The Importance of Developmental Repatterning in the Evolution of Trilobites
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Morphology and Developmental Traits of the Trilobite Changaspis Elongata from the Cambrian Series 2 of Guizhou, South China
Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China GUANG-YING DU, JIN PENG, DE-ZHI WANG, QIU-JUN WANG, YI-FAN WANG, and HUI ZHANG Du, G.-Y., Peng, J., Wang, D.-Z., Wang, Q.-J., Wang, Y.-F., and Zhang, H. 2019. Morphology and developmental traits of the trilobite Changaspis elongata from the Cambrian Series 2 of Guizhou, South China. Acta Palaeontologica Polonica 64 (4): 797–813. The morphology and ontogeny of the trilobite Changaspis elongata based on 216 specimens collected from the Lazizhai section of the Balang Formation (Stage 4, Series 2 of the Cambrian) in Guizhou Province, South China are described. The relatively continuous ontogenetic series reveals morphological changes, and shows that the species has seventeen thoracic segments in the holaspid period, instead of the sixteen as previously suggested. The development of the pygid- ial segments shows that their number gradually decreases during ontogeny. A new dataset of well-preserved specimens offers a unique opportunity to investigate developmental traits after segment addition is completed. The ontogenetic size progressions for the lengths of cephalon and trunk show overall compliance with Dyar’s rule. As a result of different average growth rates for the lengths of cephalon, trunk and pygidium, the length of the thorax relative to the body shows a gradually increasing trend; however, the cephalon and pygidium follow the opposite trend. Morphometric analysis across fourteen post-embryonic stages reveals growth gradients with increasing values for each thoracic segment from anterior to posterior. The reconstruction of the development traits shows visualization of the changes in relative growth and segmentation for the different body parts. -
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. -
The Evolution of Trilobite Body Patterning
ANRV309-EA35-14 ARI 20 March 2007 15:54 The Evolution of Trilobite Body Patterning Nigel C. Hughes Department of Earth Sciences, University of California, Riverside, California 92521; email: [email protected] Annu. Rev. Earth Planet. Sci. 2007. 35:401–34 Key Words First published online as a Review in Advance on Trilobita, trilobitomorph, segmentation, Cambrian, Ordovician, January 29, 2007 diversification, body plan The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The good fossil record of trilobite exoskeletal anatomy and on- 10.1146/annurev.earth.35.031306.140258 togeny, coupled with information on their nonbiomineralized tis- Copyright c 2007 by Annual Reviews. sues, permits analysis of how the trilobite body was organized and All rights reserved developed, and the various evolutionary modifications of such pat- 0084-6597/07/0530-0401$20.00 terning within the group. In several respects trilobite development and form appears comparable with that which may have charac- terized the ancestor of most or all euarthropods, giving studies of trilobite body organization special relevance in the light of recent advances in the understanding of arthropod evolution and devel- opment. The Cambrian diversification of trilobites displayed mod- Annu. Rev. Earth Planet. Sci. 2007.35:401-434. Downloaded from arjournals.annualreviews.org ifications in the patterning of the trunk region comparable with by UNIVERSITY OF CALIFORNIA - RIVERSIDE LIBRARY on 05/02/07. For personal use only. those seen among the closest relatives of Trilobita. In contrast, the Ordovician diversification of trilobites, although contributing greatly to the overall diversity within the clade, did so within a nar- rower range of trunk conditions. -
Early and Middle Cambrian Trilobites from Antarctica
Early and Middle Cambrian Trilobites From Antarctica GEOLOGICAL SURVEY PROFESSIONAL PAPER 456-D Early and Middle Cambrian Trilobites From Antarctica By ALLISON R. PALMER and COLIN G. GATEHOUSE CONTRIBUTIONS TO THE GEOLOGY OF ANTARCTICA GEOLOGICAL SURVEY PROFESSIONAL PAPER 456-D Bio stratigraphy and regional significance of nine trilobite faunules from Antarctic outcrops and moraines; 28 species representing 21 genera are described UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-190734 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2071 CONTENTS Page Page Abstract_ _ ________________________ Dl Physical stratigraphy______________________________ D6 I&troduction. _______________________ 1 Regional correlation within Antarctica ________________ 7 Biostratigraphy _____________________ 3 Systematic paleontology._____-_______-____-_-_-----_ 9 Early Cambrian faunules.________ 4 Summary of classification of Antarctic Early and Australaspis magnus faunule_ 4 Chorbusulina wilkesi faunule _ _ 5 Middle Cambrian trilobites. ___________________ 9 Chorbusulina subdita faunule _ _ 5 Agnostida__ _ _________-____-_--____-----__---_ 9 Early Middle Cambrian f aunules __ 5 Redlichiida. __-_--------------------------_---- 12 Xystridura mutilinia faunule- _ 5 Corynexochida._________--________-_-_---_----_ -
Coupled Oceanic Oxygenation and Metazoan Diversification During the Early–Middle Cambrian?
Coupled oceanic oxygenation and metazoan diversification during the early–middle Cambrian? Chao Li1*, Chengsheng Jin1, Noah J. Planavsky2, Thomas J. Algeo1,3,4, Meng Cheng1, Xinglian Yang5, Yuanlong Zhao5, and Shucheng Xie1 1State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China 2Department of Geology and Geophysics, Yale University, New Haven, Connecticut 06520, USA 3State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China 4Department of Geology, University of Cincinnati, Cincinnati, Ohio 45221-0013, USA 5College of Resource and Environment, Guizhou University, Guiyang 550003, China ABSTRACT We conducted a high-resolution Fe-trace element geochemical study The early–middle Cambrian (Fortunian to Age 4) is characterized of lower-middle Cambrian (Fortunian to Age 4) sections of the South by a significant increase in metazoan diversification. Furthermore, this China Craton representing intermediate- to deep-marine settings, includ- interval is marked by a prominent environmental and ecological expan- ing outer shelf (Jiuqunao-Wangjiaping, JW; note: Jiuqunao data were sion of arthropod- and echinoderm-rich biotas. Recent redox work has compiled from Och et al. [2016]), slope (Wuhe-Geyi, WG), and basinal suggested that this shift occurred during stable or decreasing marine (Zhalagou, ZLG) sections of the Yangtze Block (Fig. DR1 in the GSA oxygen levels, suggesting that these paleobiological and paleoecological Data Repository1). Linking our redox proxy analysis with detailed pale- transformations were decoupled from a redox control. We tested this ontological data from the lower-middle Cambrian of South China affords idea by conducting new paleoredox analyses on Age 2–Age 4 Cambrian the unique opportunity to investigate the association, if any, between outer shelf (Jiuqunao-Wangjiaping), slope (Wuhe-Geyi), and basinal ocean-redox evolution and metazoan diversification during the early to (Zhalagou) sections of the South China Craton. -
Arthropod Pattern Theory and Cambrian Trilobites
Bijdragen tot de Dierkunde, 64 (4) 193-213 (1995) SPB Academie Publishing bv, The Hague Arthropod pattern theory and Cambrian trilobites Frederick A. Sundberg Research Associate, Invertebrate Paleontology Section, Los Angeles County Museum of Natural History, 900 Exposition Boulevard, Los Angeles, California 90007, USA Keywords: Arthropod pattern theory, Cambrian, trilobites, segment distributions 4 Abstract ou 6). La limite thorax/pygidium se trouve généralementau niveau du node 2 (duplomères 11—13) et du node 3 (duplomères les les 18—20) pour Corynexochides et respectivement pour Pty- An analysis of duplomere (= segment) distribution within the chopariides.Cette limite se trouve dans le champ 4 (duplomères cephalon,thorax, and pygidium of Cambrian trilobites was un- 21—n) dans le cas des Olenellides et des Redlichiides. L’extrémité dertaken to determine if the Arthropod Pattern Theory (APT) du corps se trouve généralementau niveau du node 3 chez les proposed by Schram & Emerson (1991) applies to Cambrian Corynexochides, et au niveau du champ 4 chez les Olenellides, trilobites. The boundary of the cephalon/thorax occurs within les Redlichiides et les Ptychopariides. D’autre part, les épines 1 4 the predicted duplomerenode (duplomeres or 6). The bound- macropleurales, qui pourraient indiquer l’emplacement des ary between the thorax and pygidium generally occurs within gonopores ou de l’anus, sont généralementsituées au niveau des node 2 (duplomeres 11—13) and node 3 (duplomeres 18—20) for duplomères pronostiqués. La limite prothorax/opisthothorax corynexochids and ptychopariids, respectively. This boundary des Olenellides est située dans le node 3 ou près de celui-ci. Ces occurs within field 4 (duplomeres21—n) for olenellids and red- résultats indiquent que nombre et distribution des duplomères lichiids. -
Tentative Correlation of Cambrian Series 2 Between South China and Other Continents
Tentative correlation of Cambrian Series 2 between South China and other continents JINLIANG YUAN, XUEJIAN ZHU, JIHPAI LIN & MAOYAN ZHU The apparent absence, in Cambrian Series 2, of widespread and rapidly evolving organisms comparable to the later agnostids, graptolites, conodonts, ammonites, or planktonic foraminifers, has prevented a consistent intercontinental biostratigraphy. Occasional genera, and (rarely) species, of trilobites, archaeocyathans and other groups may be found in more than one region. Nevertheless, based on the complete trilobite and archaeocyathan successions in the shallow water Yangtze Platform and in deeper water Jiangnan Slope environment, correlation of Cambrian Series 2 between South China and other continents is discussed in detail. The oldest trilobite Parabadiella and Tsunyidiscus in South China can be correlated with the oldest trilobite Abadiella in Australia, Profallotapis in Siberia and Eofallotaspis in Morocco. • Key words: Cambrian Series 2, correlation, South China, other continents. YUAN, J.L., ZHU, X.J., LIN,J.P.&ZHU, M.Y. 2011. Tentative correlation of Cambrian Series 2 between South China and other continents. Bulletin of Geosciences 86(3), 397–404 (2 tables). Czech Geological Survey. Prague, ISSN 1214-1119. Manuscript received December 17, 2010; accepted in revised form July 1, 2011; published online Septem- ber 22, 2011; issued September 30, 2011. Jinliang Yuan, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China; [email protected] • Xuejian Zhu, Jihpai Lin & Maoyan Zhu, State Key Laboratory of Palaeontology and Stratigra- phy, Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences, Nanjing, 210008, China International correlation of Cambrian Series 2 has been a nomenclature lead to paucity of biostratigraphically useful major problem since the concept of four series within the data in key regions (Palmer 1998, Geyer 2001). -
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. -
Posterior Border
Palaeontology Practical 8 Phylum Arthropoda – Class Trilobata Arthropods • Chitinous exoskeleton • Bilaterally symmetrical • Articulated segmented bodies that are partitioned in three • Paired jointed appendages for movement and feeding • Periodic moulting (ecdysis) • Antennae and/or multiple eyes • 75% of all living animal species • Includes insects, crustaceans, spiders, extinct trilobites and eurypterids • Coelomates, possibly related to annelids • Developed nervous and circulatory systems • Advanced feeding, many have jaw structures • The most successful invertebrate group • Advanced in terms of feeding and locomotion • Able to invade different environments and modes of life • Thus, marine and terrestrial • Good geological record (hard exoskeleton) from the Lower Cambrian Trilobites • Trilobites are the oldest group of arthropods. • They first appear in rocks of Lower Cambrian and died out in the Late Permian. • They were marine, mainly benthic and had • extremely variable morphologies and lifestyles. • They have a distinctive tri lobed • morphology (hence their name) • Over 1500 genera are known and several thousand species • Usually small, between 5-8 cm but some forms could get up to 70 cm General morphology • Segmented bodies with chitinous exoskeletons and joined, paired limbs • The body is divided longitudinally into three regions: 1. The cephalon 2. The thorax 3. The pygidium • The exoskeleton covers both the dorsal and ventral side of the body • Consists of a two-layered cuticle of chitin • Usually it is hardened by the impregnation of calcium carbonate The cephalon • the head which consists of a single plate, made up of several fused segments. • sense organs are found on the head • there are also certain lines of weakness, known as cephalic sutures, which look like cracks on the surface but apparently facilitated ecdysis • They are important for taxonomic determinations • shape pentagonal to semicircular with transverse posterior edges. -
A New Representative of the Lichid Genus Ohleum (Trilobita) from the Eifelian (Middle Devonian) of Southern Belgium Peter G
GEOLOGICA BELGICA (2012) 15/3: 120-125 A new representative of the lichid genus Ohleum (Trilobita) from the Eifelian (Middle Devonian) of southern Belgium Peter G. TAGHON1, Enrico BONINO2 & Bernard MOTTEQUIN3 1 Deinse Horsweg 12, B 9031 Gent, Belgium. E-mail [email protected]. 2 Back to the Past Museum, Puerto Morelos, Quintana Roo 77580, Mexico. 3 Unité de Paléontologie animale et humaine, Université de Liège, Allée du 6 Août, Bât. B18, B 4000 Liège 1, Belgium. ABSTRACT. Trilobites of the family Lichidae are relatively poorly diversified within the Eifelian mixed siliciclastic-carbonate succession of the southern margin of the Dinant Synclinorium (Belgium). Until now, they were only represented by species belonging to the genera Ceratarges and Eifliarges. The recent discovery of a well-preserved specimen within the Eifelian-aged Jemelle Formation in the Couvin area led us to propose the first detailed description of a representative of the genusOhleum (O. magreani sp. nov.) in the Ardennes. KEYWORDS: trilobites, Lichida, Devonian, Ardennes. RESUME. Un nouveau représentant du genre lichidé Ohleum (Trilobita) de l’Eifelien (Dévonien moyen) du Sud de la Belgique. Les trilobites de la famille des Lichidae sont relativement peu diversifiés au sein de la succession eifelienne du bord sud du Synclinorium de Dinant (Belgique) qui est caractérisée par une sédimentation mixte silicoclastique à carbonatée. Jusqu’à présent, ils étaient seulement représentés par des espèces appartenant aux genres Ceratarges et Eifliarges. La découverte récente d’un spécimen bien conservé au sein de la Formation de Jemelle d’âge eifelien dans la région couvinoise nous amène à proposer la première description détaillée d’un représentant ardennais du genre Ohleum (O. -
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. -
Lower Paleozoic
Paleozoic Time Scale and Sea-Level History Sponsored, in part, by: Time ScaLe R Creator Updated by James G. Ogg (Purdue University) and Gabi Ogg to: GEOLOGIC TIME SCALE 2004 Cen Mesozoic (Gradstein, F.M., Ogg, J.G., Smith, A.G., et al.2004) Paleozoic ICS Precambrian and The Concise Geologic Time Scale (Ogg, J.G., Ogg, G. & Gradstein, F.M., 2008) Paleozoic Sequences -- Haq and Schutter (Science, 2008) Geo- magnetic Standard Chronostratigraphy Mega- Sequences Coastal Onlap and Mean Sea- Paleozoic Long- and Silurian-Ordovician Ordovician Trilobite Zones and Polarity Sequences (nomenclature by Level (intermediate term) Short-Term Sea Level Sea Level Sealevel Events major Cambrian events Conodont Zonation Graptolite Zonation Age Period Epoch Stage Primary of Sloss J. Ogg) 0 100 200m 0 100 200m 0 100 200m (Baltoscandia) South China 416.1 Monograptus bouceki - Oulodus elegans detortus transgrediens - perneri Silur-8 Monograptus branikensis - Pri-1 417.5 lochkovensis 418.02 Ozarkodina remscheidensis Pridoli Interval Zone Monograptus parultimus - ultimus 418.7 Lud-3 419.0 Ozarkodina crispa Monograptus formosus 419.75 Silur-7 Ozarkodina snajdri Interval Zone Neocucullograptus kozlowskii - 420 Ludfordian Ludlow-Pridoli Polonograptus podoliensis Lud-2 420.5 420.7 Polygnathoides siluricus mixed-polarity interval 421.0 Saetograptus leintwardinensis 421.3 Lud-1 Ancoradella ploeckensis Ludlow Lobograptus scanicus Gorstian 422.0 Silur-6 [ not zoned ] 422.9 Kockelella stauros Neodiversograptus nilssoni Gor-1 423.0 Colonograptus ludensis Colonograptus praedeubeli