Chickasaw National Recreation Area Geologic Resources Inventory Report
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Carboniferous Formations and Faunas of Central Montana
Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________ -
Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction by MACKENZIE GORDON, JR
Revision of Some of Girty's Invertebrate Fossils from the Fayetteville Shale (Mississippian) of Arkansas and Oklahoma Introduction By MACKENZIE GORDON, JR. Corals By WILLIAM J. SANDO Pelecypods By JOHN POJETA, JR. Gastropods By ELLIS L. YOCHELSON Trilobites By MACKENZIE GORDON, JR. Ostracodes By I. G. SOHN GEOLOGICAL SURVEY PROFESSIONAL PAPER 606-A, B, C, D, E, F Papers illustrating and describing certain of G. H. Girty' s invertebrate fossils from the Fayetteville Shale UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1969 UNITED STATES DEPARTMENT OF THE INTERIOR WALTER J. HICKEL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 70-650224 For sale by the Superintendent of Documents, U.S. Government Printing Office Washing.ton, D.C. 20402 CONTENTS [The letters in parentheses preceding the titles are those used to designate the chapters] Page (A) Introduction, by Mackenzie Gordon, Jr _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 1 (B) Corals, by William J. Sando__________________________________________________________________________________ 9 (C) Pelecypods, by John Pojeta, Jr _____ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 15 (D) Gastropods, by Ellis L. -
02 Inside Front Cover
156 JAMES HALL’S (1856) ROSTROCONCHS? VOL. 106 James Hall’s (1856) Rostroconchs from the Mississippian of Indiana and Illinois1 RICHARD D. HOARE, Department of Geology, Bowling Green State University, Bowling Green, OH 43403 ABSTRACT. Hall (1856) described without illustrations six species of the rostroconch Conocardium in his study of the fauna of the Salem Limestone in Indiana and the Warsaw Shale in Illinois. The species represent five genera, two of which are new, Leptoconocardium and Kyoconocardium. Other species represent the genera Hippocardia Brown, 1843; Oxyprora Hoare, Mapes, and Yancey, 2002; and Diedrorynchus Hoare and Peck, 2005. OHIO J SCI 106 (4):156-163, 2006 INTRODUCTION have reduced the outer shell layer so that fine orna- In a continuing study of Upper Paleozoic rostro- mentation is often obliterated or poorly preserved. The conchs it was thought useful to locate and examine the ornamentation may not show up when the specimens Mississippian (Meremecian) specimens described by Hall are coated for photography, but is visible when un- (1856) from the Salem Limestone in Indiana and the coated or when slightly wet. Many of the fossils in the Warsaw Shale in Illinois. This study would compliment Salem Limestone are coated with a banded, oolitic-like those made from the Mississippian in Ohio (Hyde 1953; coating which may hide the ornamentation. Remnants of Hoare 1990, 2004) and West Virginia (Hoare and Peck the larval shell are present on some specimens. 2005). The purposes of this study are: 1) to redescribe All of the specimens are small, ranging in length from and photographically illustrate Hall’s specimens; 2) to 2.3 mm to 12.0 mm. -
Wissenschaftliche Originale in Den Sammlungen BGR/LBEG, Hannover Und BGR, Berlin
Wissenschaftliche Originale in den Sammlungen BGR/LBEG, Hannover und BGR, Berlin Schriftenverzeichnis V. DANIELS, C.H., HEINKE, A., HEUNISCH, C., LINDERT, W. & WIESE, T. Papierversion: 93 Seiten; Archiv-Nr. BGR/LBEG 0117040 Berichtsdatum: 03. 03. 1998 Diese Version wurde aktualisiert am: 06. 01. 2020 durch T. Wiese Wissenschaftliche Originale in den Sammlungen BGR/LBEG, Hannover und BGR, Berlin Schriftenverzeichnis V. DANIELS, C. H., HEINKE, A., HEUNISCH, C., LINDERT, W. & WIESE, T. „Unter Original wird im folgenden jedes Stück verstanden, das in der Literatur abgebildet ist.“ (P. DIENST 1928) Wissenschaftliche Originale gehören zu den wertvollsten Stücken jeder Sammlung. Ein erheblicher Anteil der Nutzeranfragen gilt ihnen. Die Orginale-Sammlungen der Bundesanstalt für Geowissenschaften und Rohstoffe (BGR) in Hannover und Berlin sowie des Landesamtes für Bergbau, Energie und Geologie (LBEG), Hannover, sind zwar zum heutigen Zeitpunkt weitestgehend erfaßt - davon auch große Teile DV- mäßig - und damit gut recherchierbar, es fehlte jedoch bisher eine aktuelle Literaturübersicht für die interessierte Fachwelt. Mit dem vorliegenden Schriftenverzeichnis wird diese Lücke geschlossen. Die Originale-Sammlungen in Hannover und Berlin sind nicht nur räumlich getrennt, auch ihr historischer Hintergrund, ihre Quellen und die Art der Katalogisierung sind verschieden. Geschichtliches Im Jahr 1873 wurde in Berlin die Königlich-Preußische Geologische Landesanstalt gegründet, die 1939 in der Reichsstelle für Bodenforschung (ab 1941 Reichsamt für Bodenforschung) aufging. Nach Gründung der Bundesrepublik Deutschland wurden die Bundesaufgaben zunächst dem Amt für Bodenforschung in Hannover übertragen. 1958 wurde die Bundesanstalt für Bodenforschung (ab 1975 Bundesanstalt für Geowissenschaften und Rohstoffe, BGR) aus dem Bestand des Amtes für Bodenforschung errichtet. Die BGR arbeitet auf der Grundlage eines Verwaltungsabkommens eng mit dem Landesamtes für Bergbau, Energie und Geologie (LBEG) zusammen. -
Paleontological Resource Inventory at Chickasaw National Recreation Area, Oklahoma
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 5 PALEONTOLOGICAL RESOURCE INVENTORY AT CHICKASAW NATIONAL RECREATION AREA, OKLAHOMA MADISON L. ARMSTRONG1, ALYSIA S. KORN2, VINCENT L. SANTUCCI3 and JUSTIN TWEET4 1NPS Geoscientists-in-the-Parks, 413 Cottonwood St., Ardmore, OK 73401 -email: [email protected]; 2NPS Geoscientists-in-the-Parks, 411 Magee Ave., Philadelphia, PA 19111; -email: [email protected] 3National Park Service, 1201 Eye St., NW, Washington, D.C. 20005; -email: [email protected]; 4Tweet Paleo-Consulting, 9149 79th St. S., Cottage Grove, MN 55016; -email: [email protected] Abstract—Chickasaw National Recreation Area (CHIC), located in south-central Oklahoma east of the Arbuckle Mountains, is best known for its wildlife and water recreation. Few visitors are aware of the important paleontological resources that occur in the park. During the summer of 2016, a comprehensive field inventory of paleontological resources within CHIC was conducted. The inventory process involved primary literature research, an extensive field survey of fossiliferous units, and inventories of collections and repositories. The field survey yielded eight new fossiliferous localities, and eight previously undocumented taxa within CHIC. This is the first discovery of fossils in the Deese Group and Sycamore Limestone within the recreation area. During the 2016 inventory, fossils were documented at all previously known localities within CHIC, except for those localities now submerged under the Lake of the Arbuckles. Collections were made of the representative fauna found within CHIC, and 73 fossil specimens were accessioned into museum collections. -
1970 Conocardium Langenheimi SP. N. (MOLLUSCA: BIVALVIA) 13 14 CONTRIBUTIONS in SCIENCE No
1970 Conocardium langenheimi SP. N. (MOLLUSCA: BIVALVIA) 13 14 CONTRIBUTIONS IN SCIENCE No. 184 function such as brood chambers to the tubes in the dorsal parts of the valves, but, again, close analogies in living bivalves seem absent. Some of the grooves in the shell suggest ciliated tracts, but there is no certainty about this. CONCLUSIONS C. langenheimi is a member of the Conocardidoida, which is externally like the Bivalvia, has a world wide distribution, and ranges from Ordovician through Permian (Triassic?) rocks. The degree of complexity shown by the shell microstructure definitely appears to be molluscan. The paired valves sug- gest that the Order belongs in the Class Bivalvia, however the internal mor- phology and shell microstructure is unlike others in that class. If typical of the order, these suggest need for a reconsideration of the systematic position at the class or higher level. LITERATURE CITED BRANSON, C. C., A. LAROCQUE, AND N. D. NEWELL. 1969. Order Conocardioida, in Treatise on invertebrate paleontology, R. C. MOORE, ed., Bivalvia: Part N. Geol. Soc. America and Univ. Kans. Press, Lawrence, Kansas. 2:491-951, figures. DECHASEAUX, COLETTE. 1952. Etude systematique, in Traite de Paleontologie, J. PIVETEAU, ed. Masson et Cie., Paris. 2:261-364, figs. 35-215. HIND, W. 1900. A monograph of the British Carboniferous Lambellibranchiata, part V. Paleont. Soc., London. 361-476, pis. 40-54. LINNAEUS, CAROLUS. 1758. Systema naturae. Editio decima. Laurentii Salvii, Stock- holm. 1-824. MILLER, S. A. 1889. North American geology and palaeontology for the use of amateurs, students, and scientists. Western Methodist Book Concern, Cincinnati. -
The Yellowstone Paleontological Survey
E PALEONT ON O T LO S G W I O C L A L L E National Y Park The Yellowstone Service Department of the Interior Paleontological Survey SURVEY Vincent L. Santucci Yellowstone Center for Resources National Park Service Yellowstone National Park, Wyoming YCR-NR-98-1 1998 How to cite this document: Santucci, V. L. 1998. The Yellowstone Paleontological Survey. Yellowstone Center for Resources, National Park Service, Yellowstone National Park, Wyoming,YCR-NR-98-1. Current address for Vincent L. Santucci is National Park Service, P.O. Box 592, Kemmerer, WY 83101. The Yellowstone Paleontological Survey To Lt. Col. Luke J. Barnett, III “Uncle by blood, brother in spirit!” Vincent L. Santucci Yellowstone Center for Resources National Park Service Yellowstone National Park, Wyoming YCR-NR-98-1 1998 Table of Contents Introduction .................................................................................................... 1 Stratigraphy .................................................................................................... 4 Fossil Chronology........................................................................................... 6 Taxonomy ..................................................................................................... 12 Localities ...................................................................................................... 15 Interpretation ................................................................................................ 19 Paleontological Resource Management....................................................... -
Mollusksmollusks the Paleontological Society Http:\\Paleosoc.Org
MollusksMollusks The Paleontological Society http:\\paleosoc.org Mollusks The concept Mollusca brings together a great deal of cept Mollusca is unified by anatomical similarities, by information about animals that at first glance appear to be embryological similarities, and by evidence from fossils radically different from one another—snails, slugs, of the evolutionary history of the species placed within mussels, clams, oysters, octopuses, squids, and others. the phylum; all this information indicates a common The diversity of the phylum is shown by at least eight ancestry for the groups placed in the phylum. known classes (cover). Estimates of the number of species alive today range from 50,000 to 130,000. Most Most mollusks are free-living multicellular animals that of the shells found on the beaches of the modem world have a multilayered calcareous shell or conch on their belong to mollusks and mollusks are probably the most backs. This exoskeleton provides support for the soft abundant invertebrate animals in modern oceans. organs including a muscular foot and the organs of digestion, respiration, excretion, reproduction, and others. Living mollusks range in size from microscopic snails Around all of the soft parts is a space called the mantle and clams to almost 60 foot long (18 meters) squids. cavity, which is open to the outside. The mantle cavity is They live in most marine and freshwater environments, a passageway for incoming feeding and respiratory and some snails and slugs live on land. In the sea, mol- currents, and an exit for the discharge of wastes. The lusks range from the intertidal zone to the deepest ocean outer wall of the mantle cavity is a thin flap of tissue basins and they may be bottom-dwelling, swimming, or called the mantle, which secretes the shell. -
Arbuckle Project
Arbuckle Project Christopher J. McCune Historic Reclamation Projects Bureau of Reclamation 2002 Table of Contents Table of Contents..............................................................1 The Arbuckle Project...........................................................2 Project Location.........................................................2 Historic Setting .........................................................3 Project Authorization.....................................................5 Construction History .....................................................8 Post-Construction History................................................15 Settlement of the Project .................................................19 Uses of Project Water ...................................................20 Conclusion............................................................21 About the Author .............................................................21 Bibliography ................................................................22 Archival Collections ....................................................22 Government Documents .................................................22 Articles...............................................................22 Internet...............................................................22 Other ................................................................22 Index ......................................................................23 1 The Arbuckle Project In 1962, President John F. Kennedy, authorized -
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. -
Geologic Map of Chickasaw National Recreation Area, Murray County, Oklahoma
Prepared in cooperation with the National Park Service Geologic Map of Chickasaw National Recreation Area, Murray County, Oklahoma Pamphlet to accompany Scientific Investigations Map 3258 U.S. Department of the Interior U.S. Geological Survey 1 2 3 4 Cover photographs: 1 Massive sandstone, Vanoss Formation (*vs), see fig. 5. 2 Old abandoned quarry exposing Hunton Group (DSOh) and crest of Tishomingo anticline in southeastern part of map area (looking east-southest), see map sheet. 3 Lower Hunton Group (SOhl, Cochrane Formation), see fig. 4. 4 Woodford Shale (MDsw), see fig. 5. Geologic Map of Chickasaw National Recreation Area, Murray County, Oklahoma By Charles D. Blome, David J. Lidke, Ronald R. Wahl, and James A. Golab Prepared in cooperation with the National Park Service Pamphlet to accompany Scientific Investigations Map 3258 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2013 Revised May 8, 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. -
Title Permian Bivalves of Japan Author(S) Nakazawa, Keiji; Newell
Title Permian Bivalves of Japan Author(s) Nakazawa, Keiji; Newell, D. Norman Memoirs of the Faculty of Science, Kyoto University. Series of Citation geology and mineralogy (1968), 35(1): 1-108 Issue Date 1968-10-11 URL http://hdl.handle.net/2433/186552 Right Type Departmental Bulletin Paper Textversion publisher Kyoto University MEMOIRs oF THE FAcuLTy oF SclENcE, KyOTo UNIvERslTY, SERIEs oF GEoL. MINERAL.& Vol. XXXV, No. 1, pp. 1-108, Pls. 1-11 Permian Bivalves of Japan By Keiji NAKAzAwA and Norman D. NEwELL* (Received Aprii 28, 1968) Abstract Permian bivalve molluscs ofJapan shed interesting new light on the paleontological com- position of the youngest, post-fusulinid, marine faunas of the highest Paleozoic, and the bivalves tend to bridge the gap between the uppermost Permian and the lowest Triassic occupied in most regions ofthe world by a hiatus. However, there is a noteworthy break, even inJapan, between the Permian and Triassic ,systems where there are no bivalve species in common between the Permian and Triassic. Ninety-six species belonging to 46 genera of bivalves are distinguished in theJapanese Perrnian. Among these, 58 species, ofwhich 18 are new, are described in this paper. TowaPteria, Ensi teria, Tambanelta, HayasakaPecten, and Gnjocardita are proposed herein as new genera, and PermoPerna is presented as a new subgenus of Waagenoperna. It is worthy of note that the bivalves did not decrease in number and diversity during the late Permian, in contrast to some other invertebrates, and that the late Permian Gujo Formation con- tains a mixed fauna of Permian and Triassic aspect. Some Mesozoic types, such as Neoschizodus, Costatoria and WaagemoPerna, appeared in the middle Permian Kanokura Series.