Full Text -.: Palaeontologia Polonica
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
THE POWER of OUR IDEAS GEOLOGICAL SURVEY of CANADA L\1EMOIR 430
THE POWER OF OUR IDEAS GEOLOGICAL SURVEY OF CANADA l\1EMOIR 430 SUBSURFACE GEOLOGY OF PRE-MESOZOIC STRATA, GREAT BEAR RIVER MAP AREA, DISTRICT OF MACKENZIE D.C. Pugh 1993 'f' Minister of Supply and Services Canada 1993 Avai lable in Canada through authorized bookstore agcnts and other bookstores or by mail from Canada Communication Group - Publishing Ottawa. Canada KI A OS9 and from Geological Survey of Canada otTiccs: 60 I Booth Street Ottawa. Canada KI A OE8 3303-33rd Street N.W .. Calgary. Alberta T2L :lA7 A deposit copy of this publication is also <wailahk for n:J'crcnce in public libraries across Canada Cat. No. M46-430E ISBN 0-660-14271\-3 Price suhject to change without notice Critical readers J.D. Ailken D./I", Morro\!' D.G. Cook 8.S XOIford N.J. :\lcillillan Scientific editor l\',C OllerenshalV Editor Jo MacGillivray Typesetting and layout Institute o/SedimelJ/Gly and Petroleum Geology Cartography unit Instilute o/Sedimentary and Petroleum Geology Author's address ]()7. 92./ - 7th Ave. SW Calgary. Alberta T2P IA./ Original manuscript received: 85-(}6- 1./ Final version approved/or publication: 87-()8-U PREFACE Over the last forty years much has been published on the sedimentary geology of Great Bear River area. The discoveries of oil in the Devonian reef at Norman Wells and in Cambrian sands at Tedji Lake have attested to the area's hydrocarbon potential. Surface mapping and local studies have revealed rock sequences and crustal structures of great potential value to our understanding of global geology. The aim of this report is to assist evaluation of the economic potential and to improve the interpretation of the geological history. -
Corals (Anthozoa, Tabulata and Rugosa)
Bulletin de l’Institut Scientifique, Rabat, section Sciences de la Terre, 2008, n°30, 1-12. Corals (Anthozoa, Tabulata and Rugosa) and chaetetids (Porifera) from the Devonian of the Semara area (Morocco) at the Museo Geominero (Madrid, Spain), and their biogeographic significance Andreas MAY Saint Louis University - Madrid campus, Avenida del Valle 34, E-28003 Madrid, Spain e-mail: [email protected] Abstract. The paper describes the three tabulate coral species Caliapora robusta (Pradáčová, 1938), Pachyfavosites tumulosus Janet, 1965 and Thamnopora major (Radugin, 1938), the rugose coral Phillipsastrea ex gr. irregularis (Webster & Fenton in Fenton & Fenton, 1924) and the chaetetid Rhaphidopora crinalis (Schlüter, 1880). The specimens are described for the first time from Givetian and probably Frasnian strata of Semara area (Morocco, former Spanish Sahara). The material is stored in the Museo Geominero in Madrid. The tabulate corals and the chaetetid demonstrate close biogeographic relationships to Central and Eastern Europe as well as to Western Siberia. The fauna does not show any special influence of the Eastern Americas Realm. Key words: Anthozoa, biogeography, Devonian, tabulate corals, Morocco, West Sahara palaeogeographic province Coraux (Anthozoa, Tabulata et Rugosa) et chaetétides (Porifera) du Dévonien de la région de Smara (Maroc) déposés au Museo Geominero (Madrid) et leur signification biogéographique. Résumé. L´article décrit trois espèces de coraux tabulés : Caliapora robusta (Pradáčová, 1938), Pachyfavosites tumulosus Janet, 1965, et Thamnopora major (Radugin, 1938), le corail rugueux Phillipsastrea ex gr. irregularis (Webster & Fenton in Fenton & Fenton, 1924) ainsi que le chaetétide Rhaphidopora crinalis (Schlüter, 1880). Les spécimens, entreposés au Museo Geominero de Madrid, proviennent des couches givétiennes et probablement frasniennes de différents gisements de la région de Smara (Maroc, ancien Sahara espagnol), d’où elles sont décrites pour la première fois. -
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--.-------.- ___________________ -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
4. Arbeitstreffen Deutschsprachiger Echinodermenforscher Wien, Oktober 08
4. Arbeitstreffen deutschsprachiger Echinodermenforscher Wien, Oktober 08 4. Arbeitstreffen deutschsprachiger Echinodermenforscher, Wien, Okt. 08 4th Workshop of German & Austrian Echinoderm Research 4. Arbeitstreffen deutschsprachiger Echinodermenforscher 4th Workshop of German & Austrian Echinoderm Research 24.-26. October 2008 ABSTRACTS Andreas Kroh & Brigitta Schmid Naturhistorisches Museum Wien 4. Arbeitstreffen deutschsprachiger Echinodermenforscher 4th Workshop of German & Austrian Echinoderm Research Impressum Eigentümer, Herausgeber und Verleger: © 2008 Natuhistorisches Museum Wien Alle Rechte vorbehalten. Für den Inhalt der Beiträge sind die Autoren verantwortlich. Redaktion: Naturhistorisches Museum Wien Burgring 7, A-1010 Wien, Österreich (Austria) Tel.: +43 (1) 521 77 / 576 (Kroh); +43 (1) 521 77 / 564 (Schmid) Fax: +43 (1) 521 77 / 459 e-mail: [email protected] e-mail: [email protected] Redaktionelle Bearbeitung (EDV, Layout, Grafik): Andreas Kroh Umschlagentwurf: Andreas Kroh Titelbild: Coelopleurus (Keraiophorus) exquisitus COPPARD & SCHULTZ, 2006; Neukaledonien (NHMW 2005z0277/0016; Photo von Alice SCHUMACHER, NHM Wien). 24.-26. October 2008 iii 4. Arbeitstreffen deutschsprachiger Echinodermenforscher 4th Workshop of German & Austrian Echinoderm Research Inhalt Encrinus sp. cf. E. robustus (Crinoidea, Encrinidae) aus dem Unteren Muschelkalk von Niedersachsen (Poster) Ulrich Bielert, Friedrich Bielert & Hans Hagdorn...........................................1 Classification of pre- and postmortem -
Tabulate . Corals from Dalnia in the Ho19 Cross Mts
acta geologlca polonica Vol. 23, No. 1 War.zawa 1973 ANNA; STASmSKA Tabulate . corals from Dalnia in the Ho19 Cross Mts ABSTRACT: Four new species of tabulate corals have been described from the nep tunian dy~es on Dalnia Hill (Wooklumeria or Gattendorfia Stage) in the Holy Cross Mts. These species, viz. Emmornsia dalniae sp. n.~ Michelinopora sZt.Uczewskii sp. n., Acaciapora infracarbonica sp. n. and Kueichowpora polonicasp. n. are indicative of Lower Carboniferous age of the deposits they are contained in. INTRODUCTION The present paper includes the resulb; Of studies on tabulate corals from a new faunal locality at Dalnia near Kie:lce' in the Holy Cross M ts (cf. Szulczewskii 1973). Among the anthozoans founld at Da,lnia (cf. SzulczeWSki 1973, Fedo !rowski ·1973), the tabuLate corais represent a not very numerous group. They 'beloog to the g.enera Ernnnonsia, Michelinopora, Acaciapora and Kueichowpora, each of them !being r~esen'ted !by one new species. These species 'are most ,clloseily related 'to Carrboni:fieEdus or PeTmian forms, in particula!r to ' the species descrilbed rrdm the Lower CaJribondlferous. It should !be, t1hereiore, assumed that the age of the deposits they occur in on the Dalnia Hill isa!lso Lower CaII'lboniferous. As folldWs from studies on · conodonts (Szulczewski 1973), the entire stratigraphic range of the Dalnia deposits represents WocklumelI"ia through Gattendorma stage. The investigateld talbularte corals !from D8!1nia 'are marked !by very small dimensions of colonies which, as recognized iby SzUllczewSki ,(1973), may .indiCate unfavornble environmental! conditiOiIlS for lOCal 'anthozoan communities. Acknowledgements. The Wl'iter feels indebted to Docent M. -
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. -
Corals of Falls of the Ohio State Park
The Rugose Corals Tabulate Corals A Devonian coral garden Tabulae Rugose corals get their name because the exterior of Tabulate corals are always colonial. There are 212 species of corals many of their forms has a wrinkly appearance. They are Their name is derived from a flat shelf known from the fossil beds at the often called “horn corals” because their form may resemble (tabula) that separates individuals Falls of the Ohio. Not all occur in CORALS the horn of a cow or goat. In fact, the largest horn coral vertically in the colony (figure 6). The the coral beds; some may be found (Siphonophrentis elongata, figure 1) was referred to as a individual corallites that make up the in the slightly higher (younger) at “petrified buffalo horn” by colony are typically 0.5 - 8 mm wide. rock layers. Additional studies may Figure 11. Underside Falls of the Ohio settlers due to its shape. Figure 6. Despite the small individuals, these reveal more or fewer species. It takes of Alveolites coral Horn corals show a wide corals can be quite large. The most experience to identify corals with State Park variation in form, although common coral is a form called Favosites (Emmonsia). accuracy. The random orientation of many of the solitary external form is not a Emmonsia was given its own genus name, but some rugose corals make identification even more difficult. Alan Goldstein, Interpretive Naturalist distinguishing feature for specialists consider it to be a sub-genus of Favosites. These Look for evidence of Devonian hurricanes. Can you find identification. -
Heliophyllum a Study in Survival
Heliophyllum A Study in Survival Buffalo Geological Society Education Committee Bulletin – December 2019 ACKNOWLEDGEMENTS The Buffalo Geological Society thanks the members of our Education committee for their time and effort in producing what we hope to be the first of many informational bulletins on various facets of our hobby. Committee chairman Walter Drabek coordinated the project with the able assistance of several club members. Photography and photographic design were provided by Paul Leuchner whose nature photography is widely acclaimed in Western New York. Long time club member and amateur paleontologist Joseph Sullivan was responsible for technical review, enlisting the expertise of Dan Krisher of the Rochester Academy of Science and ensuring factual integrity. Mr. Krisher is a local coral expert who has worked with numerous organizations to produce fossil related publications and other educational events. Mark Castner of Canisius College provided editing and readability review as well as technical production support. Thin sections and acetate peels where produced at the Buffalo Museum of Science by Joseph Butch currently on the faculty at Buffalo State College and photographed by Michael Grenier of the Rochester Academy of Science. Specimens appearing in this pamphlet, that are not otherwise designated, are from the collections of various Club members. Finally, the Officers and Board need to be acknowledged for their support and critiquing of the final version. We dedicate this inaugural work to Bruce and Ruth Banick, Life Members of our organization and avid fossil collectors. The generous and ongoing commitment of their time and knowledge to our organization along with their extensive field work and the exhibition of their collections at numerous club events over the course of many years has inspired countless members to “keep on digging” and learning along the way. -
Corals from Well Cores of Madison Group, Williston Basin I + by WILLIAM J
Corals From Well Cores of Madison Group, Williston Basin i + By WILLIAM J. SANDO CONTRIBUTIONS TO GENERAL GEOLOGY ^GEOLOGICAL SURVEY BULLETIN 1071-F A description of ILarly Mississippian corals from three wells in northeastern Montana with special reference to their value as fades and time indicators UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. - Price $1 (paper cover) CONTENTS Page Abstract________________________________________________________ 157 Introduction._____________________________________________________ 157 Stratigraphic summary.____________________________________________ 158 Biologic analysis......_____________________________________________ 160 Coral distribution in the Madison group__-__-_--_---_______-_--_-._-_ 161 Stratigraphic value of corals of Madison group ________________________ 164 Systematic descriptions..___________________________________________ 165 Nondissepimented solitary corals. ___-- _-_--__--_________________ 166 Dissepimented solitary corals.______________--_--_-_----_-_--_-_ 174 Colonial corals___-_____----_-_-_-__-___---_--_---__---_-_-_--- 181 Register of collections..-___-_____-____-___-_____._________---_-_-_- 185 Literature cited.__----_-_---_-_---___---------_----_-_-__------__- 186 Index.___.____._______..___._____.._________....___.._.__.___._._ 189 ILLUSTRATIONS [Plates 16-20 follow index] PLATE 13. Stratigraphic ranges of coral genera in the Madison group. In pocket 14. Frequency distribution of specimens of coral genera in forma tions of the Madison group.________________________ In pocket 15. Frequency distribution of coral types in formations of the Madison group. __________________________________ In pocket 16. -
Tabulata from the Givetian of the South-Eastern Poland
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. 21 1976 No 3 ANNA STASINSKA & ALEKSANDER NOWINSKI TABULATA FROM THE GIVETIAN OF THE SOUTH-EASTERN POLAND Abstract. - The characteristics of a Tabulata assemblage from the Devonian of the Lublin area are given; the coral-bearing strata are correlated with the Givetian of other parts of Poland as well as west and east European regions. INTRODUCTION The Devonin of the Lublin area has been investigated by the Geological Institute of Poland and the petroleum industry since the sixties. Strati graphic, petrographic and palaeontological analyses of the core material (see Pajchlowa, 1968, 1975) have shown that the section of the Devonian is complete in the Radom-Lublin area, ranging from the Silurian-Devonian junction beds to the Upper Famennian, the Gedinnian and the Lower Siegenian strata, developed in marine facies, yield innumerous fragments of Coelenterata. The Upper Siegenian and the Emsian are developed in the Old Red facies and the Middle and Upper Devonian - in the carbonate facies. Coelenterata are known from the lowermost Eifelian, Givetian and Frasnian. Tabulata are most common in the Givetian. The collection of Devonian Tabulata from the core material from the Lublin area was made available to the authors through the courtesy of Dr. L. Milaczewski and Dr. A. Zelichowski of the Geological Institute of Poland; the material from the Holy Cross Mts - through the courtesy of Dr. T. Wroblewski of the Kielce Branch of the Geological Institute. Thanks are due to Mrs. M. Nowiilska and Mr. Z. Strqk who prepared thin sections, and to Miss E. -
LOWER PENINSULA Veritable Remains of Once Living Organisms
GEOLOGICAL SURVEY OF MICHIGAN. During the fourteenth century the hypothesis of the origin of fossils by lusus naturæ began to lose credit, and it became generally recognized that they were the LOWER PENINSULA veritable remains of once living organisms. This being 1873-1876 acknowledged, the thought of ascribing the origin of ACCOMPANIED BY A fossils to the scriptural deluge recommended itself as GEOLOGICAL MAP. plausible, and they were at once, without critical examination of the correctness of this view, universally believed to be the remains of the animals which perished VOL. III. during this catastrophe, which belief was obstinately held PART II. PALÆONTOLOGY—CORALS. up to the end of the eighteenth century. At that time, with the progress made in natural history, so many facts BY contradicting this theory had accumulated, that it could C. ROMINGER no longer be held. It was clearly recognized that the STATE GEOLOGIST deluge could not account for fossils generally; that there existed an immense difference in the age of fossils, and that a large number of animal and vegetable creations PUBLISHED BY AUTHORITY OF THE LEGISLATURE OF MICHIGAN. came and disappeared again, in long-continued UNDER THE DIRECTION OF THE succession, involving the lapse of spaces of time far BOARD OF GEOLOGICAL SURVEY. exceeding former conceptions of the age of the globe. The study of the fossils and of the conditions under NEW YORK which they were found threw an entirely new light on the JULIUS BIEN earth's history. Formerly the fossils were mere objects 1876 of curiosity; now they became important witnesses to a Entered according to Act of Congress, in the year 1876, by long series of progressive changes which the earth must GOVERNOR J.