Using Marine Fossils to Unlock the Middle Devonian Paleoenvironments of Western New York (For K-12 Teachers and Collectors)
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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. -
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. -
Paleozoic Life in the Seas
Paleozoic Life in the Seas • Environmental variables to watch – Sea level – Positions of land and sea (continents & oceans) – Climate • Patterns of diversity • Mass extinctions • Cast of characters 1 The “Sepksoski Curve” From Sepkoski, Paleobiology, 1982 2 The Big 5 Mass Extinctions 3 4 From Alroy et al. PNAS (2001) 5 6 7 Cambrian Period 543 - 490 million years ago 8 Cambrian Trilobites 9 Archaeocyathids Cambrian seascape, painting by Zdenek Burian, ca. 1960 10 Ordovician Period 490 to 443 Million Years Ago 11 Ordovician Brachiopods Brachiopods, Ordovician, Ohio Ordovician Corals Rugose Tabulate www.humboldt.edu/~natmus/Exhibits/Life_time/Ordovician.web/55b.jpg 12 Maclurites at Crown Point, Lake Champlain, NY Leviceraurus Asaphus Ordovician Trilobites Isotelus 13 The largest known trilobite Isotelus rex, Late Ordovician, northern Manitoba Triarthrus, Ordovician, New York 14 Kentucky Ordovician Nautiloids Ohio Minnesota 15 Giant nautiloid Rayonnoceras solidiforme Mississippian, Fayetteville, ARK 16 Ordovician crinoids www.emc.maricopa.edu/faculty/ farabee/BIOBK/1ord04b.gif Ordovician vertebrates Harding Sandstone, Utah 17 www.karencarr.com/images/Gallery / gallery_ordovician.jpg Ordovician seascape Ordovician seascape www.pbs.org/wgbh/nova/link/images/ hist_img_03_ordo.jpg 18 Ordovician seascape http://www.ucmp.berkeley.edu/ordovician/ordovicsea.gif Ordovician seascape www.emc.maricopa.edu/faculty/farabee/BIOBK/1ord04b.gif 19 Silurian Period 443 to 417 Million Years Ago 20 Bumastus Arctinurus Silurian Trilobites Dalmanites Eurypterids -
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. -
Middle Devonian)
F-l Paleontological Problems of the Hamilton Group (Middle Devonian) H.B. Rollins, N. Eldridge, R.M. Linsley The stratigraphy of the Hamilton Group of the'Middle Devonian of New York State was most recently treated in its entirety by Cooper (1930, 1957). The Hamilton Group of the Chenango Valley (see chart 1) consists primarily of fine clastic sediments and occupies a mid position in this wedge shaped body of rock. In the east the wedge is thickest (about 1,680' in Schoharie Valley (Gruban, 1903, p. 213) and it thins to 285' at Lake Erie in the west (Cooper, 1930, p. 121). In the Chenango Valley the Hamilton Group is 1, 465' thick (op. cit. p. 121) and has a dip to the southwest of 65-75 feet per mile (op. cit. p. 119). The Hamilton Group lies unconformably on the Onondaga Limestone and is overlain unconformably by the Tully Formation. In a very crude sense the Hamilton Group of the Chenango Valley is composed of fine-grained black shales and limestones at the base (the Marcellus Formation) and more clastic units in the upper portion (Skaneateles, Ludlowville and Moscow Formations). However within each of these formations there exists considerable variation from true mud shales through siltstones and up to fine-grained sandstones. The nature of the substrate obviously had a great effect on the faunas associated with them. The black shales are typically associated with a Leiorhynchus fauna, gray shales and siltstones with a Tropidoleptus fauna and the fine-grained sandstones are dominated by bivalves. A more detailed discussion of some of these problems will follow in sections relating to each of the three stops of this trip. -
4. the Phylogeny and Disparity of the Odontopleurida (Trilobita)
University of Bath PHD Trilobita: phylogeny and evolutionary patterns Pollitt, Jessica R. Award date: 2006 Awarding institution: University of Bath Link to publication Alternative formats If you require this document in an alternative format, please contact: [email protected] General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the public portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the public portal ? Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. Download date: 10. Oct. 2021 TRILOBITA: PHYLOGENY AND EVOLUTIONARY PATTERNS Jessica R. Pollitt A thesis submitted for the degree of Doctor of Philosophy University of Bath Department of Biology & Biochemistry September 2006 COPYRIGHT Attention is drawn to the fact that copyright of this thesis rests with its author. This copy of the thesis has been supplied on condition that anyone who consults it is understood to recognise that its copyright rests with its author and that no quotation from the thesis and no information derived from it may be published without the prior written consent of the author. -
Field Studies of the Middle Devonian Ludlowville-Moscow Sequence in the Genesee and Seneca Valleys, New York State
FIELD STUDIES OF THE MIDDLE DEVONIAN LUDLOWVILLE-MOSCOW SEQUENCE IN THE GENESEE AND SENECA VALLEYS, NEW YORK STATE STEPHEN M. MAYER Department of Geology SUNY College at Fredonia Fredonia, NY 14063 INTRODUCTION Numerous authors have studied and described in detail the unique depositional environments and the excellent fossil preservation found in the Middle Devonian Hamilton Group sediments of New York State (Grabau, 1899; Cooper, 1930; Grasso, 1973; Brett and others, 1986; Savarese and others, 1986). The advancement of high resolution stratigraphic mapping has permitted detailed correlations of facies divisions in the uppermost Ludlowville Formation across western and central New York (Mayer, 1989; Mayer and others, 1994). The focus of this field trip is to examine the spatial and temporal sedimentary relationships as well as the abundant and well preserved fossils in the Upper Ludlowville-Lower Moscow Formations of the Hamilton Group; in particular, the uppermost Wanakah Shale, Jaycox Shale and Tichenor Limestone Members in the Genesee and Seneca Valleys (Figure 1). N Lake 'ontario r Co. Ludlowville & Mo. cow Fm •• o 10 20. 30 Mil •• I Co. o 10 20 30 <40 50 Kill Figure 1. Key Ludlowville - Moscow outcrops in the Genesee Valley and Seneca Valley region. Modified from Baird (1979). GEOLOGIC SETTING The sediments of the Hamilton Group were deposited as part of the prograding Catskill Delta Complex at the northern margin of the Appalachian Basin in North America. Reconstruction of North American paleolatitudes, based on paleomagnetic studies, have placed the continental landmass across the paleoequator with the Hamilton deposition 491 o occurring at approximately 0-30- S latitude (Oliver, 1976; Ettensohn, 1985; Van der Voo, 1988). -
A Window Into the Devonian Period of Western New York
PENN DIXIE FOSSIL PARK & NATURE RESERVE: A WINDOW INTO THE DEVONIAN PERIOD OF WESTERN NEW YORK Philip J. Stokes, PhD and Holly A. Schreiber, PhD Penn Dixie Fossil Park & Nature Reserve, 3556 Lakeshore Road, Suite 230, Blasdell, NY 14219 E-mail: [email protected]; [email protected] An Image Caught in Time – Earth was very different four hundred million years ago (Figure 1). Eons before the first dinosaurs scuttled through prehistoric forests, North America and Europe together formed a large landmass along the Tropic of Capricorn (Figure 2B). Western New York was submerged beneath tropical seas, which were teeming with both old and new forms of life. The Devonian Period (419 to 359 million years ago) marked an important chapter in Earth history. Life on land was just starting to take root — literally, as Earth’s first forests produced the oxygen needed by the earliest amphibians who hunted giant insects at the water’s edge. Along the Eastern half of North America, mountains rose as the Acadian Orogeny (i.e., mountain building event) -- was underway. Like a highway pileup, the Proto-African Plate crashed into and onto the North American plate, causing earthquakes, intense volcanic activity, and crustal deformation (Figure 2C). Beginning in the middle of the Devonian Period and lasting for 60 million years, The Acadian Orogeny set the stage for our unique assemblage of fossils. To the West of the coastal collision zone, the Earth’s crust flexed and bent to accommodate the incoming mass of another continent. Like a compressed accordion, land was forced downwards. Over centuries, the ocean meandered its way along the widening and deepening depression towards New York. -
The Trilobite Subfamily Homalonotinae from the Upper Silurian and Lower Devonian of Poland
ACT A PAL A EON T 0 LOG ICA POL 0 N I C A Vol. XX 1975 No.1 EWA TOMCZYKOWA THE TRILOBITE SUBFAMILY HOMALONOTINAE FROM THE UPPER SILURIAN AND LOWER DEVONIAN OF POLAND Abstract. - Twelve species of trilobites, including six new ones (Dipleura praecox sp. n., Trimerus lobatus sp. n., T. novus sp. n., Digonus bostoviensis sp. n., D. elegans sp. n., and Parahomalonotus angusticostatus sp. n.), assigned to five genera of the subfamily Homalonotinae from the Upper Ludlovian, Upper Gedinnian and Lower Siegenian of Poland are described below. Taxonomic criteria of this subfamily are discussed, along with its outline phylogeny. INTRODUCTION Relatively frequently found, the specimens of Homalonotinae are, in general, poorly preserved and, therefore, they are among the groups of trilobites that have so far been rather insufficiently studied. Since their occurrence is limited to the Llandovery through Middle Devonian, they may serve as a good index fossil. Their paleogeographical and correlative importance in the Upper Silurian and Lower Devonian was discussed se parately (Tomczykowa, 1974). The materials, on which the present paper is based, were collected by the writer in 1956-1958 in the Holy Cross Mts. Most of them, how ever, come from the boreholes managed by the Geological Institute, that is, from Goldap, Bost6w, Ciepie16w, Bialopole, Krowie Bagno, Lopiennik, Strzelce IG-2 and Zakrzew IG-3, as well as from the drillings of the Oil Research Survey (Malochwiej and Rozkopaczew boreholes) (Text-fig. 1). The writ.er's remarks on the species described thus far are based on the observation of the casts of holotypes and other specimens from clas sic collections. -
(Upper Hamilton Group). in the Tully Valley, Onondaga County Thomas X
Benthic Communities of the Ludlowville and Moscow Formations (Upper Hamilton Group). in The Tully Valley, Onondaga County Thomas X. Grasso. Prof. Geoscience Dept., Monroe Community College, Rochester, New York 14623 INTRODUCTION The Devonian System in New York State varies from carbon ates below (Ulsterian and lowest Erian Series) to coarse con tinental clastics at the top (Chautauqua n Ser i es). and repre sents a westward migrating deltaic complex built during Midd l e and Late Devonian ti me . This deltaic complex. the Catskill Delta. is today repre sented by a wedge of sedimentary rock that thickens and coarsens eastward . The clastic wedge is pierced at several hor i zo ns by relatively thin. but geograp hica l ly widespread, litho l ogically dis t inct units that do not change facies as rapidly as the rocks above or below . Serving as time pl anes. these key beds subdivide the clastic wedge into a number of major time-stratigraphic units . Three carbonate keybeds in the lower portion of the wedge serve t o su bdivide the lowest time stratig r aphic unit. the Ilami l ton Group (M i ddle Devonian), into four f ormations; which are from oldest to youngest. the Marce ll us, Skaneateles, Ludlowville and Moscow Formations. The Middle Devonian Hamilton Group of New York State is structural l y simp l e and hi ghly foss il iferous. thereby lending itself t o detai l ed stratigraph i c, pa l eonto l ogic. and pa l eo ecologic studies. I n Centra l New York it consists of approx imately 1 , 000 feet of sha l es. -
Geology and Mineral Resources of Frederick County
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY AND MINERAL RESOURCES OF FREDERICK COUNTY Charles Butts and Raymond S. Edmundson BULLETIN 80 VIRGINIA DIVISION OF MINERAL RESOURCES James L. Calver Commissioner ol Mineral Resources and State Geologisl CHARLOTTESVI LLE, VI RGINIA | 966 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY AND MINERAL RESOURCES OF FREDERICK COUNTY Charles Butts and "'"Raymond S. Edmundson BULLETIN 80 VIRGINIA DIVISION OF MINERAL RESOURCES James L. Calver Commissioner of Mineral Resources and State Geologist CHARLOTTESVILLE, VIRGINIA I 966 Couuorwnlr-trr or VnctNrl Dnp,llruBxt oF PuRctrAsEs eto Suppr-v Rrcrrruorqo 1966 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond, Virginia MenvrN M. Surrronr,ltNo, Director A. S. Recrrat, J*., Executiue Assistant BOARD Canr,rsr,e H. HunrBr,srNe, Williamsburg, Chairman ANonnw A. Fenr,ov, Danville, Vice-Chairman Joe P. Gn Ls, Roanoke Ar,r,eN M. HBvwenp, Newport News Cr,euor A. Ju,ssue, Jn., Charlottesville Genraxo E. Moss, Chase City Ennu,sr L. Surrrr, Grundy JorrN S. TrronxroN, Culpeper Ancrrrr L. WENnrcH, Hopewell CONTENTS Pecr Abstract 1 qrannage . 5 5 6 9 .'..'....',....'..',.',......''..'.'..'...'.'..'....,....-'.....'..'.......'.....'.'.....'..'.''..'.-.'.',.. l ? 12 o1 2r 24 26 28 Lincolnshire formation ,o r{unourgEdinburg rormatlonformation --. ... ... ....... ......... ......... .. .................. 30 Oranda formation ................ -
A Pictorial Guide to the Orders of Trilobites
A PICTORIAL GUIDE TO THE ORDERS OF TRILOBITES by Samuel M. Gon III, Ph.D. ORDER ORDER PROETIDA ASAPHIDA Superfamily Superfamily Superfamily Superfamily Superfamily Superfamily Superfamily Superfamily Superfamily Aulacopleuroidea Bathyuroidea Proetoidea Anomocaroidea Asaphoidea Trinucleioidea Dikelocephaloidea Cyclopygoidea Remopleuridoidea Aulacopleuridae Bathyuridae Proetidae Anomocarellidae Asaphidae Trinucleidae Dikelocephalidae Cyclopygidae Remopleurididae Aulacopleura Goniotelus Cyphoproetus Glyphaspis Ogygiocaris Cryptolithus Dikelocephalus Cyclopyge Remopleurides ORDER ORDER ORDER ORDER HARPETIDA CORYNEXOCHIDA LICHIDA ODONTOPLEURIDA Suborder Suborder Suborder Suborder Superfamily Superfamily Superfamily Harpetina Corynexochina Illaenina Leiostegiina Lichoidea Dameselloidea Odontopleuroidea Harpetidae Dorypygidae Illaenidae Kaolishaniidae Lichidae Damesellidae Odontopleuridae Harpes Olenoides Bumastus Mansuyia Arctinurus Drepanura Kettneraspis ORDER ORDER PHACOPIDA PTYCHOPARIIDA Suborder Suborder Suborder Suborder Suborder Calymenina Cheirurina Phacopina Ptychopariina Olenina Calymenidae Cheiruridae Phacopidae Acastidae Tricrepicephalidae Ptychopariidae Ellipsocephalidae Olenidae Calymene Ceraurus Phacops Kayserops Tricrepicephalus Modocia Ellipsocephalus Olenus ORDER ORDER AGNOSTIDA REDLICHIIDA Suborder Suborder Suborder Suborder Agnostina Eodiscina Olenellina Redlichiina Agnostidae Condylopygidae Eodiscidae Olenellidae Fallotaspididae Redlichiidae Paradoxididae Xystriduridae Emuellidae Agnostus Pleuroctenium Pagetia Paedeumias