Arthropod Pattern Theory and Cambrian Trilobites

Total Page:16

File Type:pdf, Size:1020Kb

Arthropod Pattern Theory and Cambrian Trilobites Bijdragen tot de Dierkunde, 64 (4) 193-213 (1995) SPB Academie Publishing bv, The Hague Arthropod pattern theory and Cambrian trilobites Frederick A. Sundberg Research Associate, Invertebrate Paleontology Section, Los Angeles County Museum of Natural History, 900 Exposition Boulevard, Los Angeles, California 90007, USA Keywords: Arthropod pattern theory, Cambrian, trilobites, segment distributions 4 Abstract ou 6). La limite thorax/pygidium se trouve généralementau niveau du node 2 (duplomères 11—13) et du node 3 (duplomères les les 18—20) pour Corynexochides et respectivement pour Pty- An analysis of duplomere (= segment) distribution within the chopariides.Cette limite se trouve dans le champ 4 (duplomères cephalon,thorax, and pygidium of Cambrian trilobites was un- 21—n) dans le cas des Olenellides et des Redlichiides. L’extrémité dertaken to determine if the Arthropod Pattern Theory (APT) du corps se trouve généralementau niveau du node 3 chez les proposed by Schram & Emerson (1991) applies to Cambrian Corynexochides, et au niveau du champ 4 chez les Olenellides, trilobites. The boundary of the cephalon/thorax occurs within les Redlichiides et les Ptychopariides. D’autre part, les épines 1 4 the predicted duplomerenode (duplomeres or 6). The bound- macropleurales, qui pourraient indiquer l’emplacement des ary between the thorax and pygidium generally occurs within gonopores ou de l’anus, sont généralementsituées au niveau des node 2 (duplomeres 11—13) and node 3 (duplomeres 18—20) for duplomères pronostiqués. La limite prothorax/opisthothorax corynexochids and ptychopariids, respectively. This boundary des Olenellides est située dans le node 3 ou près de celui-ci. Ces occurs within field 4 (duplomeres21—n) for olenellids and red- résultats indiquent que nombre et distribution des duplomères lichiids. The termination of the body generally occurs within des Trilobites du Cambrien ont été enquelque sorte sous la con- node 3 for corynexochids and within field 4 for olenellids, red- strainte d’un certain programme de patterning génétique. lichiids, and ptychopariids. In addition, the location of macro- Cependant, l’emplacementfréquent des limites ailleurs que dans pleural spines, which may indicate the location of the gonopores les endroits pronostiqués, ainsi que le déplacementpossible des or anus, generallyfalls at the predicted duplomeres. The bound- nodes suggèrent que d’autres facteurs ont été aussi impliqués ary between the prothorax and opisthothorax of olenellids oc- dans le nombre des duplomères des diverses parties du corps. curs within or near node 3. These results indicate that the num- Cette variabilité rend plausible l’idée que les Arthropodes du ber and distribution of duplomeres within Cambrian trilobites à la différence de avaient Cambrien, ceux récents, un pro- were somewhat constrained by some genetic patterning pro- gramme génétique plus simple, ce qui facilitait l’apparition de gram. However, the common distribution ofboundaries outside modifications dans le Bauplan. of the locations and the of predicted possible shifting nodes sug- gest that other factors were also controlling the number of duplomereswithin the body parts. This variation supports the Introduction idea that Cambrian arthropods, unlike modern arthropods, had which allowed for in a simpler genetic program, easily changes the Bauplan. Interpreting morphological characters to decipher phylogenies of organisms is always a challenge. This is especially true when organisms are extinct, Résumé where there are no soft-body or biochemical re- mains to supplement the limited amount of infor- Une analyse a été entreprise de la distribution des duplomères mation provided by skeletal remains. Thus, when dans le le le des (= segments) céphalon, thorax, et pygidium be made for generalizations on Baupläne can a Trilobites du Cambrien, afin de vérifier si l’Arthropod Pattern specific group, guidelines can be generated to help Theory (APT) proposée par Schram & Emerson (1991) s’ap- the observed and plique à ces fossiles. La limite céphalon/thorax se trouve, interpret morphological patterns comme pronostiqué,au niveau du node duplomère 1 (duplomère to construct phylogenies. Such a generalization has 194 F.A. Sundberg - Arthropod pattern theory and Cambrian trilobites recently been proposed by Emerson & Schram APT implications to trilobite Baupläne and Schram & Emerson (1990) (1991). They sug- gested that the location of tagmata transitions, As a prediction of APT, changes in arthropod the and terminations gonopores, anus, body occurs Baupläne should occur in quantum jumps, from within the at specific regions Bauplan of arthro- node to node. This prediction appears to hold true pods. This Arthropod Pattern Theory (APT) was for those extinct and extant taxa discussed by both fossil and modern Schram & Emerson with few based on taxa, comparative (1991) only a excep- anatomy of exterior and interior morphology, tions. Trilobites would be a good test of APT in ontogeny, and developmental genetics, although that, unlike most modern arthropod groups, they this has not been tested. APT = theory statistically vary widely in their numberof segments ( duplo- implies that there are only a limited number of ar- meres). If APT is universal for all arthropods, then rangements of segments and other morphological changes in the numberof segments within trilobites features available to arthropods. This could in- would be in jumps, from one node to the next. In the of crease potential convergenceamong distantly addition, the locations of tagmata transitions related groups because the number of segments (cephalon/thorax and thorax/pygidial boundaries) within the body and body parts or the location of should occur within the nodes. the gonopores or anus are limited. Conversely, Other morphological features that may display related taxa also would to have distributions closely be expected APT may be the location of macro- similar distributions of in the and the the segments body. pleural spines boundary between pro- Schram & Emerson (1991) have also proposed thorax and opisthothorax in some Olenellida. Ac- that most biramous arthropods are composed of cording to Harrington et al. (1959, p. 073), macro- each duplomeres, containing two primary seg- pleural spines may indicate the location of the Both of these fused If ments. segments are typically gonopores. they do, then they wouldbe expected together and in some taxa the individual segments to occur eitherwithin a node or at duplomeres 9 or can only be recognized by the internal organization 16. of soft parts. Schram & Emerson recognized two Schram & Emerson's preliminary study sug- of of and types sequences duplomeres, nodes fields gested that trilobites display a pattern where tag- (Fig. 1). They observed that morphological changes mata boundaries occur at nodes. They studied the generally occurred at three nodes within the trilobites Triarthrus, Naraoia, Olenoides, and Ag- Bauplan : node 1 = duplomeres 5 and 6; node 2 = nostus and in each case the cephalon/thorax transi- duplomeres 11-13; and node 3 = duplomeres tion occurred in node 1. In Olenoides and Triar- 18-20. The fields are duplomeres that are relatively thrus, the thorax/pygidium transition occurred in stable because do they not generally show morpho- nodes 2 and 3, respectively. If these patterns hold logical change (field 1 = 1-4, field 2 = 7-10, field true inother trilobites, then the number of thoracic 3 = field 4 = In notable and well the location of 14-17, 21-n). some ex- pygidial segments, as as ceptions, duplomeres 9 and 16 within fields 2 and macropleural spines, could be important in deter- 3, respectively, can possess gonopores or anus; and mining the evolutionary relationship among taxa. several have and terminate in taxa an anus field 4. If the pattern does not hold true, then APT is not The isopod Ligia provides an example of mor- completely applicable to trilobites, which could phological changes and other features occurring potentially make them different from most other with the nodes (from Schram & Emerson, 1991). arthropods. Ligia has its head, thorax, and abdomen terminate at the ends of nodes 1, 2 and 3, respectively. In ad- the female of in the dition, gonopore Ligia occurs Methods first duplomere of node 2, the male gonoporeis in the last of node 2 and the anus is located duplomere This test of APT is limited to Cambrian trilobites because of in last in 3. the duplomere node the difficulty in deciphering their supergeneric classification Bijdragen tot de Dierkunde, 64 (4) - 1995 195 wi frischenfeldi the bargessensis reyndidsiformis is opiki mat ovata, arctica evens geikjei lobat t s s la el lancastrioides kin roddyi Oryctocephalina Oryctocephalops Oryctocephalus Oryctocephalus Oryctocephalus Oryctocephalus Ovatoryctocara a Cheiruroides ibirica Lancastria Oryctocara Sandoveria Ton Tonkinella Fig. 1. Distribution of duplomeres ( = segments) of representatives of Oryctocephalidae(Corynexochida) relative tothe fields and nodes predicted from APT. A (Palmer & Halley, 1979) and their apparent plasticity in mor- bite specimens. total of 348 trilobite specimens representing phology (McNamara, 1986, 1988; Hughes, 1991). This contrasts 291 species from Olenellida, Redlichiida, Corynexochida, and to later trilobite groups, where phylogenies are somewhat better Ptychopariida were studied (Appendix). Only a single specimen understood and fixed in their number of recorded unless of some groups are was per species holaspids a species were thoracic segments
Recommended publications
  • Cambrian Phytoplankton of the Brunovistulicum – Taxonomy and Biostratigraphy
    MONIKA JACHOWICZ-ZDANOWSKA Cambrian phytoplankton of the Brunovistulicum – taxonomy and biostratigraphy Polish Geological Institute Special Papers,28 WARSZAWA 2013 CONTENTS Introduction...........................................................6 Geological setting and lithostratigraphy.............................................8 Summary of Cambrian chronostratigraphy and acritarch biostratigraphy ...........................13 Review of previous palynological studies ...........................................17 Applied techniques and material studied............................................18 Biostratigraphy ........................................................23 BAMA I – Pulvinosphaeridium antiquum–Pseudotasmanites Assemblage Zone ....................25 BAMA II – Asteridium tornatum–Comasphaeridium velvetum Assemblage Zone ...................27 BAMA III – Ichnosphaera flexuosa–Comasphaeridium molliculum Assemblage Zone – Acme Zone .........30 BAMA IV – Skiagia–Eklundia campanula Assemblage Zone ..............................39 BAMA V – Skiagia–Eklundia varia Assemblage Zone .................................39 BAMA VI – Volkovia dentifera–Liepaina plana Assemblage Zone (Moczyd³owska, 1991) ..............40 BAMA VII – Ammonidium bellulum–Ammonidium notatum Assemblage Zone ....................40 BAMA VIII – Turrisphaeridium semireticulatum Assemblage Zone – Acme Zone...................41 BAMA IX – Adara alea–Multiplicisphaeridium llynense Assemblage Zone – Acme Zone...............42 Regional significance of the biostratigraphic
    [Show full text]
  • Revision of the Biostratigraphic Scheme in the Cambrian Series 2 and 3 Boundary Interval of the Holy Cross Mountains (Poland)
    See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/320166540 Revision of the biostratigraphic scheme in the Cambrian Series 2 and 3 boundary interval of the Holy Cross Mountains (Poland) Conference Paper · September 2017 CITATIONS READS 0 123 2 authors: Jakub Nowicki Anna Żylińska Faculty of Geology, University of Warsaw 8 PUBLICATIONS 30 CITATIONS 38 PUBLICATIONS 776 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: 6th International Conference on Trilobites and their Relatives. To be held in Tallinn, Estonia from 7th - 10th July 2017. View project Biotic assemblage from the mid-Terreneuvian (Cambrian) of the Holy Cross Mountains in Poland View project All content following this page was uploaded by Jakub Nowicki on 02 October 2017. The user has requested enhancement of the downloaded file. 10th Baltic Stratigraphic Conference, Chęciny 12-14 September 2017 – Abstracts of oral and poster presentations Revision of the biostratigraphic scheme in the Cambrian Series 2 and 3 boundary interval of the Holy Cross Mountains (Poland) Jakub Nowicki and Anna Żylińska Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland; [email protected]; [email protected] As it is typical for Cambrian strata, the most important fossils for the biostratigraphy in the Holy Cross Mountains (HCM) are trilobites. In the middle part of the section, specimens representing members of several trilobite families can be found, largely of the Ellipsocephalidae, and Paradoxididae, accompanied by the Solenopleuridae, Dorypygidae, Palaeolenidae and trilobites from the informal Conomicmacca/Myopsolenites clade.
    [Show full text]
  • 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.
    [Show full text]
  • Smithsonian Miscellaneous Collections Volume 101
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 101. NUMBER 15 FIFTH CONTRIBUTION TO NOMENCLATURE OF CAMBRIAN FOSSILS BY CHARLES E. RESSER Curator, Division of Stratigraphic Paleontology U. S. National Museum (Publication 3682) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION MAY 22, 1942 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 101, NUMBER 15 FIFTH CONTRIBUTION TO NOMENCLATURE OF CAMBRIAN FOSSILS BY CHARLES E. RESSER Curator, Division of Stratigraphic Paleontology U. S. National Museum (Publication 3682) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION MAY 12, 1942 Z?>i Botb QBafhtnore (prcee BALTIMORE, MD., U. S. A. ' FIFTH CONTRIBUTION TO NOMENCLATURE OF CAMBRIAN FOSSILS By CHARLES E. RESSER Curator, Division of Stratigraphic Paleonlolo<jy, U. S. National Museum This is the fifth in the series of papers designed to care for changes necessary in the names of Cambrian fossils. When the fourth paper was published it was hoped that further changes would be so few and so obvious that they could be incorporated in the Cambrian bibliographic summary, and would not be required to appear first in a separate paper. But even now it is impossible to gather all of the known errors for rectification in this paper. For example, correc- tion of some errors must await the opportunity to examine the speci- mens because the published illustrations, obviously showing incorrect generic determinations, are too poor to permit a proper understanding of the fossil. In the other instances where new generic designations are clearly indicated, erection of new genera should await the pub- lication of a paper with illustrations, because better-preserved speci- mens are in hand, or undescribed species portray the generic charac- teristics more fully and should therefore be chosen as the genotypes.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • Western North Greenland (Laurentia)
    BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK · VOL. 69 · 2021 Trilobite fauna of the Telt Bugt Formation (Cambrian Series 2–Miaolingian Series), western North Greenland (Laurentia) JOHN S. PEEL Peel, J.S. 2021. Trilobite fauna of the Telt Bugt Formation (Cambrian Series 2–Mi- aolingian Series), western North Greenland (Laurentia). Bulletin of the Geological Society of Denmark, Vol. 69, pp. 1–33. ISSN 2245-7070. https://doi.org/10.37570/bgsd-2021-69-01 Trilobites dominantly of middle Cambrian (Miaolingian Series, Wuliuan Stage) Geological Society of Denmark age are described from the Telt Bugt Formation of Daugaard-Jensen Land, western https://2dgf.dk North Greenland (Laurentia), which is a correlative of the Cape Wood Formation of Inglefield Land and Ellesmere Island, Nunavut. Four biozones are recognised in Received 6 July 2020 Daugaard-Jensen Land, representing the Delamaran and Topazan regional stages Accepted in revised form of the western USA. The basal Plagiura–Poliella Biozone, with Mexicella cf. robusta, 16 December 2020 Kochiella, Fieldaspis? and Plagiura?, straddles the Cambrian Series 2–Miaolingian Series Published online 20 January 2021 boundary. It is overlain by the Mexicella mexicana Biozone, recognised for the first time in Greenland, with rare specimens of Caborcella arrojosensis. The Glossopleura walcotti © 2021 the authors. Re-use of material is Biozone, with Glossopleura, Clavaspidella and Polypleuraspis, dominates the succes- permitted, provided this work is cited. sion in eastern Daugaard-Jensen Land but is seemingly not represented in the type Creative Commons License CC BY: section in western outcrops, likely reflecting the drastic thinning of the formation https://creativecommons.org/licenses/by/4.0/ towards the north-west.
    [Show full text]
  • 71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
    ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas.
    [Show full text]
  • 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.
    [Show full text]
  • Cambrian Trilobite Ovatoryctocara Granulata Tchernysheva, 1962 and Its Biostratigraphic Significance
    Available online at www.sciencedirect.com Progress in Natural Science 19 (2009) 213–221 www.elsevier.com/locate/pnsc Cambrian trilobite Ovatoryctocara granulata Tchernysheva, 1962 and its biostratigraphic significance Jinliang Yuan a,*, Yuanlong Zhao b, Jin Peng b, Xuejian Zhu a, Jih-pai Lin c a Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, East Beijing Road 39, Nanjing 210008, China b College of Resource and Environment Science, Guizhou University, Guiyang 550003, China c School of Earth Sciences, Ohio State University, Columbus, OH 43210, USA Received 28 March 2008; received in revised form 27 May 2008; accepted 14 August 2008 Abstract The genus Ovatoryctocara Tchernysheva, 1962, and its key species Ovatoryctocara granulata Tchernysheva, 1962, are revised. Ovatoryctocara granulata occurs near the base of the Ovatoryctocara Zone and ranges up into the lower portion of the Kounamkites Zone in the Siberian Platform. O. granulata also appears in southeastern Guizhou, South China, but O. granulata in northern Greenland may represent an indefinite species. Specimens of Ovatoryctocara from Newfoundland cannot be identified to species level. Specimens includ- ing two cranidia and three pygidia from the lower part of the Aoxi Formation at Yaxi Village, Shizhu Town, eastern Tongren, north- eastern Guizhou, were previously assigned to O. granulata, which is now reassigned as a new species O. yaxiensis sp. nov. It bears the following main features: glabella club-shaped, slightly expanded medially, with four pairs of lateral furrows, of which S1–S3 are trian- gular pits, S4 is shallow, connecting with axial furrow; shorter palpebral lobe situated a little anterior to the midway of facial suture across the fixigenae, longer posterolateral area (exsag.); semielliptical pygidium consisting of seven axial rings with a terminal piece and with eight pairs of marginal tips giving a sawtooth-like shape of the lateral margins in dorsal view.
    [Show full text]
  • Durham Research Online
    Durham Research Online Deposited in DRO: 23 May 2017 Version of attached le: Accepted Version Peer-review status of attached le: Peer-reviewed Citation for published item: Betts, Marissa J. and Paterson, John R. and Jago, James B. and Jacquet, Sarah M. and Skovsted, Christian B. and Topper, Timothy P. and Brock, Glenn A. (2017) 'Global correlation of the early Cambrian of South Australia : shelly fauna of the Dailyatia odyssei Zone.', Gondwana research., 46 . pp. 240-279. Further information on publisher's website: https://doi.org/10.1016/j.gr.2017.02.007 Publisher's copyright statement: c 2017 This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/ Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk Accepted Manuscript Global correlation of the early Cambrian of South Australia: Shelly fauna of the Dailyatia odyssei Zone Marissa J.
    [Show full text]
  • Paleontological Contributions
    Paleontological Contributions Number 3 A new Cambrian arthropod, Emeraldella brutoni, from Utah Martin Stein, Stephen B. Church, and Richard A. Robison September 30, 2011 Lawrence, Kansas, USA ISSN 1946-0279 paleo.ku.edu/contributions http://hdl.handle.net/1808/8086 Paleontological Contributions September 30, 2011 Number 3 A NEW CAMBRIAN ARTHROPOD, EMERALDELLA BRUTONI, FROM UTAH Martin Stein,1* Stephen B. Church,2 and Richard A. Robison1 1University of Kansas, Department of Geology, Lawrence, Kansas 66045, USA, [email protected], [email protected]; 2Sinclair Oil & Gas Company, Salt Lake City, Utah 84130, USA, [email protected] ABSTRACT Emeraldella is a rare arthropod of relatively large body size that belongs with the trilobite-like arthropods, Artiopoda. E. brutoni n. sp. from the Wheeler Formation of west-central Utah is the second species described and marks the first confirmed occurrence of Emeraldella outside the Burgess Shale of British Columbia. An articulated, flagelliform telson, similar to that of the Burgess Shale taxon Molaria, is recognized in Emeraldella. Evidence for the presence of lamellae on the exopods of Molaria is presented, supporting affinity of that taxon with Artiopoda. A close relationship between Emeraldella and Molaria is tentatively suggested, based on the morphology of tergites and telson. Keywords: Wheeler Formation, Drum Mountains, exceptional preservation, Arthropoda INTRODUCTION others (2007), Elrick and Hinnov (2007), Brett and others (2009), Halgedahl and others (2009), and Howley and Jiang (2010), The Wheeler Formation of west-central Utah is well known have provided more detailed information about its stratigraphy for its diverse and exceptionally preserved biota, which was and depositional environments. One of us (S.B.C.) collected the reviewed by Robison (1991).
    [Show full text]