Brenda J. Chinnery

Total Page:16

File Type:pdf, Size:1020Kb

Brenda J. Chinnery CURRICULUM VITAE Brenda Joan Chinnery-Allgeier E-Mail: [email protected] Education 1995-2002 Ph.D., Functional Anatomy and Evolution Program, Johns Hopkins University School of Medicine, Baltimore, MD. Thesis title: Morphometric analysis of evolution and growth in the ceratopsian postcranial skeleton. 1991-1995 BA, Physical Anthropology, University of Colorado, Boulder, CO. Professional Employment 2007-present Research Scientist, Denver Museum of Nature and Science, Denver, Colorado. 2007 Scientific Consultant, exhibit Return of the Dino’s: Extreme Makeover, Witte Museum, San Antonio, Texas. 2004-present Lecturer, School of Biological Sciences, University of Texas, Austin, Texas. 2002-present Research Associate, Museum of the Rockies, Bozeman, Montana. 2002-2003 Postdoctoral Fellow, Museum of the Rockies, Montana State University, Bozeman, Montana. 2001-2002 Teaching Associate, University of Texas Health Science Center, San Antonio, Texas. 2000-2001 Museum exhibit research and design, Maryland Science Center, Baltimore, Maryland. Grants, Awards, and Honors 1999 Research grant, Jurassic Foundation 1999 Research grant, Paleobiological Fund 1999 Research grant, Geological Society of America 1999 Predoctoral Fellowship, Society of Vertebrate Paleontology 1998 Research grant, Sigma Xi 1997 Research grant, Western Interior Paleontological Society 1995-2000 Graduate Fellowship, Johns Hopkins University School of Medicine 1995 General and Departmental honors, University of Colorado, Boulder CO Research and Field Experience 2006-present Field research of Eocene mammals and lower vertebrates, Wyoming. Principal Investigator: Dr. Richard Stucky, Denver Museum of Nature and Science, Denver, CO. 2004 Field research in the Cretaceous of Texas. Principal Investigator: Rebecca Hunt, Texas Tech University, Lubbock, TX. 2002-present Postdoctoral research on 3-dimensional laser scanning and morphometric methodology with John Horner, Museum of the Rockies, Montana State University, Bozeman, MT. 2002 Field research in the Moenkopi Formation of Arizona. Principal Investigator: Sterling Nesbitt, University of Texas, Austin, TX. 2002 Field research in the Hell Creek Formation of Montana. Principal Investigator: John Horner, Museum of the Rockies, Montana State University, Bozeman, MT. 1999-present Ongoing collection and research of middle Cretaceous vertebrate fossils in the Moreno Hill Formation of New Mexico. Principal Investigator: Douglas Wolfe, Mesa Museum, Phoenix, AZ. 1996 Field research of Eocene aged mammals, Wyoming. Principal Investigator: Dr. Ken Rose, Johns Hopkins University School of Medicine, Baltimore, MD. 1995-1996 Research rotation at Johns Hopkins University School of Medicine with Dr. David Weishampel consisting of the description and cladistic analysis of a specimen of Montanoceratops cerorhynchus. 1995 Research on Mesohippus sp. skull, under the supervision of Dr. Bert Covert, University of Colorado, Boulder, CO. and Dr. Richard Stucky, Denver Museum of Nature and Science, Denver, CO. 1995 Field research of Eocene aged mammals, Wyoming. Principal Investigator: Dr. Richard Stucky, Denver Museum of Nature and Science, Denver, CO. 1994-1995 Field research of Eocene and Oligocene aged mammals, Badlands National Park, South Dakota. Principal Investigator: Dr. Richard Stucky, Denver Museum of Nature and Science, Denver, CO. 1994-1995 Research assistant to Dr. Richard Stucky, Department of Earth Sciences, Denver Museum of Nature and Science, Denver, CO. 1994 Field Paleontology Course through the University of Colorado, Denver, CO., taught by Dr. Richard Stucky, Denver Museum of Nature and Science, Denver, CO. 1994 Field research of dinosaur remains, Canon City, CO. Principal Investigator: Dr. Ken Carpenter, Denver Museum of Nature and Science, Denver, CO. 1993-1994 Internship under Dr. Ken Carpenter, Paleontological Preparation Laboratory, Denver Museum of Nature and Science, Denver, CO. 1993 Volunteer research assistant to Dr. Peter Robinson, Geology Museum Lab, University of Colorado, Boulder, CO. Outreach experience 2010 Scientific Seminar: Can We Bring a Dinosaur Back to Life? And Other Questions that Paleontologists are Asking Today; Odyssey Adult Enrichment Classes, University of Texas, Austin, TX. 2010 Classroom presentation: Dinosaurs and Paleontology; all kindergarten classes; Cowan Elementary School, Austin, TX. 2010 Classroom presentation: Dinosaurs and Paleontology; pre-kindergarten classes; The University of Texas Child Development Center, Austin, TX. 2009 Classroom presentation: How Paleontology is done; pre-kindergarten classes; The University of Texas Child Development Center, Austin, TX. 2007 Display booth of fossils, skeletons at Explore UT: Austin’s Biggest Open House, University of Texas, Austin, TX. 2007 Media presentation on Triceratops sp. for exhibit “Return of the Dino’s: Extreme Makeover”, Witte Museum, San Antonio, TX. 2003 Scientific seminar: What Questions Museum Visitors are Asking Today; to volunteers at the Museum of the Rockies, Bozeman, MT. 2002 Scientific seminar: Functional Anatomy; Department of Neurobiology and Anatomy, University of Texas Health Science Center, Houston, TX. 2002 Scientific seminar: Department of Cell Biology and Anatomy, University of Texas Health Science Center, San Antonio, TX. 2002 Scientific seminar: Department of Geology, College of Eastern Utah, Price, UT. Publications 2010 Chinnery, B. J. and J. I. Kirkland. An Update on the Paleobiogeography of Ceratopsian Dinosaurs. In M. Ryan, B. J. Chinnery-Allgeier, and D. Eberth, eds., New Perspectives on Horned Dinosaurs, pp. 387-404. Indiana University Press, Bloomington IL. 2010 Miyashita, T., P.J. Currie, and B. Chinnery-Allgeier. First Basal Neoceratopsian from the Oldman Formation (Belly River Group) Southern Alberta. In M. Ryan, B. J. Chinnery-Allgeier, and D. Eberth, eds., New Perspectives on Horned Dinosaurs, pp. 83-90. Indiana University Press, Bloomington IL. 2010 Wolfe, D., J. I. Kirkland, D. Smith, K. Poole, B. Chinnery-Allgeier and A. McDonald. Zuniceratops christopheri; The North American Ceratopsid Sister Taxon Reconstructed on the Basis of New Data. In M. Ryan, B. J. Chinnery- Allgeier, and D. Eberth, eds., New Perspectives on Horned Dinosaurs, pp. 91- 98. Indiana University Press, Bloomington IL. 2007 Chinnery, B. J. and J. R. Horner. A new neoceratopsian dinosaur linking North American and Asian taxa. Journal of Vertebrate Paleontology 27:625-641. 2004 Rose, K. D. and B. J. Chinnery. The postcranial skeleton of early Eocene rodents. Bulletin of the Carnegie Museum of Natural History 36:211-244. 2004 Chinnery, B. J. Morphometric analysis of evolutionary trends in the ceratopsian postcranial skeleton. Journal of Vertebrate Paleontology 24:591- 609. 2004 Chinnery, B. J. Description of Prenoceratops piikanis gen. et. Sp. Nov. (Dinosauria: Neoceratopsia) from the Two Medicine Formation of Montana. Journal of Vertebrate Paleontology 24:572-590. 1998 Chinnery, B. J. and D. B. Weishampel. Montanoceratops cerorhynchus (Dinosauria: Ceratopsia) and relationships among basal neoceratopsians. Journal of Vertebrate Paleontology 18:569-585. 1998 Chinnery, B. J., T. R. Lipka, J. I. Kirkland, J. M. Parrish, and M. K. Brett- Surman. Neoceratopsian teeth from the Lower to middle Cretaceous of North America. In: Lucas, S. G., J. I. Kirkland and J. W. Estep (eds.), Lower and Middle Cretaceous Terrestrial Ecosystems. New Mexico Museum of Natural History and Science Bulletin No. 14. Pp. 297-302. Professional Meeting Presentations 2010 Stucky, R., I. Miller, B. Chinnery-Allgeier and B. Dodge. Teen Science Scholars at the Denver Museum of Nature and Science: Nurturing the Next Generation of Scientific Leaders. 2010 GSA Denver Annual Meeting (31 October –3 November 2010) Paper No. 181-9. 2009 Chinnery, B. J. and R. Stucky. Diversity of Lower Vertebrates across the Early Eocene Climatic Optimum. Journal of Vertebrate Paleontology 29:77A. 2007 Chinnery, B. J. and J. I. Kirkland. Neoceratopsian biogeography: what’s changed in the last ten years. Ceratopsian Symposium Abstracts and Short Papers. 2007 Douglas G. Wolfe, James I. Kirkland, David Smith, Karen Poole, Brenda Chinnery- Allgeier & Andrew McDonald. Zuniceratops christopheri: an update on the North North American ceratopsid sister taxon, Zuni Basin, west-central New Mexico. Ceratopsian Symposium Abstracts and Short Papers. 2007 Chinnery, B. J. Wrap-up and Prospectus. Ceratopsian Symposium Abstracts and Short Papers. 2007 Chinnery, B. J., R. Stucky, and T. Hardy. Comparison of lower vertebrate faunas from the Bridger and Wind River Formations (Early to middle Eocene), Wyoming. Journal of Vertebrate Paleontology, 27:58A. 2003 Chinnery, B. J. and J. R. Horner. New basal neoceratopsian from the Two Medicine Formation of Montana provides a link between Asian and North American taxa. Journal of Vertebrate Paleontology, 23:40A. 2002 Chinnery, B. J. Morphometric analysis of evolution and growth in the ceratopsian postcranial skeleton. Journal of Vertebrate Paleontology, 22:43A. 2000 Chinnery, B. J. and K. D. Rose. Early Eocene rodent postcrania from the Willwood Formation. Journal of Vertebrate Paleontology, 20:35A. 1999 Chinnery, B. J. and D. Trexler. The first bone bed occurrence of a basal neoceratopsian, with new information on the skull morphology of Leptoceratops. Journal of Vertebrate Paleontology 19:38A. 1998 Chinnery, B. J. and R. E. Chapman. A morphometric study of the ceratopsid postcranial skeleton. Journal of Vertebrate Paleontology, 18:33A. 1998 Chinnery, B. J., D. G.
Recommended publications
  • Soil Survey and Reclamation Suitability Evaluation of the Proposed Nova Gas Transmission Ltd
    NOVA Gas Transmission Ltd. Environmental and Socio-Economic Assessment Norma Transmission Pipeline Project February 2013/8660 APPENDIX 3 SOIL SURVEY AND RECLAMATION SUITABILITY EVALUATION OF THE PROPOSED NOVA GAS TRANSMISSION LTD. NORMA TRANSMISSION PIPELINE PROJECT Page A3-1 SOIL SURVEY AND RECLAMATION SUITABILITY EVALUATION of the PROPOSED NOVA GAS TRANSMISSION LTD. NORMA TRANSMISSION PIPELINE Prepared for: TERA ENVIRONMENTAL CONSULTANTS On behalf of: NOVA GAS TRANSMISSION LTD. Prepared by: MENTIGA PEDOLOGY CONSULTANTS LTD. A.G. Twardy, M.Sc., P.Ag. B. Chernipeski, B.Sc., P.Ag. February 2013 11037B.1 TABLE OF CONTENTS 1.0 INTRODUCTION ............................................................................................................. 1 2.0 THE STUDY AREA .......................................................................................................... 3 2.1 Location and Extent ............................................................................................ 3 2.2 Bedrock Geology ................................................................................................ 3 2.3 Surficial Materials and Landform ........................................................................ 3 2.4 General Soil Patterns .......................................................................................... 4 2.5 Present Land Use ............................................................................................... 4 3.0 SOILS ...................................................................................................................
    [Show full text]
  • Post-Carboniferous Stratigraphy, Northeastern Alaska by R
    Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ----------------------------------
    [Show full text]
  • Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area
    ERCB/AGS Special Report 093 Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Subsurface Characterization of the Pembina-Wabamun Acid-Gas Injection Area Stefan Bachu Maja Buschkuehle Kristine Haug Karsten Michael Alberta Geological Survey Alberta Energy and Utilities Board ©Her Majesty the Queen in Right of Alberta, 2008 ISBN 978-0-7785-6950-3 The Energy Resources Conservation Board/Alberta Geological Survey (ERCB/AGS) and its employees and contractors make no warranty, guarantee or representation, express or implied, or assume any legal liability regarding the correctness, accuracy, completeness or reliability of this publication. Any digital data and software supplied with this publication are subject to the licence conditions. The data are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation, and/or any use of proprietary data formats in this release, do not constitute endorsement by the ERCB/AGS of any manufacturer's product. If this product is an ERCB/AGS Special Report, the information is provided as received from the author and has not been edited for conformity to ERCB/AGS standards. When using information from this publication in other publications or presentations, due acknowledgment should be given to the ERCB/AGS. The following reference format is recommended: Bachu, S., Buschkuehle, M., Haug, K., Michael, K. (2008): Subsurface characterization of the Pembina-Wabamun acid-gas injection area; Energy Resources Conservation Board, ERCB/AGS Special Report 093, 60 p.
    [Show full text]
  • A Battering Ram?
    A Battering Ram? All evidence suggests that Pachycephalosaur skulls were built to withstand extreme forces 9 inches of solid bone Bone organized in a radial arrangement- structural support Articulation btw back of skull and vertebrae oriented to transfer forces linearly Articulation btw back of skull and vertebral column built to withstand sideways forces Vertebral column has tongue and groove articulations Spinal column is an S-shaped shock absorber BUT There is no ‘locking’ mechanism on skull to keep battering heads aligned Some Pachycephalosaurs have imprinted blood vessels on dome These factors suggests that head- butting may not be likely Intraspecies Competition (typically male-male) Females are typically choosey Why? Because they have more to loose Common rule in biology: Females are expensive to lose, males are cheap (e.g. deer hunting) Females choose the male most likely to provide the most successful offspring Males compete with each other for access to female vs. female chooses the strongest male Choosey females // Strong males have more offspring => SEXUAL selection Many ways to do this... But: In general, maximize competition and minimize accidental deaths (= no fitness) http://www.youtube.com/watch?v=PontCXFgs0M http://www.metacafe.com/watch/1941236/giraffe_fight/ http://www.youtube.com/watch? http://www.youtube.com/watch?v=DYDx1y38vGw http://www.youtube.com/watch?v=ULRtdk-3Yh4 Air-filled horn cores vs. solid bone skull caps... Gotta have a cheezy animated slide. Homalocephale Pachycephalosaurus Prenocephale Tylocephale Stegoceras Head butting Pachycephalosaurs Bone structure was probably strong enough to withstand collision Convex nature would favor glancing blows Instead, dome and spines seem better suited for “flank butting” So..
    [Show full text]
  • 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.
    [Show full text]
  • 2.2.2. Ceratopsia
    Evolution der Dinosaurier Ornithischia (Vogelbecken) Ein Beitrag von Ralf Krüger 2. Cerapoda (2) 2.2.2. Ceratopsia Die Vertreter der Ceratopsia gehören zu pflanzenfressenden (herbivore) Dinosaurier. Sie besaßen häufig einen Nackenschild und /oder Hörner. Die Vorderbeine waren stets kürzer als die Hinterbeine. Die Ceratopsia enthielten die Familien der Neoceratopsia, die der Psittacosauridae und die der Ceratopsidae. 2.2.2.1. Neoceratopsia Die Neoceratopsia liefen sowohl biped als auch quadruped. Sie waren mit wenigen Ausnahmen nur 0,5 bis 3 Meter lang. Yinlong (urtümlicher Ceratopsia) Zeit: Jura 163-157 Fundort: Yinlong, China Länge: 1,2 m Höhe: 0,4 Gewicht: 30 kg Rekonstruktionsbild vom Yinglong Quelle: Nobu Tamura (CC BY-SA 3.0) Chaoyangsaurus Zeit: Jura 160-145 Fundort: Chaoyang, China Länge: 1,5 m Höhe: 0,5 m Gewicht: 40 kg Rekonstruktionsbild vom Chaoyangsaurus Quelle: Nobu Tamura (CC BY-SA 3.0) Archaeoceratops Zeit: Kreide 126-113 Fundort: Gansu, China Länge: 1,3 m Höhe: 0,4 m Gewicht: 35 kg Rekonstruktionsbild vom Archaeoceratops Quelle: Nobu Tamura (CC BY-SA 3.0) Auroraceratops Zeit: Kreide 126-113 Fundort: Gansu, China Länge: 5,5 m Höhe: 2 m Gewicht: 650 kg Rekonstruktionsbild vom Auroraceratops Quelle: Nobu Tamura (CC BY-SA 3.0) GSE-Team 2016 Seite 1 von 9 © Ralf Krüger Evolution der Dinosaurier Ornithischia (Vogelbecken) Ein Beitrag von Ralf Krüger Liaoceratops Zeit: Kreide 139-128 Fundort: Liaoning, China Länge: 1 m Höhe: 0,3 m Gewicht: 20 kg Rekonstruktionsbild vom Liaoceratops Quelle: Nobu Tamura (CC BY-SA 3.0) Yamaceratops
    [Show full text]
  • Bedrock Geology of Alberta
    Alberta Geological Survey Map 600 Legend Bedrock Geology of Alberta Southwestern Plains Southeastern Plains Central Plains Northwestern Plains Northeastern Plains NEOGENE (± PALEOGENE) NEOGENE ND DEL BONITA GRAVELS: pebble gravel with some cobbles; minor thin beds and lenses NH HAND HILLS FORMATION: gravel and sand, locally cemented into conglomerate; gravel of sand; pebbles consist primarily of quartzite and argillite with minor amounts of sandstone, composed of mainly quartzite and sandstone with minor amounts of chert, arkose, and coal; fluvial amygdaloidal basalt, and diabase; age poorly constrained; fluvial PALEOGENE PALEOGENE PALEOGENE (± NEOGENE) PALEOGENE (± NEOGENE) UPLAND GRAVEL: gravel composed of mainly white quartzite cobbles and pebbles with lesser amounts of UPLAND GRAVEL: gravel capping the Clear Hills, Halverson Ridge, and Caribou Mountains; predominantly .C CYPRESS HILLS FORMATION: gravel and sand, locally cemented to conglomerate; mainly quartzite .G .G and sandstone clasts with minor chert and quartz component; fluvial black chert pebbles; sand matrix; minor thin beds and lenses of sand; includes gravel in the Swan Hills area; white quartzite cobbles and pebbles with lesser amounts of black chert pebbles; quartzite boulders occur in the age poorly constrained; fluvial Clear Hills and Halverson Ridge gravels; sand matrix; ages poorly constrained; extents poorly defined; fluvial .PH PORCUPINE HILLS FORMATION: olive-brown mudstone interbedded with fine- to coarse-grained, .R RAVENSCRAG FORMATION: grey to buff mudstone
    [Show full text]
  • Map 600: a New 1:1 000 000 Bedrock Geology Map of Alberta G.J
    Map 600: A New 1:1 000 000 Bedrock Geology Map of Alberta G.J. Prior*, Alberta Geological Survey, 402, 4999-98th Ave., Edmonton, Alberta [email protected] B. Hathway, Alberta Geological Survey, 402, 4999-98th Ave., Edmonton, Alberta P. Glombick, Alberta Geological Survey, 402, 4999-98th Ave., Edmonton, Alberta D.I. Pana, Alberta Geological Survey, 402, 4999-98th Ave., Edmonton, Alberta C.J. Banks, Alberta Geological Survey, 402, 4999-98th Ave., Edmonton, Alberta D.C. Hay, Neftex Petroleum Consultants, 97 Milton Park, Abingdon, Oxfordshire, England C.L. Schneider, University of Alberta, 116 St. and 85 Ave., Edmonton, Alberta M. Grobe, Alberta Geological Survey, 402, 4999-98th Ave, Edmonton, Alberta R. Elgr, Alberta Geological Survey, 402, 4999-98th Ave, Edmonton, Alberta J.A. Weiss, Alberta Geological Survey, 402, 4999-98th Ave, Edmonton, Alberta Summary Map 600 is the new 1:1 000 000 bedrock geology map of Alberta prepared by the Alberta Geological Survey (AGS). This map supersedes Map 236 (Hamilton et al., 1999) and Map 27 (Green, 1972). Map 600 represents the compilation of existing geological maps and new geological mapping by staff of the Alberta Geological Survey (AGS). The representation of the Canadian Shield and Athabasca Basin is based on compilation. The geology of the Rocky Mountains and the Rocky Mountain Foothills is also the product of compilation with rare instances of new geological interpretation (e.g. the interpretation of bedrock geology beneath drift-filled valleys). The Devonian geology of northeast Alberta is also largely a product of compilation with some reinterpretation based, in part, on field observations.
    [Show full text]
  • Download a PDF of This Web Page Here. Visit
    Dinosaur Genera List Page 1 of 42 You are visitor number— Zales Jewelry —as of November 7, 2008 The Dinosaur Genera List became a standalone website on December 4, 2000 on America Online’s Hometown domain. AOL closed the domain down on Halloween, 2008, so the List was carried over to the www.polychora.com domain in early November, 2008. The final visitor count before AOL Hometown was closed down was 93661, on October 30, 2008. List last updated 12/15/17 Additions and corrections entered since the last update are in green. Genera counts (but not totals) changed since the last update appear in green cells. Download a PDF of this web page here. Visit my Go Fund Me web page here. Go ahead, contribute a few bucks to the cause! Visit my eBay Store here. Search for “paleontology.” Unfortunately, as of May 2011, Adobe changed its PDF-creation website and no longer supports making PDFs directly from HTML files. I finally figured out a way around this problem, but the PDF no longer preserves background colors, such as the green backgrounds in the genera counts. Win some, lose some. Return to Dinogeorge’s Home Page. Generic Name Counts Scientifically Valid Names Scientifically Invalid Names Non- Letter Well Junior Rejected/ dinosaurian Doubtful Preoccupied Vernacular Totals (click) established synonyms forgotten (valid or invalid) file://C:\Documents and Settings\George\Desktop\Paleo Papers\dinolist.html 12/15/2017 Dinosaur Genera List Page 2 of 42 A 117 20 8 2 1 8 15 171 B 56 5 1 0 0 11 5 78 C 70 15 5 6 0 10 9 115 D 55 12 7 2 0 5 6 87 E 48 4 3
    [Show full text]
  • Sexual Selection and Macroevolution
    Morphology and Evolution of the Ceratopsian Skull Andrew Knapp Submitted in partial fulfilment of the requirements of the Degree of Doctor of Philosophy School of Biological and Chemical Sciences Queen Mary University of London September 2019 Appendix A: Required statement of originality for inclusion in research degree theses I, Andrew Knapp, confirm that the research included within this thesis is my own work or that where it has been carried out in collaboration with, or supported by others, that this is duly acknowledged below and my contribution indicated. Previously published material is also acknowledged below. I attest that I have exercised reasonable care to ensure that the work is original, and does not to the best of my knowledge break any UK law, infringe any third party’s copyright or other Intellectual Property Right, or contain any confidential material. I accept that the College has the right to use plagiarism detection software to check the electronic version of the thesis. I confirm that this thesis has not been previously submitted for the award of a degree by this or any other university. The copyright of this thesis rests with the author and no quotation from it or information derived from it may be published without the prior written consent of the author. Signature: Andrew Knapp Date: 24th September 2019 1 Details of collaboration and publications: Publications arising from this thesis: Knapp A, Knell RJ, Farke AA, Loewen MA and Hone DWE (2018). Patterns of divergence in the morphology of ceratopsian dinosaurs: sympatry is not a driver of divergence. Proc. R.
    [Show full text]
  • Ankylosaur and Theropod Coevolution Dinosauriekrig: Samevolution Hos Ankylosaurier Och Theropoder
    Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 401 Dinosaur Warfare: Ankylosaur and Theropod Coevolution Dinosauriekrig: samevolution hos ankylosaurier och theropoder Christopher Freer INSTITUTIONEN FÖR GEOVETENSKAPER DEPARTMENT OF EARTH SCIENCES Examensarbete vid Institutionen för geovetenskaper Degree Project at the Department of Earth Sciences ISSN 1650-6553 Nr 401 Dinosaur Warfare: Ankylosaur and Theropod Coevolution Dinosauriekrig: samevolution hos ankylosaurier och theropoder Christopher Freer ISSN 1650-6553 Copyright © Christopher Freer Published at Department of Earth Sciences, Uppsala University (www.geo.uu.se), Uppsala, 2017 Abstract Dinosaur Warfare: Ankylosaur and Theropod Coevolution Christopher Freer Ankylosauria is a clade of armoured dinosaurs that, throughout the Mesozoic, demonstrates divergent evolution of defensive traits, between the robust spikes and osteoderms of nodosaurids to the ankylosaurid tail clubs and lightweight armour. One of the longer-standing hypotheses, which is supported by histological data, stipulates that armament was a direct result of a predator-prey relationship between theropods and ankylosaurians. Such a hypothesis predicts that predatory pressures from Theropoda drive the evolution of armament. Here we investigate the coevolutionary hypothesis in a phylogenetic context by searching for reciprocal selection and clade interactions. We undertake two separate analyses. The first is a host-parasite test (ParaFit), which tests, within a phylogenetic framework, the null hypothesis that the evolutionary history of two groups was independent. The second produced principal coordinates from 30 ankylosaurian armour-related traits and was correlated in a linear regression against theropod body mass. The analysis was conducted across 53 theropod species that were sympatric, within a geological formation, with 44 ankylosaur species.
    [Show full text]
  • Erratum To: Palaeoenvironmental Drivers of Vertebrate Community Composition in the Belly River Group (Campanian) of Alberta
    Cullen and Evans BMC Ecol (2017) 17:1 DOI 10.1186/s12898-016-0111-y BMC Ecology ERRATUM Open Access Erratum to: Palaeoenvironmental drivers of vertebrate community composition in the Belly River Group (Campanian) of Alberta, Canada, with implications for dinosaur biogeography Thomas M. Cullen1,2* and David C. Evans1,2 Erratum to: BMC Ecol (2016) 16:52 sensitivity has historically been difficult, as many species DOI 10.1186/s12898-016-0106-8 were collected with only limited geological data or strati- After publication of the original article [1], it was graphic information, and were known by very low sample brought to our attention that the phrase ‘a lack of sensi- sizes [24, 43, 47], though ongoing work relocating these tivity to subtle environmental gradients casts doubt on sites and incorporating them into the broader stratigra- these forces acting as a driver of putative endemism of phy is ameliorating some of these issues [23, 24, 43, 44, dinosaur populations in the Late Cretaceous of North 48]’ in “Background” section should read ‘the ability to America’ in “Conclusion” section should read ‘a lack of test hypotheses about dinosaur biogeography, endemism, sensitivity to subtle environmental gradients casts doubt and environmental sensitivity has historically been diffi- on these forces acting as a driver of altitudinal zonation cult, as many specimens were collected with only limited of dinosaur communities in the Late Cretaceous of North geological data or stratigraphic information, and known America’. by very low sample sizes [24, 43, 47], though ongoing The phrase ‘this hypothesis is based on the resilience to work collecting new specimens, relocating these sites, environmental variation and broad latitudinal distribu- and incorporating them into the broader stratigraphy is tions seen in many groups of large mammals today [2, 7, ameliorating some of these issues [23, 24, 43, 44, 48]’.
    [Show full text]