Conodonta.Pdf

Total Page:16

File Type:pdf, Size:1020Kb

Conodonta.Pdf THE CONODONTA G- lesources,and Morphology,Taxonomy, Paleoecology, andEvolutionary History of a Long-ExtinctAnimal Phylum 3 azI High-pressure WALTERC.SWEEL EE: TheOhio State University fIt;:t F by the -i-:ztlog' fr, :.1 a olution- b.-;:n- New York . Oxford CLARENDON PRESS. OXFORD . 1988 PREFACE Conodonts are common fossils.Almost anyone portant group, I ofer my account of the who dealson a regularbasis with Paleozoicand Conodonta. Triassic marine rocks has probably seena few For their "witting" or unwitting contribu- of them. Through the last 30 yedrs conodonts tions to what I believe I know about the fasci- have come to be of exceptionalvalue in bio- nating gtoup of extinct animals described on stratigraphy, and they now have pride of place the following pages,I am gateful to a long list as index fossils in many parts of the geologic of my students and faculty colleaguesat The column. But conodonts are extinct and are un- Ohio StateUniversity, especiallyStig M. Bergs- knowo to most neontologists. The sketchiness trijm, and to members of the Pander Society, ofinformation about them in most texts on in- an intemational group of exceptionally good- vertebrate paleontology may result either fiom natured "conodontologists"that has met fre- the fact that they are microfossils that haye quently and infomally thougl the last 20 only lately come to be important as strati- years to share infomation about conodonts, graphic tools, or from the fact that nothing argueconclusions, and correct the misappre- quite like them exists today, so their zoologic hensionsof its seniormembers. relations axeuncertain. Karen Tyler, faculty illustrator at The Ohio In this monograph, I provide a summary of State University, drafted nea y all the figures information about a group with which I have from my very crude copy and assistedwith la- worked all my adult life. Charts that name con- beling others. Dr. Jerzy Dzik, of the Polish odont-based biozones and show stratigraphic Acaderny of Sciences, Warszawa, provided rangeofselected conodont speciesare included about half the stippled drawings of conodonts as Appendix B. However, I have purposely that gace various figuresin Chapter 5- The an- avoided a recap of conodont biostratigtaphy istry of tlrese two good friends is plainly evi- becauseit is constantly changing and cunent dent in their work and is warmlY views are readily available in various other acknowledged. places.Instead, I focus here on the conodonts I am also grateful to Sue Shipley and David as a group of extinct animals, about which it is Little, of The Ohio State University, for their important to know as much as possible be- help in completing various parts of the manu- fore assessing their distribution biostrati- script and illustrations, and to Mark Klefner, graphically. who graciously cornpiled information on the Of course, one takes considerablerisk in at- ranges of Silurian conodonts and assembled tempting such a summary, particularly of a the Silurian chart in Appendix B. The Depart- group of animals known only from its fossil re- ment of Geology and Mineralology generously cord, becausemost of what I think I know assumedmuch of the expenseof drafting and about conodontsas animals is either conjecture photogaphy. or a highly personalinterpretation ofa still-irn- perfect fossil record. So, with the caveal that Columbus, Ohio w.c.s. whal followsis only one way of viewingan im- February 1988 CONTENTS l. Inhoduction l.l History ofdiscovery and study 3 1.2 Achievements 7 1.3 Pending problems 8 2. Skeletal anatomy 11 2.1 Composition of conodont elements ll 2.2 Structure of skeletalelements t2 2.3 Shapesof element crowns t4 2.3.1 Coniform crowns l5 2.3.2 Ramiform crowns t6 2.3.3 Rastratecrowns l8 2.3.4 Pectiniformcrowns t9 2.4 Symmetry- and curvature-transitionseries 22 2.5 Skeletalapparatuses 2.6 Symmetry of elements,element pairs, and apparatuses 25 J. Whole-animal anatomy 28 3.1 The Scottish Carboniferousspecimens 28 3.2 The Waukeshaspecimen 3Z 3.3 Histology of demineralizedtissues 33 3.4 Summary JJ 4. Taxonomy 35 4.1 Form taxonomy J) 4.2 Multielementtaxonomy 36 4.2.1 Multielementmethodology 4-3 Multielement classifications 4l 4.4 A revised multielement classification 41 5. The major conodontgroups 45 5.1 Introduction 45 5.2 Cavidonti and Conodonti 45 5.3 The Proconodontida (Cavidonti) and its families (Fig. 5.1) 45 5.4 The Belodellida and its families (Fig. 5.1) 49 5.5 OrderProtopanderodontida, new 5l 5.5.1 Family ProtopanderodontidaeLindstrtim, 1970 52 5.5.2 Family ClavohamulidaeLindstrdm, 1970 53 5.5.3 Family AcanthodontidaeLindstritm, 1970 54 5.5.4 Family DrepanoistodontidaeFihraeus and Nowlan, 1978 54 t vtl III eIc,(Ju?rrr^opro ele-I pue opprw z.€.9 B €€l II pue I selci(c I'9 9 B €[l selc,brsplo-puoces t.g ) r'8 ztr selc^crurel-?uo'I Z'2 9 t ztr uroll?dIpre^O lZ'9 I 0€r surened./hrsJe^r( Z'g I 6ZI uorpnporlul I'9 ) €'8 s z'8 6Zl suraDEd.tftuopnlo^fi v r'8 'lqeN pu? uosuerge"p4uopoeloJ qal oql '8 tzr ??6I I.0l.s tzr u,l^Irrrrs{ ou)lun JspJO 0I'S zzl 196l 'sapoqupue u4snv a?pqleuaolse^flurq €1.6.s 'sepoqupu? u48nv e"pqleuEsn^?Jr{lrureJ L 0zl I86I zl.6.s 'reulu e"pqleuEolee^\s,{Iulec L Ltl 9g6l I I.6's SII 'IJelJ eap4uopoqpuftqruvi(Iu"c {. 9'L 7,L61 01.6.s €II 'quoiasauuloHpu? srxeH eeprluopoql"u8orpl L e€6I 6.6's III snqQuSpSoApue DaUqroT^lrtued g'6 L S ll\au.eep4uopoqleuc dlrued L 60r L.6.s 'sepoqupu? urlsnv eepqleuSolcrla L 90r Ig6I 9.6.9 ,reu.e?prdelolerul?d^lluleg^lrued I SL z0l 5.6.5 .relssegesprqlsuai(lod flruleg L 66 sz6l ,.6.s 'redooJeup4uopornBdsoreld ]{lrurEJ L 86 LL6l E 6.s Ltt 'reddelxeeprTlele{co) {[u]BJ L Ig6I 2.6.5 s ?'r 06 6S6l 'sseHe"p4uopoqleu8oqteds I.6.s 68 'Irzq ?prurpolrBzo^IruBJ eqJ L 916l 6's L8 'uro.4spurla?prTlelopuoc /(Iuleg L 016I s.g.s g tL s8 zL6l'TrelJeuprruoslllg/([rrrEg t.g.s .ur-o.4spur.Ie"pr-rlleuEorlceg I zL €8 016l r{lrureJ €.9.s I8 :relssege"puporuogd /{lrluec q IL 9Z6l z.g.s OL tt6l 'Iqew pue uosu?rge?prqleutorqc {IIu"c I.g's FOslEd '' 8L ,{\ou'eprurporuoFd aql g s 9L 016I'ruo4spur-IsBprluopouod,(lruJel zI. L's SL 016I 'urgrtspur.I*pqtsuEoprdrqu ll' L.s s 8'9 NL 6S6l 'ss?Hosprluoporuo!^J ,tllru?{^lrru?d 0I.L.s 9 ct ,r\eu'eeprurpopald ,qFued 6'L'g 9 ZL tg6l 'slrrsH e"p4uopolsro4lnll g.t.s rruorlstrege"pql"utoceld^lod^llure{ x L9 IL Ig6l ^Irue{ L.L-9 9 69 ts6l 'rellnn pu? relml I e?pnuopoucl.,(Iuleg g L.s 9 /o Ig6I 'redd"Dl eepquopouolsr(IJ{lruleg S-L-S 9 s9 1l\eu'eepqlepoucl/(IIuIug v'L's f. 9'9 t9 6S6l 'sseHe"pqleuEopg ,{IurBJ E L.s rI s'9 z9 9z6l 'r3lss?ge?pquoporuoud {lrrrrBJ z.L's a v9 09 016l 'ur-o.4spur.Ie"puuopolsro lL.s 9 6S 9L6I'I:IZ(, sprluoporuoud^lruru eqJ ,'s r 9 9S 0t6I'rrrojtspur.I e?prluopolepued^lrruBJ I.9.S v 9 ss spquoporepuedeql 9'9 hl SJNAINOC IITA L \,,, CONTENTS lx 55 6.3.3 Siluriancycles r34 fb 6.3.4 Devonian and Carboniferouscycles 135 59 6.3.5 Permian and Triassic cycles r37 60 6.4 Extinction 138 62 6.5 Iterativeevolutionarypatterns 140 63 6.6 Evolutionary trends t42 65 6.6.1 Apparatuselaboration t42 67 6.6.2 Apparatusreduction 143 69 6.6.3 Elaboration of elementsin P positions 144 7l 6.7 Developmentalslralegies 145 72 6.7.1 Recapitulation 145 6.7.2 Paedomorphosrs t46 74 6.8 Summary t46 75 76 78 7. Paleoecologyand paleobiogeography 149 79 8l 7.1 Introduction 149 83 7.2 Mode of life, or habit, of conodonts 149 7.3 Ecologicmodels 6) 150 87 1.3.1 Thedepth-stratificationmodel l5l 89 1.3.2 The lateral-segegationmodel 152 90 7.4 Selectedstudies of conodont ecology 152 9'7 7.4.1 Ordovician paleoecologyof Cincinnati Region t52 98 7.4.2 Mississippianpaleoecology, western United States 157 99 7.4.3 Paleoecologyof Pennsylvanianconodonts 160 t02 7.5 Ecologicgeneralizations 164 r06 7.5.1 Depth as a factor 165 109 7.5.2 Ternperutureas a factor 165 tlt 7.5.3 Nearshoreand ofshore faunas 165 7.5.4 Phyletic changesin ecologicaldistribution l_ - ::l 113 t66 115 7.6 Paleobiogeography 166 |7 7.6.1 Late Cambrian and Ordovician paleobiogeography t67 t20 7.6.2 l-ater Paleozoicand Triassic paleobiogeography 167 122 123 8, The phylum Conodonta 170 t23 8.1 A personalbias 170 t29 8.2 Summary of conodont characters 170 8.3 Conodonts as invertebrates t7l r29 8.3.1 Arthropod and annelid connections t7l r30 8.3.2 Molluscanconnections 172 132 8.3.3 Connectionswith other invertebrates 173 132 8.4 Conodonts as chordates 175 133 8.4.1 The opinions of Pander 175 133 8.4.2 Newberry, Hinde, Huxley and Myxine r75 t34 8.4.3 Macfarlane and the nemertineanconnection 176 s07 XAPUI 68r sueqc e?uerrrqder8uats g xrpuaddv s8l etuopouoJ eql Jo uo4?cgrsselctuputuns v v xpuoddv z8l ro^ug..I g.g I8I seuru{geol?pJoqc ?urlecrpur sernlee3 Jo fu?ruruns 6.t.g 6LI auxftl,tJ1o snteredd?pnAuq eqJ g.r.g suourceds LLI snolgJruoqJ?Jqsr ors eqlJo suorlelsrfualuy 4.7.g LLI slualuoleJo qyro:8 pue uoqrsodruoJ 9.t.9 9LI IBllaletu ,{uoq pseq Jo uorl"laJfuelur pue fus^ocsrq S.r'g 9LI relsssgpu? qslrlnJoJerTeq eqL n.v.g troJ eqJ SJ-NETNOi) The Conodonta 176 t76 t77 t77 t79 181 t82 185 189 lu) sr Jl ? -ro j I SUOIlqer ,i(qroN h or e,ia ',(e^rnslmrEoloaC srourlll ,{q peqsruJnJ,tlpuDl se^ntsod -EIp Jolo3 uro+ apeIII quud 'snpoqwug ^oupoU P SJTUEe_I elrq^\ pue \Jelg Jo seroads_ed^lpel?u8rsap ,{lluacor s?^{ rr qcrgA '(,(punou) snpaultrq snpoqpug slueseJderpue eueluol uI $lcoJ snoJeJruoqffCrando-I t FxuJs .srourll I , il sruoq uro{ sr e8elqueswurouog ur $IcoJ(u"unossrl I) ueru?Al^suusdruo{ ,(sepoql{)snrld,t mqpuSo .gtx ,slueuale |$O-XJ Jq us Jo ed,tloloqsr dol tp atelqruassv luopouocJosaEelqruesie prnlep F suopo r {qr uI 'tuJsard + m uJrq F J{OZOel lfuL\los le lxxroJ Jql q leql lnq cfed srql D :{IO lsEAI lE-fueduroJ slrsso_I qer naql :qr:roru b ;mssed ?rI _to fg G rGololq hs Eruoq |D 'ulued r|e F:ujeal ppol-t ou1 r -iqdB-6'u Fdar rsot! &1u.uo5 x sdno-6 IP|:-j llJto lEseq lual lsqf, ale.$ t D Jrqde6 3122\ $.el e lEi sFsso_I FB PaESU lsso_loDlur lla-rur luJn FisE lsour P IJOJ Juu r ls.n! Fl.\\ ?J 'I I.L\I tt 4! 1.
Recommended publications
  • Maquetación 1
    ISSN (print): 1698-6180. ISSN (online): 1886-7995 www.ucm.es /info/estratig/journal.htm Journal of Iberian Geology 33 (2) 2007: 163-172 Sephardiellinae, a new Middle Triassic conodont subfamily Sephardiellinae, una nueva subfamilia de conodontos del Triásico Medio P. Plasencia1, F. Hirsch2, A. Márquez- Aliaga1 1Instituto Cavanilles de Biodiversidad y Biología Evolutiva and Departamento de Geología. Universidad de Valencia, Dr. Moliner 50, 46100 Burjassot, Spain. [email protected], [email protected] 2Naruto University of Education, Naruto, Tokushima,Tokushima, Japan. [email protected] Received: 26/02/06 / Accepted: 09/10/06 Abstract Sephardiellinae (nov. subfam.) encompasses a Middle Triassic Gondolleloid lineage that originated in the Sephardic realm, west- ernmost shallow Neotethys, from where, in the course of the Ladinian and earliest Carnian, some of its species spread to the world oceans, before extinction as a result of the Carnian salinity crisis. It is composed of two genera, Sephardiella and Pseudofurnishius. Differential criteria in its septimembrate apparatus are the basal cavity structure of P1 element and morphological variations in the P2 and S3 elements. Keywords: Conodonts, Middle Triassic, Sephardiellinae, Sephardic Realm, Neotethys. Resumen La nueva subfamilia Sephardiellinae está comprendida dentro del linaje de Gondolellidae del Triásico Medio y se originó en el Dominio Sefardí, la parte más occidental del Neotetis. Durante el Ladiniense-Carniense Inferior, algunas de sus especies irradian y se distribuyen por todos los océanos. Su extinción está relacionada con la crisis de salinidad que tuvo lugar en el Carniense. La nueva subfamilia está constituida por dos géneros, Sephardiella y Pseudofurnishius las diferencias morfológicas de su aparato sep- timembrado, como son la estructura de la cavidad basal del elemento P1 y las variaciones morfológicas de los elementos P2 y S3, constituyen el criterio utilizado.
    [Show full text]
  • BIASES in INTERPRETATION of the FOSSIL RECORD of CONODONTS by MARK A
    [Special Papers in Palaeontology, 73, 2005, pp. 7–25] BETWEEN DEATH AND DATA: BIASES IN INTERPRETATION OF THE FOSSIL RECORD OF CONODONTS by MARK A. PURNELL* and PHILIP C. J. DONOGHUE *Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK; e-mail: [email protected] Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK; e-mail: [email protected] Abstract: The fossil record of conodonts may be among and standing generic diversity. Analysis of epoch ⁄ stage-level the best of any group of organisms, but it is biased nonethe- data for the Ordovician–Devonian interval suggests that less. Pre- and syndepositional biases, including predation there is generally no correspondence between research effort and scavenging of carcasses, current activity, reworking and and generic diversity, and more research is required to bioturbation, cause loss, redistribution and breakage of ele- determine whether this indicates that sampling of the cono- ments. These biases may be exacerbated by the way in which dont record has reached a level of maturity where few genera rocks are collected and treated in the laboratory to extract remain to be discovered. One area of long-standing interest elements. As is the case for all fossils, intervals for which in potential biases and the conodont record concerns the there is no rock record cause inevitable gaps in the strati- pattern of recovery of different components of the skeleton graphic distribution of conodonts, and unpreserved environ- through time. We have found no evidence that the increas- ments lead to further impoverishment of the recorded ing abundance of P elements relative to S and M elements spatial and temporal distributions of taxa.
    [Show full text]
  • Back Matter (PDF)
    Index Page numbers in italic denote Figures. Page numbers in bold denote Tables. Acadian Orogeny 224 Ancyrodelloides delta biozone 15 Acanthopyge Limestone 126, 128 Ancyrodelloides transitans biozone 15, 17,19 Acastella 52, 68, 69, 70 Ancyrodelloides trigonicus biozone 15, 17,19 Acastoides 52, 54 Ancyrospora 31, 32,37 Acinosporites lindlarensis 27, 30, 32, 35, 147 Anetoceras 82 Acrimeroceras 302, 313 ?Aneurospora 33 acritarchs Aneurospora minuta 148 Appalachian Basin 143, 145, 146, 147, 148–149 Angochitina 32, 36, 141, 142, 146, 147 extinction 395 annulata Events 1, 2, 291–344 Falkand Islands 29, 30, 31, 32, 33, 34, 36, 37 comparison of conodonts 327–331 late Devonian–Mississippian 443 effects on fauna 292–293 Prague Basin 137 global recognition 294–299, 343 see also Umbellasphaeridium saharicum limestone beds 3, 246, 291–292, 301, 308, 309, Acrospirifer 46, 51, 52, 73, 82 311, 321 Acrospirifer eckfeldensis 58, 59, 81, 82 conodonts 329, 331 Acrospirifer primaevus 58, 63, 72, 74–77, 81, 82 Tafilalt fauna 59, 63, 72, 74, 76, 103 ammonoid succession 302–305, 310–311 Actinodesma 52 comparison of facies 319, 321, 323, 325, 327 Actinosporites 135 conodont zonation 299–302, 310–311, 320 Acuticryphops 253, 254, 255, 256, 257, 264 Anoplia theorassensis 86 Acutimitoceras 369, 392 anoxia 2, 3–4, 171, 191–192, 191 Acutimitoceras (Stockumites) 357, 359, 366, 367, 368, Hangenberg Crisis 391, 392, 394, 401–402, 369, 372, 413 414–417, 456 agnathans 65, 71, 72, 273–286 and carbon cycle 410–413 Ahbach Formation 172 Kellwasser Events 237–239, 243, 245, 252
    [Show full text]
  • Durham E-Theses
    Durham E-Theses Biotic recovery of conodonts following the end-Ordovician mass extinction Radclie, Gail How to cite: Radclie, Gail (1998) Biotic recovery of conodonts following the end-Ordovician mass extinction, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/4686/ 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 Durham E-Theses • 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 Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk Biotic Recovery of Conodonts following the End-Ordovician Mass Extinction Gail Radcliffe Department of Geological Sciences University of Durham The copyright of this thesis rests with the author. No quotation from it should be published without the written consent of the author an information derived from it should be acknowledged. Volume 2 1? ..... .A thesis submitted in partial fulfilment of the degree of Doctor of Philosophy , University of Durham 1998 / Volume 2 Table of Contents Title Page i Table of Contents ii Appendix A: Systematic Palaeontology A.1 Introduction Al A.
    [Show full text]
  • A Database of Triassic Conodonts from a Comprehensive Revision of Literature
    SPANISH JOURNAL OF PALAEONTOLOGY A database of Triassic conodonts from a comprehensive revision of literature Pablo PLASENCIA1,2*, Ana MÁRQUEZ-ALIAGA2 & Jingeng SHA1 1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology (CAS), Nanjing, 39 East Beijing Road, Nanjing, 210008, People’s Republic of China; [email protected]; [email protected] 2 Departamento de Geología, Universitat de Valencia, Dr. Moliner, 50, 46100 Burjassot, Valencia, Spain; [email protected] * Corresponding author Plasencia, P., Márquez-Aliaga, A. & Sha, J. 2013. A data base of Triassic conodonts from a comprehensive revision of literature. [Una base de datos de conodontos triásicos a partir de una completa revisión de la literatura]. Spanish Journal of Palaeontology, 28 (2), 215-226. Manuscript received 08 September 2012 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 19 December 2012 ABSTRACT RESUMEN The revision of a comprehensive amount of bibliography La revisión de una amplia cantidad de bibliografía ha hecho has made possible the development of a database containing posible el desarrollo de una base de datos en la que fi guran los the stratigraphic ranges of the conodont species from the rangos estratigráfi cos de las especies de conodontos presentes uppermost Permian and the Triassic, with a total of 336 species desde el Pérmico superior y el Triásico, con un total de 336 in 52 genera. This database is aimed at biostratigraphy and especies y 52 géneros. Esta base de datos está dirigida a la studies related to biological, evolutional and palaeodiversity bioestratigrafía y a estudios relacionados con las dinámicas dynamics.
    [Show full text]
  • Durham E-Theses
    Durham E-Theses The palaeobiology of the panderodontacea and selected other euconodonts Sansom, Ivan James How to cite: Sansom, Ivan James (1992) The palaeobiology of the panderodontacea and selected other euconodonts, Durham theses, Durham University. Available at Durham E-Theses Online: http://etheses.dur.ac.uk/5743/ 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 Durham E-Theses • 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 Durham E-Theses policy for further details. Academic Support Oce, Durham University, University Oce, Old Elvet, Durham DH1 3HP e-mail: [email protected] Tel: +44 0191 334 6107 http://etheses.dur.ac.uk The copyright of this thesis rests with the author. No quotation from it should be pubHshed without his prior written consent and information derived from it should be acknowledged. THE PALAEOBIOLOGY OF THE PANDERODONTACEA AND SELECTED OTHER EUCONODONTS Ivan James Sansom, B.Sc. (Graduate Society) A thesis presented for the degree of Doctor of Philosophy in the University of Durham Department of Geological Sciences, July 1992 University of Durham. 2 DEC 1992 Contents CONTENTS CONTENTS p. i ACKNOWLEDGMENTS p. viii DECLARATION AND COPYRIGHT p.
    [Show full text]
  • Papers in Press
    Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2017PR023 Missourian (Kasimovian, Late Pennsylvanian) conodonts from limestone boulders, Mizuboradani Valley, Gifu Prefecture, central Japan AcceptedTAKUMI MAEKAWA1, TOSHIFUMI KOMATSU2, GENGO TANAKA3, MARK WILLIAMS4, CHRISTOPHER P. STOCKER4, MASATOSHI OKURA5 and AKIHIRO UMAYAHARA6 1Center for Water Cycle, Marine Environment, and Disaster Management, Marine Science Laboratory, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 850-8555, Japan (e-mail: [email protected]) 2Faculty of Advanced Science and Technology, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 860-8555, Japan ([email protected]) 3Institute of Liberal Arts and Science, Kanazawamanuscript University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan (e-mail: [email protected]) 4School of Geography, Geology and Environment, University of Leicester, University Road, Leicester, LEI 7RH, UK ([email protected]) 5Naka 86, Minamiyama-cho, Konan, Aichi 483-8155, Japan 6Graduate School of Science and Technology, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 860-8555, Japan Abstract. Two Late Pennsylvanian conodont species, Gondolella sublanceolata Gunnell and Idiognathodus sulciferus Gunnell, were extracted from limestone boulders in the Mizuboradani Valley, Fukuji district, central Japan.
    [Show full text]
  • An Early Triassic Conodont with Periodic Growth?
    Journal of Micropalaeontology, 16: 6572. 0262-821X/97 $10.00 0 1997 British Micropalaeontological Society. An Early Triassic conodont with periodic growth? ZHANG SHUNXIN’, RICHARD J. ALDRIDGE2 & PHILIP C. J. DONOGHUEZ93 China University of Geosciences, 29 Xueyuan Road, Beijing 100083, China. 2Department of Geology, University of Leicester, Leicester LE1 7RH, UK. Present address: School of Earth Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK. ABSTRACT - Elements of a new Triassic conodont genus Parapachycladina, from the Lower Triassic Beisi Formation of western Guangxi Province, China, show a characteristic pattern of lamellar edges in the recessive basal margin. The lamellae are grouped in sets of 8-10, with broad interlamellar spaces between each set. If this apparent periodicity reflects annual cycles, the specimens were not more than four years old when they ceased growing. .I.Micropalaeontol. 16(1): 65-12, May 1997. INTRODIJCTION 1991), sample YT228, Beisi Formation (Lower Triassic), Lower Triassic conodonts were fkst described by Muller (1956), Taiping, Pingguo, Western Guangxi Province, China. Holotype: and have subsequently become quite well known. One char- specimen 59875, China University of Geosciences, Beijing acteristic member of the fauna is the genus Pachycladina, which (Zhang, in Zhang and Yang, 1991, pl. 3, figs 7a, 7b). occurs in shallow-water deposits in Europe, North America and Diagnosis. Apparatus seximembrate, composed of ramiform China. Founded by Staesche (1964) as a form genus, with P. elements with intergrading morphology. Pa extensiform digy- obliqua Staesche as type species, the multielement nature of rate, Pb extensiform to breviform digyrate, M breviform Pachycladina was recognized by Sweet (198 1) in the Treatise on digyrate, Sa alate with posterior process, Sb breviform digyrate, Invertebrate Paleontology.
    [Show full text]
  • Sepkoski, J.J. 1992. Compendium of Fossil Marine Animal Families
    MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions . In BIOLOGY and GEOLOGY Number 83 March 1,1992 A Compendium of Fossil Marine Animal Families 2nd edition J. John Sepkoski, Jr. Department of the Geophysical Sciences University of Chicago Chicago, Illinois 60637 Milwaukee Public Museum Contributions in Biology and Geology Rodney Watkins, Editor (Reviewer for this paper was P.M. Sheehan) This publication is priced at $25.00 and may be obtained by writing to the Museum Gift Shop, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Orders must also include $3.00 for shipping and handling ($4.00 for foreign destinations) and must be accompanied by money order or check drawn on U.S. bank. Money orders or checks should be made payable to the Milwaukee Public Museum. Wisconsin residents please add 5% sales tax. In addition, a diskette in ASCII format (DOS) containing the data in this publication is priced at $25.00. Diskettes should be ordered from the Geology Section, Milwaukee Public Museum, 800 West Wells Street, Milwaukee, WI 53233. Specify 3Y. inch or 5Y. inch diskette size when ordering. Checks or money orders for diskettes should be made payable to "GeologySection, Milwaukee Public Museum," and fees for shipping and handling included as stated above. Profits support the research effort of the GeologySection. ISBN 0-89326-168-8 ©1992Milwaukee Public Museum Sponsored by Milwaukee County Contents Abstract ....... 1 Introduction.. ... 2 Stratigraphic codes. 8 The Compendium 14 Actinopoda.
    [Show full text]
  • Dhanda, R., Murdock, DJE, Repetski, JE, Donoghue, PCJ, & Smith, MP
    Dhanda, R., Murdock, D. J. E., Repetski, J. E., Donoghue, P. C. J., & Smith, M. P. (2019). The apparatus composition and architecture of Erismodus quadridactylus and the implications for element homology in prioniodinin conodonts. Papers in Palaeontology, 5(4), 657-677. https://doi.org/10.1002/spp2.1257 Peer reviewed version Link to published version (if available): 10.1002/spp2.1257 Link to publication record in Explore Bristol Research PDF-document This is the author accepted manuscript (AAM). The final published version (version of record) is available online via Wiley at https://onlinelibrary.wiley.com/doi/full/10.1002/spp2.1257 . Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ THE APPARATUS COMPOSITION AND ARCHITECTURE OF ERISMODUS QUADRIDACTYLUS AND THE IMPLICATIONS FOR ELEMENT HOMOLOGY IN PRIONIODININ CONODONTS By ROSIE DHANDA1, DUNCAN J. E. MURDOCK2, JOHN E. REPETSKI3 and PHILIP C. J. DONOGHUE4 and M. PAUL SMITH2 * 1School of Geography, Earth and Environmental Sciences, University of Birmingham, Edgbaston, Birmingham B15 2TT, UK; [email protected] 2 Oxford University Museum of Natural History, Parks Road, Oxford, OX1 3PW, UK; [email protected], [email protected] 3 U.S. Geological Survey, MS 926A
    [Show full text]
  • Conodonts (Vertebrata)
    Journal of Systematic Palaeontology 6 (2): 119–153 Issued 23 May 2008 doi:10.1017/S1477201907002234 Printed in the United Kingdom C The Natural History Museum The interrelationships of ‘complex’ conodonts (Vertebrata) Philip C. J. Donoghue Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK Mark A. Purnell Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK Richard J. Aldridge Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK Shunxin Zhang Canada – Nunavut Geoscience Office, 626 Tumit Plaza, Suite 202, PO Box 2319, Iqaluit, Nunavut, Canada X0A 0H0 SYNOPSIS Little attention has been paid to the suprageneric classification for conodonts and ex- isting schemes have been formulated without attention to homology, diagnosis and definition. We propose that cladistics provides an appropriate methodology to test existing schemes of classification and in which to explore the evolutionary relationships of conodonts. The development of a multi- element taxonomy and a concept of homology based upon the position, not morphology, of elements within the apparatus provide the ideal foundation for the application of cladistics to conodonts. In an attempt to unravel the evolutionary relationships between ‘complex’ conodonts (prioniodontids and derivative lineages) we have compiled a data matrix based upon 95 characters and 61 representative taxa. The dataset was analysed using parsimony and the resulting hypotheses were assessed using a number of measures of support. These included bootstrap, Bremer Support and double-decay; we also compared levels of homoplasy to those expected given the size of the dataset and to those expected in a random dataset.
    [Show full text]
  • ABSTRACT BOOK a Cura Della Società Geologica Italiana
    https://doi.org/10.3301/ABSGI.2019.04 Milano, 2-5 July 2019 ABSTRACT BOOK a cura della Società Geologica Italiana 3rd International Congress on Stratigraphy GENERAL CHAIRS Marco Balini, Università di Milano, Italy Elisabetta Erba, Università di Milano, Italy - past President Società Geologica Italiana 2015-2017 SCIENTIFIC COMMITTEE Adele Bertini, Peter Brack, William Cavazza, Mauro Coltorti, Piero Di Stefano, Annalisa Ferretti, Stanley C. Finney, Fabio Florindo, Fabrizio Galluzzo, Piero Gianolla, David A.T. Harper, Martin J. Head, Thijs van Kolfschoten, Maria Marino, Simonetta Monechi, Giovanni Monegato, Maria Rose Petrizzo, Claudia Principe, Isabella Raffi, Lorenzo Rook ORGANIZING COMMITTEE The Organizing Committee is composed by members of the Department of Earth Sciences “Ardito Desio” and of the Società Geologica Italiana Lucia Angiolini, Cinzia Bottini, Bernardo Carmina, Domenico Cosentino, Fabrizio Felletti, Daniela Germani, Fabio M. Petti, Alessandro Zuccari FIELD TRIP COMMITTEE Fabrizio Berra, Mattia Marini, Maria Letizia Pampaloni, Marcello Tropeano ABSTRACT BOOK EDITORS Fabio M. Petti, Giulia Innamorati, Bernardo Carmina, Daniela Germani Papers, data, figures, maps and any other material published are covered by the copyright own by the Società Geologica Italiana. DISCLAIMER: The Società Geologica Italiana, the Editors are not responsible for the ideas, opinions, and contents of the papers published; the authors of each paper are responsible for the ideas opinions and con- tents published. La Società Geologica Italiana, i curatori scientifici non sono responsabili delle opinioni espresse e delle affermazioni pubblicate negli articoli: l’autore/i è/sono il/i solo/i responsabile/i. © Società Geologica Italiana, Roma 2019 STRATI 2019 ABSTRACT INDEX ST1.1 History of Stratigraphy in Italian environments (17th – 20th centuries) ........................................
    [Show full text]