polyps&lt;br /&gt;Septa&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 skeleton material&lt;/div&gt;
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