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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. -
Deinogalerix : a Giant Hedgehog from the Miocene
Annali dell’Università di Ferrara ISSN 1824-2707 Museologia Scientifica e Naturalistica Volume 6 (2010) Deinogalerix : a giant hedgehog from the Miocene Boris VILLIER* * Dipartimento di scienze della Terra, Università degli Studi di Torino [email protected] SUPERVISORS: Marco Pavia e Marta Arzarello __________________________________________________________________________________ Abstract During the Miocene the Abruzzo/Apulia region (Italy), isolated from the continent, was the theatre of the evolution of a vertebrate ecosystem in insular context. At the late Miocene the protagonists of this ecosystem called “ Mikrotia fauna ” show a high endemic speciation level with spectacular giant and dwarf species of mammals and birds. Most of the remains of this peculiar fauna are found exclusively in the “Terre rosse” of Gargano, except for the oldest genus: Deinogalerix and Hoplitomeryx , also found at Scontrone. Deinogalerix is one of the most uncommon forms of the “ Mikrotia fauna ”. It’s the largest Erinaceidea ever lived. Deinogalerix was described for the first by Freudenthal (1972) then by Butler (1980). Today the five species yet described are under discussion cause of the high intraspecific variations in an insular evolution context. In this study we valuated the information that could bring the new discoveries of Deinogalerix remains. The work was divided into three main parts: the preparation of the material, the drawing reconstructions and the anatomical description. The most important specimen was the second sub-complet skeleton ever found. We gave the most objective anatomical description for futures comparison with the first skeleton from a different specie. We put the finger on new juvenile features and on the relation between the growth of Deinogalerix and his feeding behaviours. -
Dolomites Offer Delightful Via Ferratas
spring-loaded device, which, if a fall takes place, will minimize the impact on the climber who is usually linked to a fixed cable. I sometimes used my climbing shoes whereas Helmut used his lightweight mountaineering boots. Most ferrata climb- ers hung on to the cables, whereas we mostly free climbed with a few exceptions. Upon arrival from Munich, Helmut, his wife, Giselle, and I checked in at the Hotel Christiania in Alta Badia/Stern, where Helmut had stayed previ- ously several times. Full board and lodging were very much appreciated. All approaches to the climbs were comfortably accomplished in a day from this elegant hotel, where we could always have a full breakfast, afternoon snacks and dinner in the evenings. Although the weather forecast for the first week was for rain showers, we enjoyed sunshine every day for the following 11 days, except when cloud and thunderstorms sometimes moved in late in the afternoons and/or evenings. The next day, Helmut led me to my first ferrata, Pizzes da Cir; a perfect introduction to the ferratas being a short but pleasant route, starting from a chairlift. The following day, after paying a heavy toll for the private access road to one of the best known ferratas in the Dolomites, we hiked along with hundreds of other tourists to the start of the De Luca/Innerkofler protected wartime climbing path, which, partway along, includes a 400-metre tunnel (headlamp required). We enjoyed a fairly long day in good weather. For our next outing, Diego was our guide to climb Cinque Dita (five fin- gers) in the Sasso Lungo Langkofel group, leading to a 2996-metre summit. -
Dolomiten Dolomiti Dolomites
Reinhold Messner Dolomiten Dolomiti Dolomites Die schönsten Berge der Welt – UNESCO Welterbe Dolomites Le montagne più belle del mondo – Patrimonio mondiale UNESCO The most beautiful mountains in the world – UNESCO World Heritage Site athesia-tappeiner.com9,90 € (I/D/A) Dolomiti Dolomiten Reinhold Messner Umschlag-Titelseite: Oben links: der Schlern | Oben Mitte: der Rosengarten | Oben rechts: das Ranuikirchlein und die Geislerspitzen Unten links: der Langkofel | Unten Mitte: der Sellastock | Unten rechts: die Drei Zinnen Umschlag-Rückseite: Oben links: die Brentagruppe | Oben Mitte: der Monte Agnèr | Oben rechts: der Heiligkreuzkofel Unten links: der Lago di Coldai und Monte Pelmo | Unten Mitte: die Marmolata | Unten rechts: der Monte Cristallo Foto di copertina: In alto a sinistra: lo Sciliar | In alto al centro: il Catinaccio | In alto a destra: la chiesetta di Ranui e le Odle In basso a sinistra: il Sassolungo | In basso al centro: il Gruppo di Sella | In basso a destra: le Tre Cime di Lavaredo Retrocopertina: In alto a sinistra: il Gruppo di Brenta | In alto al centro: il Monte Agnèr | In alto a destra: il Sasso di Santa Croce In basso a sinistra: il Lago di Coldai e il Monte Pelmo | In basso al centro: la Marmolada | In basso a destra: il Monte Cristallo Cover photos Top left: the Schlern | Top centre: the Rosengarten | Top right: Ranui chapel and the Geislerspitzen Bottom left: the Langkofel group | Bottom centre: the Sella massif | Bottom right: the Drei Zinnen Back cover: Top left: the Brenta group | Top centre: the Monte Agnèr | Top right: the Heiligkreuzkofel Bottom left: the Monte Pelmo with Lake Coldai | Bottom centre: the Marmolada | Bottom right: the Monte Cristallo Die vergletscherte Nordseite der Marmolata Il versante nord della Marmolada coperto di ghiaccio The glaciated north side of the Marmolada Inhalt | Indice | Content Dolomiten UNESCO Welterbe | Dolomiti Patrimonio mondiale UNESCO | Dolomites UNESCO World Heritage Site . -
Apulia, Italy)
Published by Associazione Teriologica Italiana Online first – 2016 Hystrix, the Italian Journal of Mammalogy Available online at: http://www.italian-journal-of-mammalogy.it/article/view/11677/pdf doi:10.4404/hystrix-27.2-11677 Research Article New Hoplitomeryx Leinders, 1984 remains from the Late Miocene of Gargano (Apulia, Italy) Alessandro Urciuoli1,2, Daniel DeMiguel2,∗, Salvador Moyà-Solà3, Lorenzo Rook1 1Dipartimento di Scienze della Terra, Università di Firenze, Via G. La Pira 4, 50121 Firenze, Italy 2Institut Català de Paleontologia Miquel Crusafont (ICP), Edifici Z, c/ de les Columnes, s/n. Campus de la UAB, 08193 Cerdanyola del Vallès, Barcelona, Spain 3ICREA at ICP and Unitat d’Antropologia Biològica (Dept. BABVE), Universitat Autònoma de Barcelona, Edifici Z, c/ de les Columnes, s/n. Campus de la UAB s/n, 08193 Cerdanyola del Vallès, Barcelona, Spain Keywords: Abstract endemism Ruminantia Natural selection in isolated environments led to the positive selection of species bearing an ex- southern Italy traordinary array of morphological traits and a very high grade of endemism. The unbalanced systematics mammal assemblage found in the Upper Miocene karst infillings of the Gargano Peninsula (south- evolution ern Italy), and especially the intriguing ruminant Hoplitomeryx, is one of the best examples of fast, isolated evolution. Hoplitomeryx exhibits a peculiar combination of craniodental and postcranial Article history: characters, some of which are unique among the other ruminant families. For this reason, its phylo- Received: 8 January 2016 genetic position is still puzzling and far from being clarified. Thus, every contribution to a more Accepted: 3 April 2016 comprehensive knowledge of the genus is crucial to better understand the evolutionary process that led to such an advanced and peculiarly adapted ruminant. -
The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus
19 The Early Jurassic Ornithischian Dinosaurian Ichnogenus Anomoepus Paul E. Olsen and Emma C. Rainforth nomoepus is an Early Jurassic footprint genus and 19.2). Because skeletons of dinosaur feet were not produced by a relatively small, gracile orni- known at the time, he naturally attributed the foot- A thischian dinosaur. It has a pentadactyl ma- prints to birds. By 1848, however, he recognized that nus and a tetradactyl pes, but only three pedal digits some of the birdlike tracks were associated with im- normally impressed while the animal was walking. The pressions of five-fingered manus, and he gave the name ichnogenus is diagnosed by having the metatarsal- Anomoepus, meaning “unlike foot,” to these birdlike phalangeal pad of digit IV of the pes lying nearly in line with the axis of pedal digit III in walking traces, in combination with a pentadactyl manus. It has a pro- portionally shorter digit III than grallatorid (theropod) tracks, but based on osteometric analysis, Anomoepus, like grallatorids, shows a relatively shorter digit III in larger specimens. Anomoepus is characteristically bi- pedal, but there are quadrupedal trackways and less common sitting traces. The ichnogenus is known from eastern and western North America, Europe, and southern Africa. On the basis of a detailed review of classic and new material, we recognize only the type ichnospecies Anomoepus scambus within eastern North America. Anomoepus is known from many hundreds of specimens, some with remarkable preservation, showing many hitherto unrecognized details of squa- mation and behavior. . Pangea at approximately 200 Ma, showing the In 1836, Edward Hitchcock described the first of what areas producing Anomoepus discussed in this chapter: 1, Newark we now recognize as dinosaur tracks from Early Juras- Supergroup, eastern North America; 2, Karoo basin; 3, Poland; sic Newark Supergroup rift strata of the Connecticut 4, Colorado Plateau. -
The Dinosaurs of North America
FEOM THE SIXTEENTH ANNUAL KEPOKT OF THE U. S, GEOLOGICAL SURVEY THE DINOSAURS OF NORTH AMERICA OTHNIEL CHARLES MARSH TALE UNIVERSITY WASHINGTON 1896 ^33/^, I/BRAKt 4 ,\ . THE DINOSAURS OF NORTH AMERICA. BY OTHNIEL CHARLES MARSH. 133 CONTENTS. Pajje. Introduction 143 Part I. —Triassic dinosaurs 146 Theropoda 146 Anchisaurida? 147 Anchisaurus 147 The skull 148 The fore limbs 149 The hind limbs 149 Anchisaurus solus 149 Amniosaurus rTT 150 Eestoration of Anchisaurus 150 Dinosaurian footprints 151 Distribution of Triassic dinosaurs 152 Part II. —Jurassic dinosaurs 152 Theropoda : 153 Hallopus 153 Fore and hind limbs 154 Coelurus _ 155 The vertebra:- 155 The hind limbs 156 Ceratosaurus 156 The skull 157 The brain 159 The lower iaws 159 The vertebra: 159 The scapular arch 160 The pelvic arch 160 The metatarsals 162 Eestoration of Ceratosaurus 163 Allosaurus 163 European Theropoda 163 Sauropoda 164 Atlantosaurus beds 164 Families of Sauropoda 165 Atlantosauridie 166 Atlantosaurus 166 Apatosaurus 166 The sacral cavity 166 The vertebra- 167 Brontosaurus 168 The scapular arch 168 The cervical vertebra.- 169 The dorsal vertebree 169 The sacrum 170 The caudal vertebra- 171 The pelric arch 172 The fore limbs 173 The hind limbs 173 135 136 CONTENTS. Part II. —Jurassic dinosaurs—Continued. Page. Sauropoda—Continued. Atlantosaurida? —Continued. Restoration of Brontosaurus 173 Barnsaurus 174 Diplodoeida? 175 Diplodocus 175 The skull 175 The brain 178 The lower jaws 178 The teeth 179 The vertebra; 180 The sternal bones 180 The pelvic girdle 180 Size and habits 180 Morosaurida? 181 Morosaurus 181 The skull 181 The vertebra? 181 The fore limbs 182 The pelvis 182 The hind limbs 183 Pleuroccelida? : 183 Pleurocoelus 183 The skull 183 The vertebras 183 Distribution of the Sauropoda 185 Comparison with European forms 185 Predentata ». -
Tectonostratigraphy of the Western Dolomites in the Context of the Development of the Western Tethys 51-56 Geo.Alp, Vol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Geo.Alp Jahr/Year: 2019 Band/Volume: 0016 Autor(en)/Author(s): Brandner Rainer, Gruber Alfred Artikel/Article: Tectonostratigraphy of the Western Dolomites in the context of the development of the Western Tethys 51-56 Geo.Alp, Vol. 16 2019 TECTONOSTRATIGRAPHY OF THE WESTERN DOLOMITES IN THE CONTEXT OF THE DEVELOPMENT OF THE WESTERN TETHYS → Rainer Brandner 1 & Alfred Gruber 2 1 Institut für Geologie, Universität Innsbruck, Austria; e-mail: [email protected] 2 Geologische Bundesanstalt, Wien, Austria; e-mail: [email protected] In the Dolomites, the transition from the post-Variscan to into Central Europe ("Central European Extensional Province", the Alpine orogen cycle generally takes place in a domain of Kroner et al., 2016) and is accompanied by the widespread lithospheric stretching, which is recorded in several plate thermal event ("Permian metamorphic event", Schuster & tectonically controlled megacycles in the sediment sequences. Stüwe, 2008). Early Permian and Middle Triassic magmatism are associated with this development. In contrast to the "post-Variscan" magmatism, however, the Middle Triassic magmatism gives 2ND TECTONOSTRATIGRAPHIC MEGACYCLE (MIDDLE PERMIAN TO rise to numerous discussions due to its orogenic chemistry LOWER ANISIAN) in the extensional setting of the Dolomites. A new analysis of the tectonostratigraphic development now revealed an With the cooling of the crust, continental and marine interpretation of the processes that differs from the general sedimentation starts in large areas in the Middle and Upper opinion. Within the general extensional development in the Permian, which overlaps the graben-like extensional tectonics Permo-Mesozoic there are four distinct unconformities caused relief like mantle (see Wopfner, 1984 and Italian IGCP 203 Group, by compressive or transpressive tectonic intervals. -
Disentangling Adaptive Evolutionary Radiations and the Role of Diet In
www.nature.com/scientificreports OPEN Disentangling adaptive evolutionary radiations and the role of diet in promoting diversification Received: 17 March 2016 Accepted: 20 June 2016 on islands Published: 13 July 2016 Daniel DeMiguel Although the initial formulation of modern concepts of adaptive radiation arose from consideration of the fossil data, rigorous attempts to identify this phenomenon in the fossil record are largely uncommon. Here I focus on direct evidence of the diet (through tooth-wear patterns) and ecologically- relevant traits of one of the most renowned fossil vertebrates-the Miocene ruminant Hoplitomeryx from the island of Gargano-to deepen our understanding of the most likely causal forces under which adaptive radiations emerge on islands. Results show how accelerated accumulation of species and early- bursts of ecological diversification occur after invading an island, and provide insights on the interplay between diet and demographic (population-density), ecological (competition/food requirements) and abiotic (climate-instability) factors, identified as drivers of adaptive diversification. A pronounced event of overpopulation and a phase of aridity determined most of the rate and magnitude of radiation, and pushed species to expand diets from soft-leafy foods to tougher-harder items. Unexpectedly, results show that herbivorous mammals are restricted to browsing habits on small-islands, even if bursts of ecological diversification and dietary divergence occur. This study deepens our understanding of the mechanisms promoting adaptive radiations, and forces us to reevaluate the role of diet in the origins and evolution of islands mammals. Islands have long been recognised as nature’s test tubes of great value in studying macroevolutionary processes even since Darwin’s early proposal of natural selection1. -
Studio Dei Muridi E Cricetidi Delle Terre Rosse Del Gargano E Dei Processi Di Colonizzazione Di Ambienti Isolati
Chissà chissà domani su che cosa metteremo le mani se si potrà contare ancora le onde del mare e alzare la testa Lucio Dalla, Futura Ai miei genitori STUDIO DEI MURIDI E CRICETIDI DELLE TERRE ROSSE DEL GARGANO E DEI PROCESSI DI COLONIZZAZIONE DI AMBIENTI ISOLATI Riassunto I depositi delle “Terre Rosse” del Gargano sono riempimenti di fessure carsiche sviluppatesi in piattaforma carbonatica mesozoica e costituiscono una notevole fonte di informazioni per ricostruzioni palegeografiche e per la comprensione dei fenomeni evolutivi in ambiente insulare. Questi depositi hanno restituito faune endemiche che testimoniano eventi di popolamento in un ambiente considerato di arcipelago. Sebbene questa fauna insulare messiniana del settore di avampaese della paleobioprovincia Abruzzo-Apula sia conosciuta da svariate decadi, i mammiferi delle Terre Rosse hanno ancora molte storie da raccontare. Negli ultimi dieci anni i ruminanti, i gliridi, gli insettivori, i cricetidi delle Terre Rosse ma anche gli aspetti biocronologici, paleogeografici e biogegrafici sono stati oggetto di numerose pubblicazioni. Per la prima volta dalla scoperta di questa fauna, nuovi ritrovamenti di fossili, rinvenuti durante gli scavi da parte dell'Università di Torino tra il 2005 ed il 2009, hanno arricchito la lista faunistica dell'associazione endemica del Gargano. Il presente lavoro è focalizzato su due nuovi taxa, un cricetide gigante e un muride che è ancestrale rispetto al genere endemico Mikrotia, ma anche sul cosidetto “Apodemus”, la cui presenza è stata riportata sin dalla scoperta della fauna fossile del Gargano, ma che non è mai stato studiato in dettaglio. Inoltre, i pattern evolutivi di Mikrotia sono stati descritti e analizzati tramite diversi parametri, usati come proxy per la taglia e la complessità morfologica dei molari. -
Jahresbericht 2010 Der Generaldirektion Der Staatlichen Naturwissenschaftlichen Sammlungen Bayerns Herausgegeben Von: Prof
Jahresbericht 2010 der Generaldirektion der Staatlichen Naturwissenschaftlichen Sammlungen Bayerns Herausgegeben von: Prof. Dr. Gerhard Haszprunar, Generaldirektor Generaldirektion der Staatlichen Naturwissenschaftlichen Sammlungen Bayerns (SNSB) Menzinger Straße 71, 80638 München München November 2010 Zusammenstellung und Endredaktion: Dr. Eva Maria Natzer (Generaldirektion) Unterstützung durch: Maria-Luise Kaim (Generaldirektion) Iris Krumböck (Generaldirektion) Susanne Legat (Generaldirektion) Druck: Digitaldruckzentrum, Amalienstrasse, München Inhaltsverzeichnis Bericht des Generaldirektors ...................................................................................................5 Wissenschaftliche Publikationen ................................................................................................6 Drittmittelübersicht ...................................................................................................................37 Organigramm ............................................................................................................................49 Generaldirektion .....................................................................................................................50 Personalvertretung ....................................................................................................................52 Museen Museum Mensch und Natur (MMN) ........................................................................................53 Museum Reich der Kristalle (MRK) ........................................................................................59 -
Programm Und Kurzfassungen – Program and Abstracts
1 Zitteliana An International Journal of Palaeontology and Geobiology Series B/Reihe B Abhandlungen der Bayerischen Staatssammlung für Paläontologie und Geologie 29 Paläontologie im Blickpunkt 80. Jahrestagung der Paläontologischen Gesellschaft 5. – 8. Oktober 2010 in München Programm und Kurzfassungen – Program and Abstracts München 2010 Zitteliana B 29 118 Seiten München, 1.10.2010 ISSN 1612-4138 2 Editors-in-Chief/Herausgeber: Gert Wörheide, Michael Krings Mitherausgeberinnen dieses Bandes: Bettina Reichenbacher, Nora Dotzler Production and Layout/Bildbearbeitung und Layout: Martine Focke, Lydia Geissler Bayerische Staatssammlung für Paläontologie und Geologie Editorial Board A. Altenbach, München B.J. Axsmith, Mobile, AL F.T. Fürsich, Erlangen K. Heißig, München H. Kerp, Münster J. Kriwet, Stuttgart J.H. Lipps, Berkeley, CA T. Litt, Bonn A. Nützel, München O.W.M. Rauhut, München B. Reichenbacher, München J.W. Schopf, Los Angeles, CA G. Schweigert, Stuttgart F. Steininger, Eggenburg Bayerische Staatssammlung für Paläontologie und Geologie Richard-Wagner-Str. 10, D-80333 München, Deutschland http://www.palmuc.de email: [email protected] Für den Inhalt der Arbeiten sind die Autoren allein verantwortlich. Authors are solely responsible for the contents of their articles. Copyright © 2010 Bayerische Staassammlung für Paläontologie und Geologie, München Die in der Zitteliana veröffentlichten Arbeiten sind urheberrechtlich geschützt. Nachdruck, Vervielfältigungen auf photomechanischem, elektronischem oder anderem Wege sowie