Encrinurus" Variolaris Plexus (Trilobita)."

Total Page:16

File Type:pdf, Size:1020Kb

Encrinurus AMERICAN MUSEUM NornItates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK, N.Y. 10024 Number 2968, 22 pp., 9 figs. April 25, 1990 Mackenziurus, a New Genus of the Silurian "Encrinurus" variolaris Plexus (Trilobita) GREGORY D. EDGECOMBE' AND BRIAN D. E. CHATTERTON2 ABSTRACT Mackenziurus reimeri n. gen. n. sp., from Wen- common ancestry with Balizoma Holloway is a lock strata in the Mackenzie Mountains, North- competing hypothesis. Paraphyletic "Nucleurus" west Territories, Canada, is designated type species Ramsk6ld groups the sister taxa of Balizoma, ofa new genus ofthe "Encrinurus" variolaris plex- Mackenziurus + Fragiscutum, and Frammia Hol- us. Mackenziurus n. gen. also includes Wenlock tedahl. A silicified growth series for Mackenziurus species from Wisconsin-Illinois and Arkansas. A reimeri provides new data on ontogenetic trans- sister-group relationship with Fragiscutum Whit- formations for the variolaris plexus. tington and Campbell is suggested; more recent INTRODUCTION The systematics ofSilurian encrinurine tri- whereas E. (Nucleurus) Ramsk6ld, 1986a, lobites were set in an explicit genealogical represents the plesiomorphic Llandovery core framework by Strusz (1980) who distin- of the variolaris plexus. The latter group was guished three "phylogenetic plexi" within envisioned as ancestral to restricted Wen- Encrinurus Emmrich, 1844. Ramskold's lock?-Ludlow offshoots (Fragiscutum Whit- (1986a) subgeneric revision of Encrinurus tington and Campbell, 1967; Frammia Hol- formalized these relationships: E. (Encrinu- tedahl, 1914) as well as to geographically rus) and E. (Pacificurus) Ramsk6ld, 1986b, widespread and morphologically conserva- comprise the Euramerican punctatus and tive Wenlock-Ludlow Balizoma Holloway, Australasian mitchelli plexi, respectively, 1980. ' Graduate student, Department of Invertebrates, American Museum of Natural History; and Department of Geological Sciences, Columbia University. 2Professor, Department of Geology, University of Alberta, Edmonton, Alberta, Canada T6G 2E3. Copyright © American Museum of Natural History 1990 ISSN 0003-0082 / Price. $2.75 2 AMERICAN MUSEUM NOVITATES NO. 2968 a b c d e f k I m a b c d e f h i i k I m 3 j k I m A 0 0 I ICI Fig. 1. Cladograms expressing component information retrieved from encrinurine classification (com- ponents analysis as outlined by Nelson and Platnick, 1981). A. Derivative cladogram from unsequenced generic list classification (Strusz, 1980: 8; cf. Hamada, 1961; Evitt and Tripp, 1977) predicts no com- ponent information additional to general component 0 (Encrinurinae). B. Cladogram expressing hy- pothesis of phylogenetic relationship for the same terminal taxa (from Strusz, 1980: fig. 9) is more informative, predicting three components. Unresolved polytomies within components 0, 1, and 3 result partly from paraphyletic ancestral taxa (0-Encrinuroides; 1 -Coronocephalus; 3-Encrinurus; see C for example). C. Hypothesis of relationships between terms of component 3 (from Strusz, 1980: fig. 9); Encrinurus ("i") is paraphyletic. Terminal taxa abbreviated as follows: a, Encrinuroides; b, Physema- taspis; c, Cromus; d, Coronocephalus; e, Kailia; f, Senticucullus; g, Erratencrinurus; h, Celtencrinurus; i, Encrinurus; j, Paraencrinurus; k, Batocara; 1, Fragiscutum; m, Frammia. The present survey offers an assessment of Terminology applied to encrinurine mor- variolaris plexus relationships and taxonomy phology follows Evitt and Tripp (1977), with incorporating methods of phylogenetic sys- the exception that the conventional "axis" is tematics. We have thus attempted to recog- used rather than "rachis." Description of en- nize monophyletic taxa (sensu Hennig, 1966) crinurine early ontogeny is as outlined by based on synapomorphies, and to integrate Edgecombe et al. (1988). The preglabellar lat- these components into the hierarchical struc- eral lobe is termed PL following Howells ture of classification. The information con- (1982), and description of glabellar furrows/ tent (Mickevich and Platnick, 1989) of cur- lobes is as recommended for the revision of rent encrinurine classifications is adversely the Treatise on Invertebrate Paleontology, affected by paraphyletic ancestral taxa (see Part 0 (H. B. Whittington and S. R. A. Kelly, fig. 1). A distinctive cluster of North Amer- unpubl.). Ramskold's (1986a) notations for ican Wenlock species of the variolaris plexus fixigenal "circumocular tubercles" and ter- is herein recognized as a monophyletic tax- minal pygidial pleural ribs, as well as pygidial on and are described as the new genus Mack- "R/P ratio," are adopted. "Major row" and enziurus, with type species M. reimeri n. sp., "inter-row" glabellar tubercles are as intro- from the Wenlock of the Mackenzie Moun- duced by Edgecombe and Chatterton (1987). tains, Northwest Territories, Canada. Certain Orientations use the typical abbreviations for Wenlock species from Illinois, Wisconsin, and sagittal (sag.), exsagittal (exsag.), and trans- Arkansas previously referred to Encrinurus verse (tr.). and Balizoma are reassigned to Mackenziu- rus n. gen. Type and figured specimens of ACKNOWLEDGMENTS Mackenziurus reimeri are housed in the pa- leontological type collections of the Univer- This study was funded by operating grants sity of Alberta (UA). from the Natural Sciences and Engineering 1 990 EDGECOMBE AND CHATTERTON: MACKENZIURUS 3 Research Council of Canada, and Energy, and an adaxially narrowing cranidial anterior Mines and Resources (Canada) to Chatterton border. Although the usefulness of "a vario- and from the Boreal Institute for Northern laris group" has been questioned on phenetic Studies to Edgecombe. We thank Dr. Lars grounds (Temple and Tripp, 1979), mono- Ramsk6ld and Mr. R. P. Tripp for helpful phyly of the variolaris plexus is supported by comments on a preliminary version of this these unique characters; we hold that mono- paper, as well as formal reviews. Thorough phyly is both a necessary and sufficient cri- criticism from Dr. D. J. Holloway forced us terion for a taxon's utility. to reevaluate many of our arguments. Pho- Enlarged L2-L4 lateral glabellar and adax- tographs of a well-preserved Mackenziurus ial fixigenal tuberculation, and reduced genal cephalon from the Racine Dolomite at Wau- spines, are derived characters uniting this watosa, Wisconsin, were kindly provided by plexus with Pacificurus Ramsk6ld. It must be L. Ramsk6ld. These, as well as loan of spec- noted, however, that the occurrence of these imens in the Milwaukee Public Museum col- states in certain Llandovery species with sev- lections (arranged by Dr. R. Watkins) and eral diagnostic characters of the punctatus correspondence with Mr. K. C. Gass, aided plexus (e.g., E. squarrosus Howells, 1982) greatly in the generic diagnosis. cautions that they may be symplesiomor- phies, and thus specify a more inclusive group SYSTEMATICS OF THE (Encrinurus sensu Ramsk6ld, 1986a). (That VARIOLARIS PLEXUS hypothesis would demand reversals in de- rived parts of the punctatus plexus.) Predict- Strusz's (1980) Encrinurus variolaris plex- ing the component variolaris plexus + Pa- us included species referred by Ramskold cificurus at the exclusion of the punctatus (1986a) to Encrinurus (Nucleurus) and Bali- plexus, Encrinurus (cf. Strusz, 1980: 54), zoma Holloway. Fragiscutum and Frammia questions the grouping of Encrinurus, Paci- were perceived as "offshoots," i.e., descen- ficurus, and "Nucleurus" as a unique taxon dants excluded from the plexus. This dis- (i.e., as subgenera of Encrinurus). Although tinction between ancestral and descendant that grade group might reflect the equivocal taxa (Haeckelian ancestry of Rieppel, 1988) relationships of certain Llandovery species, is not endorsed here; the variolaris plexus is it predicts that "Nucleurus" shares indepen- expanded to include all descendants of a dent history with Pacijicurus and Encrinurus unique common ancestor which would itself rather than with other parts of the variolaris be part ofthe group. "Nucleurus, " Balizoma, plexus. This statement [as retrieved from the Fragiscutum, Mackenziurus n. gen., and classification; derivative cladogram (Nelson Frammia inclusively form a monophyletic and Platnick, 1981) in fig. 2a] is incongruent group for which the informal name "vario- with the phylogenetic hypothesis endorsed by laris plexus" is retained. Restricting this group Ramskold (1986a) and herein that "Nucleu- to an ancestral/primitive core (e.g., "Nucleu- rus" is most closely related to other genera rus," with or without Balizoma) but exclud- of the variolaris plexus (fundamental clado- ing Frammia and Fragiscutum (based on their gram in fig. 2b). Following Ramskold's uniquely derived characters) results in a para- (1986a) diagnoses, Encrinurus (the punctatus phyletic group. Schrank's (1972) synonymy plexus) and Pacificurus are treated as separate of Fragiscutum and Reed's (1928) Encrinu- generic taxa herein to eliminate the paraphy- rus variolaris group with Frammia would letic "Encrinurus" created by grouping them eliminate several generic names widely used with plesiomorphic parts of the variolaris by subsequent workers. It seems most infor- plexus (the "Nucleurus" grade). This problem mative to retain existing names for express- of paraphyly is only compounded when we ing relationships between parts of the more entertain excluded (autapomorphic) sister inclusive variolaris plexus. groups for the other "subgenera" ofEncrinu- Characteristic of the variolaris plexus are rus.
Recommended publications
  • 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]
  • Silurian Rugose Corals of the Central and Southwest Great Basin
    Silurian Rugose Corals of the Central and Southwest Great Basin GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 Silurian Rugose Corals of the Central and Southwest Great Basin By CHARLES W. MERRIAM GEOLOGICAL SURVEY PROFESSIONAL PAPER 777 A stratigraphic-paleontologic investigation of rugose corals as aids in age detern2ination and correlation of Silurian rocks of the Great Basin with those of other regions UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600082 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price $2.15 (paper cover) Stock Number 2401-00363 CONTENTS Page Page Abstract--------------------------------------------------------------------------- 1 Systematic and descriptive palaeontology-Continued Introduction -------------------------------------------------------------------- 1 Family Streptelasmatidae-Continued Purpose and scope of investigation-------------------------------­ 1 Dalmanophyllum ------------------------------------------------- 32 History of investigation ----------------------------------------------­ 1 Family Stauriidae ------------------------------------------------------- 32 Methods of study-------------------------------------------------------­ 2 Cyathoph y llo ides-------------------------------------------------- 32 Acknowledgments------------------------------------------------------- 4 Palaeophyllum
    [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]
  • United States
    DEPARTMENT OF THE INTERIOR BULLETIN OF THE UNITED STATES ISTo. 146 WASHINGTON GOVERNMENT Pit IN TING OFFICE 189C UNITED STATES GEOLOGICAL SURVEY CHAKLES D. WALCOTT, DI11ECTOK BIBLIOGRAPHY AND INDEX NORTH AMEEICAN GEOLOGY, PALEONTOLOGY, PETEOLOGT, AND MINERALOGY THE YEA.R 1895 FEED BOUGHTON WEEKS WASHINGTON Cr O V E U N M K N T P K 1 N T I N G OFFICE 1890 CONTENTS. Page. Letter of trail smittal...... ....................... .......................... 7 Introduction.............'................................................... 9 List of publications examined............................................... 11 Classified key to tlio index .......................................... ........ 15 Bibliography ............................................................... 21 Index....................................................................... 89 LETTER OF TRANSMITTAL DEPARTMENT OF THE INTEEIOE, UNITED STATES GEOLOGICAL SURVEY, DIVISION OF GEOLOGY, Washington, D. 0., June 23, 1896. SIR: I have the honor to transmit herewith the manuscript of a Bibliography and Index of North American Geology, Paleontology, Petrology, and Mineralogy for the year 1895, and to request that it be published as a bulletin of the Survey. Very respectfully, F. B. WEEKS. Hon. CHARLES D. WALCOTT, Director United States Geological Survey. 1 BIBLIOGRAPHY AND INDEX OF NORTH AMERICAN GEOLOGY, PALEONTOLOGY, PETROLOGY, AND MINER­ ALOGY FOR THE YEAR 1895. By FRED BOUGHTON WEEKS. INTRODUCTION. The present work comprises a record of publications on North Ameri­ can geology, paleontology, petrology, and mineralogy for the year 1895. It is planned on the same lines as the previous bulletins (Nos. 130 and 135), excepting that abstracts appearing in regular periodicals have been omitted in this volume. Bibliography. The bibliography consists of full titles of separate papers, classified by authors, an abbreviated reference to the publica­ tion in which the paper is printed, and a brief summary of the con­ tents, each paper being numbered for index reference.
    [Show full text]
  • Lines in Paradoxides Forchhammeri - Evidence of Lateral Inhibition
    Spatial organization of tubercles and terrace lines in Paradoxides forchhammeri - evidence of lateral inhibition 0YVIND HAMMER Hammer, 0. 2000. Spatial organization of tubercles and terrace lines in Paradoxides forchhammeri - evidence of lateral inhibition. -Acta Palaeontologica Polonica 45,3, 251-270. Spatial statistics on the positions of trilobite tubercles indicate the existence of a develop- mental spacing mechanism. Similar spacing between sensory bristles, due to lateral inhi- bition, is well known in insects, and the genetic basis for these patterns has been thor- oughly studied. Tubercles (granules) in the Middle Cambrian trilobite Paradoxides forchhammeri are spaced out, but otherwise randomly positioned. Assuming that similar genetic principles are in operation for the positioning of peripheral neuronal elements in all arthropods, it can even be speculated that genes with functions similar to Delta, Notch, achaete and scute were active in trilobite cuticular patterning. Also, in f? forchhammeri, terrace lines (ridges) seem to display transitions into granulation, indicating that these two types of structure share an underlying pattern formation mechanism. Key words : Trilobites, tubercles, terrace lines, pattern formation, evolution, Notch. 0yvind Hammer [[email protected]],Paleontological Museum, University of Oslo, Sars gt. 1, 0562 Oslo, Norway. Introduction Trilobite tubercles (Starrmer 1980; Wilmot 1991; Whittington 1997) are cuticular structures that may have formed in connection with sensory devices such as setae or other mechano- or chemoreceptors. As such, they may be compared with sensilla in the cuticles of other arthropods (Starrmer 1980). In particular, the molecular basis for the development of spaced bristles in Drosophila has been the subject of extensive re- search (reviewed in Simpson et al.
    [Show full text]
  • Morphology, Faunas and Genesis of Ordovician Hardgrounds from Southern Ontario, Canada
    Palaeogeogmphy, Paheoclimatology, Pudoeoecology, 46 (1984): 233-290 Elsevier Science Publishers B.V., Amsterdam -Printed in The Netherlands MORPHOLOGY, FAUNAS AND GENESIS OF ORDOVICIAN HARDGROUNDS FROM SOUTHERN ONTARIO, CANADA CARLTON E. BRETT and MICHAEL E. BROOKFIELD' Depnrtmenl of Geological Sciences, University of Rochester, Rochester, NY 14627 (U.S.A,] Department v f Land Resources Sciences, GueIph University, Guelph, Ont. N.l G 2 W1 (Canada) {keceived May 19, 1983;revised version accepted March 13, 1984) ABSTRACT Brett, C. E. and Brookfield, M. E., 1984. Morphology, faunas and genesis of Ordovician hardgrounds from southern Ontario, Canada. Palaeogeogr., PaIaeoclirnatol., PalaeoecoI., 46: 233-290. We have used associations of different rnicrofacies to define facies (or microfaties associations) which fom reasonably welldefined sequences, which we infer, from amlo- gies with recent and ancient carbonate environments, to have been deposited in a shelf environment characterized by small-scde topographic differentiation into shoal, slope and basinal environments. Shoal environments are characterized by typically cross-bedded, well-sorted biocktic sands, with intershoal areas consisting oP interbedded bioclastic sands and heavily biotur- bated f iner-grained carbonates. Slope and "basinal" environments are typically represented by "proximal" and "distal" cycles respectively. These we compare with deposits of carbonate ramp bypass channels, and with the more thoroughly studied deep-water elastic submarine fans. Many of the strong variations in environmental energy in these proximal and distal cycles can be attributed ta migration of channels on the fans and to the effect of funnelling of storm surges dawn the channels, Mthough hardground morphology and faunas are mostly related to local effects rmch as intensity of scouring, time of exposure, topographic differentiation of the surface and other factors, differing hardground types tend to be found in different environments.
    [Show full text]
  • Trilobites from the Silurian of New South Wales
    AUSTRALIAN MUSEUM SCIENTIFIC PUBLICATIONS Fletcher, Harold O., 1950. Trilobites from the Silurian of New South Wales. Records of the Australian Museum 22(3): 220–233, plates xv–xvi. [27 January 1950]. doi:10.3853/j.0067-1975.22.1950.603 ISSN 0067-1975 Published by the Australian Museum, Sydney nature culture discover Australian Museum science is freely accessible online at http://publications.australianmuseum.net.au 6 College Street, Sydney NSW 2010, Australia TRILOBITES FROM THE SILURIAN OF NEW SOUTH WALES. By H. O. FLETCHER. Curator of Palaeontology, The Australian Museum. (Plates xv-xvi.) In this paper three new species of trilobites are described from a Lower Silurian horizon at Borenore, near Orange, New South Wales, as Encrinurus borenorensis, Phacops macdonaldi and Dicranogmus bartonensis. The genus Encrinurus Emmrich, 1844, is discussed and it is considered that the genus Gryptonymus Eichwald, 1825, is an abandoned name and cannot be used outside certain limits. Reference is made to the recorded Australian species of the family Lichidae and their geological age. The fossil material was originally found and forwarded to the Australian Museum by Mr. George McDonald, of "Rosyth", Borenore, on whose property the new horizon of fossils is situated. The author visited the locality later and collected additional specimens of all the described species. My thanks are due to Mr. McDonald for his assistance and interest, which have made possible the preparation of this paper. I am also indebted to Mr. F. Booker and Mr. L. Hall, of the Geological Survey of New South Wales, for assistance in determining the geological succession of the area.
    [Show full text]
  • Tayside, Central and Fife Tayside, Central and Fife
    Detail of the Lower Devonian jawless, armoured fish Cephalaspis from Balruddery Den. © Perth Museum & Art Gallery, Perth & Kinross Council Review of Fossil Collections in Scotland Tayside, Central and Fife Tayside, Central and Fife Stirling Smith Art Gallery and Museum Perth Museum and Art Gallery (Culture Perth and Kinross) The McManus: Dundee’s Art Gallery and Museum (Leisure and Culture Dundee) Broughty Castle (Leisure and Culture Dundee) D’Arcy Thompson Zoology Museum and University Herbarium (University of Dundee Museum Collections) Montrose Museum (Angus Alive) Museums of the University of St Andrews Fife Collections Centre (Fife Cultural Trust) St Andrews Museum (Fife Cultural Trust) Kirkcaldy Galleries (Fife Cultural Trust) Falkirk Collections Centre (Falkirk Community Trust) 1 Stirling Smith Art Gallery and Museum Collection type: Independent Accreditation: 2016 Dumbarton Road, Stirling, FK8 2KR Contact: [email protected] Location of collections The Smith Art Gallery and Museum, formerly known as the Smith Institute, was established at the bequest of artist Thomas Stuart Smith (1815-1869) on land supplied by the Burgh of Stirling. The Institute opened in 1874. Fossils are housed onsite in one of several storerooms. Size of collections 700 fossils. Onsite records The CMS has recently been updated to Adlib (Axiel Collection); all fossils have a basic entry with additional details on MDA cards. Collection highlights 1. Fossils linked to Robert Kidston (1852-1924). 2. Silurian graptolite fossils linked to Professor Henry Alleyne Nicholson (1844-1899). 3. Dura Den fossils linked to Reverend John Anderson (1796-1864). Published information Traquair, R.H. (1900). XXXII.—Report on Fossil Fishes collected by the Geological Survey of Scotland in the Silurian Rocks of the South of Scotland.
    [Show full text]
  • Kielan, 1955). the Staurocephalus Clavifrons Beds in the Holy Cross
    A CT AP AL A EON T 0 LO G I C A POLONI CA Vol. II 1 9 5 7 No s, 2-3 ZO FIA K IELAN ON THE TRILOBITE F AMILY STA UROCEPHALIDAE Abstract . - The ventral cephalic sutures of the ge nus Staurocepha[us B ar ra n de, 1846, a re descr ibed a nd are sho wn to be e u- p ty chopariid type, the ro stral pla te be ing extremely large . The origin of this struct ure in St au Tocep ha[u s is discussed. T he si milarities b etween Stauroceph a[u s and Oedicy be[e Whitt in gton, 1938, are poin ted 'out an d th e two genera a re taken to constitute a separate family - the Staurocephalida e. Staul"Ocepha[us c/a v ijrons A nge lin , Sta urocepha[ us sp , n, St auro­ cephohis so . b, St auTocepha[us sp. c, and O edicybd e k ingi Whit tington a re d escribed. INTRO DUCTION In connec tion wi th a s tudy of the Upper Ordovician trilobites of the H oly Cross Mountains (G6ry Swietok rzyskie) in Central Poland, the present writer had an opportunity to exam ine the ventral cep halic su tu res of the ge nus S taurocephaius Barrande and the entire ex oskele ton of the gen us Oediqjb ele Whittington. As publication of the monographic treatment of the whole Upper Ordo vi cian trilobite fauna men tion ed above may take some time, it is though t desirable to publish sepa rate ly the results bea rin g on the morphology and tax on om y of these ge nera.
    [Show full text]
  • Late Silurian Trilobite Palaeobiology And
    LATE SILURIAN TRILOBITE PALAEOBIOLOGY AND BIODIVERSITY by ANDREW JAMES STOREY A thesis submitted to the University of Birmingham for the degree of DOCTOR OF PHILOSOPHY School of Geography, Earth and Environmental Sciences University of Birmingham February 2012 University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. ABSTRACT Trilobites from the Ludlow and Přídolí of England and Wales are described. A total of 15 families; 36 genera and 53 species are documented herein, including a new genus and seventeen new species; fourteen of which remain under open nomenclature. Most of the trilobites in the British late Silurian are restricted to the shelf, and predominantly occur in the Elton, Bringewood, Leintwardine, and Whitcliffe groups of Wales and the Welsh Borderland. The Elton to Whitcliffe groups represent a shallowing upwards sequence overall; each is characterised by a distinct lithofacies and fauna. The trilobites and brachiopods of the Coldwell Formation of the Lake District Basin are documented, and are comparable with faunas in the Swedish Colonus Shale and the Mottled Mudstones of North Wales. Ludlow trilobite associations, containing commonly co-occurring trilobite taxa, are defined for each palaeoenvironment.
    [Show full text]
  • Described Sections and Correlation of Paleozoic Rocks at Gilbert, Carver, and Marshall, Arkansas
    GEOLOGICAL SURVEY CIRCULAR 160 DESCRIBED SECTIONS AND CORRELATION OF PALEOZOIC ROCKS AT GILBERT, CARVER, AND MARSHALL, ARKANSAS By John C. Maher and Robert J. Lantz UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director GEOLOGICAL SURVEY CIRCULAR 160 DESCRIBED SECTIONS AND CORRELATION OF PALEOZOIC ROCKS AT GILBERT, CARVER, AND MARSHALL, ARKANSAS By John C. Maher and Robert J. Lantz Washington, D. C., 1952. Free on application to the Geological Survey, Washington 25, D. C. BOONE R.I9W. R.I8W. R.I7W. R.I6W. 5 Miles Figure 1. --Location of Paleozoic sections and Marshall water well, Newton and Searcy Counties, Ark. DESCRIBED SECTIONS AND CORRELATION OF PALEOZOIC ROCKS AT GILBERT, CARVER, AND MARSHALL, ARKANSAS CONTENTS Page Page1 ' Introduction ............................ Representative measured sections of Representative measured sections Paleozoic rocks Continued of Paleozoic rocks ..................... 3 Upper part of Boone formation, Everton formation, Gilbert .......... 3 Gilbert ......................... St. Peter sandstone, Gilbert ......... 3 Lower part of Boone formation, Plattin limestone, Gilbert ........... 3 Gilbert ......................... Fernvale limestone, Gilbert ......... 4 Batesville sandstone, Ruddell shale, Cason shale, Gilbert ................ 5 and Moorefield formation, Gilbert, Brassfield limestone, Gilbert ........ 5 Carboniferous (Mississippian) and Lafferty and St. Clair limestone, Ordovician rocks, Carver ... k ..., 10 Gilbert ......................... 6 Log of Marshall water well 3, Marshall 12 ILLUSTRATION Page Figure 1. Location of Paleozoic sections and Marshall water well, Newton and Searcy Counties, Ark. INTRODUCTION tions do not represent the maximum thickness of the beds within the area. Vertical intervals were meas­ In 1949 the U. S. Geological Survey, with the ured by hand level and tape, marked, and numbered cooperation of the Division of Geology, Arkansas on the outcrops.
    [Show full text]
  • The Bulletin of Zoological Nomenclature. Vol 12, Part 10
    VOLUME 12. Part 10. 31s£ October 1956 pp. 257-288; 1 pi. THE BULLETIN OF ZOOLOGICAL NOMENCLATURE The Official Organ of THE INTERNATIONAL COMMISSION ON ZOOLOGICAL NOMENCLATURE Edited by FRANCIS HEMMING, C.M.G., C.B.E. Secretary to the International Commission on Zoological Nomenclature Contents : Notices prescribed by the International Congress of Zoology : Page Date of commencement by the International Commission on Zoological Nomenclature by voting on applications published in the Bulletin of Zoological Nomenclature .. .. .. 257 Notice of the possible use by the International Commission on Zoological Nomenclature of its Plenary Powers in certain cases .. .. .. .. .. .. .. .. .. 257 (icontinued on inside back wrapper) LONDON: Printed by Order of the International Trust for Zoological Nomenclature and Sold on behalf of the International Commission on Zoological Nomenclature by the International Trust at its Publication Office, 41, Queen's Gate, London, S.W.7 1956 Price One Pound, One Shilling and Sixpence (Alt rights reserved) Original from and digitized by National University of Singapore Libraries INTERNATIONAL COMMISSION ON ZOOLOGICAL NOMENCLATURE A. The Officers of the Commission Honorary Life President: Dr. Karl Jordan (British Museum (Natural History), Zoological Museum, Tring, Herts, England) President-. Professor James Chester Bradley (Cornell University, Itliaca, N.Y., U.S.A.) (12th August 1953) Vice-President: Senkor Dr. Afranio do Amaral (Sao Paulo, Brazil) (12t,li August 1953) Secretary : Mr. Francis Hemming (London, England) (27tli July 1948) B. The Members of the Commission (Arranged in order of precedence by reference to date of election or of most recent re-election, as prescribed by the International Congress of Zoology) Professor H. Boschma (Rijksmuseum van Natuurlijke Historie, Leiden, The Netherlands) (1st January 1947) Senor Dr.
    [Show full text]