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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. -
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. -
Mode of Growth and Functional Morphology of Autozooids in Some Recent and Paleozoic Tubular Bryozoa
Mode of Growth and Functional Morphology of Autozooids in Some Recent and Paleozoic Tubular Bryozoa SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY NUMBER 8 SERIAL PUBLICATIONS OF THE SMITHSONIAN INSTITUTION The emphasis upon publications as a means of diffusing knowledge was expressed by the first Secretary of the Smithsonian Institution. In his formal plan for the Insti tution, Joseph Henry articulated a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This keynote of basic research has been adhered to over the years in the issuance of thousands of titles in serial publications under the Smithsonian imprint, com mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Annals of Flight Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in History and Technology In these series, the Institution publishes original articles and monographs dealing with the research and collections of its several museums and offices and of profes sional colleagues at other institutions of learning. These papers report newly acquired facts, synoptic interpretations of data, or original theory in specialized fields. These publications are distributed by mailing lists to libraries, laboratories, and other in terested institutions and specialists throughout the world. Individual copies may be obtained from the Smithsonian Institution Press as long as stocks are available. S. -
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 -
A New Family of Trepostome Bryozoans from the Ordovician Simpson Group of Oklahoma
700 JOURNAL OF PALEONTOLOGY, V. 64, NO. 5, 1990 --, B. D. PRATI, AND A. J. ROWELL. 1989. Early Cambrian reefs, Holyoake Range, Antarctica. New Zealand Journal of Geology and reef complexes, and associated lithofacies of the Shackleton Lime Geophysics, 31:397-404. stone, Transantarctic Mountains. Sedimentology, 36:341-362. Sowv'Ev, I. A., AND G. E. GRIKUROV. 1979. Novie dannie o ras --, AND A. J. ROWELL. In press. The pre-Devonian Palaeozoic elas prostranenii Kembriyskikh trilobitov v khrebtakh Ardzhentina i She tics of the central Transantarctic Mountains: stratigraphy and depo klton [New data on the spread of Cambrian trilobites in the Argentina sitional setting. In M. R. A. Thomson, J. W. Crame, and J. W. Thom and Shackleton Mountains]. Antarktika, 18:54-73. son (eds.), Geologic Evolution of Antarctica. Cambridge University TATE, R. 1892. The Cambrian fossils ofSouth Australia. Transactions Press, Cambridge. and Proceedings of the Royal Society of South Australia, 15:183- ROWELL, A. J., K. R. EvANs, AND M. N. REES. 1989. Fauna of the 189. Shackleton Limestone. Antarctic Journal of the United States, 1988 WRONA, R. 1987. Cambrian microfossil Hadimopanel/a Gedik from Review, 23(5):13-14. glacial erratics in West Antarctica. Palaeontological Polonica, 49:37- --, AND M. N. REES. 1989. Early Palaeozoic history of the upper 48. Beardmore Glacier area: implications for a major Antarctic structural Y OCHELSON, E. L. AND E. STUMP. 1977. Discovery of Early Cambrian boundary within the Transantarctic Mountains. Antarctic Science, l: fossils at Taylor Nunatak, Antarctica. Journal of Paleontology, 81: 249-260. 872-875. --, --, R. A. COOPER, AND B. R. -
Ordovician Fauna
II ORDOVICIAN FAUNA By ARTHUR C. McFARLAN THE ORDOVICIAN FAUNA OF KENTUCKY By ARTHUR C. McFARLAN INTRODUCTION HIGH BRIDGE SERIES (M. R. CAMPBELL, 1898) Massive, cliff-forming limestone of Chazy and Stones River age. Three formations are recognized: CAMP NELSON (A. M. Miller, 1905, p. 10). Limestone composed of irregular patches and ramifications of granular rock of the Oregon type distributed through a matrix of dense limestone of the Tyrone type, presumably algal in origin. On weathering the surface becomes honeycombed. Fossils are not common, the more characteristic being Maclurites bigsbyi, Escharopora ramosa, a species of Rhinidictya, and various cephalopods. OREGON—Kentucky River Marble (A. M. Miller, 1905, p. 10). Grey to cream colored, granular, magnesian limestone. TYRONE—Birdseye Limestone of Linney (A. M. Miller, 1905, p. 10). Dense gray, dove, or cream colored limestone, breaking with conchoidal fracture and with small facets of Fig. 25. Map of Kentucky showing outcrop of Ordovician rocks. 50 THE PALEONTOLOGY OF KENTUCKY coarsely crystalline calcite. On weathering the surface becomes white, in which the darker facets are conspicuous, giving rise to the name Birdseye. A bed of bentonite, a greenish clay, occurs near the top. Fossils are few and include such forms as Strophomena incurvata, (see p. 80) Orthis tricenaria, Leperditia fabulites, and the cephalopods Endoceras, Actinoceras, and Cameroceras. LEXINGTON LIMESTONE (M. R. Campbell, 1898) This is the Trenton of Kentucky. As originally defined it included the strata between the Tyrone and Flanagan Chert. As later applied by Miller (1905, p. 18) and Foerste everything up to the base of the Cynthiana is included. -
Bryozoan Fauna of the Upper Clays Ferry, Kope, and Lower Fairview Formations (Edenian, Upper Ordovician) at Moffett Road, Northe
Bryozoan fauna of the upper Clays Ferry, Kope, and lower Fairview Formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky By Olgerts L. Karklins U.S. Geological Survey Open-File Report 83-31 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Contents Page Abstract 1 Introduction 2 Description of locality 5 Previous work 5 Materials and methods 6 Moffett Road section 7 Composition 8 Abundance and distribution 10 Biostratigraphy 10 Bryozoans of the Edenian Stage in the Moffett Road section 14 Systematic Paleontology 15 Order Trepostomata 17 Family Monticuliporidae 17 Heterotrypidae 20 Batostomellidae 24 Amplexoporidae 26 Trematoporidae 28 Caloporidae 30 Family unknown 33 Order Cystoporata 34 Family Ceramoporidae 34 Constellariidae 37 Order Cryptostomata 38 Suborder Fenestelloidea 38 Family Phylloporinidae 38 ii (contents, cont.) Page Suborder Ptilodictyoidea ' 39 Family Ptilodictyidae 39 Stictoporellidae 41 Ehinidictyidae 41 References cited 43 Illustrations Table 1. Ranges of species in feet, relative abundance in percent and the number of prepared specimens of each species in stratigraphic order above the base of the Moffett Road section. Figure 1. Index maps of location of Moffett Road section (A) and the De Mossville 1:24000 quadrangle (B) in northern Kentucky. Figure 2. Pie diagram of relative abundance of species in the Moffett Road section. Plate 1. Occurrence of species and stratigraphic positions of collections in the Moffett Road section. Plate 2. Stratigraphic ranges and relative abundances of species in the Moffett Road section. iii Bryozoan fauna of the upper Clays Ferry, Kope, and lower Fairview Formations (Edenian, Upper Ordovician) at Moffett Road, northern Kentucky Abstract Bryozoans are abundant and highly diversified in the Kope Formation (Upper Ordovician) of the proposed stratotype section for the Edenian Stage in Kentucky. -
Epizoan and Endoskeletozoan Distribution Across Reassembled Ramose Stenolaemate Bryozoan Zoaria from the Upper Ordovician (Katian) of the Cincinnati Arch Region, USA
Epizoan and endoskeletozoan distribution across reassembled ramose stenolaemate bryozoan zoaria from the Upper Ordovician (Katian) of the Cincinnati Arch region, USA PATRICK N. WYSE JACKSON & MARCUS M. KEY, JR WYSE JACKSON, P.N. & KEY, M.M., JR, 2019:11:15. Epizoan and endoskeletozoan distribution across reassembled ramose stenolaemate bryozoan zoaria from the Upper Ordovician (Katian) of the Cincinnati Arch region, USA. Australasian Palaeontological Memoirs 52, 169–178. ISSN 2205–8877. The Upper Ordovician (Katian) of the Cincinnati, Ohio, USA region has yielded bedding-plane assemblages of ramose stenolaemate bryozoans. Sixteen colonies were reassembled which provide valuable data on the settlement patterns of epizoans and endoskeletozoans, information on the timing of infestation and encrustation, and on environmental and taphonomic conditions affecting the bryozoan colonies. Various parameters were assessed: the size, incidence and position of borings; whether or not they show a regeneration rim that would indicate an in-vivo relationship between host and boring organism; and the position on branches of epizoans, measured on proximal and distal colony portions, and on the upper-facing or lower- facing sides of colonies as they lay on the substrate. Epizoans include thin adnate colonies of Crepipora and other unidentified cystoporate bryozoans, cornulitids, the problematicum Hederella and the cnidarian Sphenothallus. Encrustation was generally slight and in all but one colony was evenly distributed on all sides of branches indicating probable in-vivo infestation. The one exception suggests that the colony acted as a hardground once it had toppled over and was lying on the substrate. Boring into the zoarial skeleton took place both before and after death of colonies. -
Kentucky Geological Survey
Kentucky Geological Survey, CHARLES J. NORWOOD, Director. Bulletin No.5. The Upper Ordovician Rocks of Kentucky and their Bryozoa. BY JOHN M. NICKLES. Office of the Survey: Lexington, Ky. 1905. PRINTED BY THE GEO. G. FETTER COMPANY, LOUISVILLE. 1905. Letter of Transmittal. To His Excellency, J. C. W. BECKHAM, Governor of Kentucky. Sir:—I have the honor to herewith submit for publication a report on the Upper Ordovician Rocks of Kentucky and their Bryozoa, by Professor John M. Nickles. This is a contribution toward the proper classification of our geological formations, which, as has been stated in another report, is necessary for an intelligent and adequate understanding of their economic values. In order, for example, that we may be able to estimate the depth below the surface at which a known oil or gas-bearing stratum may be found, we must be able to identify the beds seen at the surface and know their relations to other beds in the series of which the oil-bearing stratum forms a member. The identification of particular beds or a group of beds in a series of stratified rocks largely depends upon a knowledge of their characteristic fossils. There is less general knowledge of bryozoa than of other fossil forms, and yet they are often the only trustworthy means for discriminating some of the minor divisions of a formation series. The Survey has been fortunate in having the services of Professor Nickles in dealing with that difficult feature of our classification studies, as they relate to the Upper Ordovician or Cincinnatian rocks. The general study of the Cincinnatian series is in the hands of Professor Aug.