Mode of Growth and Functional Morphology of Autozooids in Some Recent and Paleozoic Tubular Bryozoa
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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. -
Palaeontologia Electronica DISCRIMINATION OF
Palaeontologia Electronica http://palaeo-electronica.org DISCRIMINATION OF FENESTRATE BRYOZOAN GENERA IN MORPHOSPACE Steven J. Hageman and Frank K. McKinney ABSTRACT Concepts for generic diagnoses and discrimination of biserial fenestrate Bryozoa (Fenestellidae) have varied historically, but have largely been based on specialized colony forms (e.g., Archimedes), the shape and budding arrangement of chambers and other internal skeletal features such as hemisepta, and occasionally on the pres- ence or absence of discrete characters, such as placement of nodes on the frontal sur- face (e.g., Minilya). The question remains as to whether biserial fenestrate genera represent real biological clades, or whether they are convenient groupings of morpho- types based on untested characters. This study evaluates the distribution of 1075 operational taxonomic units (OTUs) from 15 fenestrate genera with measurements for nine morphometric characters – external features are not emphasized in most generic diagnoses. Here, each OTU represents a composite or idealized individual from a col- ony. Results show that OTUs plotted in principal component space do largely form coherent clusters based on a priori generic assignments. Thus the groupings based on characters other than the ones used to originally define them, add support to the notion of biological significance for recognized genera. The exceptions actually highlight and help resolve known issues. Therefore, we recognize Alternifenestella as a junior syn- onym of the genus Spinofenestella, and propose reassignment of Laxifenestella serrat- ula in Snyder (1991) to Fenestella serratula, and Fenestella sp. 1 in Ernst and Schroeder (2007) as Rectifenestella. We do not advocate that biserial fenestrate generic concepts should be based on the nine external characters used in this study, but rather that they can be used independently to evaluate the coherence of genera based on other discrete characters. -
Reconstructions of Late Ordovician Crinoids and Bryozoans from the Decorah Shale, Upper Mississippi Valley Sibo Wang Senior Inte
Reconstructions of Late Ordovician crinoids and bryozoans from the Decorah Shale, Upper Mississippi Valley Sibo Wang Senior Integrative Exercise March 10, 2010 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree from Carleton College, Northfield, Minnesota TABLE OF CONTENTS ABSTRACT INTRODUCTION ........................................................................................................ 01 GEOLOGIC SETTING ................................................................................................ 03 Late Ordovician world ................................................................................. 03 Southern Minnesota and the Decorah Shale ............................................... 03 Benthic community ....................................................................................... 05 Marine conditions ........................................................................................ 05 CRINOIDS ................................................................................................................. 06 General background and fossil record ........................................................ 06 Anatomy ....................................................................................................... 07 Decorah Shale crinoids ................................................................................10 BRYOZOANS ............................................................................................................. 10 General background and -
Bryozoan Skeletal Index (BSI): a Measure of the Degree of Calcification in Stenolaemate Bryozoans
BRYOZOAN STUDIES 2019 Bryozoan Skeletal Index (BSI): a measure of the degree of calcification in stenolaemate bryozoans Patrick N. Wyse Jackson1*, Marcus M. Key, Jr.2 and Catherine M. Reid3 1 Department of Geology, Trinity College, Dublin 2, Ireland [*corresponding author: e-mail: [email protected]] 2 Department of Earth Sciences, Dickinson College, Carlisle, Pennsylvania 17013-2896, USA [e-mail: [email protected]] 3 School of Earth and Environment, University of Canterbury, Private Bag 4800, Christchurch, New Zealand [e-mail: [email protected]] ABSTRACT minimal. In this study the differences observed in The Upper Ordovician of the Cincinnati Arch region BSI between trepostome and cystoporate species in of the United States has yielded a highly diverse the Cincinnatian is significant, and ramose colonies bryozoan fauna, and which provides an excellent show a higher BSI than encrusting zoaria in the data source for use in this study that proposes same fauna. a novel measure of the degree of skeletal material in Palaeozoic stenolaemate bryozoans. This study is based on 16 trepostome species and one cystoporate INTRODUCTION species described from the Dillsboro Formation Bryozoans of the Class Stenolaemata are characterised (Maysvillian to early Richmondian, Cincinnatian) of by having autozooecial chambers that are broadly Indiana and in 20 species (15 trepostomes and five tubular in nature. They were significant members of cystoporates) from the Lexington Limestone and the Palaeozoic faunas appearing in the Ordovician Clays Ferry -
The Classic Upper Ordovician Stratigraphy and Paleontology of the Eastern Cincinnati Arch
International Geoscience Programme Project 653 Third Annual Meeting - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett – Kyle R. Hartshorn – Allison L. Young – Cameron E. Schwalbach – Alycia L. Stigall International Geoscience Programme (IGCP) Project 653 Third Annual Meeting - 2018 - Athens, Ohio, USA Field Trip Guidebook THE CLASSIC UPPER ORDOVICIAN STRATIGRAPHY AND PALEONTOLOGY OF THE EASTERN CINCINNATI ARCH Carlton E. Brett Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Kyle R. Hartshorn Dry Dredgers, 6473 Jayfield Drive, Hamilton, Ohio 45011, USA ([email protected]) Allison L. Young Department of Geology, University of Cincinnati, 2624 Clifton Avenue, Cincinnati, Ohio 45221, USA ([email protected]) Cameron E. Schwalbach 1099 Clough Pike, Batavia, OH 45103, USA ([email protected]) Alycia L. Stigall Department of Geological Sciences and OHIO Center for Ecology and Evolutionary Studies, Ohio University, 316 Clippinger Lab, Athens, Ohio 45701, USA ([email protected]) ACKNOWLEDGMENTS We extend our thanks to the many colleagues and students who have aided us in our field work, discussions, and publications, including Chris Aucoin, Ben Dattilo, Brad Deline, Rebecca Freeman, Steve Holland, T.J. Malgieri, Pat McLaughlin, Charles Mitchell, Tim Paton, Alex Ries, Tom Schramm, and James Thomka. No less gratitude goes to the many local collectors, amateurs in name only: Jack Kallmeyer, Tom Bantel, Don Bissett, Dan Cooper, Stephen Felton, Ron Fine, Rich Fuchs, Bill Heimbrock, Jerry Rush, and dozens of other Dry Dredgers. We are also grateful to David Meyer and Arnie Miller for insightful discussions of the Cincinnatian, and to Richard A. -
Phylogenetic Analysis of the Bryozoan Suborder Rhabdomesina Open PDF in Browser
' >' ' W“ nu MUM-h“, l LIBRARY my Midligan State nlversity This is to certify that the thesis entitled PHYLOGENETIC ANALYSIS OF THE BRYOZOAN SUBORDER RHABDOMESINA presented by LANCE PAQUETI'E has been accepted towards fulfillment of the requirements for the MS. degree in Geological Sciences flaw Major ProfessoFESngQture floater 20, 2003’ d , Date MSU is an atfinnative-action, equal-opportunity employer I----o---c----o--------c---------o—-o---.----.--.-n-o-.-u-------o-o-u-u--u-.-.-.-------o-o-o-v-o-u- PLACE IN RETURN BOX to remove this checkout from your record. TO AVOID FINES return on or before date due. MAY BE RECALLED with earlier due date if requested. DATE DUE DATE DUE DATE DUE 5/08 K:/Proleoc&Pres/ClRC/DateDueindd PHYLOGENETIC ANALYSIS OF THE BRYOZOAN SUBORDER RHABDOMESINA By Lance Paque’tte A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Geological Sciences 2008 ABSTRACT PHYLOGENETIC ANALYSIS OF THE BRYOZOAN SUBORDER RHABDOMESINA By Lance Paquette The Suborder Rhabdomesina is a group of Paleozoic bryozoans that has been taxonomically problematic when it comes to the evolutionary pattern and relationships within the group. It is not even well understood if it merits subordinal or ordinal rank. No prior phylogenetic attempts have uncovered the evolutionary history of the group. This cladistic study uses genera from many different published sources that have been placed within this order/suborder at any given time. The character list that was used to code each individual genus was developed from a variety of published sources and also some were developed independently during the research and coding process of this study. -
Contributions to the Geology of the North-Western Himalayas 1-59 ©Geol
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 1975 Band/Volume: 32 Autor(en)/Author(s): Fuchs Gerhard Artikel/Article: Contributions to the Geology of the North-Western Himalayas 1-59 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Contributions to the Geology of the North-Western Himalayas GERHARD FUCHS 64 Figures and 5 Plates BAND 32 • WIEN 1975 EIGENTÜMER, HERAUSGEBER UND VERLEGER: GEOLOGISCHE BUNDESANSTALT, WIEN SCHRIFTLEITUNG: G.WOLETZ DRUCK: BRÜDER HOLLINEK, WIENER NEUDORF ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at 3 Abh. Geol. B.-A. Band 32 59 Seiten 64 Fig., 5 Beilagen Wien, Feber 1975 Contribution to the Geology of the North-Western Himalayas By GERHARD FUCHS With 64 figures and 5 plates (= Beilage 1—5) Data up to 1972, except PI. 1 'I NW-Himalaya U Stratigraphie i3 Tektonik £ Fazies Contents Zusammenfassung 3 1.3.1. The Hazara Slates 40 Abstract 4 1.3.2. The Tanol Formation 40 Preface 5 1.3.3. The Sequence Tanakki Boulder Bed — Introduction 5 Sirban Formation 41 1. Descriptive Part 6 1.3.4. The Galdanian and Hazira Formations 42 1.1. Kashmir 6 1.3.5. The Meso-Cenozoic Sequence 44 1.1.1. The Riasi-Gulabgarh Pass Section 6 1.4. Swabi — Nowshera 46 1.1.2. The Apharwat Area . 11 1.4.1. Swabi 46 1.1.3. The Kolahoi-Basmai Anticline (Liddar valley) ... 17 1.4.2. -
Colony-Wide Water Currents in Living Bryozoa
COLONY-WIDE WATER CURRENTS IN LIVING BRYOZOA by Patricia L Cook British Museum (Natural History), Cromwell Rd., London, SW7 5BD, Gt.Brltain. Résumé Les divers types de courants d'eau des colonies de Bryozoaires sont décrits et analysés. Pour les formes encroûtantes, il en existe au moins trois à l'heure actuelle. Pour les petites colonies de Cyclostomes (Lichenopora), il n'existe qu'un courant centripète se dirigeant vers l'extérieur. Chez certaines Chéilostomes (Hippoporidra) et Cténostomes (Alcyonidium nodosum), des «monticules» sont formés par des groupes de zoïdes dont les couronnes de tentacules sont absentes, réduites ou ne se nourrissent pas. Les « monticules » sont le siège de courants passifs, dirigés vers l'extérieur. Chez d'autres Chéilostomes (Schizoporella, Hippo- porina et Cleidochasma) et des Cténostomates (Flustrellidra hispida), des groupes de zoïdes à couronnes de tentacules hétéromorphes constituent des « cheminées » produisant des courants actifs se dirigeant vers l'extérieur. Des suggestions sont faites concernant une suite d'observations sur les colonies vivantes. Introduction Observation of living colonies is increasingly becoming an essential feature in the study of Bryozoa. Not only is it the primary method of discovering the function of zooids or parts of zooids, it is the first step in testing the established inferences about analogous and homologous structures in preserved material. The study of the functions of whole colonies and the degree and kind of integrative factors contributing to colony-control of these functions is in its early stages. These primary observations can only be made on living colonies. The wide variation in astogeny and ontogeny of structures and their functions in Bryozoa require much further work on many species before any general patterns may become obvious. -
Paleobiogeographic Associations Among Mississippian Bryozoans
PALEOBIOGEOGRAPHIC ASSOCIATIONS AMONG MISSISSIPPIAN BRYOZOANS BY Ryan FitzGerald Morgan A THESIS Submitted to Michigan State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Geological Sciences 2010 i ABSTRACT PALEOBIOGEOGRAPHIC ASSOCIATIONS AMONG MISSISSIPPIAN BRYOZOANS BY Ryan FitzGerald Morgan Area cladograms produced by parsimony analysis of endemicity coupled with seriation, paired group cluster, principal coordinates, and detrended correspondence analyses demonstrate endemic associations of Mississippian-age bryozoans. These methods identified three major biogeographic associations (North America I, North America II, and Old World Realms), and nine minor associations (Waverly, Keokuk, Warsaw, Burlington, St. Louis, Chester, Tethys I, Tethys II, Russia, Kazakhstan-Siberia Provinces). These associations, along with latitudinal diversity gradients, provide support for an early closure of the tropical seaway (Rheic Ocean) that existed between Laurussia and Gondwana, along with support for faunal shifts due to the onset of Gondwanan glaciation and the restriction of North American faunas from the more eastern Tethyan faunas. ii DEDICATION This thesis is dedicated to my mother, Christena Morgan, in recognition of her encouragement, support, and gift of an inquisitive mind. iii ACKNOWLEDGEMENTS I would like to first acknowledge Dr Robert L Anstey, both for all the help and guidance he has supplied over the course of my education and this thesis, and also for providing the push to engage in this field of study. I would also like to acknowledge my wife, Christina L Gurski, who has spent many long hours listening to me ramble about all sorts of ideas, and for providing much needed distraction from this thesis; if not for her it would have been completed ages ago. -
Upper Ordovician Bryozoa from the Montagne De Noire, Southern France
Journal of Systematic Palaeontology 5 (4): 359–428 Issued 19 November 2007 doi:10.1017/S1477201907002155 Printed in the United Kingdom C The Natural History Museum Upper Ordovician Bryozoa from the Montagne de Noire, southern France Andrej Ernst∗ Institut f¨ur Geowissenschaften der Christian-Albrechts-Universit¨at zu Kiel, Ludewig-Meyn-Str. 10, D-24118 Kiel, Germany Marcus Key† Department of Geology, P.O. Box 1773, Dickinson College, Carlisle, PA 17013-2896, USA SYNOPSIS This study focuses on bryozoans from the Upper Ordovician rocks of the Montagne de Noire, southern France and additional material from contemporary rocks of the Carnic Alps. Based on museum collections, 68 bryozoan species were identified with 18 species being new: Ceramo- porella grandis sp. nov., Crassalina fungiforme sp. nov., Lichenalia nodata sp. nov., Atactoporella magnopora sp. nov., Dekayia buttleri sp. nov., Stigmatella carnica sp. nov., Trematopora gracile sp. nov., Bythopora tenuis sp. nov., Nicholsonella divulgata sp. nov., N. recta sp. nov., Matsutrypa elegantula sp. nov., M. rogeri sp. nov., Nematotrypa punctata sp. nov., Stellatodictya valentinae sp. nov., Ptilodictya feisti sp. nov., Pseudohornera dmitrii sp. nov., Ralfinella elegantula sp. nov. and Moorephylloporina contii sp. nov. Trepostomes are the most abundant and diverse group with 40 of the total 68 species, but cyclostomes, cystoporates and cryptostomes are also present. The age of the fauna is Caradoc to Ashgill, according to the distribution of species and genera. The fauna has palaeogeographical -
Annals 2/Ross & Ross
Paper in: Patrick N. Wyse Jackson & Mary E. Spencer Jones (eds) (2008) Annals of Bryozoology 2: aspects of the history of research on bryozoans. International Bryozoology Association, Dublin, pp. viii+442. TWO HUNDRED YEARS OF AUSTRALIAN BRYOZOOLOGY 271 Two hundred years of Australian bryozoology June R.P. Ross* and Charles A. Ross† *Department of Biology, MS 9160 Western Washington University, Bellingham, WA 98225, USA. †Department of Geology, MS 9080 Western Washington University, Bellingham, WA 98225, USA. 1. Introduction 1.1 Development of Australian bryozoology 1.2 Stratigraphic Distribution of Studies 1.3 Geographic Distribution of Studies 2. Tertiary and Recent Bryozoologists 2.1 Early Discoveries 2.2 Second half of the 19th century 3. Twentieth century 3.1 Further Exploration of Coastal Seas 3.2 Western Australia 3.3 Introduced bryozoans 3.4 Bryozoan sediment facies 4. Paleozoic Bryozoa 4.1 Late Paleozoic 4.2 Lower Paleozoic 4.3 Current Knowledge 5. Acknowledgements 6. Bibliography of Australian bryozoology and selected references 1. Introduction 1.1 Development of Australian bryozoology In the 18th and 19th centuries the southern seas remained one of the vast unknown areas of the world as explorers sought to discover new regions of the globe. Australia remained a largely poorly known region; its continental coasts unmapped except in the vaguest outline. Flinder’s survey in 1825 in the small vessel ‘Tom Thumb’ succeeded in mapping the entire coast line. Early Australian bryozoan studies up until about 1850 parallel these explorations and are from collections that were returned to Europe by French and British 272 ANNALS OF BRYOZOOLOGY 2 Figure 1.—Map of Australia showing various basins and ‘basement’ areas. -
The Geology of the Country Between Arthur's Lakes and the Lake Rivel', Tasmania
The Geology of the Country between Arthur's Lakes and the Lake Rivel', Tasmania By ALAN H. VOISEY Departnwnl: of GCO/ogN and Geo!TI'(lphy, the New Enylond University College, ArmJrtnle (Communicated by Professor S. W. Carey) PLATE IV and FlO. 1 INTRODUCTION The country between Arthur'~ Lakes and the Lake HiveI' shown on Plate IV is drained in the western part by Tumbledown Creek and .Tones Rivulet which flow into the Eastern Lake, and in the eastern by the tributaries of the Lab' River. The escarpment of the Western Tiers marks the eastem margin of the Central Plateau of Tasmania. Mapping was carried out with the assistance of aerial photographs and the structure-l ines of the dolerites were (,btained from them, This paper is submitted as a small contribution to the aerial mapping of Tasmania. GENERAL GEODOGY Three main groups of rocks were found outcropping in the area mapped. (i) A series of metamorphosed rocks of probable Cambrian age consisting of slates, quartzites and 'porphyroids' which is laced by quartz veins. (ii) A series of fossiliferous sandstones, shales and glacial beds of Permian age. (iii) The .T urassic dolerites which are in the form of sills i11j eded into the other formations, There are also deposits of glacial material resulting from the presence of the Pleistocene Ice sheets and masseR of dolerite talus of more recent origin., Alluvium occupies areas marginal to the main streams. (1) CAMBRIAN No fossils have been found in the metarYlorphosed rocks assigned to this system but S. W. Carey (verbal communication) regards them as being the equivalents of similar bcds of Cambrian age elsevvhere in Tasmania.