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The Wingtips of the Pterosaurs: Anatomy, Aeronautical Function and Palaeogeography, Palaeoclimatology, Palaeoecology Xxx (2015) Xxx Xxx 3 Ecological Implications
Our reference: PALAEO 7445 P-authorquery-v11 AUTHOR QUERY FORM Journal: PALAEO Please e-mail your responses and any corrections to: Article Number: 7445 E-mail: [email protected] Dear Author, Please check your proof carefully and mark all corrections at the appropriate place in the proof (e.g., by using on-screen annotation in the PDF file) or compile them in a separate list. Note: if you opt to annotate the file with software other than Adobe Reader then please also highlight the appropriate place in the PDF file. To ensure fast publication of your paper please return your corrections within 48 hours. For correction or revision of any artwork, please consult http://www.elsevier.com/artworkinstructions. We were unable to process your file(s) fully electronically and have proceeded by Scanning (parts of) your Rekeying (parts of) your article Scanning the article artwork Any queries or remarks that have arisen during the processing of your manuscript are listed below and highlighted by flags in the proof. Click on the ‘Q’ link to go to the location in the proof. Location in article Query / Remark: click on the Q link to go Please insert your reply or correction at the corresponding line in the proof Q1 Your article is registered as a regular item and is being processed for inclusion in a regular issue of the journal. If this is NOT correct and your article belongs to a Special Issue/Collection please contact [email protected] immediately prior to returning your corrections. Q2 Please confirm that given names and surnames have been identified correctly. -
Squires and Saul—Pacific Slope Cretaceous
SQUIRES AND SAUL—PACIFIC SLOPE CRETACEOUS GASTROPODS 53 but, in terms of the internal spiral ridge on the base, the new matrix of a boulder conglomerate consisting of metavolcanic species is very similar to Xenophora (Xenophora) sp. Darragh clasts and associated with Otostoma sharonae new species. and Kendrick (1994, p. 34-38, figs. 6C-F, 7A-C) from the Upper Genus Xenophora ranges from the Late Cretaceous (Cenoman- Maastrichtian Miria Formation, Carnarvon basin, northwestern ian) to Recent (Ponder, 1983; Dockery, 1993). On the Pacific Australia. The new species differs from this Australian species by slope of North America, Xenophora is represented by six species. having a more depressed shell base, no umbilicus, a more thick- Two are of Late Cretaceous age and include X. willisi and the ened inner lip, much more pebble armor, and a lack of ornamen- new species. The other four are of Tertiary age. Xenophora zitteli tation on the body whorl and on the shell base. Weaver (1905, p. 118-119, pi. 12, fig. 8) and Xenophora simiensis The only other Cretaceous species of Xenophora from the Pa- Nelson (1925, p. 422, pi. 55, figs. 7a-c) are of late Paleocene age cific slope of North America is Xenophora willisi Webster (1983, and are found in California (Zinsmeister, 1983). Xenophora stocki p. 1092, 1095, figs. 2A-F, 3A) from the Upper Cretaceous (upper? Dickerson (1916, p. 502-503, pi. 37, figs. 4a,b) is of early to Campanian to early? Maastrichtian) Rosario Formation at Arroyo middle Eocene age and is found in Baja California Sur, Mexico; Santa Catarina and near San Antonio del Mar in the northern part California; and Oregon (Squires and Demetrion, 1992; Squires, of the state of Baja California, Mexico. -
SG125 035-140 Veldmeijer 16-01-2007 07:46 Pagina 35
SG125 035-140 veldmeijer 16-01-2007 07:46 Pagina 35 Description of Coloborhynchus spielbergi sp. nov. (Pterodactyloidea) from the Albian (Lower Cretaceous) of Brazil. André J. Veldmeijer Veldmeijer, A.J. Coloborhynchus spielbergi sp. nov. (Pterodactyloidea) from the Albian (Lower Cretaceous) of Brazil. Scripta Geologica 125: 35-139, 22 figs., 16 pls; Leiden, May 2003. André J. Veldmeijer, Mezquitalaan 23, 1064 NS Amsterdam, The Netherlands ([email protected]). A new species of pterosaur, Coloborhynchus spielbergi sp. nov. (Pterodactyloidea), from the Romualdo Member (Albian) of the Santana Formation is described. The type consists of the skull, mandible and many of the post-cranial bones. The specimen displays a high degree of co-ossification indicating that the animal was an adult and likely quite old when it died. The wingspan is reconstructed at nearly 6 m. Among the characteristic features are a large anteriorly positioned premaxillary sagittal crest and a smaller, also anteriorly positioned dentary sagittal crest, a flat anterior aspect of the skull from which two teeth project and a ventrally fused pelvis. Comments on Brazilian pterosaurs are made in connec- tion with the classificiation of the Leiden specimen. Keywords –– Pterosaur, Coloborhynchus, Santana Formation, Lower Cretaceous, Brazil. Contents Introduction ..................................................................................................................................................... 35 Material ............................................................................................................................................................. -
On Two Pterosaur Humeri from the Tendaguru Beds (Upper Jurassic, Tanzania)
“main” — 2009/10/20 — 22:40 — page 813 — #1 Anais da Academia Brasileira de Ciências (2009) 81(4): 813-818 (Annals of the Brazilian Academy of Sciences) ISSN 0001-3765 www.scielo.br/aabc On two pterosaur humeri from the Tendaguru beds (Upper Jurassic, Tanzania) FABIANA R. COSTA and ALEXANDER W.A. KELLNER Museu Nacional, Universidade Federal do Rio de Janeiro, Departamento de Geologia e Paleontologia Quinta da Boa Vista s/n, São Cristóvão, 20940-040 Rio de Janeiro, RJ, Brasil Manuscript received on August 17, 2009; accepted for publication on September 30, 2009; contributed by ALEXANDER W.A. KELLNER* ABSTRACT Jurassic African pterosaur remains are exceptionally rare and only known from the Tendaguru deposits, Upper Jurassic, Tanzania. Here we describe two right humeri of Tendaguru pterosaurs from the Humboldt University of Berlin: specimens MB.R. 2828 (cast MN 6661-V) and MB.R. 2833 (cast MN 6666-V). MB.R. 2828 consists of a three- dimensionally preserved proximal portion. The combination of the morphological features of the deltopectoral crest not observed in other pterosaurs suggests that this specimen belongs to a new dsungaripteroid taxon. MB.R. 2833 is nearly complete, and because of a long and round proximally placed deltopectoral crest it could be referred to the Archaeopterodactyloidea. It is the smallest pterosaur from Africa and one of the smallest flying reptiles ever recorded. These specimens confirm the importance of the Tendaguru deposits for the Jurassic pterosaur record. This potential, however, has to be fully explored with more field work. Key words: Tendaguru, Tanzania, Africa, Upper Jurassic, Pterosauria. INTRODUCTION in providing isolated remains up to now (Kellner and Mader 1997, Wellnhofer and Buffetaut 1999, Mader Africa shows a great potential for pterosaur material and Kellner 1999). -
Analyzing Pterosaur Ontogeny and Sexual Dimorphism with Multivariate Allometry Erick Charles Anderson [email protected]
Marshall University Marshall Digital Scholar Theses, Dissertations and Capstones 2016 Analyzing Pterosaur Ontogeny and Sexual Dimorphism with Multivariate Allometry Erick Charles Anderson [email protected] Follow this and additional works at: http://mds.marshall.edu/etd Part of the Animal Sciences Commons, Ecology and Evolutionary Biology Commons, and the Paleontology Commons Recommended Citation Anderson, Erick Charles, "Analyzing Pterosaur Ontogeny and Sexual Dimorphism with Multivariate Allometry" (2016). Theses, Dissertations and Capstones. 1031. http://mds.marshall.edu/etd/1031 This Thesis is brought to you for free and open access by Marshall Digital Scholar. It has been accepted for inclusion in Theses, Dissertations and Capstones by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected], [email protected]. ANALYZING PTEROSAUR ONTOGENY AND SEXUAL DIMORPHISM WITH MULTIVARIATE ALLOMETRY A thesis submitted to the Graduate College of Marshall University In partial fulfillment of the requirements for the degree of Master of Science in Biological Sciences by Erick Charles Anderson Approved by Dr. Frank R. O’Keefe, Committee Chairperson Dr. Suzanne Strait Dr. Andy Grass Marshall University May 2016 i ii ii Erick Charles Anderson ALL RIGHTS RESERVED iii Acknowledgments I would like to thank Dr. F. Robin O’Keefe for his guidance and advice during my three years at Marshall University. His past research and experience with reptile evolution made this research possible. I would also like to thank Dr. Andy Grass for his advice during the course of the research. I would like to thank my fellow graduate students Donald Morgan and Tiffany Aeling for their support, encouragement, and advice in the lab and bar during our two years working together. -
Chapter 2 Physical Characteristics of the Study Area
CHAPTER 2 PHYSICAL CHARACTERISTICS OF THE STUDY AREA 2.1. Location of study area The study area incorporates part of north Hertfordshire, south and mid- Bedfordshire as well as the southwest corner of Cambridgeshire and lies approximately 40 km north of London (Figure 1.1). Coverage of the area by British Geological Survey (BGS) 1:50,000 map sheets is shown in Figure 2.1. 2.2. Bedrock geology The strikes of the solid geological formations are approximately northeast- southwest across the study area (Figure 2.2). The solid geological succession is shown in Table 2.1. To the northwest of the Chiltern Hills the Gault Clay forms a rich agricultural landscape, representing a continuation of the Vale of Aylesbury. Beyond this, running approximately from Bow Brickhill (SP915343) to Gamlingay (TL234525) is a discontinuous ridge formed by the Woburn Sands Formation, part of the Lower Greensand. This prominent ‘Greensand Ridge’, rising to 170 m O.D. at Bow Brickhill, separates the Cretaceous clays from the Jurassic Oxford and Ampthill Clays to the northwest. The oldest formation is recorded in a borehole (TL23NE1) at Ashwell (TL286390), where Devonian strata were reached at a depth of 186.54 m, i.e. 93 m below O.D. (Smith, 1992). Lying just beyond the northern boundary of the present study area, north of the River Ouse, a borehole (TL15NE2) at Wyboston (TL175572) penetrated Ordovician rocks of Tremadoc age at a depth of approximately 230 m (Moorlock et al ., 2003). The Oxford Clay of the Upper Jurassic represents the oldest formation outcropping within the study area. -
Is Our Understanding of Santana Group Pterosaur Diversity Biased by Poor Biological and Stratigraphic Control?
Anhanguera taxonomy revisited: is our understanding of Santana Group pterosaur diversity biased by poor biological and stratigraphic control? Felipe L. Pinheiro1 and Taissa Rodrigues2 1 Laboratório de Paleobiologia, Universidade Federal do Pampa, São Gabriel, RS, Brazil 2 Departamento de Ciências Biológicas, Universidade Federal do Espírito Santo, Vitória, ES, Brazil ABSTRACT Background. Anhanguerids comprise an important clade of pterosaurs, mostly known from dozens of three-dimensionally preserved specimens recovered from the Lower Cretaceous Romualdo Formation (northeastern Brazil). They are remarkably diverse in this sedimentary unit, with eight named species, six of them belonging to the genus Anhanguera. However, such diversity is likely overestimated, as these species have been historically diagnosed based on subtle differences, mainly based on the shape and position of the cranial crest. In spite of that, recently discovered pterosaur taxa represented by large numbers of individuals, including juveniles and adults, as well as presumed males and females, have crests of sizes and shapes that are either ontogenetically variable or sexually dimorphic. Methods. We describe in detail the skull of one of the most complete specimens referred to Anhanguera, AMNH 22555, and use it as a case study to review the diversity of anhanguerids from the Romualdo Formation. In order to accomplish that, a geometric morphometric analysis was performed to assess size-dependent characters with respect to the premaxillary crest in the 12 most complete skulls bearing crests that are referred in, or related to, this clade, almost all of them analyzed first hand. Results. Geometric morphometric regression of shape on centroid size was highly Submitted 4 January 2017 statistically significant (p D 0:0091) and showed that allometry accounts for 25.7% Accepted 8 April 2017 Published 4 May 2017 of total shape variation between skulls of different centroid sizes. -
Pterosaur Distribution in Time and Space: an Atlas 61
Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W. -
Review of the Pterodactyloid Pterosaur Coloborhynchus 219
Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Pa lä on to lo gie und Geologie B28 DAVID W. E. HONE & ERIC BUFFETAUT (Eds) Flugsaurier: pterosaur papers in honour of Peter Wellnhofer CONTENTS/INHALT Dedication 3 PETER WELLNHOFER A short history of pterosaur research 7 KEVIN PADIAN Were pterosaur ancestors bipedal or quadrupedal?: Morphometric, functional, and phylogenetic considerations 21 DAVID W. E. HONE & MICHAEL J. BENTON Contrasting supertree and total-evidence methods: the origin of the pterosaurs 35 PAUL M. BARRETT, RICHARD J. BUTLER, NICHOLAS P. EDWARDS & ANDREW R. MILNER Pterosaur distribution in time and space: an atlas 61 LORNA STEEL The palaeohistology of pterosaur bone: an overview 109 S. CHRISTOPHER BENNETT Morphological evolution of the wing of pterosaurs: myology and function 127 MARK P. WITTON A new approach to determining pterosaur body mass and its implications for pterosaur fl ight 143 MICHAEL B. HABIB Comparative evidence for quadrupedal launch in pterosaurs 159 ROSS A. ELGIN, CARLOS A. GRAU, COLIN PALMER, DAVID W. E. HONE, DOUGLAS GREENWELL & MICHAEL J. BENTON Aerodynamic characters of the cranial crest in Pteranodon 167 DAVID M. MARTILL & MARK P. WITTON Catastrophic failure in a pterosaur skull from the Cretaceous Santana Formation of Brazil 175 MARTIN LOCKLEY, JERALD D. HARRIS & LAURA MITCHELL A global overview of pterosaur ichnology: tracksite distribution in space and time 185 DAVID M. UNWIN & D. CHARLES DEEMING Pterosaur eggshell structure and its implications for pterosaur reproductive biology 199 DAVID M. MARTILL, MARK P. WITTON & ANDREW GALE Possible azhdarchoid pterosaur remains from the Coniacian (Late Cretaceous) of England 209 TAISSA RODRIGUES & ALEXANDER W. -
New Information on the Tapejaridae (Pterosauria, Pterodactyloidea) and Discussion of the Relationships of This Clade
AMEGHINIANA (Rev. Asoc. Paleontol. Argent.) - 41 (4): 521-534. Buenos Aires, 30-12-2004 ISSN 0002-7014 New information on the Tapejaridae (Pterosauria, Pterodactyloidea) and discussion of the relationships of this clade Alexander Wilhelm Armin KELLNER1 Abstract. A phylogenetic analysis indicates that the Tapejaridae is a monophyletic group of pterodactyloid pterosaurs, diagnosed by the following synapomorphies: premaxillary sagittal crest that starts at the anterior tip of the premaxilla and extends posteriorly after the occipital region, large nasoantorbital fenestra that reaches over 45% of the length between premaxilla and squamosal, lacrimal process of the jugal thin, distinct small pear- shaped orbit with lower portion narrow, and broad tubercle at the ventroposterior margin of the coracoid. Several cranial and postcranial characters indicate that the Tapejaridae are well nested within the Tapejaroidea, in sister group relationship with the Azhdarchidae. A preliminary study of the ingroup relationships within the Tapejaridae shows that Tupuxuara is more closely related to Thalassodromeus relative to Tapejara. At present tape- jarid remains have been found in the following deposits: Crato and Romualdo members of the Santana Formation (Aptian-Albian), Araripe Basin, Brazil; Jiufotang Formation (Aptian), Jehol Group of western Liaoning, China; and in the redbeds (Cenomanian) of the Kem Kem region, Morocco. An incomplete skull found in the Javelina Formation (Maastrichtian), Texas also shows several tapejarid features and might be a member of this clade. Although information is still limited, the present distribution of the Tapejaridae indicates that this clade of pterosaurs was not exclusive of Gondwana, and was more widespread than previously known. Resumen. NUEVA INFORMACIÓN SOBRE LOS TAPEJARIDAE (PTEROSAURIA, PTERODACTYLOIDEA) Y DISCUSIÓN SOBRE LAS RELACIONES DE ESTE CLADO. -
A New Species of Coloborhynchus (Pterosauria, Ornithocheiridae) from the Mid- Cretaceous of North Africa
Accepted Manuscript A new species of Coloborhynchus (Pterosauria, Ornithocheiridae) from the mid- Cretaceous of North Africa Megan L. Jacobs, David M. Martill, Nizar Ibrahim, Nick Longrich PII: S0195-6671(18)30354-9 DOI: https://doi.org/10.1016/j.cretres.2018.10.018 Reference: YCRES 3995 To appear in: Cretaceous Research Received Date: 28 August 2018 Revised Date: 18 October 2018 Accepted Date: 21 October 2018 Please cite this article as: Jacobs, M.L., Martill, D.M., Ibrahim, N., Longrich, N., A new species of Coloborhynchus (Pterosauria, Ornithocheiridae) from the mid-Cretaceous of North Africa, Cretaceous Research (2018), doi: https://doi.org/10.1016/j.cretres.2018.10.018. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. 1 ACCEPTED MANUSCRIPT 1 A new species of Coloborhynchus (Pterosauria, Ornithocheiridae) 2 from the mid-Cretaceous of North Africa 3 Megan L. Jacobs a* , David M. Martill a, Nizar Ibrahim a** , Nick Longrich b 4 a School of Earth and Environmental Sciences, University of Portsmouth, Portsmouth PO1 3QL, UK 5 b Department of Biology and Biochemistry and Milner Centre for Evolution, University of Bath, Bath 6 BA2 7AY, UK 7 *Corresponding author. Email address : [email protected] (M.L. -
Taxonomy of the Lonchodectidae (Pterosauria, Pterodactyloidea)
Proceedings of the Zoological Institute RAS Vol. 324, No. 1, 2020, pp. 41–55 10.31610/trudyzin/2020.324.1.41 УДК 568.182 Taxonomy of the Lonchodectidae (Pterosauria, Pterodactyloidea) A.O. Averianov Zoological Institute of the Russian Academy of Sciences, Universitetskaya Emb. 1, 199034 Saint Petersburg, Russia; e-mail: [email protected], [email protected] ABSTRACT The pterodactyloid family Lonchodectidae includes three genera, Lonchodectes Hooley, 1914, Lonchodraco Rodrigues et Kellner, 2013, and Ikrandraco Wang et al., 2014, and four species, Lonchodectes compressirostris (Owen, 1851), Lonchodraco giganteus (Bowerbank, 1846), Ikrandraco avatar Wang et al., 2014, and Ikrandraco machaerorhynchus (Seeley, 1870) comb. nov. [=Ornithocheirus microdon Seeley, 1870 syn. nov.]. The holotype of Lonchodectes compressirostris (NHMUK PV 39410) consists of two fragments of the anterior rostrum, not the mandibular and rostrum fragments as was supposed previously. The difference between Lonchodectes and Ikrandraco is not clear and the taxa could be synonyms. The diagnostic characters for the Lonchodectidae are the presence of the palatal ridge, elevated alveolar margin of the upper and lower jaws, small teeth that are not varying in size, and a prominent mandibular crest (unknown for Lonchodectes). The family includes taxa with long and low rostrum and prominent mandibular crest (Ikrandraco and, possibly, Lonchodectes), or with both premaxil lary and mandibular crests (Lonchodraco). Various phylogenetic analyses place the Lonchodectidae within the Ornithocheiroidea, frequently as a sister taxon to the Anhangueria. The family is known from the midCretaceous (AlbianTuronian) of England (Lonchodectes compressirostris, Lonchodraco giganteus, Ikrandraco machaero- rhynchus), the Lower Cretaceous (Aptian) of China (Ikrandraco avatar), and the Late Cretaceous (Cenomanian) of European Russia (Lonchodraco (?) sp.).