Nomenclatural Changes for Three Preoccupied Trilobites Genera
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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. -
Copertina Guida Ai TRILOBITI V3 Esterno
Enrico Bonino nato in provincia di Bergamo nel 1966, Enrico si è laureato in Geologia presso il Dipartimento di Scienze della Terra dell'Università di Genova. Attualmente risiede in Belgio dove svolge attività come specialista nel settore dei Sistemi di Informazione Geografica e analisi di immagini digitali. Curatore scientifico del Museo Back to the Past, ha pubblicato numerosi volumi di paleontologia in lingua italiana e inglese, collaborando inoltre all’elaborazione di testi e pubblicazioni scientifiche a livello nazonale e internazionale. Oltre alla passione per questa classe di artropodi, i suoi interessi sono orientati alle forme di vita vissute nel Precambriano, stromatoliti, e fossilizzazioni tipo konservat-lagerstätte. Carlo Kier nato a Milano nel 1961, Carlo si è laureato in Legge, ed è attualmente presidente della catena di alberghi Azul Hotel. Risiede a Cancun, Messico, dove si dedica ad attività legate all'ambiente marino. All'età di 16 anni, ha iniziato una lunga collaborazione con il Museo di Storia Naturale di Milano, ed è a partire dal 1970 che prese inizio la vera passione per i trilobiti, dando avvio a quella che oggi è diventata una delle collezioni paleontologiche più importanti al mondo. La sua instancabile attività di ricerca sul terreno in varie parti del globo e la collaborazione con professionisti del settore, ha permesso la descrizione di nuove specie di trilobiti ed artropodi. Una forte determinazione e la costruzione di un nuovo complesso alberghiero (AZUL Sensatori) hanno infine concretizzzato la realizzazione -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
An Bolaspide Doza, Argentina
Matematisk-fysiske Meddelelser udgivet af Det Kongelige Danske Videnskabernes Selskab Bind 32, nr. 11 Mat. Fys. Medd. Dan. Vid. Selsk. 32, no. 11 (1960) DANISH SCIENTIFIC INVESTIGATIONS IN ARGENTINA UNDER THE AUSPICES OF FUNDAC1ÖN WILLIAMS, BUENOS AIRES MIDDI AN BOLASPIDE 01 DOZA, ARGENTINA BY CHIU POULSEN København I960 i kommission hos Ejnar Munksgaard CONTENTS Page Page Introduction................................................. 3 Stigmagnostus canotensis (Rusconi). 15 Remarks on the locality, Cerrillo El Soli- Prometeoraspis canotensis n. sp........... 17 tario........................................................... 5 Williamsina cortesi n. sp...................... 19 Descriptions of genera and species .... 5 harringtoni n. sp............. 20 Brachiopoda............................................. 5 mikkelseni n. sp.............. 21 Dicellomus? sp. ind............................... 5 ornata n. sp..................... 22 Mollusca?................................................... 5 Talbotinella communis n. sp................... 24 Orthotheca sp.......................................... 5 leanzai n. sp..................... 25 Trilobita..................................................... 6 rusconii n. sp.................... 27 Agnostus exsulatus n. sp....................... 6 Bolaspidella lucieae n. sp..................... 28 Baltagnostus hospitus n. sp.................. 7 Canotaspis aliéna ................................ 29 — mendozertsis n. sp............ 8 Goycoia tellecheai Rusconi................ 30 CAavagnostus chipiquensis -
Dinosaur Provincial Park, Alberta
For Potuakhali University - http://www.pstu.ac.bd/ Fossil insect from Green River Formation Eocene Green River Shale, Wasatch County, Utah, USA http://www.ucmp.berkeley.edu/tertiary/eoc/greenriver.h tml https://en.wikipedia.org/wiki/Green_River_Formation Along the White River south of Bonanza, Utah. The low light colored outcrops near the river on the right are the Green River Formation Ammonite (Hematite replacement) Era – Cretaceous From – Morocco Triassic Scute Locality- Saint john, Arizona, USA (Blue-green Algae/ cyanobacterial colony) Stromatolite from Morocco Billion Years – 600 Million Years Old. Pre-Cambrian Locality – Near Atlas Mountain, Ourzarzate Morocco https://www.geocaching.com/geocache/GC2NKN4_moroccan- stromatolites http://epod.usra.edu/blog/2006/02/morocco- stromatolites.html Mosasaur Tooth, Cretaceous, Morocco . Triassic/Permian reptile bone ? Need better picture Ancient Mollusk, The Orthoceras 400 MYO, Devonian Morocco http://www.fossils-facts-and-finds.com/orthoceras.html https://en.wikipedia.org/wiki/Orthoceras Echinoid fossil Jurassic, Morocco Baltic Amber (Please confirm) 44 MYO - Eocene epoch Baltic amber (succinite) From-Poland (collected from Baltic Sea shores) Dinosaur Bone and black iron stone from Dinosaur Provincial park, Canada. Cretaceous ~65 MYO (reference Pictures below) Silurian Horn Coral – Rugos Kentucky, USA Jelly fish Carboniferous Era, Mazon Creek , USA (reference Pictures below) Carboniferous Trilobite, 300 Million Years=৩০ ক ো綿 বছর পুরোন ো Era – Carboniferous Locality – Bangor Limestone Formation, Northern Alabama, USA http://mrdata.usgs.gov/geology/state/sgmc- unit.php?unit=TNMbh%3B3 https://books.google.ca/books?id=zcdUAAAAYAAJ&pg=SL8- PA7&lpg=SL8- PA7&dq=Bangor+Limestone+Formation&source=bl&ots=JlCU5 _bKBc&sig=wCZ87cTc8hWHZHzXfSsteqG5azA&hl=en&sa=X&ve d=0ahUKEwi- lqL7_qnKAhULjZQKHQgzBQMQ6AEIOjAF#v=onepage&q=Bang or%20Limestone%20Formation&f=false LAVA STONE - SNOWFLAKE OBSIDIAN Could not recognize from picture the left one and the one under the paper & the one under the bigger ammonite in Ziplock. -
(Upper Cambrian, Paibian) Trilobite Faunule in the Central Conasauga River Valley, North Georgia, Usa
Schwimmer.fm Page 31 Monday, June 18, 2012 11:54 AM SOUTHEASTERN GEOLOGY V. 49, No. 1, June 2012, p. 31-41 AN APHELASPIS ZONE (UPPER CAMBRIAN, PAIBIAN) TRILOBITE FAUNULE IN THE CENTRAL CONASAUGA RIVER VALLEY, NORTH GEORGIA, USA DAVID R. SCHWIMMER1 WILLIAM M. MONTANTE2 1Department of Chemistry & Geology Columbus State University, 4225 University Avenue, Columbus, Georgia 31907, USA <[email protected]> 2Marsh & McLennan, Inc., 3560 Lenox Road, Suite 2400, Atlanta, Georgia 30326, USA <[email protected]> ABSTRACT shelf-to-basin break, which is interpreted to be east of the Alabama Promontory and in Middle and Upper Cambrian strata the Tennessee Embayment. The preserva- (Cambrian Series 3 and Furongian) in the tion of abundant aphelaspine specimens by southernmost Appalachians (Tennessee to bioimmuration events may have been the re- Alabama) comprise the Conasauga Forma- sult of mudflows down the shelf-to-basin tion or Group. Heretofore, the youngest re- slope. ported Conasauga beds in the Valley and Ridge Province of Georgia were of the late INTRODUCTION Middle Cambrian (Series 3: Drumian) Bo- laspidella Zone, located on the western state Trilobites and associated biota from Middle boundary in the valley of the Coosa River. Cambrian beds of the Conasauga Formation in Two new localities sited eastward in the Co- northwestern Georgia have been described by nasauga River Valley, yield a diagnostic suite Walcott, 1916a, 1916b; Butts, 1926; Resser, of trilobites from the Upper Cambrian 1938; Palmer, 1962; Schwimmer, 1989; Aphelaspis Zone. Very abundant, Schwimmer and Montante, 2007. These fossils polymeroid trilobites at the primary locality and deposits come from exposures within the are referable to Aphelaspis brachyphasis, valley of the Coosa River, in Floyd County, which is a species known previously in west- Georgia, and adjoining Cherokee County, Ala- ern North America. -
An Appraisal of the Great Basin Middle Cambrian Trilobites Described Before 1900
An Appraisal of the Great Basin Middle Cambrian Trilobites Described Before 1900 By ALLISON R. PALMER A SHORTER CONTRIBUTION TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 264-D Of the 2ty species described prior to I(?OO, 2/ are redescribed and 2C} refigured, and a new name is proposedfor I species UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price $1 (paper cover) CONTENTS Page Abstract..__________________________________ 55 Introduction ________________________________ 55 Original and present taxonomic names of species. 57 Stratigraphic distribution of species ____________ 57 Collection localities._________________________ 58 Systematic descriptions.______________________ 59 Literature cited____________________________ 82 Index __-_-__-__---_--______________________ 85 ILLUSTRATIONS [Plates 13-17 follow page 86] PLATE 13. Agnostidae and Dolichometopidae 14. Dorypygidae 15. Oryctocephalidae, Dorypygidae, Zacanthoididae, and Ptychoparioidea 16. Ptychoparioidea 17. Ptychoparioidea FIGUBE 3. Index map showing collecting localities____________________________ . Page 56 in A SHORTER CONTRIBUTION TO GENERAL GEOLOGY AN APPRAISAL OF THE GREAT BASIN MIDDLE CAMBRIAN TRILOBITES DESCRIBED BEFORE 1900 By ALLISON R. PALMER ABSTRACT the species and changes in their generic assignments All 29 species of Middle Cambrian trilobites -
First Record of the Ordovician Fauna in Mila-Kuh, Eastern Alborz, Northern Iran
Estonian Journal of Earth Sciences, 2015, 64, 2, 121–139 doi: 10.3176/earth.2015.22 First record of the Ordovician fauna in Mila-Kuh, eastern Alborz, northern Iran Mohammad-Reza Kebria-ee Zadeha, Mansoureh Ghobadi Pourb, Leonid E. Popovc, Christian Baarsc and Hadi Jahangird a Department of Geology, Payame Noor University, Semnan, Iran; [email protected] b Department of Geology, Faculty of Sciences, Golestan University, Gorgan 49138-15739, Iran; [email protected] c Department of Geology, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, United Kingdom; [email protected], [email protected] d Department of Geology, Faculty of Sciences, Ferdowsi University, Azadi Square, Mashhad 91775-1436, Iran; [email protected] Received 12 May 2014, accepted 5 September 2014 Abstract. Restudy of the Cambrian–Ordovician boundary beds, traditionally assigned to the Mila Formation Member 5 in Mila- Kuh, northern Iran, for the first time provides convincing evidence of the Early Ordovician (Tremadocian) age of the uppermost part of the Mila Formation. Two succeeding trilobite assemblages typifying the Asaphellus inflatus–Dactylocephalus and Psilocephalina lubrica associations have been recognized in the uppermost part of the unit. The Tremadocian trilobite fauna of Mila-Kuh shows close similarity to contemporaneous trilobite faunas of South China down to the species level, while affinity to the Tremadocian fauna of Central Iran is low. The trilobite species Dactylocephalus levificatus and brachiopod species -
Th TRILO the Back to the Past Museum Guide to TRILO BITES
With regard to human interest in fossils, trilobites may rank second only to dinosaurs. Having studied trilobites most of my life, the English version of The Back to the Past Museum Guide to TRILOBITES by Enrico Bonino and Carlo Kier is a pleasant treat. I am captivated by the abundant color images of more than 600 diverse species of trilobites, mostly from the authors’ own collections. Carlo Kier The Back to the Past Museum Guide to Specimens amply represent famous trilobite localities around the world and typify forms from most of the Enrico Bonino Enrico 250-million-year history of trilobites. Numerous specimens are masterpieces of modern professional preparation. Richard A. Robison Professor Emeritus University of Kansas TRILOBITES Enrico Bonino was born in the Province of Bergamo in 1966 and received his degree in Geology from the Depart- ment of Earth Sciences at the University of Genoa. He currently lives in Belgium where he works as a cartographer specialized in the use of satellite imaging and geographic information systems (GIS). His proficiency in the use of digital-image processing, a healthy dose of artistic talent, and a good knowledge of desktop publishing software have provided him with the skills he needed to create graphics, including dozens of posters and illustrations, for all of the displays at the Back to the Past Museum in Cancún. In addition to his passion for trilobites, Enrico is particularly inter- TRILOBITES ested in the life forms that developed during the Precambrian. Carlo Kier was born in Milan in 1961. He holds a degree in law and is currently the director of the Azul Hotel chain. -
Olenid Trilobites: the Oldest Known Chemoautotrophic Symbionts?
Olenid trilobites: The oldest known chemoautotrophic symbionts? Richard Fortey* Department of Paleontology, Natural History Museum, Cromwell Road, London SW7 5BD, United Kingdom Communicated by Lynn Margulis, University of Massachusetts, Amherst, MA, April 3, 2000 (received for review March 1, 2000) Late Cambrian to early Ordovician trilobites, the family Olenidae, Given the widespread occurrence and taxonomic spread of were tolerant of oxygen-poor, sulfur-rich sea floor conditions, and chemoautotrophic symbiosis, it is likely to have been an ancient a case is made that they were chemoautotrophic symbionts. adaptation. Because direct evidence of the fossil bacteria seldom Olenids were uniquely adapted to this habitat in the Lower preserves, evidence of such habits tends to be inferred from Paleozoic, which was widespread in the Late Cambrian over Scan- taxonomic and͞or morphological data, which is not always dinavia. This life habit explains distinctive aspects of olenid mor- reliable (11). The long-ranging solemyid and lucinid bivalves (10) phology: wide thoraces and large numbers of thoracic segments, indicate that by the Silurian (ca. 420 million years), this life mode thin cuticle and, in some species, degenerate hypostome, and the already had been adopted by some groups with living descen- occasional development of brood pouches. Geochemical and field dants. Ancient vent associations have been recognized from at evidence is consistent with this interpretation. Olenids occupied least the Devonian (12). their specialized habitat for 60 million years until their extinction I show in this paper that even by the late Cambrian period (505 at the end of the Ordovician. million years ago) certain extinct arthropods, trilobites belonging to the family Olenidae, evolved features best understood as evidence olorless sulfur bacteria, a heterogeneous category of bacte- of sulfur chemoautotrophic mode of metabolism. -
IL Libro Del Museo by Enrico Bonino and Carlo Kier Is a Pleasant Treat
Trilobite_book_Copertina_Hi_res2.pdf 1 11/09/2009 18:24:55 Mu seu With regard to human interest in fossils, trilobites may rank second only to dinosaurs. Having studied trilobites most of my life, to m ck th a e Trilobiti – IL libro del Museo by Enrico Bonino and Carlo Kier is a pleasant treat. I am captivated by the abundant color images B P ● a of more than 500 diverse species of trilobites, mostly from the authors’ own collections. A s t Z Specimens amply represent famous trilobite localities around the world and typify forms from most of the 250-million-year U L ● history of trilobites. Numerous specimens are masterpieces of modern professional preparation. I eagerly await a promised TRILOBITI S e l n e s t English edition. Carlo Kier a o tori H Richard A. Robison Bonino Enrico Professor Emeritus University of Kansas IL libro del Museo L’idea di colmare una lacuna italiana di un libro scritto in lingua patria sui trilobiti non può che trovare il mio più incoraggiante appoggio. Alla base di tutto questo sta non solo la reciproca stima, ma una vera passione per gli argomenti trattati. Se a questo si aggiunge una buona competenza informatica di elaborazione dati ed un buon gusto estetico non può che nascere un buon libro che spicca rispetto a tanti per la dovizia di belle immagini corroborate da una scelta puntuale ed esplicativa al massimo dell’eccellenza. Prof. Maurizio Gnoli Titolare del corso di “Paleontologia” e “Paleontologia dei Vertebrati” Università degli Studi di Modena-Reggio Emilia. C M Y CM MY CY CMY Enrico Bonino nato in provincia di Bergamo nel 1966, Enrico si è laureato in Geologia presso il Dipartimento di K Scienze della Terra dell'Università di Genova. -
Middle Cambrian Trilobites (Miaolingian, Ehmaniella Biozone) from the Telt Bugt Formation of Daugaard-Jensen Land, Western North Greenland
BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK · VOL. 68 · 2020 Middle Cambrian trilobites (Miaolingian, Ehmaniella Biozone) from the Telt Bugt Formation of Daugaard-Jensen Land, western North Greenland JOHN S. PEEL Peel, J.S. 2020. Middle Cambrian trilobites (Miaolingian, Ehmaniella Biozone) from the Telt Bugt Formation of Daugaard-Jensen Land, western North Greenland. Bulletin of the Geological Society of Denmark, vol. 68, pp. 1–14. ISSN 2245-7070. https://doi.org/10.37570/bgsd-2020-68-01 A small fauna of middle Cambrian trilobites is described from the upper Telt Bugt Geological Society of Denmark Formation of Daugaard-Jensen Land, western North Greenland, and the formation https://2dgf.dk is formally defined.Blainiopsis holtedahli and Blainiopsis benthami, originally described from the equivalent Cape Wood Formation of Bache Peninsula, Nunavut, Canada, are Received 9 October 2019 documented in an assemblage assigned to the Ehmaniella Biozone (Topazan Stage of Accepted in revised form North American usage), Miaolingian Series, Wuliuan Stage, of the international stan- 5 February 2020 dard. Two new species are proposed: Ehmaniella sermersuaqensis and Clappaspis tupeq. Published online 9 March 2020 Keywords: Laurentia, North Greenland, Cambrian, Miaolingian (Wuliuan), tri- © 2020 the authors. Re-use of material is lobites. permitted, provided this work is cited. Creative Commons License CC BY: John S. Peel [[email protected]], Department of Earth Sciences (Palaeobiology), https://creativecommons.org/licenses/by/4.0/ Uppsala University, Villavägen 16, SE-75236 Uppsala, Sweden. The first Cambrian fossils from the Nares Strait setti 1951; Cooper et al. 1952; Palmer & Halley 1979). region, the narrow waterway separating northern- Several of the lithostratigraphic and biostratigraphic most Greenland and Canada, were collected from problems recognised in Poulsen’s (1927) studies were Bache Peninsula (Fig.