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	<title>PalArch &#187; La Brea tar pits</title>
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		<title>Syverson, Valerie J. &amp; Donald R. Prothero. 2010. Evolutionary Patterns in Late Quaternary California Condors. – PalArch’s Journal of Vertebrate Palaeontology 7, 1: 1-18</title>
		<link>http://www.palarch.nl/2010/03/syverson-valerie-j-donald-r-prothero-2010-evolutionary-patterns-in-late-quaternary-california-condors-%e2%80%93-palarch%e2%80%99s-journal-of-vertebrate-palaeontology-7-1-1-18/</link>
		<comments>http://www.palarch.nl/2010/03/syverson-valerie-j-donald-r-prothero-2010-evolutionary-patterns-in-late-quaternary-california-condors-%e2%80%93-palarch%e2%80%99s-journal-of-vertebrate-palaeontology-7-1-1-18/#comments</comments>
		<pubDate>Thu, 11 Mar 2010 06:35:48 +0000</pubDate>
		<dc:creator>PalArch Editor (AV)</dc:creator>
				<category><![CDATA[PalArch's Journal of Vertebrate Palaeontology]]></category>
		<category><![CDATA[condor]]></category>
		<category><![CDATA[dwarfing]]></category>
		<category><![CDATA[extinctions]]></category>
		<category><![CDATA[Holocene]]></category>
		<category><![CDATA[La Brea tar pits]]></category>
		<category><![CDATA[Pleistocene]]></category>

		<guid isPermaLink="false">http://www.palarch.nl/?p=1588</guid>
		<description><![CDATA[Abstract Pleistocene fossils related to the living California condor (Gymnogyps californianus) have been found in several locations in western North America. Different authors have either assigned these to the species G. amplus or considered them a chronological subspecies of G. californianus. We examined the morphology of the genus Gymnogyps from the late Pleistocene to the [...]]]></description>
			<content:encoded><![CDATA[<p><strong><a href="http://www.palarch.nl/wp-content/Front_syverson_prothero.jpg"><img class="alignleft size-full wp-image-1570" style="margin: 5px; border: 1px solid black;" title="Front_syverson_prothero" src="http://www.palarch.nl/wp-content/Front_syverson_prothero.jpg" alt="Front_syverson_prothero" width="150" height="225" /></a>Abstract</strong> <span class="wpgallery">Pleistocene fossils related to the living California condor (</span><span class="wpgallery"><em>Gymnogyps californianus</em></span><span class="wpgallery">) have been found in several locations in western North America. Different authors have either assigned these to the species </span><span class="wpgallery"><em>G. amplus</em></span><span class="wpgallery"> or considered them a chronological subspecies of </span><span class="wpgallery"><em>G. californianus</em></span><span class="wpgallery">. We examined the morphology of the genus </span><span class="wpgallery"><em>Gymnogyps</em></span><span class="wpgallery" style="font-style: normal;"> from the late Pleistocene to the present, using hundreds of specimens from the asphalt deposits of Rancho La Brea (RLB) and 62 partial modern skeletons. The limb bones (using seven variables on each element) and skulls (using 13 variables) were quantitatively compared using bivariate and multivariate techniques. No significant size or shape change through time was apparent in RLB samples ranging from the late Pleistocene (35,000 radiocarbon years b.p.) to the early Holocene (9000 radiocarbon years b.p.), suggesting evolutionary stasis in the face of the climatic changes of the last glacial-interglacial cycle. Proximal limb elements and skulls showed patterns of variation consistent with a species distinction between the RLB specimens and modern </span><span class="wpgallery"><em>G. californianus</em></span><span class="wpgallery">. This confirms Fisher’s (1944) contention that the RLB species is referable to </span><span class="wpgallery"><em>G. amplus</em></span><span class="wpgallery"> Miller 1911, and not referable to the modern species. A set of specimens from a 9000-year-old Indian midden in Oregon as well as the presence of </span><span class="wpgallery"><em>Gymnogyps</em></span><span class="wpgallery"> in early Holocene Pit 10 at RLB suggest that the modern and ancient </span><span class="wpgallery"><em>Gymnogyps</em></span><span class="wpgallery"> may have coexisted with each other as well as with humans, and not died out or become dwarfed with the extinction of the rest of the Pleistocene megafauna, as suggested by some authors</span><span style="font-family: Arial;">.</span></p>
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<hr style="height: 1px;" size="1" /><a class="wpgallery" href="http://www.palarch.nl/wp-content/syverson_vj_dr_prothero_evolutionary_patterns_in_late_quaternary_california_condors_palarchs_journal_of_vertebrate_palaeontology_7_1_2010.pdf" target="_blank"><span style="text-decoration: underline;"><span style="font-family: Georgia; font-size: small;"><span>PDF file (2.4 MB)</span></span></span></a></p>
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