Class Trilobita Walch, 1771. In: Zhang, Z.-Q. (Ed.) Animal Biodiversity: an Outline of Higher-Level Classification and Survey of Taxonomic Richness”
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Trilobites of the Hagastrand Member (Tøyen Formation, Lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining Non-Asaphid Groups
Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: Remaining non-asaphid groups OLE A. HOEL Hoel, O. A.: Trilobites of the Hagastrand Member (Tøyen Formation, lowermost Arenig) from the Oslo Region, Norway. Part Il: remaining non-asaphid groups. Norsk Geologisk Tidsskrift, Vol. 79, pp. 259-280. Oslo 1999. ISSN 0029-196X. This is Part Il of a two-part description of the trilobite fauna of the Hagastrand Member (Tøyen Formation) in the Oslo, Eiker Sandsvær, Modum and Mjøsa areas. In this part, the non-asaphid trilobites are described, while the asaphid species have been described previously. The history and status of the Tremadoc-Arenig Boundary problem is also reviewed, and I have found no reason to insert a Hunnebergian Series between the Tremadoc and the Arenig series, as has been suggested by some workers. Descriptions of the localities yielding this special trilobite fauna are provided. Most of the 22 trilobite species found in the Hagastrand Member also occur in Sweden. The 12 non-asaphid trilobites described herein belong to the families Metagnostidae, Shumardiidae, Remopleurididae, Nileidae, Cyclopygidae, Raphiophoridae, Alsataspididae and Pliomeridae. One new species is described; Robergiella tjemviki n. sp. Ole A. Hoel, Paleontologisk Museum, Sars gate l, N-0562 Oslo, Norway. Introduction contemporaneous platform deposits in Sweden are domi nated by a condensed limestone succession. In Norway, the The Tremadoc-Arenig Boundary interval is a crucial point Tøyen Formation is divided into two members: the lower in the evolution of several invertebrate groups, especially among the graptolites and the trilobites. In the graptolites, this change consisted most significantly in the loss of bithekae and a strong increase in diversity. -
The Case of the Diminutive Trilobite Flexicalymene Retrorsa Minuens from the Cincinnatian Series (Upper Ordovician), Cincinnati Region
EVOLUTION & DEVELOPMENT 9:5, 483–498 (2007) Evaluating paedomorphic heterochrony in trilobites: the case of the diminutive trilobite Flexicalymene retrorsa minuens from the Cincinnatian Series (Upper Ordovician), Cincinnati region Brenda R. Hundaa,Ã and Nigel C. Hughesb aCincinnati Museum Center, 1301 Western Avenue, Cincinnati, OH 45203, USA bDepartment of Earth Sciences, University of California, Riverside, CA 92521, USA ÃAuthor for correspondence (email: [email protected]) SUMMARY Flexicalymene retrorsa minuens from the upper- rate of progress along a common ontogenetic trajectory with most 3 m of the Waynesville Formation of the Cincinnatian respect to size, coupled with growth cessation at a small size, Series (Upper Ordovician) of North America lived ‘‘sequential’’ progenesis, or non-uniform changes in the rate of approximately 445 Ma and exhibited marked reduction in progress along a shared ontogenetic trajectory with respect to maximum size relative to its stratigraphically subjacent sister size, can also be rejected. Rather, differences between these subspecies, Flexicalymene retrorsa retrorsa. Phylogenetic subspecies are more consistent with localized changes in analysis is consistent with the notion that F. retrorsa retrorsa rates of character development than with a global hetero- was the ancestor of F. retrorsa minuens. F. retrorsa minuens chronic modification of the ancestral ontogeny. The evolution has been claimed to differ from F. retrorsa retrorsa ‘‘in size of F. retrorsa minuens from F. retrorsa retrorsa was largely alone,’’ and thus presents a plausible example of global dominated by modifications of the development of characters paedomorphic evolution in trilobites. Despite strong similarity already evident in the ancestral ontogeny, not by the origin of in the overall form of the two subspecies, F. -
Instituto De Geociências Revisão Sistemática E
UNIVERSIDADE DE SÃO PAULO INSTITUTO DE GEOCIÊNCIAS REVISÃO SISTEMÁTICA E PALEOBIOGEOGRÁFICA DE TRILOBITAS PHACOPIDA (HOMALONOTIDAE E CALMONIIDAE) DO DEVONIANO DAS BACIAS DO PARNAÍBA E AMAZONAS, BRASIL Felipe van Enck Meira Tese apresentada ao Programa de Pós- Graduação em Geoquímica e Geotectônica do Instituto de Geociências da Universidade de São Paulo, como parte dos requisitos para a obtenção do título de doutor. Orientadora: Prof. Dra. Juliana de Moraes Leme TESE DE DOUTORAMENTO Programa de Pós-graduação em Geoquímica e Geotectônica São Paulo 2016 “Kites rise highest against the wind - not with it.” - Winston Churchill Agradecimentos Agradeço a Deus, por sempre iluminar o caminho durante esses anos de altos e baixos do Doutorado. Agradeço a Ele também por enviar dois verdadeiros anjos da guarda à minha vida – minha esposa Angela Faleiros van Enck Meira e meu filho, Thomas Faleiros van Enck Meira. Agradeço a meus pais, José Carlos e Sylvia, e à minha irmã, Patrícia, pelo apoio durante a jornada, ainda que à distância, por vezes. Sou grato aos meus sogros, Jair e Lucia, que sempre foram como verdadeiros pais e conselheiros. À FAPESP (Processo n° 2012/07075-3), pelo suporte financeiro, sem o qual o Doutorado não seria viável. À minha orientadora, Drª. Juliana de Moraes Leme, pela orientação, discussões e esclarecimentos pertinentes ao projeto. Ao Doutorando Fabio Carbonaro e ao Dr. Renato Ghilardi (UNESP-Bauru), pela parceria e por discussões importantes na realização do trabalho. À Drª. Niède Guidon (FUMDHAM), pelo empréstimo de fósseis da região de São João Vermelho (Piauí), estudados aqui. Sou grato às seguintes pessoas, por permitirem meu acesso às instituições para visita de acervos, e por sua disponibilidade, atenção e ajuda durante minha permanência: Bushra Hussaini (AMNH), Flávia Alessandra Figueiredo, Mônica de Medina Coeli, Dr. -
Smithsonian Miscellaneous Collections Volume 148, Number 3
—r SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 148, NUMBER 3 UPPER CAMBRIAN TRILOBITE FAUNAS OF NORTHEASTERN TENNESSEE (With 21 Plates) By FRANCO RASETTI The Johns Hopkins University Baltimore, Md. (Publication 4598) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION June 10, 1965 ,v, . SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 148, NUMBER 3 l^psfarrl| 3F«ttb UPPER CAMBRIAN TRILOBITE FAUNAS OF NORTHEASTERN TENNESSEE (With 21 Plates) By FRANCO RASETTI The Johns Hopkins University Baltimore, Md. (Publication 4598) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION June 10, 1965 <.%'^ Q^fii^ CONNECTICUT PRINTERS, INC. HARTFORD, CONN., U.S.A. CONTENTS Part I. Stratigraphy and Faunas Pj^ge Acknowledgments 3 Descriptions of Localities and Sections 3 General statement 3 Hawkins County 4 Hamblen County 10 Grainger County 12 Jefferson County I5 Union County 19 Claiborne County 21 Knox County 22 Monroe County 23 Purchase Ridge, Scott Coimty, Virginia 24 Index of Localities 25 Fauna of the Cedaria Zone 26 Fauna of the Crepicephalus Zone 28 Fauna of the Aphelaspis Zone 30 Part II. Systematic Paleontology General Statement 38 Descriptions of Trilobite Genera and Species Order AGNOSTIDA 38 Family AGNOSTIDAE 38 Order CORYNEXOCHIDA 39 Family DORYPYGIDAE 39 Order PTYCHOPARHDA 40 Family LONCHOCEPHALIDAE 40 Family CATILLICEPHALIDAE 44 Family CREPICEPHALIDAE 45 Family TRI CREPICEPHALIDAE 54 Family ASAPHISCIDAE 55 Family KINGSTONIIDAE 60 Family MENOMONIIDAE 61 Family NORWOODIIDAE 64 Family CEDARIIDAE 69 Family ELVINIIDAE 71 Family PTEROCEPHALIIDAE 72, PTYCHOPARHDA of uncertain affinities 102 Undetermined trilobites 112 References 115 Explanation of Plates 118 UPPER CAMBRIAN TRILOBITE FAUNAS OF NORTHEASTERN TENNESSEE By FRANCO RASETTI The Johns Hopkins University PART I. STRATIGRAPHY AND FAUNAS The purpose of this paper is both to describe the fossils and to present them in their proper stratigraphic setting. -
Available Generic Names for Trilobites
AVAILABLE GENERIC NAMES FOR TRILOBITES P.A. JELL AND J.M. ADRAIN Jell, P.A. & Adrain, J.M. 30 8 2002: Available generic names for trilobites. Memoirs of the Queensland Museum 48(2): 331-553. Brisbane. ISSN0079-8835. Aconsolidated list of available generic names introduced since the beginning of the binomial nomenclature system for trilobites is presented for the first time. Each entry is accompanied by the author and date of availability, by the name of the type species, by a lithostratigraphic or biostratigraphic and geographic reference for the type species, by a family assignment and by an age indication of the type species at the Period level (e.g. MCAM, LDEV). A second listing of these names is taxonomically arranged in families with the families listed alphabetically, higher level classification being outside the scope of this work. We also provide a list of names that have apparently been applied to trilobites but which remain nomina nuda within the ICZN definition. Peter A. Jell, Queensland Museum, PO Box 3300, South Brisbane, Queensland 4101, Australia; Jonathan M. Adrain, Department of Geoscience, 121 Trowbridge Hall, Univ- ersity of Iowa, Iowa City, Iowa 52242, USA; 1 August 2002. p Trilobites, generic names, checklist. Trilobite fossils attracted the attention of could find. This list was copied on an early spirit humans in different parts of the world from the stencil machine to some 20 or more trilobite very beginning, probably even prehistoric times. workers around the world, principally those who In the 1700s various European natural historians would author the 1959 Treatise edition. Weller began systematic study of living and fossil also drew on this compilation for his Presidential organisms including trilobites. -
Copertina Guida Ai TRILOBITI V3 Esterno
Enrico Bonino nato in provincia di Bergamo nel 1966, Enrico si è laureato in Geologia presso il Dipartimento di Scienze della Terra dell'Università di Genova. Attualmente risiede in Belgio dove svolge attività come specialista nel settore dei Sistemi di Informazione Geografica e analisi di immagini digitali. Curatore scientifico del Museo Back to the Past, ha pubblicato numerosi volumi di paleontologia in lingua italiana e inglese, collaborando inoltre all’elaborazione di testi e pubblicazioni scientifiche a livello nazonale e internazionale. Oltre alla passione per questa classe di artropodi, i suoi interessi sono orientati alle forme di vita vissute nel Precambriano, stromatoliti, e fossilizzazioni tipo konservat-lagerstätte. Carlo Kier nato a Milano nel 1961, Carlo si è laureato in Legge, ed è attualmente presidente della catena di alberghi Azul Hotel. Risiede a Cancun, Messico, dove si dedica ad attività legate all'ambiente marino. All'età di 16 anni, ha iniziato una lunga collaborazione con il Museo di Storia Naturale di Milano, ed è a partire dal 1970 che prese inizio la vera passione per i trilobiti, dando avvio a quella che oggi è diventata una delle collezioni paleontologiche più importanti al mondo. La sua instancabile attività di ricerca sul terreno in varie parti del globo e la collaborazione con professionisti del settore, ha permesso la descrizione di nuove specie di trilobiti ed artropodi. Una forte determinazione e la costruzione di un nuovo complesso alberghiero (AZUL Sensatori) hanno infine concretizzzato la realizzazione -
Enrollment and Coaptations in Some Species of the Ordovician Trilobite Genus Placoparia
Enrollment and coaptations in some sp eeies of the Ordovician trilobite genus Placoparia JEAN-LOUIS HENRY AND EUAN N.K. CLARKSON Henry, J.-L. & Clarkson, E.N.K. 1974 12 15: Enrollment and coaptations in some species of the Ordovician trilobite genus Placoparia. Fossils and Strata, No. 4, pp. 87-95. PIs. 1-3. Oslo ISSN 0300-949l. ISBN 82-00-04963-9. The species Pl. (Placoparia) cambriensis, Pl. (Coplacoparia ) tournemini and Pl. (Coplacoparia ) borni, described by Hammann (1971) from the Spanish Ordovician, are found in Brittany in formations attributed to the Llanvirn and the LIandeilo. The lateral borders of the librigenae of Pl. (Coplacoparia) tournemini and Pl. (Coplacoparia ) borni bear depressions into which the distal ends of the thoracic pleurae and the tips of the first pair of pygidial ribs come and fit during enrollment. These depressions, or coaptative structures sensu Cuenot (1919), are also to be observed in Pl. (Placoparia) zippei and Pl. (Hawleia) grandis, from the Ordovician of Bohemia. However, in the species tournemini and borni, additional depressions appear on the anterior cephalic border, and the coaptations evolve towards an increasing complexity. From Pl. (Placoparia) cambriensis, an ancestrai form with a wide geographic distribution, two distinct populations se em to have individu· alised by a process of allopatric speciation; one of these, probably neotenous, is represented by Pl. (Coplacoparia ) tournemini (Massif Armoricain and Iberian Peninsula), the other by Pl. (Placoparia ) zippei (Bohemia). Geo graphic isolation may be indirectly responsible for the appearance of new coaptative devices. jean-Louis Henry, Laboratoire de Paleontologie et de Stratigraphie, Institut de Geologie de l'Universite, B.P. -
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. -
001-012 Primeras Páginas
PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9. -
Universidade Estadual Paulista/Unesp
UNIVERSIDADE DE SÃO PAULO INSTITUTO DE GEOCIÊNCIAS SISTEMÁTICA, TAFONOMIA E PALEOECOLOGIA DE TRILOBITA, PHACOPIDA (HOMALONOTIDAE, CALMONIIDAE), FORMAÇÃO PONTA GROSSA (DEVONIANO), SUB-BACIA APUCARANA, ESTADO DO PARANÁ, BRASIL Sabrina Pereira Soares Orientador: Prof. Dr. Marcello Guimarães Simões DISSERTAÇÃO DE MESTRADO Programa de Pós-Graduação em Geologia Sedimentar SÃO PAULO 2007 ÍNDICE I. AGRADECIMENTOS i II. APRESENTAÇÃO iii III. RESUMO vi IV. ABSTRACT viii 1. INTRODUÇÃO 01 2. DEFININDO O PROBLEMA 01 2.1. Problemática envolvida I: Sistemática dos Homalonotidae 01 2.1. Problemática envolvida II: Papel da Tafonomia na Sistemática dos Homalonotidae e Calmoniidae 03 3. ESCOPO DO ESTUDO 04 4. OBJETIVOS 08 5. DISCUSSÃO 09 5.1. Sistemática, Tafonomia e Paleoecologia dos Homalonotidae do Devoniano Paranaense 09 5.2. O Papel da Tafonomia na Taxonomia dos Homalonotidae e Calmoniidae (Trilobita, Phacopida) do Devoniano Paranaense 10 5.3. Metacryphaeus rotundatus, Um Novo Elemento da Fauna de Trilobites Calmoniidae (Phacopida), da Formação Ponta Grossa (Devoniano), Bacia do Paraná, Brasil 12 6. CONCLUSÕES 15 7. PERSPECTIVAS PARA ESTUDOS FUTUROS 16 8. REFERÊNCIAS 19 ANEXO 1 27 ANEXO 2 86 ANEXO 3 122 ANEXO 4 140 Soares, S.P. (2007) Sistemática, Tafonomia e Paleoecologia de Trilobita, Phacopida... Agradecimentos Dissertação de Mestrado. I. AGRADECIMENTOS A pós-graduanda gostaria de manifestar os mais sinceros agradecimentos às diversas pessoas e instituições que contribuíram, com grande esforço, para a realização desta Dissertação de Mestrado, dentre -
Phylogenetic Analysis of the Olenellina Walcott, 1890 (Trilobita, Cambrian) Bruce S
2 j&o I J. Paleont., 75(1), 2001, pp. 96-115 Copyright © 2001, The Paleontological Society 0022-3360/01 /0075-96$03.00 PHYLOGENETIC ANALYSIS OF THE OLENELLINA WALCOTT, 1890 (TRILOBITA, CAMBRIAN) BRUCE S. LIEBERMAN Departments of Geology and Ecology and Evolutionary Biology, University of Kansas, Lindley Hall, Lawrence 66045, <[email protected]> ABSTRACT—Phylogenetic analysis was used to evaluate evolutionary relationships within the Cambrian suborder Olenellina Walcott, 1890; special emphasis was placed on those taxa outside of the Olenelloidea. Fifty-seven exoskeletal characters were coded for 24 taxa within the Olenellina and two outgroups referable to the "fallotaspidoid" grade. The Olenelloidea, along with the genus Gabriellus Fritz, 1992, are the sister group of the Judomioidea Repina, 1979. The "Nevadioidea" Hupe, 1953 are a paraphyletic grade group. Four new genera are recognized, Plesionevadia, Cambroinyoella, Callavalonia, and Sdzuyomia, and three new species are described, Nevadia fritzi, Cirquella nelsoni, and Cambroinyoella wallacei. Phylogenetic parsimony analysis is also used to make predictions about the ancestral morphology of the Olenellina. This morphology most resembles the morphology found in Plesionevadia and Pseudoju- domia Egorova in Goryanskii and Egorova, 1964. INTRODUCTION group including the "fallotaspidoids" plus the Redlichiina, and HE ANALYSIS of evolutionary patterns during the Early Cam- potentially all other trilobites. Where the Agnostida fit within this T brian has relevance to paleontologists and evolutionary bi- evolutionary topology depends on whether or not one accepts the ologists for several reasons. Chief among these are expanding our arguments of either Fortey and Whittington (1989), Fortey (1990), knowledge of evolutionary mechanisms and topologies. Regard- and Fortey and Theron (1994) or Ramskold and Edgecombe ing evolutionary mechanisms, because the Cambrian radiation (1991). -
Introduction to the Trilobites: Morphology, Ecology, Macroevolution and More by Michelle M
Introduction to the Trilobites: Morphology, Ecology, Macroevolution and More By Michelle M. Casey1, Perry Kennard2, and Bruce S. Lieberman1, 3 1Biodiversity Institute, University of Kansas, Lawrence, KS, 66045, 2Earth Science Teacher, Southwest Middle School, USD497, and 3Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, KS 66045 Middle level laboratory exercise for Earth or General Science; supported provided by National Science Foundation (NSF) grants DEB-1256993 and EF-1206757. Learning Goals and Pedagogy This lab is designed for middle level General Science or Earth Science classes. The learning goals for this lab are the following: 1) to familiarize students with the anatomy and terminology relating to trilobites; 2) to give students experience identifying morphologic structures on real fossil specimens 3) to highlight major events or trends in the evolutionary history and ecology of the Trilobita; and 4) to expose students to the study of macroevolution in the fossil record using trilobites as a case study. Introduction to the Trilobites The Trilobites are an extinct subphylum of the Arthropoda (the most diverse phylum on earth with nearly a million species described). Arthropoda also contains all fossil and living crustaceans, spiders, and insects as well as several other extinct groups. The trilobites were an extremely important and diverse type of marine invertebrates that lived during the Paleozoic Era. They only lived in the oceans but occurred in all types of marine environments, and ranged in size from less than a centimeter to almost a meter across. They were once one of the most successful of all animal groups and in certain fossil deposits, especially in the Cambrian, Ordovician, and Devonian periods, they are extremely abundant.