First Major Appearance of Brachiopod-Dominated Benthic Shelly Communities in the Reef Ecosystem During the Early Silurian Cale A.C

Total Page:16

File Type:pdf, Size:1020Kb

First Major Appearance of Brachiopod-Dominated Benthic Shelly Communities in the Reef Ecosystem During the Early Silurian Cale A.C Western University Scholarship@Western Electronic Thesis and Dissertation Repository August 2016 First Major Appearance of Brachiopod-Dominated Benthic Shelly Communities in the Reef Ecosystem during the Early Silurian Cale A.C. Gushulak The University of Western Ontario Supervisor Dr. Jisuo Jin The University of Western Ontario Joint Supervisor Dr. Rong-yu Li The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the requirements for the degree in Master of Science © Cale A.C. Gushulak 2016 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Evolution Commons, Other Ecology and Evolutionary Biology Commons, Paleobiology Commons, and the Paleontology Commons Recommended Citation Gushulak, Cale A.C., "First Major Appearance of Brachiopod-Dominated Benthic Shelly Communities in the Reef Ecosystem during the Early Silurian" (2016). Electronic Thesis and Dissertation Repository. 3972. https://ir.lib.uwo.ca/etd/3972 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected], [email protected]. Abstract The early Silurian reefs of the Attawapiskat Formation in the Hudson Bay Basin preserved the oldest record of major invasion of the coral-stromatoporoid skeletal reefs by brachiopods and other marine shelly benthos, providing an excellent opportunity for studying the early evolution, functional morphology, and community organization of the rich and diverse reef-dwelling brachiopods. Biometric and multivariate analysis demonstrate that the reef-dwelling Pentameroides septentrionalis evolved from the level- bottom-dwelling Pentameroides subrectus to develop a larger and more globular shell. The reef-dwelling brachiopods in the paleoequatorial Hudson Bay Basin were more diverse than contemporaneous higher latitude reef-dwelling brachiopod faunas, with ten distinct community associations recognized in the Attawapiskat Formation. The absence or paucity of hurricane-grade storms in the paleoequatorial Hudson Bay Basin is interpreted as a major factor in the evolutionary success of the reef-dwelling brachiopods in the Attawapiskat Formation. Keywords Reef-dwelling brachiopods, early Silurian, paleoecology, evolution, Laurentia Co-Authorship Statement A more succinct version of Chapter 3 “The Paleolatiudinal morpho-gradient of Pentameroides in Telychian Laurentia” has been published by Gushulak, C.A.C., Jin, J., and Rudkin, D.M. in the Canadian Journal of Earth Sciences under the title “Paleolatitudinal morpho-gradient of the early Silurian brachiopod Pentameroides in Laurentia.” J. Jin provided assistance with the interpretation of results and editing of the manuscript while D.M. Rudkin provided additional information on the geology of the Attawapiskat Formation and editing the manuscript. ii Acknowledgments I would not have been able to finish this thesis without the support and encouragement from many people. First, I would like to thank my supervisors Dr. Jisuo Jin and Dr. Rong-yu Li. Dr. Jin’s advice and support over these last two years have been an immense help to me. Although not in London, I always appreciated Dr. Li’s support from Manitoba and friendly meetings when I was back home. I would like to thank Dr. Paul Copper for kindly making his fossil collections from Manitoulin and Anticosti islands freely available during this project. I also thank Mr. David Rudkin and Mr. Peter Fenton from the Royal Ontario Museum for their guidance and assistance in field work on Akimiski Island and the James Bay lowlands. Mr. Rudkin is thanked again for his input on Chapter 3 of this thesis and the subsequent publication. I also thank the territorial government of Nunavut for allowing access to Akimiski Island. Logistics and funding support for the Hudson Bay lowlands fieldwork were provided by the Ontario Ministry and Natural Resources and the Natural Sciences and Engineering Research Council of Canada. I would like to thank my lab-mates Nikole Bingham-Koslowski, Shuo Sun, and Colin Sproat. It has been great working with you over the past two years. Special thanks to Colin for dealing with my rants and explaining how cameras work. I thank the Western Taekwondo Club for accepting me into their family with open arms and being great friends during my time at Western. Apologies are given if I have kicked any of you too hard, graduate work can be stressful. iii Finally, I need to thank my family for their continuing and unwavering support of academic goals. Without your encouragement I would not have had the courage to move across the country and complete this degree. Research is impossible without funding. Funding for this project was provided by a University of Western Ontario entrance scholarship, teaching assistanceships in the Department of Earth Sciences, and a Western Graduate Research Sholarship from the Univeristy of Western Ontario; an Ontario Graduate Scholarship to Cale A.C. Gushulak from the Ontario provincial government; and an NSERC discovery grant to J. Jin. iv Table of Contents Abstract ............................................................................................................................... i Co-Authorship Statement ............................................................................................... ii Acknowledgments ........................................................................................................... iii Table of Contents ............................................................................................................. vi List of Tables .................................................................................................................... x List of Figures .................................................................................................................. xi List of Equations .......................................................................................................... xxii List of Appendices ......................................................................................................... xiii 1 Chapter 1 – Introduction ............................................................................................ 1 1.1 Introduction ............................................................................................................. 1 1.2 The Silurian World .................................................................................................. 3 1.2.1 Paleogeography and Tectonism ..................................................................... 3 1.2.2 Climate and Sea Level ................................................................................... 6 1.2.3 Ocean Circulation and Chemistry .................................................................. 9 1.2.4 Silurian Recovery Fauna .............................................................................. 10 1.3 Brachiopods and their Importance as Paleoecological Indicators.......................... 13 1.3.1 Pentameride Brachiopods in the Silurian ..................................................... 15 1.4 Silurian Level-Bottom Brachiopod Communities ................................................. 16 1.5 The Reef Environment ........................................................................................... 19 1.6 The Cause of Tropical Biodiversity ....................................................................... 21 1.7 Overall Objectives of Thesis Projects .................................................................... 22 1.8 Organization of the Thesis ..................................................................................... 23 References ................................................................................................................... 25 v 2 Chapter 2 – Geological Settings ............................................................................... 42 2.1 Tectonic Arrangement of Laurentia ....................................................................... 42 2.2 Coral-Stromatoporoid Reefs in the Llandovery ..................................................... 45 2.3 The Attawapiskat Formation, Hudson Platform .................................................... 48 2.3.1 Materials ...................................................................................................... 53 2.4 Anticosti Island ...................................................................................................... 56 2.4.1 Laframboise Member, Ellis Bay Formation ................................................ 57 2.4.2 East Point Member, Meniér Formation ....................................................... 59 2.4.3 Pavillon Member, Jupiter Formation ........................................................... 61 2.4.4 Chicotte Formation ...................................................................................... 63 2.5 Michigan Basin ...................................................................................................... 63 2.5.1 Fossil Hill Formation, Manitoulin Island..................................................... 64 2.5.2 Racine Formation, Wisconsin ...................................................................... 65 2.6 Högklint Formation, Gotland, Sweden (Baltica) ................................................... 66 2.7 Biostratigraphic correlations
Recommended publications
  • Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois
    2UJ?. *& "1 479 S 14.GS: CIR479 STATE OF ILLINOIS c. 1 DEPARTMENT OF REGISTRATION AND EDUCATION Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois H. B. Willman GEOLOGICAL ILLINOIS ""SURVEY * 10RM* APR 3H986 ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief Urbano, IL 61801 CIRCULAR 479 1973 CONTENTS Page Abstract 1 Introduction 1 Time-stratigraphic classification 3 Alexandrian Series 5 Niagaran Series 5 Cayugan Series 6 Regional correlations 6 Northeastern Illinois 6 Development of the classification 9 Wilhelmi Formation 12 Schweizer Member 13 Birds Member 13 Elwood Formation 14 Kankakee Formation 15 Drummond Member 17 Offerman Member 17 Troutman Member 18 Plaines Member 18 Joliet Formation 19 Brandon Bridge Member 20 Markgraf Member 21 Romeo Member 22 Sugar Run Formation . „ 22 Racine Formation 24 Northwestern Illinois 26 Development of the classification 29 Mosalem Formation 31 Tete des Morts Formation 33 Blanding Formation 35 Sweeney Formation 36 Marcus Formation 3 7 Racine Formation 39 References 40 GEOLOGIC SECTIONS Northeastern Illinois 45 Northwestern Illinois 52 FIGURES Figure 1 - Distribution of Silurian rocks in Illinois 2 2 - Classification of Silurian rocks in northeastern and northwestern Illinois 4 3 - Correlation of the Silurian formations in Illinois and adjacent states 7 - CM 4 Distribution of Silurian rocks in northeastern Illinois (modified from State Geologic Map) 8 - lis. 5 Silurian strata in northeastern Illinois 10 ^- 6 - Development of the classification of the Silurian System in |§ northeastern Illinois 11 7 - Distribution of Silurian rocks in northwestern Illinois (modified ;0 from State Geologic Map) 2 7 8 - Silurian strata in northwestern Illinois 28 o 9 - Development of the classification of the Silurian System in CO northwestern Illinois 30 10 - Index to stratigraphic units described in the geologic sections • • 46 ROCK STRATIGRAPHY OF THE SILURIAN SYSTEM IN NORTHEASTERN AND NORTHWESTERN ILLINOIS H.
    [Show full text]
  • Strophomenide and Orthotetide Silurian Brachiopods from the Baltic Region, with Particular Reference to Lithuanian Boreholes
    Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes PETRAS MUSTEIKIS and L. ROBIN M. COCKS Musteikis, P. and Cocks, L.R.M. 2004. Strophomenide and orthotetide Silurian brachiopods from the Baltic region, with particular reference to Lithuanian boreholes. Acta Palaeontologica Polonica 49 (3): 455–482. Epeiric seas covered the east and west parts of the old craton of Baltica in the Silurian and brachiopods formed a major part of the benthic macrofauna throughout Silurian times (Llandovery to Pridoli). The orders Strophomenida and Orthotetida are conspicuous components of the brachiopod fauna, and thus the genera and species of the superfamilies Plec− tambonitoidea, Strophomenoidea, and Chilidiopsoidea, which occur in the Silurian of Baltica are reviewed and reidentified in turn, and their individual distributions are assessed within the numerous boreholes of the East Baltic, particularly Lithua− nia, and attributed to benthic assemblages. The commonest plectambonitoids are Eoplectodonta(Eoplectodonta)(6spe− cies), Leangella (2 species), and Jonesea (2 species); rarer forms include Aegiria and Eoplectodonta (Ygerodiscus), for which the new species E. (Y.) bella is erected from the Lithuanian Wenlock. Eight strophomenoid families occur; the rare Leptaenoideidae only in Gotland (Leptaenoidea, Liljevallia). Strophomenidae are represented by Katastrophomena (4 spe− cies), and Pentlandina (2 species); Bellimurina (Cyphomenoidea) is only from Oslo and Gotland. Rafinesquinidae include widespread Leptaena (at least 11 species) and Lepidoleptaena (2 species) with Scamnomena and Crassitestella known only from Gotland and Oslo. In the Amphistrophiidae Amphistrophia is widespread, and Eoamphistrophia, Eocymostrophia, and Mesodouvillina are rare. In the Leptostrophiidae Mesoleptostrophia, Brachyprion,andProtomegastrophia are com− mon, but Eomegastrophia, Eostropheodonta, Erinostrophia,andPalaeoleptostrophia are only recorded from the west in the Baltica Silurian.
    [Show full text]
  • Hydrogeology of the Silurian Dolomite Aquifer in Parts of Northwestern Illinois
    W.SS; qj>^^^ Hydrogeology of the Silurian Dolomite Aquifer in Parts of Northwestern Illinois Timothy H. Larson • Anne M. Graese • Phillip G. Orozco 1993 ENVIRONMENTAL GEOLOGY 145 Department of Energy and Natural Resources ILLINOIS STATE GEOLOGICAL SURVEY a* ILLINOIS STATE GEOLOGICAL SURVEY 3 3051 00005 4670 Hydrogeology of the Silurian Dolomite Aquifer in Parts of Northwestern Illinois Timothy H. Larson • Anne M. Graese • Phillip G. Orozco 1993 ENVIRONMENTAL GEOLOGY 145 ILLINOIS STATE GEOLOGICAL SURVEY Morris W. Leighton, Chief - Natural Resources Building ^> ' v£* 615 East Peabody Drive ^ ^P Champaign, IL 61820-6964 nvV\>&\^ & Cover photo Reef in the Silurian Racine Formation at Morrison, Whiteside County, Illinois. Photo by Anne M. Graese. Printed by authority of the State of Illinois/1993/1000 ) printed on recycled paper 91 ABSTRACT 1 INTRODUCTION 1 METHODS 1 GEOLOGIC FRAMEWORK 2 Previous Studies 2 Stratigraphy 2 Mosalem Formation 2 Tete des Morts Formation 6 Blanding Formation 6 Sweeney Formation 6 Marcus Formation 6 Racine Formation 6 Weathering Character 6 HYDROGEOLOGIC FRAMEWORK 9 Previous Studies 9 Hydrostratigraphy 9 Midwest Bedrock Aquigroup 9 Upper Bedrock Aquigroup 9 Prairie Aquigroup 10 Aquifers and Aquitards in the Upper Bedrock Aquigroup 10 Ancell Aquifer 10 Galena-Platteville Unit 10 Maquoketa Confining Unit 10 Silurian Dolomite Aquifer 10 Hydrogeologic History of the Carbonate Aquifers 1 Aquifer Potential 13 Contamination Potential 15 SUMMARY 17 ACKNOWLEDGMENTS 17 REFERENCES 17 APPENDIX A: CORE ANALYSIS 1 Visual Examination
    [Show full text]
  • The Earliest Known Kinnella, an Orthide Brachiopod from the Upper Ordovician of Manitoulin Island, Ontario, Canada
    The earliest known Kinnella, an orthide brachiopod from the Upper Ordovician of Manitoulin Island, Ontario, Canada CHRISTOPHER A. STOTT and JISUO JIN Stott, C.A. and Jin, J. 2007. The earliest known Kinnella, an orthide brachiopod from the Upper Ordovician of Manitoulin Island, Ontario, Canada. Acta Palaeontologica Polonica 52 (3): 535–546. A new species of the orthide brachiopod genus Kinnella is described from the Upper Member of the Georgian Bay Forma− tion (Upper Ordovician) of Manitoulin Island, Ontario, Canada. This species, herein designated as Kinnella laurentiana sp. nov., occurs in strata of Richmondian (mid−Ashgill; Katian) age, most likely correlative with the eastern North Ameri− can Dicellograptus complanatus Zone. This occurrence extends the known stratigraphic range of Kinnella downward considerably from its previously inferred basal Hirnantian inception. The new species is characterized by a moderately convex dorsal valve and an apsacline ventral interarea rarely approaching catacline. This is the third reported occurrence of Kinnella in North America, and is the only species known to have inhabited the epicontinental seas of Laurentia. The associated benthic shelly fauna indicates a depositional environment within fair weather wave base (BA 2). The ancestry of Kinnella and this species appears most likely to lie among older, morphologically similar members of the Draboviidae which were seemingly confined to higher latitude faunal provinces prior to the Hirnantian glacial event. Thus, the mid−Ashgill occurrence of Kinnella laurentiana in the palaeotropically located Manitoulin Island region suggests the mixing of a probable cooler water taxon with the warmer water epicontinental shelly fauna of Laurentia, as well as a pos− sible earlier episode of low−latitude oceanic cooling.
    [Show full text]
  • Combined Analysis of Extant Rhynchonellida (Brachiopoda) Using Morphological and Molecular Data
    Syst. Biol. 67(1):32–48, 2018 © The Author(s) 2017. Published by Oxford University Press, on behalf of the Society of Systematic Biologists. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited. DOI:10.1093/sysbio/syx049 Advance Access publication May 8, 2017 Combined Analysis of Extant Rhynchonellida (Brachiopoda) using Morphological and Molecular Data ,∗ , DAV I D W. BAPST1 ,HOLLY A. SCHREIBER1 2, AND SANDRA J. CARLSON1 1Department of Earth and Planetary Sciences, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA; and 2Penn Dixie Fossil Park and Nature Reserve, 3556 Lakeshore Rd, Ste. 210 Blasdell, NY 14219, USA ∗ Correspondence to be sent to: Department of Earth and Planetary Sciences, University of California, Davis, One Shields Avenue, Davis, CA 95616, USA; E-mail: [email protected]. Received 5 August 2016; reviews returned 14 October 2016; accepted 28 April 2017 Associate Editor: Ken Halanych Abstract.—Independent molecular and morphological phylogenetic analyses have often produced discordant results for certain groups which, for fossil-rich groups, raises the possibility that morphological data might mislead in those groups for which we depend upon morphology the most. Rhynchonellide brachiopods, with more than 500 extinct genera but only 19 extant genera represented today, provide an opportunity to explore the factors that produce contentious phylogenetic signal across datasets, as previous phylogenetic hypotheses generated from molecular sequence data bear little agreement with those constructed using morphological characters.
    [Show full text]
  • Ordovician (Billingen and Volkhov Stages) Brachiopod Faunas of the East Baltic
    Eva Egerquist Ordovician (Billingen and Volkhov stages) brachiopod faunas of the East Baltic 1 Dissertation presented at Uppsala University to be publicly examined in Lecture Theatre, Palaeontology building, Uppsala, Friday, June 4, 2004 at 13.00 for the degree of Doctor of Philosophy. The examination will be conducted in English. Abstract Egerquist E. 2004. Ordovician (Billingen and Volkhov stages) brachiopod faunas of the East Baltic. 34 pp. Uppsala. ISBN 91-506-1756-7 Lower-Middle Ordovician (Arenig) successions in the East Baltic have been investigated for more than one hundred and fifty years. Nevertheless detailed sampling still yields new species and better knowledge of the environment in which these organisms lived. The successions are well suited for bed by bed sampling because of the lack of tectonic disturbance and because the sequences are well documented. This study analyses collections of Billingen-Volkhov age mainly from the St. Petersburg region, but also from Estonia. A great deal of the material was obtained from the marly to clayey, soft sediment that intercalates the compact packstones and wackestones in the succession. Twenty-nine of these clay horizons were used for diversity estimates on the fauna through the succession. The most thoroughly investigated groups for this investigation were rhynchonelliformean brachiopods, conodonts and ostracodes. The results indicate that variances in diversity and abundance levels for these groups were not correlated, either to each other or to the small-scale sea level fluctuations that have been suggested for the region. However, diversity dynamics of brachiopods and ostracodes confirm the large-scale upward shallowing of the basin into the Upper Volkhov.
    [Show full text]
  • Abhandlungen Der Geologischen Bundesanstalt in Wien
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 1999 Band/Volume: 54 Autor(en)/Author(s): Hladil Jindrich, Melichar Rostislav, Otava Jiri, Arnost Krs, Man Otakar, Pruner Petr, Cejchan Petr, Orel Petr Artikel/Article: The Devonian in the Easternmost Variszides, Moravia: a Holistic Analysis Directed Towards Comprehension of the Original Context 27-47 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0016–7800 ISBN 3-85316-02-6 Band 54 S. 27–47 Wien, Oktober 1999 North Gondwana: Mid-Paleozoic Terranes, Stratigraphy and Biota Editors: R. Feist, J.A. Talent & A. Daurer The Devonian in the Easternmost Variscides, Moravia: a Holistic Analysis Directed Towards Comprehension of the Original Context JINDRICH HLADIL, ROSTISLAV MELICHAR, JIRI OTAVA, ARNOST GALLE, MIROSLAV KRS, OTAK AR MAN, PETR PRUNER, PETR CEJCHAN & PETR OREL*) 11 Text-Figures and 1 Table Czech Republic Moravia Bohemian Massif Devonian Variscides Facies Tectonics Palaeomagnetism Biodynamics Contents Zusammenfassung ....................................................................................................... 27 Abstract .................................................................................................................. 28 1. Current Concepts .......................................................................................................
    [Show full text]
  • The Late Ordovician Mass Extinction
    P1: FXY/GBP P2: aaa February 24, 2001 19:23 Annual Reviews AR125-12 Annu. Rev. Earth Planet. Sci. 2001. 29:331–64 Copyright c 2001 by Annual Reviews. All rights reserved THE LATE ORDOVICIAN MASS EXTINCTION Peter M Sheehan Department of Geology, Milwaukee Public Museum, Milwaukee, Wisconsin 53233; e-mail: [email protected] Key Words extinction event, Silurian, glaciation, evolutionary recovery, ecologic evolutionary unit ■ Abstract Near the end of the Late Ordovician, in the first of five mass extinctions in the Phanerozoic, about 85% of marine species died. The cause was a brief glacial interval that produced two pulses of extinction. The first pulse was at the beginning of the glaciation, when sea-level decline drained epicontinental seaways, produced a harsh climate in low and mid-latitudes, and initiated active, deep-oceanic currents that aerated the deep oceans and brought nutrients and possibly toxic material up from oceanic depths. Following that initial pulse of extinction, surviving faunas adapted to the new ecologic setting. The glaciation ended suddenly, and as sea level rose, the climate moderated, and oceanic circulation stagnated, another pulse of extinction occurred. The second extinction marked the end of a long interval of ecologic stasis (an Ecologic-Evolutionary Unit). Recovery from the event took several million years, but the resulting fauna had ecologic patterns similar to the fauna that had become extinct. Other extinction events that eliminated similar or even smaller percentages of species had greater long-term ecologic effects. INTRODUCTION The Late Ordovician extinction was the first of five great extinction events of the by Universidad Nacional Autonoma de Mexico on 03/15/13.
    [Show full text]
  • Preliminary Bedrock Geologic Map of Walworth, Racine, Kenosha
    R 22 E R 23 E R 18 E FOND DU LAC CO R 19 E R 20 E SHEBOYGAN CO R 21 E 1 6 1 6 6 1 6 1 6 1 6 45 Preliminary bedrock geologic map 28 32 43 57 Sm Sm Sr of Walworth, Racine, Kenosha, 28 41 144 Sr T 12 N Milwaukee, Waukesha, Ozaukee, On Dlc Sm Swb Milwaukee and Washington Counties Milwaukee Sm 36 31 36 31 Om 36 31 36 31 36 31 1 6 6 6 T. J. Evans, K.M. Massie-Ferch, 1 1 6 1 1 6 and R.M. Peters Sr 175 Sr 33 OZAUKEE T 11 N 33 River Sr 2004 Sm Om Om On Sm Sr 33 EXPLANATION DODGE CO Sm ake 31 Map units shown are covered by younger, unconsolidated sediment varying in thickness from a few feet to more than 500 feet. 36 31 36 36 31 31 36 31 POST-DEVONIAN C e d a r L 32 L 6 1 6 1 6 Lamprophyre 6 1 6 1 Sm WASHINGTON DEVONIAN 57 Dlc Sm Sr 45 Sr Sm U Da Antrim Shale. Mudstone to very argillaceous dolomite; dark gray to black. Sm D Dm Milwaukee Formation. Argillaceous dolomite, dolomitic siltstone, and shale; gray; locally fossiliferous. T 10 N D Dt Theinsville Formation. Dolomite, argillaceous dolomite, and dolomitic siltstone; brown to brownish gray; some fossils. U Dt/Dlc Theinsville and Lake Church Formations, undifferentiated. Sr River Sm Sr Dlc Lake Church Formation. Argillaceous dolomite, and dolomite; brownish gray; locally fossiliferous. On Om 31 36 31 Sr 36 31 31 31 41 36 36 SILURIAN Swb Waubakee Formation.
    [Show full text]
  • Xerox University Microfilms
    information t o u s e r s This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1.The sign or "target” for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, they are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on the film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again - beginning below the first row and continuing on until complete. 4. The majority of usefs indicate that the textual content is of greatest value, however, a somewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation.
    [Show full text]
  • Åsa Erlfeldt Brachiopod Faunal Dynamics During the Silurian Ireviken Event, Gotland, Sweden
    Brachiopod faunal dynamics during the Silurian Ireviken Event, Gotland, Sweden Åsa Erlfeldt Examensarbeten i Geologi vid Lunds universitet - Berggrundsgeologi, nr. 199 Geologiska institutionen Centrum för GeoBiosfärsvetenskap Lunds universitet 2006 Contents 1 Introduction........................................................................................................................................................5 1.1 Brachiopods 5 2 The Ireviken Event.............................................................................................................................................6 3 Geological setting and stratigraphy..................................................................................................................7 3.1 The Lower and Upper Visby formations 8 4 Materials and methods ......................................................................................................................................9 4.1 Sampled materials 9 4.2 Literature studies 9 4.3 Preparation 9 5 Results ...............................................................................................................................................................10 5.1 Systematic palaeontology 10 6 Discussion..........................................................................................................................................................17 6.1 Comparison of sampled material and the data from the literature 18 6.1.1 The number of brachiopod species in the Lower and Upper Visby formations 18 6.1.2
    [Show full text]
  • A Kralodvorian (Upper Katian, Upper Ordovician)
    A Kralodvorian (upper Katian, Upper Ordovician) benthic association from the Ferradosa Formation (Central Portugal) and its significance for the redefinition and subdivision of the Kralodvorian Stage JORGE COLMENAR, SOFIA PEREIRA, MIGUEL PIRES, CARLOS MARQUES DA SILVA, ARTUR ABREU SÁ & TIMOTHY P. YOUNG A new upper Katian (Kralodvorian Regional Stage) benthic association from the Riba de Cima Member of the Ferradosa Formation, Portugal, is described. It is dominated by bryozoans and echinoderms but brachiopods and trilobites are also present. More than 20 species of brachiopods, nine of trilobites and eight of echinoderms have been identified in the four studied localities. Among the brachiopods Kjaerina (Villasina) meloui Colmenar, 2016, Dolerorthis abeirensis Mélou, 1990 and Bicuspina cf. armoricana Mélou, 1990 are significant. These species were previously recorded only in the uppermost Rosan Formation (Armorican Massif, France). Porambonites dreyfussi Havlíček, 1981 is also reported in this paper for the first time besides its type horizon in the upper part of the Kralodvorian Gabian Formation (Montagne Noire, France). Most of the identified trilobite taxa were previously documented only in the Kralodvorian Cystoid Limestone Formation (Iberian Chains, Spain), except Parillaenus? cf. creber Hammann, 1992 and Amphoriops cf. inflatus (Hammann, 1992), whose referred species are also present in the upper Berounian–Kralodvorian Portixeddu Formation in Sardinia. The record of “Ceraurinus” meridianus (Hammann, 1992), “Bumastus” aff. commodus Apollonov, 1980 and Amphoriops cf. inflatus represent the first occurrence of these genera-groups in Portugal. These records are import- ant additions to the knowledge of the Portuguese Late Ordovician benthic marine communities, providing crucial new data to constrain the biostratigraphy of the Riba de Cima Member and the palaeogeographical setting of this region at that time.
    [Show full text]