Stuttgarter Beiträge Zur Naturkunde

Total Page:16

File Type:pdf, Size:1020Kb

Stuttgarter Beiträge Zur Naturkunde S^5 ( © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at Stuttgarter Beiträge zur Naturkunde Serie B (Geologie und Paläontologie) Herausgeber: Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart Stuttgarter Beitr. Naturk. Ser. B Nr. 278 175 pp., 4pls., 54figs. Stuttgart, 30. 12. 1999 Comparative osteology oi Mastodonsaurus giganteus (Jaeger, 1828) from the Middle Triassic (Lettenkeuper: Longobardian) of Germany (Baden-Württemberg, Bayern, Thüringen) By Rainer R. Schoch, Stuttgart With 4 plates and 54 textfigures Abstract Mastodonsaurus giganteus, the most abundant and giant amphibian of the German Letten- keuper, is revised. The study is based on the excellently preserved and very rieh material which was excavated during road construction in 1977 near Kupferzeil, Northern Baden- Württemberg. It is shown that there exists only one diagnosable species of Mastodonsaurus, to which all Lettenkeuper material can be attributed. All finds from other horizons must be referred to as Mastodonsauridae gen. et sp. indet. because of their fragmentary Status. A sec- ond, definitely diagnostic genus of this family is Heptasaurus from the higher Middle and Upper Buntsandstein. Finally a diagnosis of the family Mastodonsauridae is provided. Ä detailed osteological description of Mastodonsaurus giganteus reveals numerous un- known or formerly inadequately understood features, yielding data on various hitherto poor- ly known regions of the skeleton. The sutures of the skull roof, which could be studied in de- tail, are significantly different from the schemes presented by previous authors. The endocra- nium and mandible are further points of particular interest. The palatoquadrate contributes a significant part to the formation of the endocranium by an extensive and complicated epi- pterygoid. The neurocranium is dominated by the exoccipital, otic, and several portions of the sphenethmoid. For the first time the stapes is found in articulation and uncompressed. The mandible is slender and bears a massive postglenoid area, and the symphyseal area is extend- ed to accommodate giant tusks. The prearticular forms a pronounced process anterior to the glenoid facet. The axial skeleton is strongly ossified. It consists of massive, cylindrical intercentra that tend to be lower towards the tail and which have a dorsal incisure for the chorda, further it contains paired pleurocentra which are set in facets of the neural arch and intercentrum, and finally it bears low neural arches possessing posteriorly inclined, short and unfinished Proces- sus spinosi and broad, laterally extended transverse processes. The costal apparatus is wide, bearing broadened ribs in the anterior and middle part of the trunk which are strcngthened by two different uncmate processes. While in the trunk these processes disappear tailwards, the tail base and anterior tail proper again bear wide ribs with markcd processes. Doctoral dissertation Univ. Tübingen 1998. © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at 2 STUTTGARTER BEITRÄGE ZUR NATURKUNDE Ser. B, Nr. 278 The girdles and appendages are well represented in the Kupferzell material, with the excep- tion of the pes; because of their disarticulated State their original arrangement has to be recon- structed. The dermal bones of the pectoral girdle consist of broad and flattened claviculae and a wide, rhomboidal interclavicle which has, as is typical of capitosaurs, a stilette-like anterior process with a broadened tip. The ontogeny of the cleithrum and scapulocoracoid is docu- mented in detail. Scapula and coracoid are separate at first, but later in development fuse to give a Compound ossification, whose coracoid portion tends to increase in area. In addition the geometry and surface of the glenoid facet changes during ontogeny. The humerus is rela- tively slender and long, yet poorly differentiated with respect to most other temnospondyls. Only in the largest specimens are there definite epicondyles and a faint supinator process. Ra- dius and ulna are well differentiated and elongate, and the manus consists mainly of slender metacarpals and phalanges. In the pelvic girdle the ilium is slender and low, with an acetabu- lum that enlarged during later development. The ischium is small and remains poorly differ- entiated. In larger specimens it appears to fuse with the pubis which is still unknown as isolat- ed element. The femur is slender, elongate, and differentiated, whereas the lower leg gains less than half the length of the upper leg and has a rudimentary structure. Finally open questions and problems regarding the reconstruction of the whole skeleton are discussed. This involves a clarification of the methods used and a discussion of the lines of evidence. A complete yet still partially provisional restoration of the skeleton of Mastodon- saurus giganteus gives an animal similar to a gigantic Salamander. Mastodonsaurus was most similar to cryptobranchid Salamanders in its bodily proportions such as the relative length of the trunk and tail, as well as the considerable breadth and flattness of the rib cage. Zusammenfassung Mastodonsaurus giganteus, das häufigste und größte Amphib der europäischen Mitteltrias, wird eingehend revidiert. Die Untersuchung geht aus von dem hervorragend erhaltenen und sehr umfangreichen Material, das beim Autobahnbau 1977 bei Kupferzell geborgen wurde. Im Lettenkeuper existiert nur eine diagnostizierbare Art von Mastodonsaurus, während die fragmentarischen Funde aus anderen Formationen lediglich der Familie Mastodonsauridae zugeordnet werden können. Die zweite, gegenwärtig faßbare Gattung dieser Familie ist Hep- tasaurus, die auf den höheren Mittleren und Oberen Buntsandstein beschränkt bleibt. Die ta- xonomische Revision schließt mit einer Diagnose der Mastodonsauridae. Im Rahmen einer detaillierten osteologischen Untersuchung von Mastodonsaurus gigante- us werden zahlreiche neue Merkmale beschrieben und viele, bisher unzureichend verstandene Regionen des Skeletts vorgestellt und rekonstruiert. Die Suturen im Schädeldach können dank der guten Erhaltung der Kupferzeller Funde erstmals genau erfaßt werden; sie weichen in einigen Punkten erheblich von den Schemata früherer Bearbeiter ab. Das Endocranium und die Mandibel von Mastodonsaurus bilden weitere Schwerpunkte. Das Palatoquadratum ist mit einem ausgedehnten und kompliziert gebauten Epipterygoid wesentlich an der Gestal- tung des Endocranium beteiligt. Im knöchernen Neurocranium dominieren das Exoccipitale, das Oticum sowie verschiedene Portionen des Sphenethmoid; der Stapes wird erstmals un- verdrückt und in Artikulation vorgefunden und vorgestellt. Im Unterkiefer, der sehr niedrig ist und eine massive, langgestreckte Postglenoid-Region besitzt, dominieren riesige Fangzäh- ne in der verbreiterten Symphyse. Ein hoher, allometrisch positiv wachsender Fortsatz des Praearticulare bildet eine knöcherne Sperre unmittelbar vor dem Unterkiefergelenk. Das Axialskelett ist stark verknöchert. Es besteht aus massiven, kurz-zylindrischen Inter- centra, die zur Cauda hin niedriger werden und eine Inzisur für die Chorda aufweisen, wei- terhin enthält es paarige Pleurocentra, die in Facetten des Neuralbogens und des Intercentrum eingelassen sind, und schließlich die Bögen selbst, die niedrig sind, mit nach hinten geneigten Dornfortsätzen und breit nach lateral vorgreifenden Transversalfortsätzen. Der Rippenkorb ist breit, im vorderen und mittleren Rumpf aus kräftigen Rippen bestehend, die mehrere Un- cinat-Fortsätze tragen können. Diese werden im hinteren Rumpfabschnitt kürzer und ver- schwinden schließlich ganz, während im Schwanzskelett die Rippen erneut größer sind und auch dort blatt- bis stilettförmige Uncinat-Fortsätze tragen. Die Gürtel und Extremitäten sind bis auf das Fußskelett gut dokumentiert, müssen jedoch weitgehend anhand disartikulierter Reste rekonstruiert werden. Der hautknöcherne Schulter- gürtel besteht aus breiten, großflächigen Claviculae und einer breitrhombischen Interclavicu- © Biodiversity SCHOCH,Heritage Library,MASTODONSAURUS http://www.biodiversitylibrary.org/;GIGANTEUS www.zobodat.at 3 la, die den für Capitosaurier typischen, vorne verbreiterten anterioren Fortsatz trägt. Die On- togenese des Cleithrum sowie der ersatzknöchernen Elemente läßt sich im Detail verfolgen. Die Scapula und das Coracoid sind anfangs getrennt und verschmelzen später suturlos, wobei sich der Coracoid-Anteil stark medial ausdehnt. Auch die Glenoidfacette erweitert und ver- kompliziert sich im Zuge der späteren Ontogenese. Der Humerus ist anfangs verhältnismäßig schlank, insgesamt relativ lang und bis in das hohe Alter von rudimentärer Gestalt verglichen mit den meisten anderen Temnospondylen; erst bei den größten Individuen bilden sich die Condyli an seinem Distalende sowie ein schwacher Supinatorfortsatz. Radius und Ulna sind lang und differenziert, und das Handskelett besteht aus überwiegend schlanken Metacarpalia und Phalangen. Im Beckengürtel findet sich ein niedriges und schlankes Ilium, dessen Anteil am Acetabulum sich im Alter vergrößert. Das Ischium ist klein und bleibt zeitlebens wenig differenziert; bei größeren Tieren scheint es mit dem Pubis, das bisher isoliert nicht bekannt ist, verschmolzen zu sein. Das Femur ist schlank, langgestreckt und differenziert, während Ti- bia und Fibula weniger als halb so lang werden und rudimentär bleiben. Die Untersuchung schließt mit der Besprechung offener Fragen und Probleme bei der Re- konstruktion des Gesamtskeletts.
Recommended publications
  • New Permian Fauna from Tropical Gondwana
    ARTICLE Received 18 Jun 2015 | Accepted 18 Sep 2015 | Published 5 Nov 2015 DOI: 10.1038/ncomms9676 OPEN New Permian fauna from tropical Gondwana Juan C. Cisneros1,2, Claudia Marsicano3, Kenneth D. Angielczyk4, Roger M. H. Smith5,6, Martha Richter7, Jo¨rg Fro¨bisch8,9, Christian F. Kammerer8 & Rudyard W. Sadleir4,10 Terrestrial vertebrates are first known to colonize high-latitude regions during the middle Permian (Guadalupian) about 270 million years ago, following the Pennsylvanian Gondwanan continental glaciation. However, despite over 150 years of study in these areas, the bio- geographic origins of these rich communities of land-dwelling vertebrates remain obscure. Here we report on a new early Permian continental tetrapod fauna from South America in tropical Western Gondwana that sheds new light on patterns of tetrapod distribution. Northeastern Brazil hosted an extensive lacustrine system inhabited by a unique community of temnospondyl amphibians and reptiles that considerably expand the known temporal and geographic ranges of key subgroups. Our findings demonstrate that tetrapod groups common in later Permian and Triassic temperate communities were already present in tropical Gondwana by the early Permian (Cisuralian). This new fauna constitutes a new biogeographic province with North American affinities and clearly demonstrates that tetrapod dispersal into Gondwana was already underway at the beginning of the Permian. 1 Centro de Cieˆncias da Natureza, Universidade Federal do Piauı´, 64049-550 Teresina, Brazil. 2 Programa de Po´s-Graduac¸a˜o em Geocieˆncias, Departamento de Geologia, Universidade Federal de Pernambuco, 50740-533 Recife, Brazil. 3 Departamento de Cs. Geologicas, FCEN, Universidad de Buenos Aires, IDEAN- CONICET, C1428EHA Ciudad Auto´noma de Buenos Aires, Argentina.
    [Show full text]
  • Cacopsamphibiala373bolt.Pdf
    v UNIVtRSlT Cp ILLINOIS I 5RARY AT URBANA-CHAMPAIGN L IOLOGY CO CO /&£^<-*x~*yw FIELDIANA Geology Published by Field Museum of Natural History Volume 37, No. 3 June 30, 1977 Cacops (Amphibia: Labyrinthodontia) From the Fort Sill Locality, Lower Permian of Oklahoma the The Library of John R. Bolt Assistant Curator, Fossil Reptiles and Amphibians 1978 Field Museum of Natural History MRRU ABSTRACT at Urbana-ChamP«* The armored dissorophid (Super family Dissorophoidea ) labyrinthodont amphi- bian Cacops aspidephorus is unusual in having a large otic notch closed posteriorly by the tabular. Cacops was previously known only from the "Cacops Bone Bed," Lower Permian of Texas. Poor preservation makes this material difficult to study. Excellently preserved, though disarticulated, Cacops material has now been recov- ered from the Fort Sill fissure fills, which are probably very close in age to the "Ca- cops Bone Bed." Identification of the Fort Sill material as Cacops is based on pala- tines (primarily), armor scutes, and quadrates; the latter are here described for the first time from Fort Sill. The Cacops quadrate resembles that of other dissorophoids in having a posterodorsal process, which is unusual in the marked anterior expan- sion of its dorsal end. Comparison with other dissorophoids having a closed otic notch shows that Cacops is not unique in this anterior expansion of the process. Orientation of the process can apparently be used to distinguish trematopsids with a slit-like, closed (by the tabular) otic notch, from dissorophids. At least one such trematopsid occurs at Fort Sill, and resembles Cacops in anterior expansion of the process.
    [Show full text]
  • Phylogeny and Evolution of the Dissorophoid Temnospondyls
    Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses.
    [Show full text]
  • Heber Den Archegosaurus Der Stciiikohleiiforntatioii. Wenn Auch
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Palaeontographica - Beiträge zur Naturgeschichte der Vorzeit Jahr/Year: 1851 Band/Volume: 1 Autor(en)/Author(s): Meyer Hermann Christian Erich von Artikel/Article: Ueber den Archegosaurus der Steinkohlenformation. 209-215 © Biodiversity Heritage Library, http://www.biodiversitylibrary.org/; www.zobodat.at Heber den Archegosaurus der Stciiikohleiiforntatioii. Von Hermann von Meyer. Die Nachrichten über das Vorkommen von Reptilien in Gebilden älter als die Formation des Zechsteins hatten sich bei genauerer Prüfung immer als unhaltbar bewiesen. Man glaubte sich daher um so mehr berechtigt, anzunehmen, dass im Zechstein die ältesten Reptilien begraben lägen, als während der Versammlung der Naturforscher in Mainz Dr. Gergens und Alex. Braun mir eine Wirbelthier- Versteinerung aus dem der Steinkohlenformation angehörigen, durch seine Fische berühmten Schieferthon von Münster- Appel in der bayerschen Pfalz vorlegten, deren Beschaffenheit mehr auf ein Wirbelthier mit Füssen als auf einen Fisch schliessen Hess. Dieses merkwürdige kleine Geschöpf habe ich Anfangs 1844, es Apateon pedestris nennend, beschrieben (Jahrb. f. Min. 1844. S. 336), später aber in den Palaeontographicis (1. S. 152. Taf. 20. Fig. t.) dargelegt. Drei Jahre darauf gelang es dem Berghauptmann v. Dechen in den Sphärosideritnieren der Steinkohlenformation zu Lebach im Saarbrücken'schen, woraus zuvor ebenfalls nur Fische bekannt waren , Ueberreste zu entdecken , welche an die Gegenwart von Sauriern in diesem Ge- bilde glauben Hessen. Mit dem zu Münster-Appel gefundenen Thier stimmten sie nicht überein. Die erste Nachricht darüber theilte Goldfuss in der Niederrheinischen Gesellschaft für Natur- und Heilkunde in Bonn am 18. Februar 1847 mit.
    [Show full text]
  • Erläuterungen Zur Wegweisungskonzeption
    Regierungspräsidium Stuttgart Straßenbauverwaltung Baden-Württemberg Straße: A 6 Heilbronn-Nürnberg BAB-km 652+000 bis 663+500 A 6 Sechsstreifiger Ausbau zwischen dem AK Weinsberg und der Landesgrenze BW/BY Bretzfeld - Öhringen (PA A6-2) PROJIS-Nr.: 08 01 9920 20 FESTSTELLUNGSENTWURF Teil A Unterlage 1 Erläuterungsbericht aufgestellt: Regierungspräsidium Stuttgart Abt. 4 Straßenwesen und Verkehr Ref. 44 Straßenplanung Stuttgart, den 30.08.2017 A 6 Heilbronn - Nürnberg Seite 2 von 205 Planungsabschnitt Bretzfeld – Öhringen (PA A6-2) Erläuterungsbericht Feststellungsentwurf Erläuterungsbericht – Feststellungsentwurf 1. Darstellung der Baumaßnahme......................................................................... 8 1.1 Planerische Beschreibung .................................................................................... 8 1.2 Straßenbauliche Beschreibung ............................................................................ 9 1.3 Streckengestaltung ............................................................................................ 10 2. Begründung des Vorhabens ........................................................................... 11 2.1 Vorgeschichte der Planung, vorausgegangene Untersuchungen und Verfahren ........................................................................................................... 11 2.2 Pflicht zur Umweltverträglichkeitsprüfung ........................................................... 12 2.3 Besonderer naturschutzfachlicher Planungsauftrag ..........................................
    [Show full text]
  • Early Tetrapod Relationships Revisited
    Biol. Rev. (2003), 78, pp. 251–345. f Cambridge Philosophical Society 251 DOI: 10.1017/S1464793102006103 Printed in the United Kingdom Early tetrapod relationships revisited MARCELLO RUTA1*, MICHAEL I. COATES1 and DONALD L. J. QUICKE2 1 The Department of Organismal Biology and Anatomy, The University of Chicago, 1027 East 57th Street, Chicago, IL 60637-1508, USA ([email protected]; [email protected]) 2 Department of Biology, Imperial College at Silwood Park, Ascot, Berkshire SL57PY, UK and Department of Entomology, The Natural History Museum, Cromwell Road, London SW75BD, UK ([email protected]) (Received 29 November 2001; revised 28 August 2002; accepted 2 September 2002) ABSTRACT In an attempt to investigate differences between the most widely discussed hypotheses of early tetrapod relation- ships, we assembled a new data matrix including 90 taxa coded for 319 cranial and postcranial characters. We have incorporated, where possible, original observations of numerous taxa spread throughout the major tetrapod clades. A stem-based (total-group) definition of Tetrapoda is preferred over apomorphy- and node-based (crown-group) definitions. This definition is operational, since it is based on a formal character analysis. A PAUP* search using a recently implemented version of the parsimony ratchet method yields 64 shortest trees. Differ- ences between these trees concern: (1) the internal relationships of aı¨stopods, the three selected species of which form a trichotomy; (2) the internal relationships of embolomeres, with Archeria
    [Show full text]
  • Summary Report of Freshwater Nonindigenous Aquatic Species in U.S
    Summary Report of Freshwater Nonindigenous Aquatic Species in U.S. Fish and Wildlife Service Region 4—An Update April 2013 Prepared by: Pam L. Fuller, Amy J. Benson, and Matthew J. Cannister U.S. Geological Survey Southeast Ecological Science Center Gainesville, Florida Prepared for: U.S. Fish and Wildlife Service Southeast Region Atlanta, Georgia Cover Photos: Silver Carp, Hypophthalmichthys molitrix – Auburn University Giant Applesnail, Pomacea maculata – David Knott Straightedge Crayfish, Procambarus hayi – U.S. Forest Service i Table of Contents Table of Contents ...................................................................................................................................... ii List of Figures ............................................................................................................................................ v List of Tables ............................................................................................................................................ vi INTRODUCTION ............................................................................................................................................. 1 Overview of Region 4 Introductions Since 2000 ....................................................................................... 1 Format of Species Accounts ...................................................................................................................... 2 Explanation of Maps ................................................................................................................................
    [Show full text]
  • Curriculum Vitae June 2021
    Curriculum Vitae June 2021 Trond Sigurdsen, PhD University of Southern California, 3616 Trousdale Pkwy, AHF 105 Los Angeles, CA 90089-0371 Phone: 310 882 9584; Email: [email protected] POSITIONS: May 2017 - Present Assistant Professor, Teaching (Promoted), Instructor in general biology, vertebrate biology, phylogenetics, and human biology, University of Southern California Jan. 2014 - May 2017 Lecturer, Instructor in human biology, anatomy, and evolution (HBIO200, HBIO300, HBIO406, HBIO 301). Lab Lecturer, Biology (BISC 120, BISC 221) and Human Biology (HBIO 200), University of Southern California Jan. 2014 - Present Research Associate (Honorary), Dinosaur Institute, Natural History Museum, LA County. Jan. 2012 - Dec. 2013 Postdoctoral Fellow, McGill University, Montreal, Canada. Postdoctoral Supervisor: Robert L. Carroll; Co-Supervisor: David M. Green. Jan. 2010 - Jan. 2012 Postdoctoral Fellow, Université de Montréal, Quebec, Canada. Postdoctoral Supervisor: Thérèse Cabana (UdeM); co- supervisor: Kevin Padian (UC Berkeley). EDUCATION: Feb. 2010 Ph.D., Biology, McGill University, Montreal, Canada. Supervisors: Robert L. Carroll and David M. Green. Started Sep. 2005, defended Nov. 25, 2009. Thesis: “The Lower Permian Dissorophoid Doleserpeton (Temnospondyli), and the Evolution of Modern Amphibians.” June 2003 Cand. Scient. degree (equivalent to M.Sc.), Biology, University of Oslo, Norway. Supervisors: Jørn H. Hurum, David Bruton, and Nils C. Stenseth. June 2000 Cand. Mag. degree (equivalent to B. Sc.), Biology, University of Oslo, Norway. 1 Trond Sigurdsen 2021 USC SERVICES AND VOLUNTEERING: -Member of committee for finding a new Section Head at MEB, Biology, USC, 2021. -Interview with MEMO (Medical, Educational, Missions, and Outreach) at USC, 2021 to inspire and help students. -Dornsife Merit Scholarship interviewer (3 days), USC, 2021.
    [Show full text]
  • Gazzetta Ufficiale L 79 Dell'unione Europea
    Gazzetta ufficiale L 79 dell'Unione europea ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ ★ 60o anno Edizione in lingua italiana Legislazione 24 marzo 2017 Sommario II Atti non legislativi REGOLAMENTI ★ Regolamento di esecuzione (UE) 2017/548 della Commissione, del 23 marzo 2017, che stabilisce un modulo standard per la giustificazione scritta relativa alla rimozione o alla rottura del sigillo del tachigrafo (1) ..................................................................................... 1 Regolamento di esecuzione (UE) 2017/549 della Commissione, del 23 marzo 2017, recante fissazione dei valori forfettari all'importazione ai fini della determinazione del prezzo di entrata di taluni ortofrutticoli .................................................................................................................... 4 Regolamento di esecuzione (UE) 2017/550 della Commissione, del 23 marzo 2017, recante fissazione del prezzo minimo di vendita di latte scremato in polvere per la settima gara parziale nell'ambito della gara aperta dal regolamento di esecuzione (UE) 2016/2080 ........................................................ 6 DECISIONI ★ Decisione (UE) 2017/551 del Consiglio, del 21 marzo 2017, relativa alla nomina di un supplente del Comitato delle regioni, conformemente alla proposta del Regno di Spagna 7 ★ Decisione di esecuzione (UE) 2017/552 della Commissione, del 22 marzo 2017, relativa alla coerenza degli obiettivi per i settori essenziali di prestazione concernenti la capacità e l'efficienza economica inclusi nei blocchi funzionali di spazio
    [Show full text]
  • The Scapulocoracoid of an Early Triassic Stem−Frog from Poland
    The scapulocoracoid of an Early Triassic stem−frog from Poland MAGDALENA BORSUK−BIAŁYNICKA and SUSAN E. EVANS Borsuk−Białynicka, M. and Evans, S.E. 2002. The scapulocoracoid of an Early Triassic stem−frog from Poland. Acta Palaeontologica Polonica 47 (1): 79–96. The scapulocoracoid of Czatkobatrachus polonicus Evans and Borsuk−Białynicka, 1998, a stem−frog from the Early Tri− assic karst locality of Czatkowice (Southern Poland), is described. The overall type of scapulocoracoid is plesiomorphic, but the subcircular shape and laterally oriented glenoid is considered synapomorphic of Salientia. The supraglenoid fora− men is considered homologous to the scapular cleft of the Anura. In Czatkobatrachus, the supraglenoid foramen occupies an intermediate position between that of the early tetrapod foramen and the scapular cleft of Anura. The cleft scapula is probably synapomorphic for the Anura. In early salientian phylogeny, the shift in position of the supraglenoid foramen may have been associated with an anterior rotation of the forelimb. This change in position of the forelimb may reflect an evolutionary shift from a mainly locomotory function to static functions (support, balance, eventually shock−absorption). Laterally extended limbs may have been more effective than posterolateral ones in absorbing landing stresses, until the specialised shock−absorption pectoral mechanism of crown−group Anura had developed. The glenoid shape and position, and the slender scapular blade, of Czatkobatrachus, in combination with the well−ossified joint surfaces on the humerus and ulna, all support a primarily terrestrial rather than aquatic mode of life. The new Polish material also permits clarifica− tion of the pectoral anatomy of the contemporaneous Madagascan genus Triadobatrachus.
    [Show full text]
  • Phylogeny and Evolution of the Dissorophoid Temnospondyls
    Journal of Paleontology, 93(1), 2019, p. 137–156 Copyright © 2018, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/15/0088-0906 doi: 10.1017/jpa.2018.67 The putative lissamphibian stem-group: phylogeny and evolution of the dissorophoid temnospondyls Rainer R. Schoch Staatliches Museum für Naturkunde, Rosenstein 1, D-70191 Stuttgart, Germany 〈[email protected]〉 Abstract.—Dissorophoid temnospondyls are widely considered to have given rise to some or all modern amphibians (Lissamphibia), but their ingroup relationships still bear major unresolved questions. An inclusive phylogenetic ana- lysis of dissorophoids gives new insights into the large-scale topology of relationships. Based on a TNT 1.5 analysis (33 taxa, 108 characters), the enigmatic taxon Perryella is found to nest just outside Dissorophoidea (phylogenetic defintion), but shares a range of synapomorphies with this clade. The dissorophoids proper are found to encompass a first dichotomy between the largely paedomorphic Micromelerpetidae and all other taxa (Xerodromes). Within the latter, there is a basal dichotomy between the large, heavily ossified Olsoniformes (Dissorophidae + Trematopidae) and the small salamander-like Amphibamiformes (new taxon), which include four clades: (1) Micropholidae (Tersomius, Pasawioops, Micropholis); (2) Amphibamidae sensu stricto (Doleserpeton, Amphibamus); (3) Branchiosaur- idae (Branchiosaurus, Apateon, Leptorophus, Schoenfelderpeton); and (4) Lissamphibia. The genera Platyrhinops and Eos- copus are here found to nest at the base of Amphibamiformes. Represented by their basal-most stem-taxa (Triadobatrachus, Karaurus, Eocaecilia), lissamphibians nest with Gerobatrachus rather than Amphibamidae, as repeatedly found by former analyses.
    [Show full text]
  • A New Species of Cyclotosaurus (Stereospondyli, Capitosauria) from the Late Triassic of Bielefeld, NW Germany, and the Intrarelationships of the Genus
    Foss. Rec., 19, 83–100, 2016 www.foss-rec.net/19/83/2016/ doi:10.5194/fr-19-83-2016 © Author(s) 2016. CC Attribution 3.0 License. A new species of Cyclotosaurus (Stereospondyli, Capitosauria) from the Late Triassic of Bielefeld, NW Germany, and the intrarelationships of the genus Florian Witzmann1,2, Sven Sachs3,a, and Christian J. Nyhuis4 1Department of Ecology and Evolutionary Biology, Brown University, Providence, G-B204, RI 02912, USA 2Museum für Naturkunde, Leibniz-Institut für Evolutions- und Biodiversitätsforschung, Invalidenstraße 43, 10115 Berlin, Germany 3Naturkundemuseum Bielefeld, Abteilung Geowissenschaften, Adenauerplatz 2, 33602 Bielefeld, Germany 4Galileo-Wissenswelt, Mummendorferweg 11b, 23769 Burg auf Fehmarn, Germany aprivate address: Im Hof 9, 51766 Engelskirchen, Germany Correspondence to: Florian Witzmann (fl[email protected]; fl[email protected]) Received: 19 January 2016 – Revised: 11 March 2016 – Accepted: 14 March 2016 – Published: 23 March 2016 Abstract. A nearly complete dermal skull roof of a capi- clotosaurus is the sister group of the Heylerosaurinae (Eo- tosaur stereospondyl with closed otic fenestrae from the mid- cyclotosaurus C Quasicyclotosaurus). Cyclotosaurus buech- dle Carnian Stuttgart Formation (Late Triassic) of Bielefeld- neri represents the only unequivocal evidence of Cycloto- Sieker (NW Germany) is described. The specimen is as- saurus (and of a cyclotosaur in general) in northern Germany. signed to the genus Cyclotosaurus based on the limited con- tribution of the frontal to the orbital margin via narrow lat- eral processes. A new species, Cyclotosaurus buechneri sp. nov., is erected based upon the following unique combina- 1 Introduction tion of characters: (1) the interorbital distance is short so that the orbitae are medially placed (shared with C.
    [Show full text]