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	<title>The Burgess Shale Geoscience Foundation</title>
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	<description>One Of The World&#039;s Most Important Fossil Sites</description>
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	<title>The Burgess Shale Geoscience Foundation</title>
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	<item>
		<title>Ancient Squatters: Hermit Behavior in Cambrian &#8220;Penis worms&#8221; (Priapulids)</title>
		<link>https://www.burgess-shale.bc.ca/ancient-squatters-hermit-behavior-in-cambrian-penis-worms-priapulids/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Fri, 26 Apr 2024 17:51:30 +0000</pubDate>
				<category><![CDATA[China]]></category>
		<category><![CDATA[Guanshan]]></category>
		<category><![CDATA[cambrian explosion]]></category>
		<category><![CDATA[evolution]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=5107</guid>

					<description><![CDATA[<p>Move over, hermit crabs! A 2021 paper published in the journal Current Biology suggests similar shell-occupying behavior in an unexpected source: Cambrian priapulid (priapulan) worms, also known as &#8220;penis worms&#8221; due to their gross morphology (overall shape of the organism) bearing a remarkable similarity to the human penis. World class quality &#8220;penis worm&#8221; fossils can be found at the Walcott [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/ancient-squatters-hermit-behavior-in-cambrian-penis-worms-priapulids/">Ancient Squatters: Hermit Behavior in Cambrian &#8220;Penis worms&#8221; (Priapulids)</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
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		<item>
		<title>Trilobite sex</title>
		<link>https://www.burgess-shale.bc.ca/trilobite-sex/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 23 Jun 2022 18:07:10 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[evolution]]></category>
		<category><![CDATA[trilobite]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=4659</guid>

					<description><![CDATA[<p>Trilobite species Olenoides serratus, has been well studied since 1909 and is one of the most fully understood trilobites in the fossil record, due to the exceptional preservation of soft tissues (labile tissue) at the Burgess Shale. Now after over 100 years of studying the species, and half a billion years since its extinction, scientists [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/trilobite-sex/">Trilobite sex</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
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		<item>
		<title>A 506 million year old hemichordate worm with tentacles</title>
		<link>https://www.burgess-shale.bc.ca/a-506-million-year-old-hemichordate-worm-with-tentacles/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 03 Dec 2020 22:48:02 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Cambrian]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
		<category><![CDATA[Yoho National Park]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=3441</guid>

					<description><![CDATA[<p>Gyaltsenglossus senis, is a newly described hemichordate from the Burgess Shale. It provides evidence on how the anatomies of the two main groups of hemichordates &#8211; enteropneusta and pterobranchia &#8211; are related.&#160;&#160; The enteropneusta and pterobranchia differ in body shape and in ecological function. However, DNA analysis of present day organisms suggests that they are [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/a-506-million-year-old-hemichordate-worm-with-tentacles/">A 506 million year old hemichordate worm with tentacles</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>Five-eyes!? Kylinxia zhangi, a new Opabinia-like fossil</title>
		<link>https://www.burgess-shale.bc.ca/five-eyes-kylinxia-zhangi-a-new-fossil-like-opabinia/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 03 Dec 2020 17:14:49 +0000</pubDate>
				<category><![CDATA[Chengjiang]]></category>
		<category><![CDATA[Cambrian]]></category>
		<category><![CDATA[evolution]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=3382</guid>

					<description><![CDATA[<p>Kylinxia zhangi is a newly described euarthropod with five-eyes. It is was discovered in a Cambrian aged deposit in Chengjiang, China, and was recently described in the journal Nature. Kylinxia looks remarkably like a cross between two Burgess Shale animals, Opabinia regalis and Anomalocaris canadensis. The Burgess Shale is currently dated to 506 million years [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/five-eyes-kylinxia-zhangi-a-new-fossil-like-opabinia/">Five-eyes!? Kylinxia zhangi, a new Opabinia-like fossil</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>Tropical Fossils: The Burgess Shale Is Not Alone!</title>
		<link>https://www.burgess-shale.bc.ca/tropical-fossils-the-burgess-shale-is-not-alone/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Sun, 15 Nov 2020 18:26:00 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Chengjiang]]></category>
		<category><![CDATA[Qingjiang]]></category>
		<category><![CDATA[Cambrian]]></category>
		<category><![CDATA[evolution]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=2422</guid>

					<description><![CDATA[<p>Tropical Fossils? The Burgess Shale fossils are found in the Canadian Rockies at a latitude of 51 North. However, the fossilized animals lived and died in the tropics. This change in latitude over time is the result of the slow action of Plate Tectonics. For the last 508 Million years the North America plate has [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/tropical-fossils-the-burgess-shale-is-not-alone/">Tropical Fossils: The Burgess Shale Is Not Alone!</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>A Mine in Yoho National Park?</title>
		<link>https://www.burgess-shale.bc.ca/a-mine-in-yoho-national-park/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Mon, 19 Oct 2020 17:13:19 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Mount Stephen]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
		<category><![CDATA[Yoho National Park]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=2417</guid>

					<description><![CDATA[<p>A mine. In a National Park. Inside a mountain. Not what you would expect but for over sixty years, zinc and lead where mined from within Mount Stephen and Mount Field in Yoho National Park. These mines were the only successful metal mines in the Canadian Rockies.&#160;&#160;Railway construction workers chanced upon lead-zinc ore in the [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/a-mine-in-yoho-national-park/">A Mine in Yoho National Park?</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>The Cambrian Explosion and the Burgess Shale</title>
		<link>https://www.burgess-shale.bc.ca/the-cambrian-explosion-and-the-burgess-shale/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 30 May 2019 16:12:56 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Cambrian]]></category>
		<category><![CDATA[cambrian explosion]]></category>
		<category><![CDATA[evolution]]></category>
		<category><![CDATA[trilobite]]></category>
		<guid isPermaLink="false">http://cpb.dvr.mybluehost.me/?p=1862</guid>

					<description><![CDATA[<p>Cambrian Explosion The early Cambrian period marks one of the most spectacular evolutionary events in the history of life &#8211; The Cambrian Explosion. This was an explosion of life. Within ten million years, a very short period geologically, a host of hard-body and soft-body animals appeared in the fossil record.&#160;Trilobites, molluscs, chordates, cnidarians, brachiopods and [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/the-cambrian-explosion-and-the-burgess-shale/">The Cambrian Explosion and the Burgess Shale</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>The Geology of the Burgess Shale (Part 3): The Cathedral Escarpment</title>
		<link>https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-the-cathedral-escarpment-part-3/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 09 May 2019 21:28:03 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Geology]]></category>
		<category><![CDATA[Mount Stephen]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
		<guid isPermaLink="false">http://cpb.dvr.mybluehost.me/?p=1795</guid>

					<description><![CDATA[<p>A spectacular submarine cliff over 100 metres high &#8211; the Cathedral Escarpment- marked the front of the algal limestones of the Cathedral Formation. The Cathedral Escarpment was initially thought to be a product of prolific algal growth and sediment accumulation during a period of sea level rise. A re-interpretation suggested that the escarpment is the [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-the-cathedral-escarpment-part-3/">The Geology of the Burgess Shale (Part 3): The Cathedral Escarpment</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>Burgess Shale Books: Where can I find more information on the Burgess Shale?</title>
		<link>https://www.burgess-shale.bc.ca/burgess-shale-books/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 02 May 2019 16:35:10 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[cambrian explosion]]></category>
		<category><![CDATA[evolution]]></category>
		<guid isPermaLink="false">http://cpb.dvr.mybluehost.me/?p=1867</guid>

					<description><![CDATA[<p>If you are booked to come on one of our hikes or are just interested in the Burgess Shale, here are some great Burgess Shale books to help you learn more.&#160; A Geoscience Guide to the Burgess Shale &#8211; This easy-to-read illustrated guide immerses the reader in the history, geology, environment and, most importantly, the [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/burgess-shale-books/">Burgess Shale Books: Where can I find more information on the Burgess Shale?</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
			</item>
		<item>
		<title>The Geology of the Burgess Shale (Part 2): What Rocks Tell Us About Life</title>
		<link>https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-what-rocks-tell-us-about-life-part-2/</link>
		
		<dc:creator><![CDATA[Antoine Archambault]]></dc:creator>
		<pubDate>Thu, 18 Apr 2019 22:42:08 +0000</pubDate>
				<category><![CDATA[Burgess Shale]]></category>
		<category><![CDATA[Geology]]></category>
		<category><![CDATA[Mount Stephen]]></category>
		<category><![CDATA[Rocky Mountains]]></category>
		<category><![CDATA[Walcott Quarry]]></category>
		<guid isPermaLink="false">https://www.burgess-shale.bc.ca/?p=2251</guid>

					<description><![CDATA[<p>The picture above features fossil ridge, situated behind and to the right of the hikers; as well as, Mt Wapta, situated behind and slightly to the left of the hikers. The former is where the Walcott Quarry is located.&#160;&#160;Below we describe why fossil ridge and Mount Wapta have mudstone (shale) rocks lower down on the [&#8230;]</p>
<p>The post <a href="https://www.burgess-shale.bc.ca/the-geology-of-the-burgess-shale-what-rocks-tell-us-about-life-part-2/">The Geology of the Burgess Shale (Part 2): What Rocks Tell Us About Life</a> appeared first on <a href="https://www.burgess-shale.bc.ca">The Burgess Shale Geoscience Foundation</a>.</p>
]]></description>
		
		
		
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