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<title>Dinosauria</title>
<link>http://dinosauria.ucoz.com/</link>
<description>Site news</description>
<lastBuildDate>Tue, 16 Sep 2008 10:02:44 GMT</lastBuildDate>
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<title>The anatomy and systematic position of the theropod dinosaur Chilantaisaurus tashuikouensis Hu, 1964 from the Early Cret. of Alanshan, China</title>
<description><![CDATA[There is little consensus on the systematic position of the colossal theropod dinosaur<br>Chilantaisaurus tashuikouensis from the Cretaceous (Aptian–?Albian or Upper Cretaceous)Ulansuhai Formation of Inner Mongolia, which has been recovered as a derived member of both Allosauroidea and Spinosauroidea by numerical phylogenetic analyses. Redescription of the type material of C. tashuikouensis reveals an unusual combination of morphological features that render determination of its systematic position problematic. It possesses anatomical features that have been proposed as synapomorphies of Neotetanurae: a preacetabular fossa on the ilium, and a wedge-shaped crosssection of the shaft of the thi...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-09-16-64</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-09-16-64</guid>
<pubDate>Tue, 16 Sep 2008 10:02:44 GMT</pubDate>
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<title>Body size evolution in Mesozoic birds: little evidence for Cope’s rule</title>
<description><![CDATA[Cope’s rule, the tendency towards evolutionary increases in body size, is a long-standing macroevolutionary generalization that has the potential to provide insights into directionality in evolution; however, both the definition and identification of Cope’s rule are controversial and problematic. A recent study [J. Evol. Biol. 21 (2008) 618] examined body size evolution in Mesozoic birds, and claimed to have identified evidence of Cope’s rule occurring as a<br>result of among-lineage species sorting. We here reassess the results of this study, and additionally carry out novel analyses testing for within-lineage patterns in body size evolution in Mesozoic birds. We demonstrate that the nonphy...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-09-16-63</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-09-16-63</guid>
<pubDate>Tue, 16 Sep 2008 09:59:16 GMT</pubDate>
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<title>Superiority, Competition, and Opportunism in the Evolutionary Radiation of Dinosaurs</title>
<description><![CDATA[The rise and diversification of the dinosaurs in the Late Triassic, from 230 to 200 million<br>years ago, is a classic example of an evolutionary radiation with supposed competitive<br>replacement. A comparison of evolutionary rates and morphological disparity of basal dinosaurs and their chief “competitors,” the crurotarsan archosaurs, shows that dinosaurs exhibited lower disparity and an indistinguishable rate of character evolution. The radiation of Triassic archosaurs as a whole is characterized by declining evolutionary rates and increasing disparity, suggesting a decoupling of character evolution from body plan variety. The results strongly suggest that historical contingency, rather t...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-09-16-62</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-09-16-62</guid>
<pubDate>Tue, 16 Sep 2008 09:56:02 GMT</pubDate>
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<title>Three-dimensional geometry of a pterosaur wing skeleton, and its implications for aerial and terrestrial locomotion</title>
<description><![CDATA[This study reports on the three-dimensional spatial arrangement and movements of the skeleton of Anhanguera santanae (Pterodactyloidea: Ornithocheiridae), determined using exceptionally well-preserved uncrushed fossil material, and a rigid-body method for analysing the joints of extinct animals. The geometric results of this analysis suggest that the ornithocheirids were inherently unstable in pitch and yaw. As a result, pitch control would<br>probably have been brought about by direct adjustment of the angle of attack of the wing, by raising or lowering the trailing edge from the root using the legs if, as is indicated in soft-tissue specimens of a number of unrelated pterosaur species, the...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-09-11-61</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-09-11-61</guid>
<pubDate>Thu, 11 Sep 2008 12:50:00 GMT</pubDate>
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<title>Adaptive Features of Protoceratopoids (Ornithischia: Neoceratopsia)</title>
<description><![CDATA[The analysis of some morphological characteristics of protoceratopoid skeletons, the extent of mobility of the vertebral column, and the probable adaptive significance of these features suggest that Bagaceratops had a mostly aquatic mode of life, Protoceratops was semiaquatic, Udanoceratops was facultatively aquatic, and Leptoceratops was predominantly terrestrial. Protoceratopoids were quadrupeds, with the prevalence of hind limbs, probably using slow or rapid trotlike gait. An asymmetrical locomotion was most likely impossible. On dry land, Bagaceratops and Protoceratops moved slowly. Udanoceratops and Leptoceratops<br>approximately equally used rapid and slow locomotor modes, although the...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-09-11-60</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-09-11-60</guid>
<pubDate>Thu, 11 Sep 2008 12:42:28 GMT</pubDate>
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<title>PROBABLE GUT CONTENTS WITHIN A SPECIMEN OF BRACHYLOPHOSAURUS CANADENSIS (DINOSAURIA: HADROSAURIDAE) FROM THE UPPER CRETACEOUS FROM MONTANA</title>
<description><![CDATA[An exceptionally preserved subadult specimen (JRF 115H) of a hadrosaurid, Brachylophosaurus canadensis, from the Judith River Formation near Malta, Montana, contains abundant plant fragments concentrated within the body cavity. We examined the taphonomy of the carcass and analyzed the gut-region material to test whether the organic remains represent fossilized gut contents. The dinosaur was buried in a fluvial channel setting, and the excellent articulation, integument impressions, and lack of scavenging indicate rapid burial. The organic material occupies a volume of at least 5750 cm3, and<br>comparable material is not found outside the carcass. The carcass contents include 63% clay, 16% ...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-09-11-59</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-09-11-59</guid>
<pubDate>Thu, 11 Sep 2008 12:39:16 GMT</pubDate>
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<title>A NEW GENUS AND SPECIES OF CAUDIPTERID DINOSAUR FROM THE LOWER CRETACEOUS JIUFOTANG FORMATION OF WESTERN LIAONING, CHINA</title>
<description><![CDATA[A new oviraptorosaur, Similicaudipteryx yixianensis gen. et sp. nov. is described from the Jiufotang Formation (120 Ma) of the Jehol Group in western Liaoning, China, which is referred to the Caudipteridae based on a dagger-like pygostyle and the shape of the ilium that are most similar to those of Caudipteryx. It differs from other oviraptorosaurids in that the ratio of pubis to ilium length is 1. 46 and the presence of two large and deep hypapophyses on dorsal vertebrae. The known caudipterids have previously been found only from the Jianshangou Member of the Yixian Formation (125 Ma) of the Sihetun area in Liaoning Province. S. yixianensis represents the first caudipterid dinosaur from th...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-08-27-58</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-08-27-58</guid>
<pubDate>Wed, 27 Aug 2008 07:33:22 GMT</pubDate>
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<title>Polar dinosaurs on parade: a review of dinosaur migration.</title>
<description><![CDATA[Cretaceous polar dinosaur faunas were taxonomically diverse, which suggests varied strategies for coping with the climatic stress of high latitudes. Some polar dinosaurs, particularly larger taxa such as the duckbill Edmontosaurus Lambe, 1917, were biomechanically and energetically capable of migrating over long distances, up to 2600 km.<br>However, current evidence strongly suggests many polar dinosaurs (including sauropods, large and small theropods, and ankylosaurs of New Zealand) overwintered in preference to migration. Certain groups also appear more predisposed to overwintering based on their physical inability (related to biomechanics, natural history, or absolute size) to migrate, su...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-08-27-57</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-08-27-57</guid>
<pubDate>Wed, 27 Aug 2008 04:58:41 GMT</pubDate>
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<title>A new titanosaurian braincase from the Allen Formation (Campanian–Maastrichtian), Rı´o Negro Province, Patagonia, Argentina</title>
<description><![CDATA[We describe a new titanosaurian braincase (MML-194), from the Upper Cretaceous (middle Campanian–lower Maastrichtian) of Río Negro Province, Argentina. Among titanosaurs, this specimen resembles Bonatitan reigi, more than any other member of the clade; the similarity is based on the supraoccipital protuberance bearing a median groove (also present in Saltasaurus and Rapetosaurus), the prominent basal tubera, the exit for the nerve VII located on the prootic crest, the occipital condyle and the foramen magnum almost of the same width. This material allows to observe some internal structures that are not appreciable in other titanosaurs, such as the pituitary cavity, the dorsum sellae and the ...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-08-19-56</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-08-19-56</guid>
<pubDate>Tue, 19 Aug 2008 17:26:56 GMT</pubDate>
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<title>Stegosaurian skin impressions from the Upper Jurassic Shangshaximiao Formation, Zigong, Sichuan, China: A new observation.</title>
<description><![CDATA[A skin impression fossil of Gigantspinosaurus sichuanensis was found in the Upper Jurassic Shangshaximiao Formation in Zigong, Sichuan. The fossil, preserved on the dorsal face of the left shoulder, clearly shows scales of Gigantspinosaurus sichuanensis. These scales are generally arranged as a net, and most of them are pentagonal, a few being quadrilateral and hexagonal. The maximum inner radius of most scales range from 5.7 to 9.2 mm. The scales are connected with each other by grooves. Scattered within small scales are a few pentagonal or hexagonal large scales, with each large scale surrounded by 13—14 scales. The surface of the scales is rough with string—like ridges. The stringy ridge ...]]></description>
<link>http://dinosauria.ucoz.com/news/2008-08-14-55</link>
<dc:creator>dinosauria</dc:creator>
<guid>http://dinosauria.ucoz.com/news/2008-08-14-55</guid>
<pubDate>Thu, 14 Aug 2008 16:28:44 GMT</pubDate>
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