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From the Early Cretaceous Wonthaggi Formation (Strzelecki Group)
Journal of Paleontology, 93(3), 2019, p. 543–584 Copyright © 2019, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/19/1937-2337 doi: 10.1017/jpa.2018.95 New small-bodied ornithopods (Dinosauria, Neornithischia) from the Early Cretaceous Wonthaggi Formation (Strzelecki Group) of the Australian-Antarctic rift system, with revision of Qantassaurus intrepidus Rich and Vickers-Rich, 1999 Matthew C. Herne,1,2 Jay P. Nair,2 Alistair R. Evans,3 and Alan M. Tait4 1School of Environmental and Rural Science, University of New England, Armidale 2351, New South Wales, Australia <ornithomatt@ gmail.com> 2School of Biological Sciences, The University of Queensland, Brisbane, Queensland 4072, Australia <[email protected]> 3School of Biological Sciences, Monash University, Melbourne, Victoria 3800, Australia <[email protected]> 4School of Earth, Atmosphere & Environment, Monash University, Melbourne, Victoria 3800, Australia <[email protected]> Abstract.—The Flat Rocks locality in the Wonthaggi Formation (Strzelecki Group) of the Gippsland Basin, southeastern Australia, hosts fossils of a late Barremian vertebrate fauna that inhabited the ancient rift between Australia and Antarc- tica. Known from its dentary, Qantassaurus intrepidus Rich and Vickers-Rich, 1999 has been the only dinosaur named from this locality. However, the plethora of vertebrate fossils collected from Flat Rocks suggests that further dinosaurs await discovery. From this locality, we name a new small-bodied ornithopod, Galleonosaurus dorisae n. -
R / 2J�J Ij Rjsj L)J J �� __Rj Ljlj F LANDED! VOLUME 2 - RAPTORS to PRATINCOLES
-_r_/ 2J�J iJ_rJsJ l)J_J �� __rJ lJlJ_f LANDED! VOLUME 2 - RAPTORS TO PRATINCOLES In 1990 Oxford Univer sity Press published Volume One Over 70 colourpl ates illustr ated of the Ha11dbook of Austra by JeffDavies feature nearly lia 11, New Zeala11d a11d every species. Antarctic Birds to widespread acclaim. Now Volume Two, VOLUME2 covering Raptors to Pratin Contains vultures, hawks and coles, has been completed. eagles, falcons, galliformes and quail, Malleefowl a11d megapodes, Four more volumes are to be cranes,crakes and rails, bustards, published making this the the Australian and New Zealand most detailed and up-to-date resident waders, a11d plovers, reference work of the birds of lapwi11gs a11d douerels. Australasia. COMPREHENSIVE Each volume exami11es all aspects of bird lifeinc luding: • field i£Jentiflca1ion • dis1ribu1io11 and popula1io11 • social orga11iza1io11 The Handbook is the most ex • social behaviour citing and significant project •movements in Australasian ornithology to •plumages day and will have an •breeding • habitat enormous impact on the direc • voice tion of future research and the •food conservation of Au stralasian and Antarctic birds. _ • AVAI�!�! BER t�n�r? Volume 2 $250 RAOU Volumes 1 & 2 $499 -- m! CJOlltlllllCOIIIIYIOOI ORDER FORM Place your order with Oxford University Press by: cgJ Reply Paid 1641, Oxford University Press, D Please send me __ copy/copies of the Handbook of GPO Box 2784Y, Melbourne3001 Aus1ralia11, New Zealondand A111arc1ic Birds Volume 2 at the 11 (03) 646 4200 FAX (03) 646 3251 special pre-publication price of $250 (nonnal retail price $295) plus $7.50 for po stage and handling OR D I enclose my cheque/money order for$ _______ D Please send me set/sets of Volumes I a11d 2 of the D Please charge my Visa/Mastercard/Bankcard no. -
A Phylogenetic Analysis of the Basal Ornithischia (Reptilia, Dinosauria)
A PHYLOGENETIC ANALYSIS OF THE BASAL ORNITHISCHIA (REPTILIA, DINOSAURIA) Marc Richard Spencer A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements of the degree of MASTER OF SCIENCE December 2007 Committee: Margaret M. Yacobucci, Advisor Don C. Steinker Daniel M. Pavuk © 2007 Marc Richard Spencer All Rights Reserved iii ABSTRACT Margaret M. Yacobucci, Advisor The placement of Lesothosaurus diagnosticus and the Heterodontosauridae within the Ornithischia has been problematic. Historically, Lesothosaurus has been regarded as a basal ornithischian dinosaur, the sister taxon to the Genasauria. Recent phylogenetic analyses, however, have placed Lesothosaurus as a more derived ornithischian within the Genasauria. The Fabrosauridae, of which Lesothosaurus was considered a member, has never been phylogenetically corroborated and has been considered a paraphyletic assemblage. Prior to recent phylogenetic analyses, the problematic Heterodontosauridae was placed within the Ornithopoda as the sister taxon to the Euornithopoda. The heterodontosaurids have also been considered as the basal member of the Cerapoda (Ornithopoda + Marginocephalia), the sister taxon to the Marginocephalia, and as the sister taxon to the Genasauria. To reevaluate the placement of these taxa, along with other basal ornithischians and more derived subclades, a phylogenetic analysis of 19 taxonomic units, including two outgroup taxa, was performed. Analysis of 97 characters and their associated character states culled, modified, and/or rescored from published literature based on published descriptions, produced four most parsimonious trees. Consistency and retention indices were calculated and a bootstrap analysis was performed to determine the relative support for the resultant phylogeny. The Ornithischia was recovered with Pisanosaurus as its basalmost member. -
A Revised Taxonomy of the Iguanodont Dinosaur Genera and Species
ARTICLE IN PRESS + MODEL Cretaceous Research xx (2007) 1e25 www.elsevier.com/locate/CretRes A revised taxonomy of the iguanodont dinosaur genera and species Gregory S. Paul 3109 North Calvert Station, Side Apartment, Baltimore, MD 21218-3807, USA Received 20 April 2006; accepted in revised form 27 April 2007 Abstract Criteria for designating dinosaur genera are inconsistent; some very similar species are highly split at the generic level, other anatomically disparate species are united at the same rank. Since the mid-1800s the classic genus Iguanodon has become a taxonomic grab-bag containing species spanning most of the Early Cretaceous of the northern hemisphere. Recently the genus was radically redesignated when the type was shifted from nondiagnostic English Valanginian teeth to a complete skull and skeleton of the heavily built, semi-quadrupedal I. bernissartensis from much younger Belgian sediments, even though the latter is very different in form from the gracile skeletal remains described by Mantell. Currently, iguanodont remains from Europe are usually assigned to either robust I. bernissartensis or gracile I. atherfieldensis, regardless of lo- cation or stage. A stratigraphic analysis is combined with a character census that shows the European iguanodonts are markedly more morpho- logically divergent than other dinosaur genera, and some appear phylogenetically more derived than others. Two new genera and a new species have been or are named for the gracile iguanodonts of the Wealden Supergroup; strongly bipedal Mantellisaurus atherfieldensis Paul (2006. Turning the old into the new: a separate genus for the gracile iguanodont from the Wealden of England. In: Carpenter, K. (Ed.), Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. -
Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex
Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex By Karen E. Poole B.A. in Geology, May 2004, University of Pennsylvania M.A. in Earth and Planetary Sciences, August 2008, Washington University in St. Louis A Dissertation submitted to The Faculty of The Columbian College of Arts and Sciences of The George Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 31, 2015 Dissertation Directed by Catherine Forster Professor of Biology The Columbian College of Arts and Sciences of The George Washington University certifies that Karen Poole has passed the Final Examination for the degree of Doctor of Philosophy as of August 10th, 2015. This is the final and approved form of the dissertation. Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex Karen E. Poole Dissertation Research Committee: Catherine A. Forster, Professor of Biology, Dissertation Director James M. Clark, Ronald Weintraub Professor of Biology, Committee Member R. Alexander Pyron, Robert F. Griggs Assistant Professor of Biology, Committee Member ii © Copyright 2015 by Karen Poole All rights reserved iii Dedication To Joseph Theis, for his unending support, and for always reminding me what matters most in life. To my parents, who have always encouraged me to pursue my dreams, even those they didn’t understand. iv Acknowledgements First, a heartfelt thank you is due to my advisor, Cathy Forster, for giving me free reign in this dissertation, but always providing valuable commentary on any piece of writing I sent her, no matter how messy. -
The Diverse Group of Plant-Eating Dinosaurs That Roamed Victoria 110 Million Years Ago 20 August 2021, by Stephen Poropat
The diverse group of plant-eating dinosaurs that roamed Victoria 110 million years ago 20 August 2021, by Stephen Poropat coexisted at the same time. So far, five ornithopod species have been named from the Cretaceous of Victoria. There are three from the Otway Coast: Atlascopcosaurus loadsi, Diluvicursor pickeringi and Leaellynasaura amicagraphica; and two from the Bass Coast: Qantassaurus intrepidus and Galleonosaurus dorisae. The rocks exposed on the Bass Coast (and the fossils they contain) are around 15 million to 20 million years older than those on the Otway Coast. During this interval, Australia's climate warmed dramatically. There's substantial evidence of glaciation in South Australia about 125 million years ago, but by 110 million years ago, warm weather-loving crocodile relatives were roaming happily in Victoria. As such, it was presumed the Bass Coast's Qantassaurus and Galleonosaurus—which lived in older, colder conditions—probably never crossed paths with the Otway Coast's Leaellynasaura, Atlascopcosaurus and Diluvicursor. But is that true? Eric The Red West The original specimen of Diluvicursor pickeringi, Thanks to research led by my former student comprising a tail, a partial shin and ankle, and a hind Ruairidh Duncan, we're now in a better position to foot. Credit: Stephen Poropat/Museums Victoria answer this question. For his Honors project, Ruairidh studied fossils from a site on Cape Otway called Eric the Red West (ETRW). During the Early Cretaceous period, 110 million to 107 million years ago, Australia was much further south than it is today. Yet fossils from several sites on the Otway Coast in Victoria show dinosaurs were common in the region. -
Dinosaur Coast Information Brochure
AU SAU R O S R O C C N O N O I I A A D D S S T T M M A A N N A A G G E P E P M U M U E O E O N T G R N T G R CULTURAL SIGNIFICANCE WHERE TO GO AND WHAT TO DO For thousands of years, Indigenous people of the Dampier Along most of the Dinosaur Coast dinosaur tracks occur in Peninsula and wider west Kimberley have had strong cultural Broome Sandstone, in the intertidal zone. Because of this DAMPIER PENINSULA, WESTERN AUSTRALIA connections with dinosaur tracks. Three-toed dinosaur tracks the best time to see most of the tracks is at low tide, when MANAGEMENT GROUP trace the journey of a Bugarrigarra (Dreamtime) creator- they are exposed. Sand along the Dinosaur Coast beaches being called Marala, also known as Emu man. is very mobile, so some tracks may be temporarily buried or new ones exposed. Each time you go tracking it is a journey The National Heritage listed coastline of the The song cycle that includes stories of Marala extends along of discovery. Dampier Peninsula preserves one of the length of the Dinosaur Coast from Bunginygun (Swan the most diverse assemblages of dinosaur The easiest places to fi nd tracks are: Point, Cape Leveque) to Wabana (Cape Bossut, near La tracks in the world. Grange) and then inland to the south-east, over a distance of approximately 450kms. Maralagun on Cable Beach – sand frequently covers this area Minyirr (Gantheaume Point) – only at extremely DINOSAUR COAST low tides, rocks very slippery 130 MILLION YEARS AGO MANAGEMENT GROUP Yinara (Reddell Beach south) – north of Reddell Point, beach can be accessed via Kavite Road During the Early Cretaceous Period, Australia formed the 10 cm eastern peninsula of the fragmenting super-continent of (if the road is open). -
Body-Size Evolution in the Dinosauria
8 Body-Size Evolution in the Dinosauria Matthew T. Carrano Introduction The evolution of body size and its influence on organismal biology have received scientific attention since the earliest decades of evolutionary study (e.g., Cope, 1887, 1896; Thompson, 1917). Both paleontologists and neontologists have attempted to determine correlations between body size and numerous aspects of life history, with the ultimate goal of docu- menting both the predictive and causal connections involved (LaBarbera, 1986, 1989). These studies have generated an appreciation for the thor- oughgoing interrelationships between body size and nearly every sig- nificant facet of organismal biology, including metabolism (Lindstedt & Calder, 1981; Schmidt-Nielsen, 1984; McNab, 1989), population ecology (Damuth, 1981; Juanes, 1986; Gittleman & Purvis, 1998), locomotion (Mc- Mahon, 1975; Biewener, 1989; Alexander, 1996), and reproduction (Alex- ander, 1996). An enduring focus of these studies has been Cope’s Rule, the notion that body size tends to increase over time within lineages (Kurtén, 1953; Stanley, 1973; Polly, 1998). Such an observation has been made regarding many different clades but has been examined specifically in only a few (MacFadden, 1986; Arnold et al., 1995; Jablonski, 1996, 1997; Trammer & Kaim, 1997, 1999; Alroy, 1998). The discordant results of such analyses have underscored two points: (1) Cope’s Rule does not apply universally to all groups; and (2) even when present, size increases in different clades may reflect very different underlying processes. Thus, the question, “does Cope’s Rule exist?” is better parsed into two questions: “to which groups does Cope’s Rule apply?” and “what process is responsible for it in each?” Several recent works (McShea, 1994, 2000; Jablonski, 1997; Alroy, 1998, 2000a, 2000b) have begun to address these more specific questions, attempting to quantify patterns of body-size evolution in a phylogenetic (rather than strictly temporal) context, as well as developing methods for interpreting the resultant patterns. -
Morphological Variation in the Hadrosauroid Dentary Morfologisk Variation I Det Hadrosauroida Dentärbenet
Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 398 Morphological Variation in the Hadrosauroid Dentary Morfologisk variation i det hadrosauroida dentärbenet D. Fredrik K. Söderblom INSTITUTIONEN FÖR GEOVETENSKAPER DEPARTMENT OF EARTH SCIENCES Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 398 Morphological Variation in the Hadrosauroid Dentary Morfologisk variation i det hadrosauroida dentärbenet D. Fredrik K. Söderblom ISSN 1650-6553 Copyright © D. Fredrik K. Söderblom Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2017 Abstract Morphological Variation in the Hadrosauroid Dentary D. Fredrik K. Söderblom The near global success reached by hadrosaurid dinosaurs during the Cretaceous has been attributed to their ability to masticate (chew). This behavior is more commonly recognized as a mammalian adaptation and, as a result, its occurrence in a non-mammalian lineage should be accompanied with several evolutionary modifications associated with food collection and processing. The current study investigates morphological variation in a specific cranial complex, the dentary, a major element of the hadrosauroid lower jaw. 89 dentaries were subjected to morphometric and statistical analyses to investigate the clade’s taxonomic-, ontogenetic-, and individual variation in dentary morphology. Results indicate that food collection and processing became more efficient in saurolophid hadrosaurids through a complex pattern of evolutionary and growth-related changes. The diastema (space separating the beak from the dental battery) grew longer relative to dentary length, specializing food collection anteriorly and food processing posteriorly. The diastema became ventrally directed, hinting at adaptations to low-level grazing, especially in younger individuals. -
A New Basal Ornithopod Dinosaur from the Lower Cretaceous of China
A new basal ornithopod dinosaur from the Lower Cretaceous of China Yuqing Yang1,2,3, Wenhao Wu4,5, Paul-Emile Dieudonné6 and Pascal Godefroit7 1 College of Resources and Civil Engineering, Northeastern University, Shenyang, Liaoning, China 2 College of Paleontology, Shenyang Normal University, Shenyang, Liaoning, China 3 Key Laboratory for Evolution of Past Life and Change of Environment, Province of Liaoning, Shenyang Normal University, Shenyang, Liaoning, China 4 Key Laboratory for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Jilin University, Changchun, Jilin, China 5 Research Center of Paleontology and Stratigraphy, Jilin University, Changchun, Jilin, China 6 Instituto de Investigación en Paleobiología y Geología, CONICET, Universidad Nacional de Río Negro, Rio Negro, Argentina 7 Directorate ‘Earth and History of Life’, Royal Belgian Institute of Natural Sciences, Brussels, Belgium ABSTRACT A new basal ornithopod dinosaur, based on two nearly complete articulated skeletons, is reported from the Lujiatun Beds (Yixian Fm, Lower Cretaceous) of western Liaoning Province (China). Some of the diagnostic features of Changmiania liaoningensis nov. gen., nov. sp. are tentatively interpreted as adaptations to a fossorial behavior, including: fused premaxillae; nasal laterally expanded, overhanging the maxilla; shortened neck formed by only six cervical vertebrae; neural spines of the sacral vertebrae completely fused together, forming a craniocaudally-elongated continuous bar; fused scapulocoracoid with prominent -
Osteology of a Near-Complete Skeleton of Tenontosaurus Tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA
Osteology of a Near-Complete Skeleton of Tenontosaurus tilletti (Dinosauria: Ornithopoda) from the Cloverly Formation, Montana, USA A report submitted in partial fulfilment of the requirements for the degree of MEarthSci Geology (Hons.), University of Manchester Jonathan Tennant 70406912 MEarthSci Geology (Hons.) School of Earth, Atmospheric and Environmental Sciences University of Manchester Williamson Building Oxford Road Manchester M13 9PL Osteology of Tenontosaurus tilletti Contents Figures and Tables..............................................................................................................................................3 1.0 Abstract .............................................................................................................................................................6 2.0 Introduction ......................................................................................................................................................7 2.1 Aims and Objectives....................................................................................................................................7 2.2 Institutional Abbreviations ........................................................................................................................9 3.0 Previous Work ............................................................................................................................................... 11 3.1 The Cloverly Formation .......................................................................................................................... -
Pebblego Animals Article List
PebbleGo Animals Article List AMPHIBIANS Hawks Iguanodon Compsognathus Sauroposeidon Frogs Herons Kentrosaurus Cryolophosaurus Suuwassea Mudpuppies Humboldt Penguins Kritosaurus Dahalokely Thecodontosaurus Newts Hummingbirds Lambeosaurus Daspletosaurus Salamanders Ibises Leaellynasaura Deinocheirus FISH Toads King Penguins Leptoceratops Deinonychus Angelfish Kingfishers Lexovisaurus Deltadromeus Barracudas ANIMAL BEHAVIOR Kiwis Lophorhothon Eoraptor Basking Sharks Animal Communication Little Penguins Maiasaura Eotyrannus Blue Sharks Animals in the Fall Loons Microceratus Falcarius Catfish Hibernation Macaroni Penguins Micropachycephalosaurus Gallimimus Clown Fish Migration Macaws Minmi Gasosaurus Coelacanths Nocturnal Animals Magellanic Penguins Montanoceratops Giganotosaurus Eels Orioles Muttaburrasaurus Guanlong Great White Sharks ANIMAL Ostriches Nedoceratops Herrerasaurus Hammerhead Sharks CLASSIFICATION Owls Nodosaurus Incisivosaurus Mako Sharks About Amphibians Parrots Olorotitan Labocania Megamouth Sharks About Birds Peacocks Oryctodromeus Liliensternus Nurse Sharks About Fish Pelicans Ouranosaurus Masiakasaurus Parrotfish About Insects Pheasants Pachycephalosaurus Metriacanthosaurus Piranhas About Invertebrates Puffins Pachyrhinosaurus Microraptor Puffer Fish About Mammals Quetzals Parasaurolophus Neovenator Salmon About Reptiles Robins Pawpawsaurus Ornithomimus Sea Horses About Spiders Rockhopper Penguins Polacanthus Ozraptor Swordfish Royal Penguins Protoceratops Protarchaeopteryx Stingrays ANIMAL HABITATS Snares Penguins Saurolophus