The Fauna and Flora of the Morrison Formation: 2006
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Estesia Mongoliensis (Squamata: Anguimorpha) and the Evolution of Venom Grooves in Lizards
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by American Museum of Natural History Scientific Publications AMERICAN MUSEUM NOVITATES Number 3767, 31 pp. January 25, 2013 New materials of Estesia mongoliensis (Squamata: Anguimorpha) and the evolution of venom grooves in lizards HONG-YU YI1,2 AND MARK A. NORELL1,2 ABSTRACT New specimens of the fossil lizard Estesia mongoliensis are described from the Upper Cre- taceous of Mongolia. Phylogenetic analysis of 86 anguimorph taxa coded with 435 morphologi- cal characters and four genes confirms the placement of Estesia mongoliensis in a monophyletic Monstersauria. Extant monstersaurs, the genus Heloderma, are the only extant lizards bearing venom-transmitting teeth with a deep venom grove in the rostral carina. Compared to the crown group, stem monstersaurs are morphologically more variable in venom-delivery appa- ratus. This study has found that Estesia mongoliensis has two shallow grooves in the rostral and caudal carinae of its dentary teeth, demonstrating a primary venom-delivery apparatus. A sum- mary of venom-delivering tooth specialization in the Anguimorpha is provided, and related morphological characters are optimized on the strict consensus tree resulting from the com- bined morphological and molecular analysis of anguimorph phylogeny. The phylogeny supports a single origination of venom grooves in the Monstersauria, and indicates that grooved teeth are currently the only reliable venom-delivery apparatus to be recognized in fossil lizards. Key Words: Estesia mongoliensis, Monstersauria, venom groove, Anguimorpha INTRODUCTION Estesia mongoliensis is the oldest fossil squamate with dental grooves comparable to venom grooves in extant species. -
This Article Appeared in a Journal Published by Elsevier. the Attached
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Cretaceous Research 32 (2011) 135e142 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A reassessment of large theropod dinosaur tracks from the mid-Cretaceous (late AlbianeCenomanian) Winton Formation of Lark Quarry, central-western Queensland, Australia: A case for mistaken identity Anthony Romilio a,*, Steven W. Salisbury a,b a School of Biological Sciences, The University of Queensland, Brisbane, Qld 4072, Australia b Vertebrate Paleontology Section, Carnegie Museum of Natural History, 4400 Forbes Ave, Pittsburgh, PA 15213-4080, USA article info abstract Article history: Multivariate analysis is used to differentiate shape variations between ichnites of theropod and Received 9 June 2010 ornithopod dinosaurs. Tracks of an alleged theropod cf. Tyrannosauropus from the mid-Cretaceous (late Accepted in revised form 10 November 2010 AlbianeCenomanian) Winton Formation of Lark Quarry, central-western Queensland, Australia were Available online 22 November 2010 examined and foot shape ratios calculated. Multivariate analysis of these shape variables indicates this track-maker was an ornithopod dinosaur. -
A New Sauropodomorph Ichnogenus from the Lower Jurassic of Sichuan, China Fills a Gap in the Track Record
Historical Biology An International Journal of Paleobiology ISSN: 0891-2963 (Print) 1029-2381 (Online) Journal homepage: http://www.tandfonline.com/loi/ghbi20 A new sauropodomorph ichnogenus from the Lower Jurassic of Sichuan, China fills a gap in the track record Lida Xing, Martin G. Lockley, Jianping Zhang, Hendrik Klein, Daqing Li, Tetsuto Miyashita, Zhongdong Li & Susanna B. Kümmell To cite this article: Lida Xing, Martin G. Lockley, Jianping Zhang, Hendrik Klein, Daqing Li, Tetsuto Miyashita, Zhongdong Li & Susanna B. Kümmell (2016) A new sauropodomorph ichnogenus from the Lower Jurassic of Sichuan, China fills a gap in the track record, Historical Biology, 28:7, 881-895, DOI: 10.1080/08912963.2015.1052427 To link to this article: http://dx.doi.org/10.1080/08912963.2015.1052427 Published online: 24 Jun 2015. Submit your article to this journal Article views: 95 View related articles View Crossmark data Citing articles: 2 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=ghbi20 Download by: [University of Alberta] Date: 23 October 2016, At: 09:07 Historical Biology, 2016 Vol. 28, No. 7, 881–895, http://dx.doi.org/10.1080/08912963.2015.1052427 A new sauropodomorph ichnogenus from the Lower Jurassic of Sichuan, China fills a gap in the track record Lida Xinga*, Martin G. Lockleyb, Jianping Zhanga, Hendrik Kleinc, Daqing Lid, Tetsuto Miyashitae, Zhongdong Lif and Susanna B. Ku¨mmellg aSchool of the Earth Sciences and Resources, China University -
Stegosaurian Footprints from the Morrison Formation of Utah and Their Implications for Interpreting Other Ornithischian Tracks Gerard D
Stegosaurian footprints from the Morrison Formation of Utah and their implications for interpreting other ornithischian tracks Gerard D. Gierliński and Karol Sabath Polish Geological Institute, Rakowiecka 4, 00-975 Warsaw, Poland. e-mail: [email protected] ABSTRACT - The supposed stegosaurian track Deltapodus Whyte & Romano, 1994 (Middle Jurassic of England) is sauro- pod-like, elongate and plantigrade, but many blunt-toed, digitigrade, large ornithopod-like footprints (including pedal print cast associated with the manus of Stegopodus Lockley & Hunt, 1998) from the Upper Jurassic of Utah, better fit the stego- saurian foot pattern. The Morrison Formation of Utah yielded other tracks fitting the dryomorph (camptosaur) foot pattern (Dinehichnus Lockley et al., 1998) much better than Stegopodus. If the Stegopodus pedal specimen (we propose to shift the emphasis from the manus to the pes in the revised diagnosis of this ichnotaxon) and similar ichnites are proper stegosaur foot- prints, Deltapodus must have been left by another thyreophoran trackmaker. Other Deltapodus-like (possibly ankylosaurian) tracks include Navahopus Baird,1980 and Apulosauripus Nicosia et al., 1999. Heel-dominated, short-toed forms within the Navahopus-Deltapodus-Apulosauripus plexus differ from the gracile, relatively long-toed Tetrapodosaurus Sternberg, 1932, traditionally regarded as an ankylosaurian track. Thus, the original interpretation of the latter as a ceratopsian track might be correct, supporting early (Aptian) appearance of ceratopsians in North America. Isolated pedal ichnites from the Morrison Formation (with a single tentatively associated manus print, and another one from Poland) and the only known trackways with similar footprints (Upper Jurassic of Asturias, Spain) imply bipedal gait of their trackmakers. Thus, problems with stegosaur tracks possibly stem from the expectation of their quadrupedality. -
Tiago Rodrigues Simões
Diapsid Phylogeny and the Origin and Early Evolution of Squamates by Tiago Rodrigues Simões A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy in SYSTEMATICS AND EVOLUTION Department of Biological Sciences University of Alberta © Tiago Rodrigues Simões, 2018 ABSTRACT Squamate reptiles comprise over 10,000 living species and hundreds of fossil species of lizards, snakes and amphisbaenians, with their origins dating back at least as far back as the Middle Jurassic. Despite this enormous diversity and a long evolutionary history, numerous fundamental questions remain to be answered regarding the early evolution and origin of this major clade of tetrapods. Such long-standing issues include identifying the oldest fossil squamate, when exactly did squamates originate, and why morphological and molecular analyses of squamate evolution have strong disagreements on fundamental aspects of the squamate tree of life. Additionally, despite much debate, there is no existing consensus over the composition of the Lepidosauromorpha (the clade that includes squamates and their sister taxon, the Rhynchocephalia), making the squamate origin problem part of a broader and more complex reptile phylogeny issue. In this thesis, I provide a series of taxonomic, phylogenetic, biogeographic and morpho-functional contributions to shed light on these problems. I describe a new taxon that overwhelms previous hypothesis of iguanian biogeography and evolution in Gondwana (Gueragama sulamericana). I re-describe and assess the functional morphology of some of the oldest known articulated lizards in the world (Eichstaettisaurus schroederi and Ardeosaurus digitatellus), providing clues to the ancestry of geckoes, and the early evolution of their scansorial behaviour. -
Final Copy 2019 10 01 Herrera
This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Herrera Flores, Jorge Alfredo A Title: The macroevolution and macroecology of Mesozoic lepidosaurs General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. A copy of this may be found at https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode This license sets out your rights and the restrictions that apply to your access to the thesis so it is important you read this before proceeding. Take down policy Some pages of this thesis may have been removed for copyright restrictions prior to having it been deposited in Explore Bristol Research. However, if you have discovered material within the thesis that you consider to be unlawful e.g. breaches of copyright (either yours or that of a third party) or any other law, including but not limited to those relating to patent, trademark, confidentiality, data protection, obscenity, defamation, libel, then please contact [email protected] and include the following information in your message: •Your contact details •Bibliographic details for the item, including a URL •An outline nature of the complaint Your claim will be investigated and, where appropriate, the item in question will be removed from public view as soon as possible. This electronic thesis or dissertation has been downloaded from Explore Bristol Research, http://research-information.bristol.ac.uk Author: Herrera Flores, Jorge Alfredo A Title: The macroevolution and macroecology of Mesozoic lepidosaurs General rights Access to the thesis is subject to the Creative Commons Attribution - NonCommercial-No Derivatives 4.0 International Public License. -
Neutron Scanning Reveals Unexpected Complexity in the Enamel Thickness of Rsif.Royalsocietypublishing.Org an Herbivorous Jurassic Reptile
Downloaded from http://rsif.royalsocietypublishing.org/ on September 11, 2018 Neutron scanning reveals unexpected complexity in the enamel thickness of rsif.royalsocietypublishing.org an herbivorous Jurassic reptile Marc E. H. Jones1,2,3, Peter W. Lucas4, Abigail S. Tucker5, Amy P. Watson2, Research Joseph J. W. Sertich6, John R. Foster7, Ruth Williams8, Ulf Garbe9, Joseph J. Bevitt9 and Floriana Salvemini9 Cite this article: Jones MEH et al. 2018 1Department of Earth Sciences, The Natural History Museum, London, UK Neutron scanning reveals unexpected 2Department of Genetics and Evolution, School of Biological Sciences, The University of Adelaide, North Terrace, complexity in the enamel thickness of Adelaide, South Australia 5005, Australia 3 an herbivorous Jurassic reptile. J. R. Soc. South Australian Museum, North Terrace, Adelaide, South Australia 5001, Australia 4Smithsonian Tropical Research Institute, Balboa, Panama Interface 15: 20180039. 5Craniofacial Development and Stem Cell Biology, King’s College London, London, UK http://dx.doi.org/10.1098/rsif.2018.0039 6Department of Earth Sciences, Denver Museum of Nature and Science, Denver, CO, USA 7Museum of Moab, Moab, UT, USA 8Department of Adelaide Microscopy, The University of Adelaide, Adelaide, South Australia 5001, Australia 9Australian Centre for Neutron Scattering, Australian Nuclear Science and Technology Organisation, Sydney, Received: 16 January 2018 Australia Accepted: 18 May 2018 MEHJ, 0000-0002-0146-9623; PWL, 0000-0001-5286-9101; AST, 0000-0001-8871-6094 Eilenodontines are one of the oldest radiation of herbivorous lepidosaurs (snakes, lizards and tuatara) characterized by batteries of wide teeth with thick enamel that bear mammal-like wear facets. Unlike most reptiles, eileno- Subject Category: dontines have limited tooth replacement, making dental longevity Life Sciences–Engineering interface particularly important to them. -
Octavio Mateus
Foster, J.R. and Lucas, S. G., eds., 2006, Paleontology and Geology of the Upper Jurassic Morrison Formation. New Mexico Museum of Natural History and Science Bulletin 36. 223 LATE JURASSIC DINOSAURS FROM THE MORRISON FORMATION (USA), THE LOURINHÃ AND ALCOBAÇA FORMATIONS (PORTUGAL), AND THE TENDAGURU BEDS (TANZANIA): A COMPARISON OCTÁVIO MATEUS Museu da Lourinhã, Rua João Luis de Moura, 2530-157 Lourinhã, Portugal. Phone: +351.261 413 995; Fax: +351.261 423 887; Email: [email protected]; and Centro de Estudos Geológicos, FCT, Universidade Nova de Lisboa, Lisbon, Portugal Abstract—The Lourinhã and Alcobaça formations (in Portugal), Morrison Formation (in North America) and Tendaguru Beds (in Tanzania) are compared. These three Late Jurassic areas, dated as Kimmeridgian to Tithonian are similar paleoenvironmentally and faunally. Four dinosaur genera are shared between Portugal and the Morrison (Allosaurus, Torvosaurus, Ceratosaurus and Apatosaurus), as well as all non-avian dinosaur families. Episodic dis- persal occurred until at least the Late Jurassic. The Portuguese dinosaurs did not developed dwarfism and are as large as Morrison and Tendaguru dinosaurs. Resumo em português—São comparadas as Formações de Lourinhã e Alcobaça (em Portugal), Formação de Morrison (na América do Norte) e as Tendaguru Beds (na Tanzânia). Estas três áreas do Jurássico Superior (Kimmeridgiano/ Titoniano) têm muitas semelhanças relativamente aos paleoambientes. Quatro géneros de dinossauros são comuns a Portugal e Morrison (Allosaurus, Torvosaurus, Ceratosaurus e Apatosaurus), assim como todas as famílias de dinossauros não-avianos. Episódios migratórios ocorreram pelo menos até ao Jurássico Superior. Os dinossauros de Portugal não desenvolveram nanismo e eram tão grandes como os dinossauros de Morrison e Tendaguru. -
Mammalian Fauna of the Late Jurassic Guimarota Ecosystem
Asociación Paleontológica Argentina. Publicación Especial 7 ISSN 0328-347X VII International Symposium on Mesozoic Terrestrial Ecosystems: 123-126. Buenos Aires, 30-6-2001 MaMMalian fauna of the Late Jurassic Guimarota ecoSyStem Thomas MARTIN1 Abstract. The Late Jurassic (Kirnmeridgian) Guimarota loca lit y near Leiria in west-central Portugal has yielded more than 800 mammalian dentaries and partial skulls representing the largest sample of Late Jurassic mammals in the world. However, despite the enormous number of specimens collected, the mam- malian fauna appears somewhat depauperate. So far, only Multituberculata (several genera of Paulchoffatiidae; 28% of total number), Docodonta (Halda nadan exspectaius Kühne and Krusat; 24%), and Holotheria (48%) represented by Paurodontidae (Henkelatherium guimaratae Krebs and Drescheratherium acutum Krebs) and Dryolestidae (Dryalestes leiriensis Martín, Krebsoiherium Iusiianicum Martin, and Guimaroiodus inflatus Martin) have been detected. "Triconodonta" and Syrnmetrodonta, which are well represented at other Late Jurassic localities (e.g., Morrison Forrnation), are missing. To recover the rare mammalian taxa of the Guimarota ecosystem, a project was initiated to study the nearly 7000 isolated mammalian teeth that had been obtained by screenwashing. With a single exception, the same taxa are represented. Among the thousands of isolated teeth, however, 25 lower and 23 upper premolars and mo- lars of a tiny primitive Zatheria have been found, of which the lower molars closely resemble the "Porto Pinheiro molar". After sorting the isolated teeth, the mammalian fauna of the Guimarota ecosystem prob- ably is completely recorded. Apparently, the coastal swamp in the Lusitanian graben where the lignite formed represented a stressed environment not appropriate for some marnmalian groups. -
A New Sphenodontian (Lepidosauria: Rhynchocephalia)
View metadata, citation and similar papersDownloaded at core.ac.uk from http://rspb.royalsocietypublishing.org/ on February 13, 2017 brought to you by CORE provided by CONICET Digital A new sphenodontian (Lepidosauria: Rhynchocephalia) from the Late Triassic of Argentina and the early origin of the herbivore opisthodontians rspb.royalsocietypublishing.org Ricardo N. Martı´nez1, Cecilia Apaldetti1,2, Carina E. Colombi1,2, Angel Praderio1, Eliana Fernandez1,2, Paula Santi Malnis1,2, 1,2 1 1 Research Gustavo A. Correa , Diego Abelin and Oscar Alcober 1Instituto y Museo de Ciencias Naturales, Universidad Nacional de San Juan, Avenida Espan˜a 400 Norte, Cite this article: Martı´nez RN, Apaldetti C, 5400 San Juan, Argentina Colombi CE, Praderio A, Fernandez E, Malnis 2Consejo Nacional de Investigaciones Cientı´ficas y Te´cnicas, CONICET, Buenos Aires, Argentina PS, Correa GA, Abelin D, Alcober O. 2013 A new sphenodontian (Lepidosauria: Rhyncho- Sphenodontians were a successful group of rhynchocephalian reptiles that dominated the fossil record of Lepidosauria during the Triassic and Jurassic. cephalia) from the Late Triassic of Argentina Although evidence of extinction is seen at the end of the Laurasian Early and the early origin of the herbivore Cretaceous, they appeared to remain numerically abundant in South America opisthodontians. Proc R Soc B 280: 20132057. until the end of the period. Most of the known Late Cretaceous record in http://dx.doi.org/10.1098/rspb.2013.2057 South America is composed of opisthodontians, the herbivorous branch of Sphenodontia, whose oldest members were until recently reported to be from the Kimmeridgian–Tithonian (Late Jurassic). Here, we report a new sphenodontian, Sphenotitan leyesi gen. -
Paleontology of the Bears Ears National Monument
Paleontology of Bears Ears National Monument (Utah, USA): history of exploration, study, and designation 1,2 3 4 5 Jessica Uglesich , Robert J. Gay *, M. Allison Stegner , Adam K. Huttenlocker , Randall B. Irmis6 1 Friends of Cedar Mesa, Bluff, Utah 84512 U.S.A. 2 University of Texas at San Antonio, Department of Geosciences, San Antonio, Texas 78249 U.S.A. 3 Colorado Canyons Association, Grand Junction, Colorado 81501 U.S.A. 4 Department of Integrative Biology, University of Wisconsin-Madison, Madison, Wisconsin, 53706 U.S.A. 5 University of Southern California, Los Angeles, California 90007 U.S.A. 6 Natural History Museum of Utah and Department of Geology & Geophysics, University of Utah, 301 Wakara Way, Salt Lake City, Utah 84108-1214 U.S.A. *Corresponding author: [email protected] or [email protected] Submitted September 2018 PeerJ Preprints | https://doi.org/10.7287/peerj.preprints.3442v2 | CC BY 4.0 Open Access | rec: 23 Sep 2018, publ: 23 Sep 2018 ABSTRACT Bears Ears National Monument (BENM) is a new, landscape-scale national monument jointly administered by the Bureau of Land Management and the Forest Service in southeastern Utah as part of the National Conservation Lands system. As initially designated in 2016, BENM encompassed 1.3 million acres of land with exceptionally fossiliferous rock units. Subsequently, in December 2017, presidential action reduced BENM to two smaller management units (Indian Creek and Shash Jáá). Although the paleontological resources of BENM are extensive and abundant, they have historically been under-studied. Here, we summarize prior paleontological work within the original BENM boundaries in order to provide a complete picture of the paleontological resources, and synthesize the data which were used to support paleontological resource protection.