114. the Silurian Proetidae (Trilobita) in Eastern Asia

Total Page:16

File Type:pdf, Size:1020Kb

114. the Silurian Proetidae (Trilobita) in Eastern Asia 422 Proc. Japan Acad., 61, Ser. B (1985) [Vol . 61(B), 114. The Silurian Proetidae (Trilobita) in Eastern Asia By Teiichi KoBAYASHI, M. J. A. (Communicated Nov. 12, 1985) The family Proetidae is the richest in the Silurian trilobites of Eastern Asia, insofar as the number of its genera totaling 12 is concerned. Now it is represented in Japan by the following four genera with three subgenera of Proetus as follows : Proetus subovalis Kobayashi and Hamada, Proetus (Gerastos) sugiharensis Kobayashi and Hamada, Proetus (Gerastos) subcarinatus Kobayashi and Hamada, Proetus (Bohemiproetus) magnicerviculus Kobayashi and Hamada and Decoroproetus granulatus Kobayashi and Hamada, all from Mt. Yokokura, Shikoku Island Prantlia biloba Kobayashi and Hamada, from Okanari, Shikoku Island. Pribyl and Vanek (1978) proposed Gomiites for Decoroproetus granulatus. As discussed in the preceding article, Prantlia biloba is properly referred to Latiproetus. An additional species in a recent paper (Kobayashi and Hamada, 1985a) is Cyphoproetus latiaxis, sp. nov. from Mt. Yokokura. Eight genera and some 30 species of Silurian proetids are reported from Central and South China. These genera and their type-species in brackets to which their age and distri- bution in China are added are as follows : Latiproetus Lu, 1962 (Proetus latilimbatus Grabau, 1925)-Lower and Middle Silurian, Central and South China Niuchangella Chang, 1974 (Niuchangella meitanensis Chang, 1974)- Early Lower Silurian, Guizhou Luojiashania Chang, 1974 (Luojiashania wuchangensis Chang, 1974)- Middle Silurian, Hubei and Sichuan Chuangianoproetus Wu, 1977 (Chuangianoproetus constrictus Wu, 1977) -Middle Silurian, Southwest China and the lower Yangtze region Hypaproetus Wu, 1977 (Hypaproetus guizhouensis Wu, 1977)-Lower Silurian, Guizhou Oidalaproetus Wu, 1977 (Oidalaproetus convexus Wu, 1977)-Lower Silurian, Guizhou Xiushuiproetus Q. Z. Zhang, 1983 (Xiushuiproetus shuangheensis Wu 1977 emend Q. Z. Zhang et Ju, 1983)-Middle Silurian, Jianxi and Sichuan Zeijiangoproetus Q. Z. Zhang et Ju, 1983 (Zeijiangoproetus f uyangensis Q. Z. Zhang et Ju, 1983) -Lower Silurian, Zhej fang. Because I have discussed already Latiproetus, Chuangianoproetus, Xiushui- proetus and Zeijiangoproetus in the preceding article, the remaining four genera are taken up for discussion. No. 9] Silurian Trilobites, Eastern Asia 423 Oidalaproetus has the glabella and eyes resembling Latiproetus, but the marginal furrow is undeveloped on the cephalon and the test tuberculate. As Wu (1977) noted, it may be allied to Cyphoproetus Kegel,1927, but the associated pygidium is trapezoidal, instead of semicircular. Its reference to the Cypho- proetinae is provisional. Fig. 1. Hypaproetus guizhouensis Wu (after Wu, 1977). Fig. 2. Gomiites granulatus (Kobayashi and Hamada) (after Pribyl and Vanek, 1978). Hypaproetus (Fig. 1) was compared with Astroproetus by Wu (1977) and Chatterton and Campbell (1981), but it looks to me nearer to Gomiites in view of the glabellar and preglabellar aspects, particularly the latter divided into highly convex marginal rim and low convex frontal limb by a profound furrow. Although Gomiites (Fig. 2) has the glabella rather ovate and its pygidium is much broader than that of Hypaproetus. Both of them belong probably to the Tropidocoryphinae. Luojiashania on the other hand bears affinities to Cornup~roetus in slight divergence of anterior facial sutures, particularly to C. (Lepidoproetus) in the aspects of glabella and eyes. Its pygidium is not very broad, but the axis is short and prominent and the marginal border not well developed. Therefore this genus may be placed in the Cornuproetinae. Niuchangella was placed in the Proetidae by Yin (1978), but monotypic N. meitanensis Chang, 1974 agrees with Radnoria Owens and Thomas, 1974 in the Cordaniinae Campbell, 1977 of the Brachymetopidae in the wide divergence of the anterior facial sutures and other generic characteristics so nicely that it can be said a Radnoria having the glabella somewhat expanded in posterior. Thus it is an important early Lower Silurian link in Eastern Asia between Llandeilian species of Newfoundland and Llandoverian-Wenlockian one in Europe (Pribyl and Vanek, 1981). Finally, no comment is added here to the following three species of proetids from the eastern Mongolian zone owing to their inadequate description and illustration. 424 T. KOBAYASHI [Vol. 61(B), Warburgella wadogouensis Nan, 1980 from Middle Silurian, Heilong- j fang, Northeast China Ungliproetus unguloides (Barrande) and Cyphoproetus sp. by Nan (1976) from Upper Silurian, Inner Mongolia, North China In summary 4 genera with 3 subgenera of Proetus in 4 subfamilies of the Proetinae are known in the middle and late Silurian fauna of Japan as follows : Proetinae : Proetus (Proetus, Gerastos, Boh emiproetus) Cyphoproetinae : Cyphoproetus Warburgellinae : Latiproetus Tropidocoryphinae : Gomiites. Among them Gomiites is a sole endemic genus. All others are widespread through open-seas or geosynclines. Another 4 subfamilies containing 5 genera with 3 subgenera of Latiproetus are recognized in the early and middle Silurian faunas of Central and South China as follows : Cyphoproetinae : Oidalaproetus Warburgellinae : Latiproetus (Latiproetus, Chuangianoproetus, Xiushui- proetus), Prantlia (Zheijiangoproetus) Cornuproetidae : Luojiashania Tropidocoryphinae : Hypaproetus. Most of these genera are products of endemic divergence and indigenous to the epicontinental embayment on the south side of the so-called Sino-Korean massif. An exception is Latiproetus which distributed widely in the Asian-Pacific province in the middle Silurian period. This palaeogeographic conclusion is in support of the remarkable contrast of the Encrinuridae between the Corono- cephalinae in the shelf sea of Central and South China (Zhang, 1983) and Japa- nese Encrinurus in the Chichibu geosyncline along the western margin of Pacific ocean (Kobayashi and Hamada, 1985b). References Campbell, K. S. W. (1977) : Trilobites of the Haragen, Bois d'Arc and Frisco forma- tion (early Devonian) Arbuckle mountains region, Oklahoma. Okla. Geol. Surv. Bull., no. 123, 227 pp. (39 pls.). Kegel, W. (1927) : Ueber obersilurische Trilobiten aus dem Harz and dem Rheinischen Schiefergebirge. Jahrb. Preuss. geol. Landesanst., 48, 616-647, pls. 31-32. Kobayashi, T., and Hamada, T. (1974) : Silurian trilobites of Japan in comparison with Asian, Pacific and other faunas. Palaeont. Soc. Japan, Sp. Pap., no. 18, 155 pp., 12 pls. (1985a) : Additional Silurian trilobites to the Yokokura-yama fauna, Shikoku, Japan. Trans. Proc. Palaeont. Soc. Japan, N. S., no. 139, pp. 206-217, pls. 28-30. (1985b) : On the Silurian trilobites and cephalopods of Mt. Yokokura. Proc. Japan Acad., 61B, 345-347. Li, Shan-Ji (1978) : Trilobites, 179-284, pls. 89-114. Southwest Inst. Geol. Sci.: Atlas of Fossil, Southwest China, Sichuan Fasc. (1), Silurian-Devonian, 617 pp., 185 pls. Nan, Run-Shan (1976) : Trilobites, 333-352, pls. 190-201. Bur. Geol. Autonomic Prov. Inner Mongolia and NE China, Inst. Geol. Sci.: Fossil Atlas of Northeast China. Inner Mongolia (1), Palaeozoic Part, 502 pp., 232 pls. No. 9] Silurian Trilobites, Eastern Asia 425 Nan, Run-Shan (1980) : Trilobita, 484-519, pls. 200-212. Shenyan Inst. Geol. Min. Resources: Palaeontological Atlas of Northeast China (1), Paleozoic Voume, 686 pp., 281 pls. Pribyl, A., and Vanek, J. (1981) : Studie zur Morphologie and Phylogenie der Familie Otarionidae R. & E. Richter, 1926 (Trilobita). Palaeontogr. A, 173, 160-208, 9 pls. Owens, R. W., and Thomas, A. T. (1975) : Radnoria, a new Silurian Proetacean trilo- bite and the origin of the Brachymeopidae. Palaeont., 18(4), 809-822 (pls. 95-96). Thomas, A. T., and Owens, R. M. (1978;): A review of the trilobite family Aulaco- pleuridae. ibid., 21(1) , 65-81, pl. 7. Yi Gong-Zhong and Li Sheng-Ji (1978) : Trilobita, 285-595, pis. 144-192. Working group of Geol. & Palaeont. of Guizhou : Fossil Atlas of Southwest China, Guizhou Fasc. (1), Cambrian-Devonian, 843 pp., 214 pls. Zhang Wen-tang (1983) : On the family Coronocephalinae ( Trilobita) . Palaeontology of Cathayana, no. 1, pp. 195-257 (9 pls.)..
Recommended publications
  • University of Michigan University Library
    CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN VOL. XI NO.6, pp. 101-157 (12 pk., 1 map) MARCH25, 1953 TRILOBITES OF THE DEVONIAN TRAVERSE GROUP OF MICHIGAN BY ERWIN C. STUMM UNIVERSITY OF MICHIGAN PRESS ANN ARBOR CONTMBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN MUSEUM OF PALEONTOLOGY Director: LEWIS B. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and also to individuals upon request. Correspondence should be directed to the University of Michigan Press. A list of the separate papers in Volumes II-IX will be sent upon request. VOL. I. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian, by C. L. Fenton and M. A. Fenton. Pages xi+260. Cloth. $2.75. VOL. 11. Fourteen papers. Pages ix+240. Cloth. $3.00. Parts sold separately in paper covers. VOL. 111. Thirteen papers. Pages viii+275. Cloth. $3.50. Parts sold separately in paper covers. VOL. IV. Eighteen papers. Pages viiif295. Cloth. $3.50. Parts sold separately in paper covers, VOL. V. Twelve papers. Pages viii+318. Cloth. $3.50. Parts sold separately in paper covers. VOL. VI. Ten papers. Pages vii+336. Paper covers. $3.00. Parts sold separately. VOLS. VII-IX. Ten numbers each, sold separately. (Continued on inside back cover) VOL.
    [Show full text]
  • Instituto De Geociências Revisão Sistemática E
    UNIVERSIDADE DE SÃO PAULO INSTITUTO DE GEOCIÊNCIAS REVISÃO SISTEMÁTICA E PALEOBIOGEOGRÁFICA DE TRILOBITAS PHACOPIDA (HOMALONOTIDAE E CALMONIIDAE) DO DEVONIANO DAS BACIAS DO PARNAÍBA E AMAZONAS, BRASIL Felipe van Enck Meira Tese apresentada ao Programa de Pós- Graduação em Geoquímica e Geotectônica do Instituto de Geociências da Universidade de São Paulo, como parte dos requisitos para a obtenção do título de doutor. Orientadora: Prof. Dra. Juliana de Moraes Leme TESE DE DOUTORAMENTO Programa de Pós-graduação em Geoquímica e Geotectônica São Paulo 2016 “Kites rise highest against the wind - not with it.” - Winston Churchill Agradecimentos Agradeço a Deus, por sempre iluminar o caminho durante esses anos de altos e baixos do Doutorado. Agradeço a Ele também por enviar dois verdadeiros anjos da guarda à minha vida – minha esposa Angela Faleiros van Enck Meira e meu filho, Thomas Faleiros van Enck Meira. Agradeço a meus pais, José Carlos e Sylvia, e à minha irmã, Patrícia, pelo apoio durante a jornada, ainda que à distância, por vezes. Sou grato aos meus sogros, Jair e Lucia, que sempre foram como verdadeiros pais e conselheiros. À FAPESP (Processo n° 2012/07075-3), pelo suporte financeiro, sem o qual o Doutorado não seria viável. À minha orientadora, Drª. Juliana de Moraes Leme, pela orientação, discussões e esclarecimentos pertinentes ao projeto. Ao Doutorando Fabio Carbonaro e ao Dr. Renato Ghilardi (UNESP-Bauru), pela parceria e por discussões importantes na realização do trabalho. À Drª. Niède Guidon (FUMDHAM), pelo empréstimo de fósseis da região de São João Vermelho (Piauí), estudados aqui. Sou grato às seguintes pessoas, por permitirem meu acesso às instituições para visita de acervos, e por sua disponibilidade, atenção e ajuda durante minha permanência: Bushra Hussaini (AMNH), Flávia Alessandra Figueiredo, Mônica de Medina Coeli, Dr.
    [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]
  • 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]
  • Type and Figured Fossils in the Worthen Collection at the Illinois
    s Cq&JI ^XXKUJtJLI 14oGS: CIR 524 c, 2 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY Lois S. Kent GEOLOGICAL ILLINOIS Illinois Department of Energy and Natural Resources, STATE GEOLOGICAL SURVEY DIVISION CIRCULAR 524 1982 COVER: This portrait of Amos Henry Worthen is from a print presented to me by Worthen's great-grandson, Arthur C. Brookley, Jr., at the time he visited the Illinois State Geological Survey in the late 1950s or early 1960s. The picture is the same as that published in connection with the memorial to Worthen in the appendix to Vol. 8 of the Geological Survey of Illinois, 1890. -LSK Kent, Lois S., Type and figured fossils in the Worthen Collection at the Illinois State Geological Survey. — Champaign, III. : Illinois State Geological Survey, 1982. - 65 p. ; 28 cm. (Circular / Illinois State Geological Survey ; 524) 1. Paleontology. 2. Catalogs and collections. 3. Worthen Collection. I. Title. II. Series. Editor: Mary Clockner Cover: Sandra Stecyk Printed by the authority of the State of Illinois/1982/2500 II I IHOI'.MAII '.I 'II Of.ir.AI MIHVI y '> 300 1 00003 5216 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY Lois S. Kent | CIRCULAR 524 1982 ILLINOIS STATE GEOLOGICAL SURVEY Robert E. Bergstrom, Acting Chief Natural Resources Building, 615 East Peabody Drive, Champaign, IL 61820 TYPE AND FIGURED FOSSILS IN THE WORTHEN COLLECTION AT THE ILLINOIS STATE GEOLOGICAL SURVEY CONTENTS Acknowledgments 2 Introduction 2 Organization of the catalog 7 Notes 8 References 8 Fossil catalog 13 ABSTRACT This catalog lists all type and figured specimens of fossils in the part of the "Worthen Collection" now housed at the Illinois State Geological Survey in Champaign, Illinois.
    [Show full text]
  • Adec Preview Generated PDF File
    Records of the Western Australian Museum 20: 353-378 (2002). Lower Devonian trilobites from Cobar, New South Wales MaIte Christian Ebach Present address: School of Botany, University of Melbourne, 3010, Australia Department of Earth and Planetary Sciences, Western Australian Museum, Francis Street Perth, Western Australia 6000, Australia e-mail: [email protected] Abstract -A Lower Devonian (Lochkovian-Pragian) trilobite fauna from the Biddabirra Formation near Cobar, New South Wales, Australia includes 11 previously undescribed species (Alberticoryphe sp., Cornuproetus sp., Gerastos sandfordi sp. nov., Cyphaspis mcnamarai sp. nov., Kainops cf. ekphymus, Paciphacops sp., AcantJwpyge (Lobopyge) edgecombei sp. nov., Crotalocephalus sp. and Leonaspis sp., a styginid sp., and a harpetid sp.). Three species belonging to the genera Paciphacops, Kainops, AcantJwpyge (Lobopyge), and Leonaspis are preserved with sufficient detail to provide enough information to be coded and analysed by two cladistic analyses. The resulting cladograms provide justification for the monophyly of Paciphacops and further support for Kainops. Leonaspis sp. is placed as the most plesiomorphic species within the monophyletic Leonaspis. INTRODUCTION P. crawfordae, P. waisfeldae and P. sp.). The Leonaspis The Lochkovian-Pragian Biddabirra Formation analysis, using Ramsk6ld and Chatterton's (1991) (Glen 1987) has yielded a trilobite fauna containing characters, includes Leonaspis sp. from Cobar. The twelve species, of which eleven have previously analysis will attempt to use species with more than been undescribed. The species include the 45% of their characters coded. fragmentary material of a styginid and harpetid, All photographed and type specimens are held in internal and external moulds of Alberticoryphe sp., the Australian Museum (prefix number AMF).
    [Show full text]
  • University of Alberta
    University of Alberta Select Devonian Proetid Trilobites of southern Morocco by Darrin Molinaro A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Master of Science Department of Earth and Atmospheric Sciences © Darrin Molinaro Spring 2012 Edmonton, Alberta Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. Where the thesis is converted to, or otherwise made available in digital form, the University of Alberta will advise potential users of the thesis of these terms. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission. Library and Archives Bibliotheque et Canada Archives Canada Published Heritage Direction du Branch Patrimoine de I'edition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre reference ISBN: 978-0-494-87864-4 Our file Notre reference ISBN: 978-0-494-87864-4 NOTICE: AVIS: The author has granted a non­ L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distrbute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non­ support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats.
    [Show full text]
  • Silver Creek Hydraulic Limestone Southeastern Indiana
    , \ " THE Silver Creek Hydraulic Limestone OF Southeastern Indiana. By C. E. SIEBENTHAL. 1900. / ! LETTER OF TRANSMITTAL. Bloomington, Ind., January 10, 1901. Dear Sir-I have the honor to transmit herewith my report upon the "Silver Creek Hydraulic Limestone," written in 1899 and em­ bodying the results of field work done in that year, but recently gone over and brought down to date. I take pleasure in acknowledging the services of Messrs. H. M. Adkinson and F. H. H.Calhoun, gradu­ ate students at the University of Chicago, who generously gave their assistance in the gathering of the data for the paper. The thanks of the Survey are also due to Prof. Stuart Weller, of the University of Chicago, for valuable assistance in the paleontological part of this report. Respectfully submitted, C. E. SIEBENTHAL. Prof. W. S. Blatchley, State Geologist. (332) ,\ THE SILVER CREEK. HYDRAULIC LIMESTONE OF SOUTHEASTERN INDIANA. By U. E. SIEBENTHAL. OUTLINK 1. STRATIGRAPHY. Historical Resume. 1827. 1. A. Lapham. 1841. Jas.Hall. 1843. Dr. A. Clapp. 1843. D. D. Owen. 1843. H. D. Rogers. 1847. Yandell & Bhumal'lI. 1857. Maj. S. S. Lyon. 1859. Lyon and CassedllY· 1860. Maj. S. S. Lyon, 1874. W. W. Borden. 1875. W. W. Borden. 1879. Jas. Hall. 1897. Aug. F. Foerste. 1899. E. M. Kindle. Stratigraphy and Paleontology. Knobstone. Rockford limestone. New Albany black shale. Sellersburg limestone. Silver Creek hydraulic IimestOlIP. Jefl'ersonville limestone. Pendleton sandstone. Upper Silurian. Lower Silurian. Local Details of Distribution and Structure. Clark County. River region. Silver Creek region. Charlestown region. Scott County. Lexington region. Woods Fork region.
    [Show full text]
  • The Silurian and Devonian Proetid and Aulacopleurid Trilobites of Japan and Their Palaeogeographical Significance
    The Silurian and Devonian proetid and aulacopleurid trilobites of Japan and their palaeogeographical significance CHRISTOPHER P. STOCKER, DEREK J. SIVETER, PHILIP D. LANE, MARK WILLIAMS, TATSUO OJI, GENGO TANAKA, TOSHIFUMI KOMATSU, SIMON WALLIS, DAVID J. SIVETER AND THIJS R. A. VANDENBROUCKE Stocker, C.P., Siveter, D.J., Lane, P.D., Williams, M., Oji, T., Tanaka, G., Komatsu, T., Wallis, S., Siveter, D.J. & Vandenbroucke, T.R.A. 2019: The Silurian and Devonian proetid and aulacopleurid trilobites of Japan and their palaeogeographical significance. Fossils and Strata, No. 64, pp. 205–232. Trilobites referable to the orders Proetida and Aulacopleurida are geographically wide- spread in the Silurian and Devonian strata of Japan. They are known from the South Kitakami, Hida-Gaien and Kurosegawa terranes. Revision of other Japanese trilobite groups, most notably the Illaenidae, Scutelluidae and Phacopidae, has extended the palaeobiogeographical ranges of several Japanese trilobite taxa, but has not signalled conclusive evidence of a consistent palaeogeographical affinity. In part, this may relate to the temporally and spatially fragmented Palaeozoic record in Japan, and perhaps also to the different ecological ranges of the trilobites. Here, we present a taxonomic revision of all previously described proetid and aulacopleurid trilobites from Japan, along with descriptions of new material, which comprises thirteen species (one new: Interproetus mizobuchii n. sp.) within nine genera, with three species described under open nomenclature. These trilobites show an endemic signal at species level, not just between Japan and other East Asian terranes, but also between individual Japanese ter- ranes. This endemicity may be explicable in terms of facies and ecology, rather than simply being a function of geographical isolation.
    [Show full text]
  • Smithsonian Miscellaneous Collections
    VOL. 52, PL. IX SMITHSONIAN MISCELLANEOUS COLLECTIONS HENRY NETTELROTH Vol. 52 1908 Smithsonian Miscellaneous Collections Vol. V Quarterly issue Part 2 THE XETTELROTH COLLECTION OF INVERTEBRATE FOSSILS By R. S. BASSLER (With 3 Plates) One of the most important accessions in the division of strati- graphic paleontology during the year 1907 was the collection of the late Henry Nettelroth, acquired jointly by the Smithsonian Institu- tion and the U. S. National Museum from his sons, H. H. Nettel- roth and Dr. Alexander Nettelroth, of Louisville, Kentucky. The registration and installation of these specimens was recently com- pleted, and it seemed in order, as well as very desirable on account of Mr. Nettelroth's work in science and of the valuable nature of his collection, to publish an article upon the subject. The collection is composed entirely of invertebrate fossils, mainly from the Silurian and Devonian strata of Indiana and Kentucky, although many other American as well as foreign localities are represented. The total number of specimens is rather small compared with the number of species represented, the collection comprising about 8,000 specimens, registered under nearly 1,000 entries; but all of the material is the best that could be had. Mr. Nettelroth prided himself upon the fact that his cabinet contained only choice specimens, representing years of careful selection. Imperfect material was retained only when it showed something of scientific interest. In exchanging. Air. Nettelroth also insisted upon a few good specimens rather than numerous poor representatives of a species. Likewise he paid par- ticular attention to a class of fossils, the mollusca, which is seldom well represented in the cabinets of even the best collectors.
    [Show full text]
  • An Inventory of Trilobites from National Park Service Areas
    Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 179 AN INVENTORY OF TRILOBITES FROM NATIONAL PARK SERVICE AREAS MEGAN R. NORR¹, VINCENT L. SANTUCCI1 and JUSTIN S. TWEET2 1National Park Service. 1201 Eye Street NW, Washington, D.C. 20005; -email: [email protected]; 2Tweet Paleo-Consulting. 9149 79th St. S. Cottage Grove. MN 55016; Abstract—Trilobites represent an extinct group of Paleozoic marine invertebrate fossils that have great scientific interest and public appeal. Trilobites exhibit wide taxonomic diversity and are contained within nine orders of the Class Trilobita. A wealth of scientific literature exists regarding trilobites, their morphology, biostratigraphy, indicators of paleoenvironments, behavior, and other research themes. An inventory of National Park Service areas reveals that fossilized remains of trilobites are documented from within at least 33 NPS units, including Death Valley National Park, Grand Canyon National Park, Yellowstone National Park, and Yukon-Charley Rivers National Preserve. More than 120 trilobite hototype specimens are known from National Park Service areas. INTRODUCTION Of the 262 National Park Service areas identified with paleontological resources, 33 of those units have documented trilobite fossils (Fig. 1). More than 120 holotype specimens of trilobites have been found within National Park Service (NPS) units. Once thriving during the Paleozoic Era (between ~520 and 250 million years ago) and becoming extinct at the end of the Permian Period, trilobites were prone to fossilization due to their hard exoskeletons and the sedimentary marine environments they inhabited. While parks such as Death Valley National Park and Yukon-Charley Rivers National Preserve have reported a great abundance of fossilized trilobites, many other national parks also contain a diverse trilobite fauna.
    [Show full text]
  • Paleozoic Seas 290809New
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Berichte des Institutes für Geologie und Paläontologie der Karl- Franzens-Universität Graz Jahr/Year: 2009 Band/Volume: 14 Autor(en)/Author(s): Anonym Artikel/Article: Distribution of Paleozoic sedimentary units of Austria. 86-87 ©Institut f. Erdwissensch., Geol. u. Paläont., Karl-Franzens-Universität Graz; download www.biologiezentrum.at Ber. Inst. Erdwiss. K.-F.-Univ. Graz ISSN 1608-8166 Band 14 Graz 2009 Paleozoic Seas Symposium Graz, 14-18th September 2009 Distribution of Paleozoic sedimentary units of Austria During the meeting we are going to see some localities of the Graz Paleozoic and the Carnic Alps. On the map the distribution of major Paleozoic sedimentary units of Austria is indicated. Graz Paleozoic (D) The sequence includes Silurian to Carboniferous strata, of which the Devonian neritic units around Graz are very well developed. We are going to visit Emsian to Givetian sections such as the road-cut at St. Pankrazen or Forstweg Attems where coral frame- and rudstones are outcropping. Additionally to a very well known algal flora and coral fauna, some of these localities yield a diverse microfauna including scolecodonts, conodonts and other vertebrate remains like shark teeth or placoderm plates. Carnic Alps (G) The sequence includes Ordovician to Permian units, of which we are going to visit the Carboniferous of Nötsch and the Nassfeld area. At the first mentioned locality brachiopods like Gigantoproductus, trilobites (Proetidae, Phillipsiidae), gastropods, crinoids and ostracods occur. At the second locality, Mount Auernig, we are going to visit the Upper Carboniferous sequence yielding calcareous algae and silicified foraminifers (Fusulinoidea), bryozoans and ostracods.
    [Show full text]