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Recommended publications
  • Goniopholididae) from the Albian of Andorra (Teruel, Spain): Phylogenetic Implications
    Journal of Iberian Geology 41 (1) 2015: 41-56 http://dx.doi.org/10.5209/rev_JIGE.2015.v41.n1.48654 www.ucm.es /info/estratig/journal.htm ISSN (print): 1698-6180. ISSN (online): 1886-7995 New material from a huge specimen of Anteophthalmosuchus cf. escuchae (Goniopholididae) from the Albian of Andorra (Teruel, Spain): Phylogenetic implications E. Puértolas-Pascual1,2*, J.I. Canudo1,2, L.M. Sender2 1Grupo Aragosaurus-IUCA, Departamento de Ciencias de la Tierra, Facultad de Ciencias, Universidad de Zaragoza, c/Pedro Cerbuna 12, 50009 Zaragoza, Spain. 2Departamento de Ciencias de la Tierra, Facultad de Ciencias, Universidad de Zaragoza, c/Pedro Cerbuna No. 12, 50009 Zaragoza, Spain. e-mail addresses: [email protected] (E.P.P, *corresponding author); [email protected] (J.I.C.); [email protected] (L.M.S.) Received: 15 December 2013 / Accepted: 18 December 2014 / Available online: 25 March 2015 Abstract In 2011 the partial skeleton of a goniopholidid crocodylomorph was recovered in the ENDESA coal mine Mina Corta Barrabasa (Escu- cha Formation, lower Albian), located in the municipality of Andorra (Teruel, Spain). This new goniopholidid material is represented by abundant postcranial and fragmentary cranial bones. The study of these remains coincides with a recent description in 2013 of at least two new species of goniopholidids in the palaeontological site of Mina Santa María in Ariño (Teruel), also in the Escucha Formation. These species are Anteophthalmosuchus escuchae, Hulkepholis plotos and an undetermined goniopholidid, AR-1-3422. In the present paper, we describe the postcranial and cranial bones of the goniopholidid from Mina Corta Barrabasa and compare it with the species from Mina Santa María.
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  • An Overview of the Lower Cretaceous Dinosaur Tracksites from the Mirambel Formation in the Iberian Range (Ne Spain)
    Khosla, A. and Lucas, S.G., eds., 2016, Cretaceous Period: Biotic Diversity and Biogeography. New Mexico Museum of Natural History and Science Bulletin 71. 65 AN OVERVIEW OF THE LOWER CRETACEOUS DINOSAUR TRACKSITES FROM THE MIRAMBEL FORMATION IN THE IBERIAN RANGE (NE SPAIN) D. CASTANERA1, I. DÍAZ-MARTÍNEZ2, M. MORENO-AZANZA3, J.I. CANUDO4, AND J.M. GASCA4 1 Bayerische Staatssammlung für Paläontologie und Geologie and GeoBioCenter, Ludwig-Maximilians-Universität, Richard-Wagner-Str. 10, 80333 Munich, Germany. [email protected]; 2 CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, General Roca 1242, 8332 General Roca, Río Negro, [email protected]; 3 Departamento de Ciências da Terra, Geobiotec. Departamento de Ciências da Terra. Faculdade de Ciências e Tecnologia, FCT, Universidade Nova de Lisboa, 2829-526. Caparica, Portugal. Museu da Lourinhã. [email protected]; 4 Grupo Aragosaurus-IUCA, Paleontología, Departamento de Ciencias de la Tierra, Facultad de Ciencias, Universidad de Zaragoza, Calle Pedro Cerbuna, 12, 50009, Zaragoza, Spain. [email protected]; [email protected] Abstract—Up to now, the ichnological vertebrate record from the Barremian Mirambel Formation (NE Spain) has remained completely unknown despite the fact that osteological findings have been reported in recent years. Here we provide an overview of 11 new dinosaur tracksites found during a fieldwork campaign in the year 2011. The majority of these tracksites (seven) preserve small- to medium-sized tridactyl tracks here assigned to indeterminate theropods. Only one footprint presents enough characters to classify it as Megalosauripus isp. Ornithopod tracks identified asCaririchnium isp. and Iguanodontipodidae indet.
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  • BGS Report, Single Column Layout
    1 The Cretaceous Continental Intercalaire in central Algeria: subsurface evidence for a fluvial to aeolian 2 transition and implications for the onset of aridity on the Saharan Platform 3 A.J. Newella*, G.A. Kirbyb, J.P.R. Sorensena, A.E. Milodowskib 4 a British Geological Survey, Maclean Building, Wallingford, OX10 8BB, UK, email: [email protected] 5 b British Geological Survey, Nicker Hill, Keyworth, Nottingham, NG12 5GG, UK 6 * Corresponding author 7 Abstract 8 The Lower Cretaceous Continental Intercalaire of North Africa is a terrestrial to shallow marine 9 continental wedge deposited along the southern shoreline of the Neotethys Ocean. Today it has a wide 10 distribution across the northern Sahara where it has enormous socio-economic importance as a major 11 freshwater aquifer. During the Early Cretaceous major north-south trending basement structures were 12 reactivated in response to renewed Atlantic rifting and in Algeria, faults along the El Biod-Hassi 13 Messaourd Ridge appear to have been particularly important in controlling thickness patterns of the 14 Lower Cretaceous Continental Intercalaire. Subsurface data from the Krechba gas field in Central Algeria 15 shows that the Lower Cretaceous stratigraphy is subdivided into two clear parts. The lower part (here 16 termed the In Salah Formation) is a 200 m thick succession of alluvial deposits with large meandering 17 channels, clearly shown in 3D seismic, and waterlogged flood basins indicated by lignites and gleyed, 18 pedogenic mudstones. The overlying Krechba Formation is a 500 m thick succession of quartz- 19 dominated sands and sandstones whose microstructure indicates an aeolian origin, confirming earlier 20 observations from outcrop.
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  • PROGRAMME ABSTRACTS AGM Papers
    The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important.
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  • Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex
    Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex By Karen E. Poole B.A. in Geology, May 2004, University of Pennsylvania M.A. in Earth and Planetary Sciences, August 2008, Washington University in St. Louis A Dissertation submitted to The Faculty of The Columbian College of Arts and Sciences of The George Washington University in partial fulfillment of the requirements for the degree of Doctor of Philosophy August 31, 2015 Dissertation Directed by Catherine Forster Professor of Biology The Columbian College of Arts and Sciences of The George Washington University certifies that Karen Poole has passed the Final Examination for the degree of Doctor of Philosophy as of August 10th, 2015. This is the final and approved form of the dissertation. Phylogeny and Biogeography of Iguanodontian Dinosaurs, with Implications from Ontogeny and an Examination of the Function of the Fused Carpal-Digit I Complex Karen E. Poole Dissertation Research Committee: Catherine A. Forster, Professor of Biology, Dissertation Director James M. Clark, Ronald Weintraub Professor of Biology, Committee Member R. Alexander Pyron, Robert F. Griggs Assistant Professor of Biology, Committee Member ii © Copyright 2015 by Karen Poole All rights reserved iii Dedication To Joseph Theis, for his unending support, and for always reminding me what matters most in life. To my parents, who have always encouraged me to pursue my dreams, even those they didn’t understand. iv Acknowledgements First, a heartfelt thank you is due to my advisor, Cathy Forster, for giving me free reign in this dissertation, but always providing valuable commentary on any piece of writing I sent her, no matter how messy.
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  • 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.
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  • A New Rich Amber Outcrop with Palaeobiological Inclusions in the Lower Cretaceous of Spain
    Cretaceous Research 28 (2007) 791e802 www.elsevier.com/locate/CretRes A new rich amber outcrop with palaeobiological inclusions in the Lower Cretaceous of Spain Enrique Penalver~ a,*, Xavier Delclo`s b, Carmen Soriano b a Museo Geominero, Instituto Geolo´gico y Minero de Espana,~ Rı´os Rosas 23, E-28003 Madrid, Spain b Departament d’Estratigrafia, Paleontologia i Geocie`ncies marines, Fac. Geologia, Martı´ i Franque`s s/n, Universitat de Barcelona, E-08028 Barcelona, Spain Received 17 April 2006; accepted in revised form 11 December 2006 Available online 1 July 2007 Abstract A new amber outcrop has been found recently in a bed of lutite within the Escucha Formation near the village of Utrillas (Teruel Province), Spain. This new fossil site, which has been named San Just, contains an exceptional quantity of amber remains associated with fossilized wood and leaves of probable araucarian origin, and is dated as EarlyeMiddle Albian (Early Cretaceous). The amber is physically and chemically similar to other Spanish Early Cretaceous ambers. Values of IRTF are also similar to other Early Cretaceous ambers, except for curve values of 800e400 cmÀ1 (in which bands are not visible) and the absence of exocyclic methylenic bands at 880 cmÀ1 and 1640 cmÀ1. The latter is also a feature of Alava amber (Penacerrada~ I and II exposures), and suggests a high degree of maturation. The San Just outcrop is the second in Teruel Province in which biological inclusions (mainly insects and chelicerates) have been found in amber. Insects are represented by hyme- nopterans (Scelionidae, Evaniidae: Cretevania, Stigmaphronidae), dipterans (Dolichopodidae: Microphorites, Ceratopogonidae), thysanopterans (Stenurothripidae), and coleopterans (Cucujidae).
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  • Teruel, Spain)
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/232388110 A systematic reassessment of Early Cretaceous multituberculates from Galve (Teruel, Spain) Article in Cretaceous Research · February 2011 DOI: 10.1016/j.cretres.2010.10.003 CITATIONS READS 12 34 3 authors: Ainara Badiola José Ignacio Canudo Universidad del País Vasco / Euskal Herriko… University of Zaragoza 15 PUBLICATIONS 109 CITATIONS 430 PUBLICATIONS 3,138 CITATIONS SEE PROFILE SEE PROFILE Gloria Cuenca-Bescós University of Zaragoza 300 PUBLICATIONS 4,166 CITATIONS SEE PROFILE All in-text references underlined in blue are linked to publications on ResearchGate, Available from: José Ignacio Canudo letting you access and read them immediately. Retrieved on: 29 July 2016 Author's personal copy Cretaceous Research 32 (2011) 45e57 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes A systematic reassessment of Early Cretaceous multituberculates from Galve (Teruel, Spain) Ainara Badiola*, José Ignacio Canudo, Gloria Cuenca-Bescós Grupo Aragosaurus-IUCA,1 Paleontología, Facultad de Ciencias, Universidad de Zaragoza, Pedro Cerbuna 12, E-50009 Zaragoza, Spain article info abstract Article history: This paper includes a systematic reassessment of the Early Cretaceous (late Hauterivianeearly Barre- Received 19 April 2010 mian) multituberculate fossils of Galve (Teruel, Spain), previously studied by Crusafont-Pairó and Adr- Accepted in revised form 1 October 2010 over, and Crusafont-Pairó and Gibert in 1966 and 1976, respectively, as well the study of other Available online 4 November 2010 unpublished specimens found in the revised collection of Institut Català de Paleontologia (ICP). We here include for the first time the emended descriptions and comparisons as well as the SEM photographs of Keywords: all the specimens found in the collection and update the biostratigraphic data that they have provided.
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  • ESTADO DE LAS INVESTIGACIONES SOBRE LOS VERTEBRADOS DEL JURASICO SUPERIOR Y CRETACICO INFERIOR DE GALVE (TERUEL)L J
    Estudios Geol., 60: 179-202 (2004) ESTADO DE LAS INVESTIGACIONES SOBRE LOS VERTEBRADOS DEL JURASICO SUPERIOR y CRETACICO INFERIOR DE GALVE (TERUEL)l J. 1. Ruiz-Omeñaca*, J. 1. Canudo*, M. Aurell**, B. Bádenas**, J. L. Barco***, G. Cuenca-Bescós* y J. Ipas** RESUMEN En Galve (Teruel) hay más de 50 localidades con restos de vertebrados continentales en las Formaciones Higueruelas (Titónico), Villar del Arzobispo (Titónico superior-Berriasien­ se medio), El Castellar (Hauteriviense terminal-Barremiense basal) y Camarillas (Barre­ miense inferior). Por tanto, «Galve» no es un único yacimiento de vertebrados mesozoicos, sino una localidad con numerosos yacimientos de vertebrados del intervalo Titónico-Barre• miense, que geológicamente pertenecen a la Cuenca cretácica inferior del Maestrazgo (Cor­ dillera Ibérica Central), Subcuenca de Galve. La mayor parte de los yacimientos contienen restos óseos, pero también son abundantes los yacimientos paleoicnológicos y paleoológi• coso Los vertebrados mejor conocidos son los mamíferos y dinosaurios, aunque también hay estudios sobre los tiburones, peces óseos, anfibios, escamosos y cocodrilos. Algunos grupos, como tortugas y pterosaurios, permanencen prácticamente sin estudiar. Galve es la localidad tipo de varios taxones de vertebrados: el tiburón Lonchidion microselachos, el anfibio Gal­ verpeton ibericum, el dinosaurio Aragosaurus ischiaticus, los mamíferos Galveodon nan­ nothus, Lavocatia alfambrensis, Eobaatar hispanicus, Parendotherium herreroi, Spalacot­ herium henkeli y Pocamus pepelui, y la cáscara de huevo de dinosaurio Macroolithus turo­ lensis. Es este trabajo se revisa el estado de conocimientos sobre los vertebrados de Galve, y se actualiza la lista faunística de sus yacimientos, siendo la primera vez que se realiza teniendo en cuenta la distribución estratigráfica de los taxones.
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  • Chronostratigraphy of the Barremian-Early Albian of the Maestrat Basin (E Iberian Peninsula): Integrating Strontium-Isotope Stra
    1 Chronostratigraphy of the Barremian-Early Albian of the Maestrat 2 Basin (E Iberian Peninsula): integrating strontium-isotope 3 stratigraphy and ammonoid biostratigraphy 4 5 Telm Bover-Arnal a,*, Josep A. Moreno-Bedmar b, Gianluca Frijia c, Enric Pascual-Cebrian d, 6 Ramon Salas a 7 8 a Departament de Geoquímica, Petrologia i Prospecció Geològica, Facultat de Geologia, 9 Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain 10 b Instituto de Geología, Universidad Nacional Autónoma de México, Ciudad Universitaria, 11 Coyoacán, 04510 México D.F., Mexico 12 c Institut für Erd- und Umweltwissenschaften, Universität Potsdam, Karl Liebknecht-Str. 24- 13 25, Potsdam-Golm 14476, Germany 14 d GeoScience Limited, Falmouth Business Park, Bickland Water Road, Falmouth TR11 4SZ, 15 UK 16 17 * Corresponding author. 18 E-mail address: [email protected] (T. Bover-Arnal). 19 20 Abstract. A revised chronostratigraphy of the Barremian-Early Albian sedimentary record of 21 the Maestrat Basin (E Iberian Peninsula) is provided based on a comprehensive synthesis of 22 previous biostratigrahic data, a new ammonoid finding and numerical ages derived from 23 87Sr/86Sr values measured on shells of rudists, oysters and brachiopods. The succession, which 24 comprises eight lithostratigraphic formations, is arranged into six major transgressive- 25 regressive sequences and plotted against numerical ages, geomagnetic polarity chrons, 26 ammonoid zones and the stratigraphic distribution of age-diagnostic ammonoids, orbitolinid 27 foraminifera and rudist bivalves. The oldest lithostratigraphic unit sampled, the marine 28 Artoles Formation, is Early to Late Barremian. Above, the dinosaur-bearing deposits of the 29 Morella Formation and its coastal to shallow-marine equivalent, the Cervera del Maestrat 30 Formation, are of Late Barremian age and span at least part of the Imerites giraudi ammonoid 31 zone.
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  • Dossier Comunicaciones.Indd
    Editado por: Pedro Huerta y Fidel Torcida-Fernández-Baldor © De esta edición: Colectivo Arqueológico y Paleontológico de Salas, C.A.S. 2007 Publica: Colectivo Arqueológico y Paleontológico de Salas, C.A.S. Plaza Jesús Aparicio 9, 1º 09600 Salas de los Infantes (Burgos) E-mail: [email protected] DEPÓSITO LEGAL: BU-338-2007 LIBRO DE RESÚMENES ABSTRACTS BOOK IV Jornadas Internacionales sobre Paleontología de Dinosaurios y su Entorno IV International Symposium about Dinosaurs Palaeontology and their environment Salas de los Infantes, 13-15 de septiembre de 2007 IV Jornadas Internacionales sobre Paleontología de Dinosaurios y su Entorno Salas de los Infantes, Burgos Comité de Honor Excma. Sra. Dª. Mercedes Cabrera Calvo–Sotelo. Ministra de Educación y Ciencia. Excmo. Sr. D. César Antonio Molina. Ministro de Cultura. Excmo. Sr. D. Juan Vicente Herrera Campo. Presidente de la Junta de Castilla y León. Excmo. Sr. D. Miguel Ángel Quintanilla Fisac. Secretario de Estado de Universidades e Investigación. Ministerio de Educación y Ciencia. Excmo. Sr. D. Octavio Granado. Secretario de Estado de Seguridad Social. Ministerio de Trabajo y Asuntos Sociales. Excmo. Sr. D. Francisco José Marcellán Español. Secretario General de Política Científi ca y Tecnológica. Ministerio de Educación y Ciencia. Excmo. Sr. D. Alejandro Tiana Ferrer. Secretario de Educación. Ministerio de Educación y Ciencia. Excmo. Sr. D. Tomás Villanueva Rodríguez. Consejero de Economía y Empleo. Junta de Castilla y León Excmo. Sr. D. Juan José Mateos. Consejero de Educación. Junta de Castilla y León. Ilma. Sra. Dª. Berta Tricio López. Subdelegada del Gobierno en Burgos Magfco. y Excmo. Sr. D. José Ramón Alonso Peña.
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  • Agora Paleobotanica the Extinct Tree Fern Tempskya Corda from the Albian of Spain: Palaeophytogeographical and Palaeoenvironmental Implications Luis M
    CORE Metadata, citation and similar papers at core.ac.uk Provided by Repositorio Universidad de Zaragoza Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 1–12, 2018 Agora Paleobotanica The extinct tree fern Tempskya Corda from the Albian of Spain: palaeophytogeographical and palaeoenvironmental implications Luis M. Sender1,2*, Harufumi Nishida2,3 and Jose´ B. Diez4 1 A´ rea de Paleontologı´a, Facultad de Ciencias Geolo´gicas, Universidad de Zaragoza, 50002 Zaragoza, Spain. Email: [email protected] 2 Faculty of Science and Engineering, Chuo University, 1-13-27 Kasuga, Bunkyo, Tokyo, Japan. 3 Graduate School of The University of Tokyo, Hongo, Bunkyo, Tokyo, Japan. 4 Departamento de Xeociencias Marin˜as e Ordenacio´n do Territorio, Facultade de Ciencias do Mar, Universidade de Vigo, 36310 Vigo, Spain. *Corresponding author ABSTRACT: New evidence of the extinct tree fern of the genus Tempskya Corda from Albian deposits in western Eurasia (northeastern Spain) is presented. These plant fossil remains consist of several silicified false trunks measuring up to 1.20 m long, some of which still preserve the apex. Rhizomes and petioles are more abundant in the apical zone of the false trunk. Some false trunks preserve charcoalified tissues that can be interpreted as evidence that palaeo-wildfires affected the false trunks several times from mostly the same direction. Sedimentological evidence suggests that the fern habitat was close to coastal, tidally influenced environments. These new fossils from the Albian of Spain fill the chronological and distributional gap of Tempskya that existed in Eurasia during the Early Cretaceous. Temporal and spatial changes in Tempskya distributions are proposed on several palaeogeographical maps.
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