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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 -
Jurassic Algae of the Perachora-Peninsula: Biostratigraphical and Paleoecological Implications
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 1994 Band/Volume: 19 Autor(en)/Author(s): Dragastan Ovidiu, Gielisch Hartwig, Richter Detlef K., Grewer Till, Kaziur Thomas, Kube Bärbel, Radusch Christoph Artikel/Article: Jurassic algae of the Perachora-Peninsula: Biostratigraphical and paleoecological implications 49-81 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont., 19:49-81, Wien 1994 Jurassic algae of the Perachora-Peninsula: Biostratigraphical and paleoecological implications Jurassische Algen der Perachora Halbinsel: Biostratigraphische und paläoökologische Folgerungen by DRAGASTAN, Ovidiu,* GIELISCH, Hartwig**, RICHTER, Detlev K.**, GREWER, TiU**, KAZIUR, Thomas**, KUBE, Bärbel **& RADUSCH, Christoph** DRAGASTAN, O., GIELISCH, H„ RICHTER, D.K., GREWER, T„ KAZIUR, T„ KUBE, B. & RADUSCH, C., 1994. Jurassic algae of the Perachora-Peninsula: Biostratigraphical and paleoecological implications. — Beitr. Palaont., 19:49-81, 9 Figures, 6 Plates, Wien. ceae), Rivularia (Rivulariaceae), Alpinelia graeca n.sp. Contents (Scytonemataceae), Girvanella, Hedstroemia (Porostro- Abstract, Zusammenfassung.................................................. 49 mata) and Microproblematicae. 1. Introduction..............................................................................50 Biostratigraphically, a succession of algae and foramini- 2. Geological setting................................................................. -
(Foram in Ifers, Algae) and Stratigraphy, Carboniferous
MicropaIeontoIogicaI Zonation (Foramin ifers, Algae) and Stratigraphy, Carboniferous Peratrovich Formation, Southeastern Alaska By BERNARD L. MAMET, SYLVIE PINARD, and AUGUSTUS K. ARMSTRONG U.S. GEOLOGICAL SURVEY BULLETIN 2031 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Robert M. Hirsch, Acting Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Text and illustrations edited by Mary Lou Callas Line drawings prepared by B.L. Mamet and Stephen Scott Layout and design by Lisa Baserga UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1993 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25286 Denver, CO 80225 Library of Congress Cataloging in Publication Data Mamet, Bernard L. Micropaleontological zonation (foraminifers, algae) and stratigraphy, Carboniferous Peratrovich Formation, southeastern Alaska / by Bernard L. Mamet, Sylvie Pinard, and Augustus K. Armstrong. p. cm.-(U.S. Geological Survey bulletin ; 2031) Includes bibtiographical references. 1. Geology, Stratigraphic-Carboniferous. 2. Geology-Alaska-Prince of Wales Island. 3. Foraminifera, Fossil-Alaska-Prince of Wales Island. 4. Algae, Fossil-Alaska-Prince of Wales Island. 5. Paleontology- Carboniferous. 6. Paleontology-Alaska-Prince of Wales Island. I. Pinard, Sylvie. II. Armstrong, Augustus K. Ill. Title. IV. Series. QE75.B9 no. 2031 [QE671I 557.3 s--dc20 [551.7'5'097982] 92-32905 CIP CONTENTS Abstract -
2Nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS
2nd International Trilobite Conference (Brock University, St. Catharines, Ontario, August 22-24, 1997) ABSTRACTS. Characters and Parsimony. Jonathan M. Adrain, Department of Palaeontology, The Natural History Museum, London SW7 5BD, United King- dom; Gregory D. Edgecombe, Centre for Evolutionary Research, Australian Museum, 6 College Street, Sydney South, New South Wales 2000, Australia Character analysis is the single most important element of any phylogenetic study. Characters are simply criteria for comparing homologous organismic parts between taxa. Homology of organismic parts in any phylogenetic study is an a priori assumption, founded upon topological similarity through some or all stages of ontogeny. Once homolo- gies have been suggested, characters are invented by specifying bases of comparison of organismic parts from taxon to taxon within the study group. Ideally, all variation in a single homology occurring within the study group should be accounted for. Comparisons are between attributes of homologous parts, (e.g., simple presence, size of some- thing, number of something), and these attributes are referred to as character states. Study taxa are assigned member- ship in one (or more, in the case of polymorphisms) character-state for each character in the analysis. A single char- acter now implies discrete groupings of taxa, but this in itself does not constitute a phylogeny. In order to suggest or convey phylogenetic information, the historical status of each character-state, and of the the group of taxa it sug- gests, must be evaluated. That is, in the case of any two states belonging to the same character, we need to discover whether one state is primitive (broadly speaking, ancestral) or derived (representative of an evolutionary innovation) relative to the other. -
Trilobite Fauna of the Šárka Formation at Praha – Červený Vrch Hill (Ordovician, Barrandian Area, Czech Republic)
Bulletin of Geosciences, Vol. 78, No. 2, 113–117, 2003 © Czech Geological Survey, ISSN 1214-1119 Trilobite fauna of the Šárka Formation at Praha – Červený vrch Hill (Ordovician, Barrandian area, Czech Republic) PETR BUDIL 1 – OLDŘICH FATKA 2 – JANA BRUTHANSOVÁ 3 1 Czech Geological Survey, Klárov 3, 118 21 Praha 1, Czech Republic. E-mail: [email protected] 2 Charles University, Faculty of Science, Institute of Geology and Palaeontology, Albertov 6, 128 43 Praha 2, Czech Republic. E-mail: [email protected] 3 National Museum, Palaeontological Department, Václavské nám. 68, 115 79 Praha 1, Czech Republic. E-mail: [email protected] Abstract. Shales of the Šárka Formation exposed in the excavation on Červený vrch Hill at Praha-Vokovice contain a common but monotonous assem- blage of phyllocarids associated with other extremely rare arthropods. Almost all trilobite remains (genera Ectillaenus Salter, 1867, Placoparia Hawle et Corda, 1847 and Asaphidae indet.) occur in a single horizon of siliceous nodules of stratigraphically uncertain position, while the surprising occurrence of possible naraoid trilobite (Pseudonaraoia hammanni gen. n., sp. n.) comes from dark grey shales. The general character of the arthropod assemblage char- acterized by an expressive dominance of planktonic and/or epi-planktonic elements (phyllocarids) indicates a specific life environment (most probably due to poor oxygenation). This association corresponds to the assemblage preceding the Euorthisina-Placoparia Community sensu Havlíček and Vaněk (1990) in the lower portion of the Šárka Formation. Key words: Ordovician, Arthropoda, Trilobita, Naraoiidae, Barrandian Introduction calities, the trilobite remains on Červený vrch Hill occur in siliceous nodules in association with rare finds of car- The temporary exposure at the Praha-Červený vrch Hill poids (Lagynocystites a.o.), frequent remains of phyllo- provided a unique possibility to study a well-exposed secti- carids (Caryocaris subula Chlupáč, 1970 and C. -
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. -
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. -
Mesozoic and Cenozoic Calcareous Algae, Praecursors of Family Codiaceae
ACTA PALAEONTOLOGICA ROMANIAE V. 6 (2008), P 83-95. MESOZOIC AND CENOZOIC CALCAREOUS ALGAE, PRAECURSORS OF FAMILY CODIACEAE Ovidiu N. DRAGASTAN1 Abstract. It is amaizing how long time was the using of the marine green – algae, Family Codiaceae and the genus Codium, as suffix of many fossil genera (Carpathocodium, Arabicodium, Calabricodium, Madonicodium), without any relation with the real morphology of the Recent genus Codium. The genus Codium is well represented on warm – cool transitional marine coasts or in the inner shelf environments of carbonate platform. The genus Codium has an unique structural plan with thallus multibranched, noncalcareous, vesiculous crossed by medullary siphons and only one layer of cortical utricles. The utricles show a great anatomical diversity with diagnostic value in separating the approximately 100 Recent species. Until now, a real representative of the Recent Family Codiaceae in the fossil state was not found. Also, the same situation is with Recent genus Pseudocodium (Family Pseudocodiaceae). Contrary, the fossils praecursors of the Recent Codiaceae were recorded, described and included now, for the first time in the Family Praecodiaceae nov. fam. This family only with fossil representatives contains calcareous thalli composed by cylindrical branches crossed by medullary siphons, few in number (4 to 6, rarely 8) and only one utricles layer. The utricles layer is variable in morphology from species to species. Beside the late Triassic Hydracara kubeae Dragastan et al.2000 are introduced the following taxa: Lupertosinnium bariensis nov.gen.nov.sp. (early Barremian), L. banatensis n.sp. (late Barremian – early Aptian ), Alpinium tragelehni nov.gen.nov.sp. (Thanetian) and Atlasinium nov.gen. -
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. -
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. -
Presence of Naraoia Walcott, 1912 in the Middle Cambrian of Europe
SPANISH JOURNAL OF PALAEONTOLOGY Presence of Naraoia Walcott, 1912 (Nektaspida, Arthropoda) in the middle Cambrian of Europe (Murero, NE Spain) Rodolfo GOZALO1*, Mª Eugenia DIES ÁLVAREZ2, José Antonio GÁMEZ VINTANED3, Juan B. CHIRIVELLA4 & Eladio LIÑÁN5 1 Departamento de Botánica y Geología, Universitat de València, c/ Dr. Moliner 50, 46100- Burjassot, Spain; [email protected] 2 Departamento de Didáctica de las Ciencias Experimentales-IUCA, Universidad de Zaragoza, c/ Valentín Carderera 4, 22003-Huesca, Spain; [email protected] 3 Department of Geosciences, Faculty of Sciences & Information Technology, Universiti Teknologi PETRONAS (UTP), 32610 Bandar Seri Iskandar (Tronoh), Perak Darul Ridzuan, Malaysia; [email protected] 4 Departamento de Ciencias de la Educación, Universidad CEU Cardenal Herrera. Avda. Seminario s/n, 46113 Moncada, Spain; [email protected] 5 Departamento de Ciencias de la Tierra-IUCA. Universidad de Zaragoza, 50009 Zaragoza, Spain; [email protected] * Corresponding author Gozalo, R., Dies Álvarez, Mª.E., Gámez Vintaned, J.A., Chirivella & Liñán, E. 2018. Presence of Naraoia Walcott, 1912 (Nektaspida, Arthropoda) in the middle Cambrian of Europe (Murero, NE Spain). [Presencia de Naraoia Walcott, 1912 (Nektaspida, Arthropoda) en el Cámbrico medio de Europa (Murero, NE de España)]. Spanish Journal of Palaeontology, 33 (1), 83-88. Manuscript received 30 January 2018 © Sociedad Española de Paleontología ISSN 2255-0550 Manuscript accepted 2 March 2018 ABSTRACT RESUMEN The genus Naraoia Walcott, 1912, a Burgess Shale-type El género Naraoia Walcott, 1912, es un fósil de tipo Burgess fossil known from the lower and middle Cambrian of British Shale, conocido en el Cámbrico inferior y medio de la Columbia (Canada), Idaho and Utah (USA), as well as from Columbia Británica (Canadá), Idaho y Utah (EE.UU.), así Yunnan and Guizhou provinces (China), is now reported from como en las provincias chinas de Yunnan y Guizhou. -
A New Phyllopod Bed-Like Assemblage from the Burgess Shale of the Canadian Rockies
ARTICLE Received 30 Dec 2013 | Accepted 7 Jan 2014 | Published 11 Feb 2014 DOI: 10.1038/ncomms4210 A new phyllopod bed-like assemblage from the Burgess Shale of the Canadian Rockies Jean-Bernard Caron1,2,3, Robert R. Gaines4,Ce´dric Aria1,2, M. Gabriela Ma´ngano5 & Michael Streng6 Burgess Shale-type fossil assemblages provide the best evidence of the ‘Cambrian explosion’. Here we report the discovery of an extraordinary new soft-bodied fauna from the Burgess Shale. Despite its proximity (ca. 40 km) to Walcott’s original locality, the Marble Canyon fossil assemblage is distinct, and offers new insights into the initial diversification of metazoans, their early morphological disparity, and the geographic ranges and longevity of many Cambrian taxa. The arthropod-dominated assemblage is remarkable for its high density and diversity of soft-bodied fossils, as well as for its large proportion of new species (22% of total diversity) and for the preservation of hitherto unreported anatomical features, including in the chordate Metaspriggina and the arthropod Mollisonia. The presence of the stem arthropods Misszhouia and Primicaris, previously known only from the early Cambrian of China, suggests that the palaeogeographic ranges and longevity of Burgess Shale taxa may be underestimated. 1 Department of Natural History-Palaeobiology, Royal Ontario Museum, 100 Queen’s Park, Toronto, Ontario, Canada M5S 2C6. 2 Department of Ecology and Evolutionary Biology, University of Toronto, 25 Willcocks Street, Toronto, Ontario, Canada M5S 3B2. 3 Department of Earth Sciences, University of Toronto, 25 Russell Street, Toronto, Ontario, Canada M5S 3B1. 4 Geology Department, Pomona College, 185 E. Sixth Street, Claremont, California 91711, USA.