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PUBLICATIONS by JAMES SPRINKLE 1965 -- Sprinkle, James
PUBLICATIONS BY JAMES SPRINKLE 1965 -- Sprinkle, James. 1965. Stratigraphy and sedimentary petrology of the lower Lodgepole Formation of southwestern Montana. M.I.T. Department of Geology and Geophysics, unpublished Senior Thesis, 29 p. (see #56 and 66 below) 1966 1. Sprinkle, James and Gutschick, R. C. 1966. Blastoids from the Sappington Formation of southwest Montana (Abst.). Geological Society of America Special Paper 87:163-164. 1967 2. Sprinkle, James and Gutschick, R. C. 1967. Costatoblastus, a channel fill blastoid from the Sappington Formation of Montana. Journal of Paleon- tology, 41(2):385-402. 1968 3. Sprinkle, James. 1968. The "arms" of Caryocrinites, a Silurian rhombiferan cystoid (Abst.). Geological Society of America Special Paper 115:210. 1969 4. Sprinkle, James. 1969. The early evolution of crinozoan and blastozoan echinoderms (Abst.). Geological Society of America Special Paper 121:287-288. 5. Robison, R. A. and Sprinkle, James. 1969. A new echinoderm from the Middle Cambrian of Utah (Abst.). Geological Society of America Abstracts with Programs, 1(5):69. 6. Robison, R. A. and Sprinkle, James. 1969. Ctenocystoidea: new class of primitive echinoderms. Science, 166(3912):1512-1514. 1970 -- Sprinkle, James. 1970. Morphology and Evolution of Blastozoan Echino- derms. Harvard University Department of Geological Sciences, unpublished Ph.D. Thesis, 433 p. (see #8 below) 1971 7. Sprinkle, James. 1971. Stratigraphic distribution of echinoderm plates in the Antelope Valley Limestone of Nevada and California. U.S. Geological Survey Professional Paper 750-D (Geological Survey Research 1971):D89-D98. 1973 8. Sprinkle, James. 1973. Morphology and Evolution of Blastozoan Echino- derms. Harvard University, Museum of Comparative Zoology Special Publication, 283 p. -
Distribution of the Middle Ordovician Copenhagen Formation and Its Trilobites in Nevada
Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Distribution of the Middle Ordovician Copenhagen Formation and its Trilobites in Nevada By REUBEN JAMES ROSS, JR., and FREDERICK C. SHAW GEOLOGICAL SURVEY PROFESSIONAL PAPER 749 Descriptions of Middle Ordovician trilobites belonging to 21 genera contribute to correlations between similar strata in Nevada) California) and 0 klahoma UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. lVIOR TON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 78-190301 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 70 cents (paper cover) Stock Number 2401-2109 CONTENTS Page Page Abstract ______________________________ -------------------------------------------------- 1 Descriptions of trilobites __________________________________________________ _ 14 Introduction ________________________________________________________________________ _ 1 Genus T1·iarth1·us Green, 1832 .... ------------------------------ 14 Previous investigations _____________________________________________ _ 1 Genus Carrickia Tripp, 1965 ____________________________________ _ 14 Acknowledgments-------------------------------------------------------· 1 Genus Hypodicranotus Whittington, 1952 _____________ _ 15 Geographic occurrences of the Copenhagen Genus Robergia Wiman, 1905·---------------------------------- -
Thesis-2002-F832d.Pdf
THE DEPOSITIONAL HISTORY OF THE SYCAMOREL~STONE By KAREN ELIZABETH FRANKLIN Bachelor ofScience Oklahoma State University Stillwater, Oklahoma 1997 Submitted to the faculty ofthe Graduate College of Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE August, 2002 THE DEPOSITIONAL HISTORY OF THE SYCAMORE LIMESTONE Thesis Approved: Thesis Adviser 11 ACKNOWLEDGEMENTS I sincerely thank my advisers for all their help and patience with this thesis. Dr. Al Shaieb provided me with confidence and an unending supply of information. Dr. Boardman and Dr. Cemen provided helpful information from their disciplines. I thank my parents for all their help as well. They supported my family and I both mentally and financially. I especially thank Mom and Dad for watching my sons when I just had to get to school to work. I cannot express how thankful I am to my husband for all his support while I was working on my thesis. Without him, this wouldn't be possible. He and my sons provided support and love when things didn't seem to be going right. Finally I would like to thank the professors in the Geology Department and my fellow students for suffering through my constant questions. Many of them provided ideas and answers that helped me continue on those days where it seemed impossible to do so. III TABLE OF CONTENTS Chapter Page I. INTRODUCTION 1 Purpose ofStudy 1 Location 1 Method ofStudy 3 Formation History 3 Previous Investigations 6 II. GEOLOGICAL SETTING 13 Regional Structure 13 Regional Stratigraphy 16 Sequence Stratigraphy 20 III. -
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. -
A Cambrian Meraspid Cluster: Evidence of Trilobite Egg Deposition in a Nest Site
PALAIOS, 2019, v. 34, 254–260 Research Article DOI: http://dx.doi.org/10.2110/palo.2018.102 A CAMBRIAN MERASPID CLUSTER: EVIDENCE OF TRILOBITE EGG DEPOSITION IN A NEST SITE 1 2 DAVID R. SCHWIMMER AND WILLIAM M. MONTANTE 1Department of Earth and Space Sciences, Columbus State University, Columbus, Georgia 31907-5645, USA 2Tellus Science Museum, 100 Tellus Drive, Cartersville, Georgia, 30120 USA email: [email protected] ABSTRACT: Recent evidence confirms that trilobites were oviparous; however, their subsequent embryonic development has not been determined. A ~ 6cm2 claystone specimen from the upper Cambrian (Paibian) Conasauga Formation in western Georgia contains a cluster of .100 meraspid trilobites, many complete with librigenae. The juvenile trilobites, identified as Aphelaspis sp., are mostly 1.5 to 2.0 mm total length and co-occur in multiple axial orientations on a single bedding plane. This observation, together with the attached free cheeks, indicates that the association is not a result of current sorting. The majority of juveniles with determinable thoracic segment counts are of meraspid degree 5, suggesting that they hatched penecontemporaneously following a single egg deposition event. Additionally, they are tightly assembled, with a few strays, suggesting that the larvae either remained on the egg deposition site or selectively reassembled as affiliative, feeding, or protective behavior. Gregarious behavior by trilobites (‘‘trilobite clusters’’) has been reported frequently, but previously encompassed only holaspid adults or mixed-age assemblages. This is the first report of juvenile trilobite clustering and one of the few reported clusters involving Cambrian trilobites. Numerous explanations for trilobite clustering behavior have been posited; here it is proposed that larval clustering follows egg deposition at a nest site, and that larval aggregation may be a homing response to their nest. -
Athenacrinus N. Gen. and Other Early Echinoderm Taxa Inform Crinoid
Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution Thomas Guensburg, James Sprinkle, Rich Mooi, Bertrand Lefebvre, Bruno David, Michel Roux, Kraig Derstler To cite this version: Thomas Guensburg, James Sprinkle, Rich Mooi, Bertrand Lefebvre, Bruno David, et al.. Athenacri- nus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution. Journal of Paleontology, Paleontological Society, 2020, 94 (2), pp.311-333. 10.1017/jpa.2019.87. hal-02405959 HAL Id: hal-02405959 https://hal.archives-ouvertes.fr/hal-02405959 Submitted on 13 Nov 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution| 4.0 International License Journal of Paleontology, 94(2), 2020, p. 311–333 Copyright © 2019, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2019.87 Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution Thomas E. -
Athenacrinus N. Gen. and Other Early Echinoderm Taxa Inform Crinoid Origin and Arm Evolution
Journal of Paleontology, 94(2), 2020, p. 311–333 Copyright © 2019, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2019.87 Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution Thomas E. Guensburg,1 James Sprinkle,2 Rich Mooi,3 Bertrand Lefebvre,4 Bruno David,5,6 Michel Roux,7 and Kraig Derstler8 1IRC, Field Museum, 1400 South Lake Shore Drive, Chicago, Illinois 60605, USA <tguensburg@fieldmuseum.org> 2Department of Geological Sciences, Jackson School of Geosciences, University of Texas, 1 University Station C1100, Austin, Texas 78712-0254, USA <[email protected]> 3Department of Invertebrate Zoology, California Academy of Sciences, 55 Music Concourse Drive, San Francisco, California 94118, USA <[email protected]> 4UMR 5276 LGLTPE, Université Claude Bernard, Lyon 1, France <[email protected]> 5Muséum National d’Histoire Naturelle, Paris, France <[email protected]> 6UMR CNRS 6282 Biogéosciences, Université de Bourgogne Franche-Comté, 21000 Dijon, France <[email protected]> 7Muséum National d’Histoire Naturelle, UMR7205 ISYEB MNHN-CNRS-UMPC-EPHE, Département Systématique et Évolution, CP 51, 57 Rue Cuvier, 75231 Paris Cedex 05, France <[email protected]> 8Department of Earth and Environmental Studies, University of New Orleans, 2000 Lake Shore Drive, New Orleans, Louisiana 70148, USA <[email protected]> Abstract.—Intermediate morphologies of a new fossil crinoid shed light on the pathway by which crinoids acquired their distinctive arms. -
Oklahoma Geological Survey Publications on Fossils Bulletins
Oklahoma Geological Survey Publications on Fossils Bulletins Bulletin Part 1. Geology of a portion of northeastern Oklahoma. Part 2. Paleontology of the 24 Chester group in Oklahoma, by L. C. Snider. 1915. Bulletin Fossiliferous boulders in the Ouachita "Caney" shale, and the age of the shale 45 containing them, by E. O. Ulrich. 1927 Bulletin Micropaleontology of the Wetumka, Wewoka, and Holdenville formations, by A. S. 53 Warthin, Jr. 1930. Bulletin Ostracoda of the Simpson Group of Oklahoma, by R. W. Harris. 1957. 75 Stratigraphy and paleontology of the Hunton Group in the Arbuckle Mountain region. Bulletin Part II, Haragan articulate brachiopods, by Thomas W. Amsden. Part III, Supplement 78 to the Henryhouse brachiopods, by Thomas W. Amsden. Part IV, New genera of brachiopods, by Arthur J. Boucot and Thomas W. Amsden. 1958. Bulletin Stratigraphy and paleontology of the Hunton Group in the Arbuckle Mountain region. 82 Part V, Bois d’Arc articulate brachiopods, by Thomas W. Amsden. 1958. Bulletin Stratigraphy and paleontology of the Hunton Group in the Arbuckle Mountain region. 84 Part VI, Stratigraphy, by Thomas W. Amsden. 1960. Bulletin Stratigraphy and paleontology of the Hunton group in the Arbuckle Mountain region. 85 Part VI, Stratigraphy, by Thomas W. Amsden. 1960. Bulletin Late Desmoinesian crinoid faunule from Oklahoma, by Harrell L. Strimple. 1961. 93 Early Devonian brachiopods of Oklahoma. Part I, Articulate brachiopods of the Frisco Formation (Devonian), by Thomas W. Amsden and W. P. S. Ventress. Part II, Bulletin Articulate brachiopods of the Sallisaw Formation (Devonian), by Thomas W. Amsden. 94 Part III, Supplement to the Haragan (Devonian) brachiopods, by Thomas W. -
Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R
University of Dayton eCommons Geology Faculty Publications Department of Geology 2015 Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R. Carlucci Midwestern State University Daniel Goldman University of Dayton, [email protected] Carlton E. Brett University of Cincinnati - Main Campus Stephen R. Westrop University of Oklahoma Stephen A. Leslie James Madison University Follow this and additional works at: https://ecommons.udayton.edu/geo_fac_pub Part of the Geology Commons, and the Stratigraphy Commons eCommons Citation Carlucci, Jesse R.; Goldman, Daniel; Brett, Carlton E.; Westrop, Stephen R.; and Leslie, Stephen A., "Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma" (2015). Geology Faculty Publications. 5. https://ecommons.udayton.edu/geo_fac_pub/5 This Article is brought to you for free and open access by the Department of Geology at eCommons. It has been accepted for inclusion in Geology Faculty Publications by an authorized administrator of eCommons. For more information, please contact [email protected], [email protected]. Stratigraphy, 12 (2) 12th International Symposium on the Ordovician System Katian GSSP and Carbonates of the Simpson and Arbuckle Groups in Oklahoma Jesse R. Carlucci1 Daniel Goldman2 Carlton E. Brett3 Stephen R. Westrop4 Stephen A. Leslie5 1Assistant Professor, Kimbell School of Geosciences, Midwestern State University, Wichita Falls TX, [email protected] 2Professor & Chair, Department of Geology, University of Dayton, Dayton OH, [email protected] 3Professor, Department of Geology, University of Cincinnati, Cincinnati OH, [email protected] 4Professor & Curator of Invertebrate Paleontology, University of Oklahoma, Sam Noble Oklahoma Museum of Natural History, Norman OK, [email protected] 5Professor & Department Head, Department of Geology and Environmental Science, James Madison University, Harrisonburg VA, [email protected] 144 Stratigraphy, 12 (2) TABLE OF CONTENTS & GPS COORDINATES pg. -
Echinoderms Newsletter
l The Echinoderms Newsletter No.8. February, 1977 Prepared in the Department of Invertebrate Zoology (Echinoderms), National Museum of Natural History, Smithsonian Institution, Washington D.C., 20560, U.S.A. With this issue we include the good news that the Third Echino- derms Conference is to be held in March, 19~. Those of you who are interested in participating are urged to complete and send to Frank Rowe the enclosed pre-registration form without delay. Regional Editors, we eagerly await your c~ntributions; please send us what you have, and we'll circulate it promptly. I think that for the first time ever we have produced two News- letters within the span of a year. This astounding feat would not have been possible at all without the monumental labors of Cynthia Gust who, becoming impatient with our well developed procrastination techniques, set to and typed virtually all of the Newsletter, duplicated it, addressed the envelopes, and did a million other things. We owe her a great vote of thanks. David L. Pawson Maureen E. Downey IThe Echinoderms Newsletter is not intended to be part of the ~~~ntific literature, and should not be cited, abstracted, or reprinted as. published document. HELP ~! - ADDRESSES UNKNOWN If you happen t~ know the addresses of any of the following people, please let us know. Thank you. J. Campbell Landenberger Judith Eastwood Paul Leviten Finn Edvardsen Karl Mauzey Losza Endelman R.G. McKellar Carol Mosher Fernandez B.F. Mcrherson Olga Grageda Richard Merrill Spencer Hamada A. T. Mu J.R. Harger P.R. Noble Ira Jones B.S. -
Chickasaw National Recreation Area Paleontological Resources Inventory (Public Version)
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Chickasaw National Recreation Area Paleontological Resources Inventory (Public Version) Natural Resource Report NPS/CHIC/NRR—2016/1276 ON THE COVER Echinoderm stalk and columnals collected from the Welling Formation at the “Veterans Lake” echinoderm locality. Photo taken by Roger Burkhalter at the Sam Noble Oklahoma Museum of Natural History at 2X magnification. Chickasaw National Recreation Area Paleontological Resources Inventory (Public Version) Natural Resource Report NPS/CHIC/NRR—2016/1276 Alysia S. Korn National Park Service Geoscientists-in-the-Parks Program Chickasaw National Recreation Area [email protected] Madison L. Armstrong National Park Service Geoscientists-in-the-Parks Program Chickasaw National Recreation Area [email protected] Vincent L. Santucci National Park Service Geologic Resources Division 1201 Eye Street, NW (Room 1146) Washington, D.C. 20005 [email protected] Justin Tweet Tweet Paleo-Consulting 9149 79th St. S. Cottage Grove, Minnesota 55016 [email protected] August 2016 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. The Natural Resource Report Series is used to disseminate comprehensive information and analysis about natural resources and related topics concerning lands managed by the National Park Service. -
Horseshoe Crab Trace Fossils from the Upper Cretaceous Two Medicine Formation of Montana, USA, and a Brief Review of the Xiphosurid Ichnological Record
Journal of Paleontology, 94(5), 2020, p. 887–905 Copyright © The Author(s), 2020. Published by Cambridge University Press on behalf of The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2020.16 Horseshoe crab trace fossils from the Upper Cretaceous Two Medicine Formation of Montana, USA, and a brief review of the xiphosurid ichnological record Masateru Shibata1 and David J. Varricchio2* 1Institute of Dinosaur Research, Fukui Prefectural University, Fukui, Japan <[email protected]> 2Earth Sciences, Montana State University, Bozeman, MT 59717, USA <[email protected]> Abstract.—A locality in the Upper Cretaceous Two Medicine Formation of Montana preserves abundant and variable horseshoe crab tracks and trails of the ichnotaxon Kouphichnium isp. These specimens span six morphologies differing in track form and trail configuration. These differences likely reflect variations in track-maker locomotion and behavior, substrate consistency, epichnial versus hypichnial preservation, and undertrack versus true tracks. Several tracks preserve the first clear appendage impressions for an extinct horseshoe crab. This discovery adds new information to the fossil horseshoe crab diversity in the Cretaceous Period. Trackway dimensions, such as the external width across the pusher legs or of the prosomal drag mark, provide information on the track-maker size. Most trackways correspond with crabs 9–14 cm wide; the abundance but limited size range of the traces suggests the large assemblage corresponds to a mating aggregation.