Animantarx Ramaljonesi Armor-Plated Ankylosaurs Skeletons: Gastonia Bur- a Similar System

Total Page：16

File Type：pdf, Size：1020Kb

Animantarx Ramaljonesi Armor-Plated Ankylosaurs Skeletons: Gastonia Bur- a Similar System

e Prehistoric Museum is home to three mounted Many herbivores, such as elephants and cows, have Animantarx ramaljonesi armor-plated ankylosaurs skeletons: Gastonia bur- a similar system. gei, Animantarx ramaljonesi, and Peloroplites ced- romontanus. ese skeletons were collected within 150 miles of the museum. ey lived 130-100 million years ago, making eastern Utah one of the rich- est places for Early Cretaceous ankylosaurs. eir descendants became extinct 66 million years ago during the Great Dinosaur Die-o . Ankylosaurs were four-legged, heavily armored dinosaurs. is armor consisted of spines or spikes along the sides of the neck, body and tail, and vari- Animantarx is the rst dinosaur to be discovered ous sized keeled plates over the rest of the body. One by technology alone. Dinosaur bones are slightly Scienti c Name: Animantarx ramaljonesi group, called the ankylosaurids, had large plates radioactive and in 1999, Ramal Jones, a retired Uni- Pronounced: AN-ih-MAN-tarks that fused together to make a club on the end of versity of Utah radiologist, used a sensitive Geiger Name Meaning: “living fortress” the tail. Even the belly of ankylosaurs was armored, counter to accidentally discover the bones just be- Time Period: 102 to 99 Million Years Ago (MYA) with marble-sized bone. Ankylosaur armor formed low the ground surface.. Early Cretaceous in the skin like it does in crocodiles. Length: 10 feet Not much is known about Animantarx consider- Height: 3 1/2 feet ing that this is the only specimen known and not Weight: 1,000 pounds all of the skeleton was found. Ray Jones found the Diet: Herbivore lower jaw, the back half of the skull, vertebrae from Places Found: Utah the neck and back and parts of both front and hind Discoverer: Prehistoric Museum legs. ese bones were enough to identify the lit- tle dinosaur as related to the gigantic Peloroplites. Both belong to the family Nodosauridae, the group of armoured dinosaurs characterized by a peculiar shoulder blade and no club on the end of the tail. Knowing this relationship, we can infer that Ani- mantarx had rows of bone plates or armor embed- e teeth are small for the size of the head and are ded in its skin. Also, that it was a plant eater although 155 East Main Street best suited for eating plants. To help digest their we do not have its teeth. is information was then Price, Utah food, ankylosaurs have a wide pelvis that holds used to reconstruct the rest of the skeleton, with the 435-637-5060 or 800-817-9949 an enormously large gut. Bacteria break down the missing bones modeled a er closely related species. usueastern.edu/museum plant, releasing the nutrients that are then absorbed. .

Copy Link

Recommended publications

And the Origin and Evolution of the Ankylosaur Pelvis
Pelvis of Gargoyleosaurus (Dinosauria: Ankylosauria) and the Origin and Evolution of the Ankylosaur Pelvis Kenneth Carpenter1,2*, Tony DiCroce3, Billy Kinneer3, Robert Simon4 1 Prehistoric Museum, Utah State University – Eastern, Price, Utah, United States of America, 2 Geology Section, University of Colorado Museum, Boulder, Colorado, United States of America, 3 Denver Museum of Nature and Science, Denver, Colorado, United States of America, 4 Dinosaur Safaris Inc., Ashland, Virginia, United States of America Abstract Discovery of a pelvis attributed to the Late Jurassic armor-plated dinosaur Gargoyleosaurus sheds new light on the origin of the peculiar non-vertical, broad, flaring pelvis of ankylosaurs. It further substantiates separation of the two ankylosaurs from the Morrison Formation of the western United States, Gargoyleosaurus and Mymoorapelta. Although horizontally oriented and lacking the medial curve of the preacetabular process seen in Mymoorapelta, the new ilium shows little of the lateral flaring seen in the pelvis of Cretaceous ankylosaurs. Comparison with the basal thyreophoran Scelidosaurus demonstrates that the ilium in ankylosaurs did not develop entirely by lateral rotation as is commonly believed. Rather, the preacetabular process rotated medially and ventrally and the postacetabular process rotated in opposition, i.e., lateral and ventrally. Thus, the dorsal surfaces of the preacetabular and postacetabular processes are not homologous. In contrast, a series of juvenile Stegosaurus ilia show that the postacetabular process rotated dorsally ontogenetically. Thus, the pelvis of the two major types of Thyreophora most likely developed independently. Examination of other ornithischians show that a non-vertical ilium had developed independently in several different lineages, including ceratopsids, pachycephalosaurs, and iguanodonts.
[Show full text]
Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal)
Alexandre Renaud Daniel Guillaume Licenciatura em Biologia celular Mestrado em Sistemática, Evolução, e Paleobiodiversidade Microvertebrates of the Lourinhã Formation (Late Jurassic, Portugal) Dissertação para obtenção do Grau de Mestre em Paleontologia Orientador: Miguel Moreno-Azanza, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Co-orientador: Octávio Mateus, Faculdade de Ciências e Tecnologia da Universidade Nova de Lisboa Júri: Presidente: Prof. Doutor Paulo Alexandre Rodrigues Roque Legoinha (FCT-UNL) Arguente: Doutor Hughes-Alexandres Blain (IPHES) Vogal: Doutor Miguel Moreno-Azanza (FCT-UNL) Júri: Dezembro 2018 MICROVERTEBRATES OF THE LOURINHÃ FORMATION (LATE JURASSIC, PORTUGAL) © Alexandre Renaud Daniel Guillaume, FCT/UNL e UNL A Faculdade de Ciências e Tecnologia e a Universidade Nova de Lisboa tem o direito, perpétuo e sem limites geográficos, de arquivar e publicar esta dissertação através de exemplares impressos reproduzidos em papel ou de forma digital, ou por qualquer outro meio conhecido ou que venha a ser inventado, e de a divulgar através de repositórios científicos e de admitir a sua cópia e distribuição com objetivos educacionais ou de investigação, não comerciais, desde que seja dado crédito ao autor e editor. ACKNOWLEDGMENTS First of all, I would like to dedicate this thesis to my late grandfather “Papi Joël”, who wanted to tie me to a tree when I first start my journey to paleontology six years ago, in Paris. And yet, he never failed to support me at any cost, even if he did not always understand what I was doing and why I was doing it. He is always in my mind. Merci papi ! This master thesis has been one-year long project during which one there were highs and lows.
[Show full text]
Notes for the Natural History of Dinosaurs 2
Notes for the Natural History of Dinosaurs 2 A word of warning. these notes are to give you the basic structural backbone for concepts in the course. This should help you study for the exam, but you should not study from it by itself. Make sure that you read the required chapters in the book, and study both your notes and the slides of the course that have been posted online. Exam 2 is in-class on Wednesday, March 07. Happy studying! Exam: Wednesday, March 07 Dinosauria Early dinosaurs • Saurischia vs. Ornithischia • Perforated acetabulum • Bipedal and carnivorous Ornithischia (basal) • Predentary, low jaw joint, inset cheek teeth, opisthopubic pelvis • Ossified tendons above sacral vertebrae (providing support for big guts) • Genosaurs = ‘Cheeky’-saurs. dinosaurs that chewed • The chewing process: Front teeth or ramphotheca (cropping); diastem (manipulation with tongue); inset cheek teeth (chewing and grinding), coronoid process (bite force) • Scissors-like chewing (carnivores) vs. angled chewing (herbivores) • Heterodontosaurus 3 kinds of teeth: snipping, chewing, and tusks for display Thyreophorans: Stegosauria • Basal forms are bipedal and small • Evolve large body sizes, become quadropeds w/ short stocky front legs and long back legs • Osteoderms (boney scutes) • Loss of ossified tendons • Hooved feet • Tall thoracic vertebrae. why??? • Diversification during the Jurassic • Diet – Narrow snout, low coronoid process (what does this mean?) – Small, leaf-shaped teeth spread out in jaw 1 – Lack of wear-surfaces – Chewing not a priority – No gastroliths – Wide vs. narrow snouts <==> specialized vs. generalized foraging – Median keel along palate. breathe while chewing! • Brains – Very small (0.001% of body mass) – Large olfactory gland.
[Show full text]
Competition Structured a Late Cretaceous Megaherbivorous Dinosaur Assemblage Jordan C
www.nature.com/scientificreports OPEN Competition structured a Late Cretaceous megaherbivorous dinosaur assemblage Jordan C. Mallon 1,2 Modern megaherbivore community richness is limited by bottom-up controls, such as resource limitation and resultant dietary competition. However, the extent to which these same controls impacted the richness of fossil megaherbivore communities is poorly understood. The present study investigates the matter with reference to the megaherbivorous dinosaur assemblage from the middle to upper Campanian Dinosaur Park Formation of Alberta, Canada. Using a meta-analysis of 21 ecomorphological variables measured across 14 genera, contemporaneous taxa are demonstrably well-separated in ecomorphospace at the family/subfamily level. Moreover, this pattern is persistent through the approximately 1.5 Myr timespan of the formation, despite continual species turnover, indicative of underlying structural principles imposed by long-term ecological competition. After considering the implications of ecomorphology for megaherbivorous dinosaur diet, it is concluded that competition structured comparable megaherbivorous dinosaur communities throughout the Late Cretaceous of western North America. Te question of which mechanisms regulate species coexistence is fundamental to understanding the evolution of biodiversity1. Te standing diversity (richness) of extant megaherbivore (herbivores weighing ≥1,000 kg) com- munities appears to be mainly regulated by bottom-up controls2–4 as these animals are virtually invulnerable to top-down down processes (e.g., predation) when fully grown. Tus, while the young may occasionally succumb to predation, fully-grown African elephants (Loxodonta africana), rhinoceroses (Ceratotherium simum and Diceros bicornis), hippopotamuses (Hippopotamus amphibius), and girafes (Girafa camelopardalis) are rarely targeted by predators, and ofen show indiference to their presence in the wild5.
[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]
Partial Skull and Endocranial Cast of the Ankylosaurian Dinosaur Hungarosaurus from the Late Cretaceous of Hungary: Implications for Locomotion
Palaeontologia Electronica palaeo-electronica.org Partial skull and endocranial cast of the ankylosaurian dinosaur Hungarosaurus from the Late Cretaceous of Hungary: implications for locomotion Attila Ősi, Xabier Pereda Suberbiola, and Tamás Földes ABSTRACT A partial skull of ankylosaur from the Upper Cretaceous (Santonian) Csehbánya Formation in Iharkút and the endocranial cast taken from it are described. The mor- phology of the exoccipital, the elongated ‘neck’ region of the basioccipital, the shape of the occipital condyle, and the different flexure of the medulla relative to the forebrain unambiguously differentiate this specimen from the basicranium of Struthiosaurus, so it is assigned to Hungarosaurus sp. Whereas the endocranial cast reflects a brain gener- ally similar to those of other ankylosaurs, the dorsally hypertrophied cerebellum (also present is Struthiosaurus transylvanicus) is quite unusual within the group suggesting a more sophisticated cerebral coordination of posture and movement, and perhaps a more cursorial locomotary habit than predicted for other ankylosaurs. Attila Ősi. Hungarian Academy of Sciences – Eötvös Loránd University, Lendület Dinosaur Research Group, Pázmány Péter sétány 1/c, Budapest, 1117, Hungary [email protected] Xabier Pereda Suberbiola. Universidad del País Vasco/Euskal Herriko Unibertsitatea, Facultad de Ciencia y Tecnología, Dpto. Estratigrafía y Paleontología, Apartado 644, 48080 Bilbao, Spain [email protected] Tamás Földes. Institute of Diagnostic Imaging and Radiation Oncology of the University of Kaposvár, Kaposvár, 7400 Guba S. 40, Hungary [email protected] Keywords: Santonian, Iharkút, Ankylosauria, Hungarosaurus, skull, endocranial cast INTRODUCTION gary, which includes disarticulated cranial bones (Ősi, 2005; Ősi and Makádi, 2009), mainly the type Cranial remains of ankylosaurs are among the material of Struthiosaurus, Struthiosaurus austria- rarest fossils from the Late Cretaceous of Europe.
[Show full text]
New Teeth of Nodosaurid Ankylosaurs from the Lower Cretaceous of Southern England
New teeth of nodosaurid ankylosaurs from the Lower Cretaceous of Southern England WILLIAM T. BLOWS and KERRI HONEYSETT Blows, W.T. and Honeysett, K. 2014. New teeth of nodosaurid ankylosaurs from the Lower Cretaceous of Southern England. Acta Palaeontologica Polonica 59 (4): 835–841. We present new nodosaurid teeth from the Valanginian of Bexhill, Sussex and the Barremian of the Isle of Wight, the first from the Lower Cretaceous of the United Kingdom. Teeth found during the mid-1800s from the Valanginian and ascribed to the nodosaurid Hylaeosaurus are probably from sauropod dinosaurs. The Isle of Wight tooth could possibly be referred to Polacanthus foxii, the teeth of which are unknown. These new English nodosaurid teeth are similar to those of North American and European Jurassic to Late Cretaceous nodosaurids, especially the American Gastonia, Texasetes, Mymoorapelta, Gargoyleosaurus, and the European Hungarosaurus. Key words: Dinosauria, Nodosauridae, Polacanthus, ankylosaur, Valanginian, Barremian, Cretaceous, England. William T. Blows [[email protected]], School of Health Sciences, City University, London, EC1A 7QN, UK; Kerri Honeysett [[email protected]], 10 Camperdown Street, Bexhill on Sea, East Sussex, TN39 5BE, UK. Received 8 November 2012, accepted 11 March 2013, available online 13 March 2013. Copyright © 2014 W.T. Blows and K. Honeysett. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. 1993). Isolated teeth from the same strata as Hylaeosaurus Introduction (NHMUK 2310, NHMUK 3326, NHMUK R739, BMBG 004179, BMBG 013516) were tentatively assigned to There are few skull and tooth remains of armoured dinosaurs Hy- by Mantell (1841) and Owen (1857).
[Show full text]
Link to Unformatted Pre-Print
1 Farke, A. A. In press. Evaluating combat in ornithischian dinosaurs. Journal of Zoology. doi: 10.1111/jzo.12111 ©Andrew A. Farke, 2014 ACCEPTED AND UNFORMATTED MANUSCRIPT NOTICE: This is the peer reviewed version of the following article: Farke, A. A. In press. Evaluating combat in ornithischian dinosaurs. Journal of Zoology. doi: 10.1111/jzo.12111, which has been published in final form at http://dx.doi.org/10.1111/jzo.12111. Changes introduced by the publisher (e.g., minor copyedits, journal style corrections, etc.) may not be incorporated here. The official version of record was published in Journal of Zoology. 2 Evaluating Combat in Ornithischian Dinosaurs Andrew A. Farke Raymond M. Alf Museum of Paleontology, 1175 West Baseline Road, Claremont, CA 91711 email: [email protected] ABSTRACT Ornithischia, a diverse clade of herbivorous dinosaurs, has numerous members with structures hypothesized to function in combat. These include the horned ceratopsids, dome- headed pachycephalosaurs, spike-thumbed iguanodonts, tail-clubbed ankylosaurs, and spiked stegosaurs, among others. Three main lines of evidence support such inferences: 1) analogy with modern animals; 2) biomechanical analysis and simulation; and 3) paleopathology. The most solid inferences utilize multiple pieces of evidence, although this is hampered by a limited understanding of combat in modern animals. Keywords: Ornithischia, Dinosauria, functional morphology, combat, modeling, paleopathology INTRODUCTION Ornithischians are a remarkably morphologically disparate group of non-avian dinosaurs, displaying a panoply of body shapes, sizes, and bony ornaments (Figures 1, 2). This clade includes the three-horned Triceratops, the plated Stegosaurus, the bone-headed Pachycephalosaurus, the tail-clubbed Ankylosaurus, and the crested Corythosaurus, to name just a few.
[Show full text]
T Riassic Jurassic Cretaceous
Millions of Years Ago 252.17 247.2 237.0 201.3 174.1 163.5 145.0 100.5 66.0 Avemetatarsalia Triassic Jurassic Cretaceous Early Middle Late Early Middle Late Early Late Scleromochlus Pterosauria Ornithodira Lagerpetidae Marasuchus Dinosauromorpha Genasauria Silesauridae Neornithsichia Nyasasaurus Dinosauriformes Thyreophora Ornithischia Eocursor ? Heterodontosauridae Pisanosaurus Dinosauria Sauropodomorpha Herrerasauria Saurischia Eodromaeus Theropoda Daemonosaurus Tawa Neotheropoda Millions of Years Ago 252.17 247.2 237.0 201.3 174.1 163.5 145.0 100.5 66.0 Triassic Jurassic Cretaceous Early Middle Late Early Middle Late Early Late Cerapoda Ornithopoda Marginocephalia Eocursor Parksosauridae Laquintasaura Kulindadromeus Othnielosaurus Jeholosauridae Neornithischia Leaellynasaura Hexinlusaurus Agilisaurus Stegosauridae Lesothosaurus Stegosaurinae Stegosauria Dacentrurinae Kentrosaurus Tuojiangosaurus Thyreophoroidea Struthiosaurinae Genasauria Huayangosauridae Eurypoda Gigantspinosaurus Panoplosaurinae Nodosauridae Sauropelta Polacanthinae Scelidosaurus Gargoyleosaurus Ankylosauridae Thyreophora Scutellosaurus Kunbarrasaurus Ankylosauria Hylaeosurus Shamosaurinae Ankylosaurinae Pinacosaurus Tianchiasaurus Ankylosaurini Millions of Years Ago 252.17 247.2 237.0 201.3 174.1 163.5 145.0 100.5 66.0 Triassic Jurassic Cretaceous Euhadrosauria Early Middle Late Early Middle Late Early Late Hadrosaurinae Hadrosauridae Hadrosauromorpha Lambeosaurinae Eotrachodon Tethyshadros Hadrosauriformes Hadrosauria Telmatosaurus Bactrosaurus Protohadros Styracosterna
[Show full text]
Campanian-Maastrictian Ankylosaurs of West Texas
Campanian-Maastrictian Ankylosaurs of West Texas by Bryanna Nicole West Bachelor of Science, 2018 Texas Tech University Lubbock, Tx Submitted to the faculty of College of Science and Engineering Texas Christain University In partial fulfillment of the requirements for the degree of Master of Science in Geology May 2020 ACKNOWLEDGMENTS I would like to thank my thesis advisor Dr. Busbey for taking me on as a graduate student and giving me the confidence to take on a project of this magnitude. I would also like to thank the rest of my advisory committee; Dr. Richard Denne who I got to know well by taking many of his courses. In addition, Dr. Tom Lehman who acted as an outside committee member and has been with me since day one to my very first geology class at Texas Tech. He has been a mentor to me for almost six years and I hope that I become a paleontologist that makes him and Dr. Busbey proud. I would also like to thank the various museum staff members who hosted me on my research trips; Nicole Ridgewell who had two ankylosaur skulls already waiting for me when I arrived at the University of New Mexico and Chris Mehling at the American Museum of Natural History who put up with my constant emails and who helped me retrieve specimens from drawers when my back gave out. And especially Dr. Chris Sagebiel and Dr. Matthew Colbert and the staff at the Vertebrate Paleontology Lab in Austin, Tx who scanned the osteoderm specimens for me. Finally, I would like to thank my family for their unwavering support.
[Show full text]
Armoured Dinosaurs from the Cretaceous of Mongolia
Armoured dinosaurs from the Cretaceous of Mongolia T47") 4N \ \ 'I'UhI Introduction were collected and later described by Gillnore (1933) as Pinacosnuvusgm?zgeri.Abundant reniains of ankylo- .\nkylosaurs, onc of the main suborders of ornithis- saors were excavated by the Palaeontological chian dinosaurs, were distributed world-wide in tlie Expedition of the USSR Academy of Sciences and Mesozoic: their remains are tbund ill Europe, Asia, described by hlaleev (1952a, 11, 19.54, 1956). North and South America, Australia and .\ntarctica Subsequently, new and well preserved ankylosaurs (see Coon~bsand Maryariska (1090) for the most were discovered in the Upper Cretaceous of Mongolia recent comprehensive review of the group). The earli- by the Polish-Mongolian Palaeontological Expedition est rcpresei~tativesof ;inkvlosaurs are known from the in the years 1963-1971 (Marva~iska,1960; 1071; 1977). Middle Jurassic (Galton, 1080; Dong, 1993), while the Rich collections, including numerous interesting latest are Idate Cretaceous (hlaastrichtian) in age (e.g., specimens of Upper Cretaceous ankylosaurs and the Carpenter and Brcithaupt, 1986). However, despite its first Lo\vcr Cretaceous representatives of the group wide distribution and representation by numeroils were excavated by the Soviet-Mongolian Expedition fossil specimc~ls,this group is still not well under- (now Mongolian-Russian Paleontological Expedi- stood. tion) during the past 20 years ('T~~rnanova,1077; 1987; In tlie former USSR remains of ankylosaurs were 1903; Kurzanov and 'l'umanova, 1978). Material col- found in t~vo1,ower Cretaceous sites, one in Yakutia lected by these t~voexpeditions and described by (now the Republic Sakha) the other in Buryatis. 'l'liey bfaryariska (1977) and Tulrianova (1987) are the prin- have also been recovered from various Upper cipal sources for the generic diagnoses of the Cretaceous horizons at 26 localities in Kazakhstan, Mongolian ankylosaurs presented in this chapter.
[Show full text]
(Ornithischia: Thyreophora) from the Mid-Cretaceous (Late Albian–Cenomanian) Winton Formation of Queensland, Australia Lucy G
This article was downloaded by: [Steven Salisbury] On: 07 June 2013, At: 16:18 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK Alcheringa: An Australasian Journal of Palaeontology Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/talc20 First evidence of ankylosaurian dinosaurs (Ornithischia: Thyreophora) from the mid-Cretaceous (late Albian–Cenomanian) Winton Formation of Queensland, Australia Lucy G. Leahey & Steven W. Salisbury Published online: 07 Jun 2013. To cite this article: Lucy G. Leahey & Steven W. Salisbury (2013): First evidence of ankylosaurian dinosaurs (Ornithischia: Thyreophora) from the mid-Cretaceous (late Albian–Cenomanian) Winton Formation of Queensland, Australia, Alcheringa: An Australasian Journal of Palaeontology, 37:2, 249-257 To link to this article: http://dx.doi.org/10.1080/03115518.2013.743703 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.tandfonline.com/page/terms-and-conditions This article may be used for research, teaching, and private study purposes. Any substantial or systematic reproduction, redistribution, reselling, loan, sub-licensing, systematic supply, or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. The accuracy of any instructions, formulae, and drug doses should be independently verified with primary sources. The publisher shall not be liable for any loss, actions, claims, proceedings, demand, or costs or damages whatsoever or howsoever caused arising directly or indirectly in connection with or arising out of the use of this material.
[Show full text]