CURRICULUM José Ignacio CANUDO SANAGUSTÍN
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Clay Diagenesis and Low-Grade Metamorphism of Tithonian and Berriasian Sediments in the Cameros Basin (Spain)
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by EPrints Complutense Clay Minerals (2001) 36, 325–333 Clay diagenesis and low-grade metamorphism of Tithonian and Berriasian sediments in the Cameros Basin (Spain) J. F. BARRENECHEA1,*, M. RODAS1 ,M.FREY2 , J. ALONSO-AZCA´ RATE3 4 AND J. R. MAS 1 Departamento de Cristalografı´a y Mineralogı´a, Universidad Complutense de Madrid, 28040 Madrid, Spain, 2 Mineralogisch-Petrographisches Institut, Basel University, CH 4056 Basel, Switzerland (deceased), 3 Facultad de Ciencias del Medio Ambiente, Universidad de Castilla-La Mancha, Fa´brica de Armas, 45071 Toledo, Spain, and 4 Departamento de Estratigrafı´a, Universidad Complutense de Madrid, 28040 Madrid, Spain (Received 29 February 2000; revised 13 October 2000) ABSTRACT: The clay mineral assemblages of the Tithonian and Berriasian sediments (Tera and Oncala Groups) in the eastern part of the Cameros basin are investigated at seven localities. The lowest-grade assemblage, located on the southern border of the basin, contains calcite + quartz + hematite + kaolinite + mixed-layer illite-smectite (R = 1, 65À85% illite layers) + discrete illite (IC = 0.5À0.65D82y). Systematic increases in the illite and chlorite crystallinities suggest increasing metamorphic grade from the northwest part of the basin to the southeast. This trend does not follow the pattern previously described for the overlying late Berriasian–early Aptian sediments (Urbio´n and Enciso Groups), which exhibit a higher metamorphic grade. This may result from local variations in sedimentary facies, as well as the circulation of hot migratory fluids. Tertiary compression occurring long after the main metamorphic event is considered to be responsible for the enhanced illite and chlorite crystallinities measured in the SE extreme of the basin. -
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. -
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. -
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. -
CURRICULUM De José Ignacio CANUDO
CURRICULUM de José Ignacio CANUDO SANAGUSTÍN 1 de Julio del 2014 Nombre: José Ignacio Apellidos: CANUDO SANAGUSTIN Lugar y Fecha de Nacimiento: Zaragoza 13/ 8/ 1960 DNI: 17.868.207 Titulación académica: Doctor en Ciencias (Paleontología) Situación Profesional: Profesor Titular de Universidad. Dirección de Trabajo: Universidad de Zaragoza. Teléfono de trabajo: 976762248 Fax: 976761088 Correo electrónico: [email protected] Página Web: http://www.aragosaurus.com/ Código Unesco: 2416 Expediente académico 2 1. EXPEDIENTE ACADEMICO 1.1 Licenciatura 1.1.1 Estudios de Licenciatura - Promoción: Licenciatura en Junio de 1985. Promoción 1980-85. Plan de Estudios de 1973. - Lugar: Licenciatura de Geológicas. Facultad de Ciencias de la Universidad de Zaragoza. 1.1.2 Tesis de Licenciatura Estudio paleontológico con énfasis bioestratigráfico del Eoceno entre Jaca y Berdún (Huesca) - Lugar: Edificio de Geológicas. Universidad de Zaragoza. - Fecha: 2 de Diciembre de 1985. - Director: Eustoquio Molina. Universidad de Zaragoza. - Tribunal: Joaquín Villena (Departamento de Estratigrafía), Gonzalo Pardo (Departamento de Estratigrafía), Doctor Eustoquio Molina (Departamento de Paleontología). - Sobresaliente (por unanimidad). 1.2 Doctorado 1.2.1 Cursos de Doctorado - Evolución y paleoecología de los homínidos. Sobresaliente. Eustoquio Molina (1985-86). - Incidencia de la Paleontología en las Ciencias Geológicas. Sobresaliente. Eladio Liñán (1985-86). - Origen y evolución de los homínidos. Sobresaliente. Eustoquio Molina (1986-87). - Relaciones entre organismo y substrato. Sobresaliente. Eladio Liñán (1986-87). 1.2.2 Tesis Doctoral Los foraminíferos planctónicos del Paleoceno-Eoceno en el Prepirineo meridional y su comparación con la Cordillera Bética. - Lugar: Edificio de Geológicas. Universidad de Zaragoza. - Fecha: 6 de Junio de 1990 - Director: Eustoquio Molina. Universidad de Zaragoza. -
The Widespread Distribution of a Late Jurassic Theropod with Well-Padded Feet
GAIA N°15, LlSBOAlLISBON, DEZEMBRO/DECEMBER 1998, pp. 339-353 (ISSN: 0871-5424) THERANGOSPODUS: TRACKWAY EVIDENCE FOR THE WIDESPREAD DISTRIBUTION OF A LATE JURASSIC THEROPOD WITH WELL-PADDED FEET Martin G. LOCKLEY Geology Department, Campus Box 172, University of Colorado at Denver. P.O. Box 173364, DENVER, COLORADO 80217-3364. USA E-mail: [email protected] Christian A. MEYER Universitat Basel, Geologisch-palaontologisches Institut. Bernoullistrasse, 32, BASEL, CH-4056. SWITZERLAND E-mail: [email protected] Joaquin J. MORATALLA Unidad de Paleontologia, Departamento Biologia, Universidad Aut6noma de Madrid. CANTOBLANCO 28049, MADRID. SPAIN ABSTRACT: Assemblages of distinctive, medium·sized theropod tracks indicative of animals with well-padded feet are known from large Upper Jurassic samples of well-preserved mate rial from North America and Asia. These tracks, herein named Therangospodus pandemi cus, always reveal a lack of distinct, separate digital pads, regardless of whether they are preserved as casts or molds. We interpret this as consistent ichnological evidence of a fleshy fool. Similar tracks from the ?Upper Jurassic-?Lower Cretaceous of Spain, first na med Therangospodus onca/ensis, are also formally described. Although the fleshy nature of the foot of this trackmaker, makes it's individual digits appear comparable with those of ornithopod trackmakers, the elongate track and asymmetric postero-medial indentation and narrow trackway, indicate that it is probably of theropod an affinity. Tracks of this type provide an instructive lesson for ichnologists and paleontologist in general because they reveal that tracks are a record of flesh on foot bones, and need not necessarily be an accura te reflection of the morphology of foot skeletons. -
Easily Altered Minerals and Reequilibrated Fluid Inclusions Provide Extensive Records of Fluid and Thermal History: Gypsum Pseud
Cent. Eur. J. Geosci. • 4(2) • 2012 • 246-260 DOI: 10.2478/s13533-011-0055-x Central European Journal of Geosciences Easily altered minerals and reequilibrated fluid inclusions provide extensive records of fluid and thermal history: gypsum pseudomorphs of the Tera Group, Tithonian-Berriasian, Cameros Basin Research Article Laura González-Acebrón1, Robert H. Goldstein2, Ramon Mas1, Jose Arribas3 1 Dpto. Estratigrafía, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid (UMC) – Instituto de Geociencias (IGEO, CSIC-UCM), Madrid, Spain 2 Department of Geology, University of Kansas, Lawrence, Kansas, USA. 3 Dpto. Petrología y Geoquímica. Facultad de Ciencias Geológicas, Universidad Complutense de Madrid (UCM) – Instituto de Geociencias (IGEO, CSIC-UCM), Madrid, Spain Received 30 October 2011; accepted 30 January 2012 Abstract: This study reports a complex fluid and thermal history using petrography, electron microprobe, isotopic analysis and fluid inclusions in replacement minerals within gypsum pseudomorphs in Tithonian-Berriasian lacustrine de- posits in Northern Spain. Limestones and dolostones, formed in the alkaline lakes, contain lenticularly shaped gypsum pseudomorphs, considered to form in an evaporative lake. The gypsum was replaced by quartz and non-ferroan calcite (Ca-2), which partially replaces the quartz. Quartz contains solid inclusions of a preexisting non-ferroan calcite (Ca-1), anhydrite and celestine. High homogenization temperatures (T h) values and inconsistent thermometric behaviour within secondary fluid inclusion assemblages in quartz (147-351◦C) and calcite (108-352◦C) indicate high temperatures after precipita- tion and entrapment of lower temperature FIAs. Th are in the same range as other reequilibrated fluid inclusions from quartz veins in the same area that are related to Cretaceous hydrothermalism. -
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. -
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. -
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. -
A New Dinosaur Tracksite with Small Footprints in the Urbión Group (Cameros Basin, Lower Cretaceous, La Rioja, Spain)
Journal of Iberian Geology 41 (1) 2015: 167-175 http://dx.doi.org/10.5209/rev_JIGE.2015.v41.n1.48661 www.ucm.es /info/estratig/journal.htm ISSN (print): 1698-6180. ISSN (online): 1886-7995 A new dinosaur tracksite with small footprints in the Urbión Group (Cameros Basin, Lower Cretaceous, La Rioja, Spain) I. Díaz-Martínez1,2*, E. García-Ortiz3, F. Pérez-Lorente1 1Universidad de La Rioja, c/Madre de Dios 51-53, 26006 Logroño (La Rioja), Spain 2CONICET - Instituto de Investigación en Paleobiología y Geología, Universidad Nacional de Río Negro, c/ General Roca 1242, 8332 Fisque Menuco-General Roca (Río Negro), Argentina. 3Universidad de León. Área de Paleontología. Dpto. Geografía y Geología. Facultad de Filosofía y Letras. Campus de Vegazana, s/n. 24071, León, Spain e-mail addresses: [email protected] (I.D.M., *corresponding author); [email protected] (E.G.O); [email protected] (F.P.L.) Received: 15 January 2014 / Accepted: 18 December 2014 / Available online: 25 March 2015 Abstract A new dinosaur tracksite (La Rueda) with ten small tridactyl footprints (the length ranges between 9 and 15 cm) from the Urbión Group (Cameros Basin, Lower Cretaceous, La Rioja, Spain) is described. The footprints are approximately as long as wide and have high divarica- tion angles between digits II-IV (~80º), some pad impressions on each digit, claw marks, a medial notch and a circular heel pad impression. They are here classified as indeterminate ornithopod footprints and contribute to the increase in the dinosaur ichnodiversity of the Urbión Group. Small dinosaur footprints are scarce in the worldwide fossil record. -
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.