Brachiopod Paleoecology, Paleobiogeography, And

Total Page:16

File Type:pdf, Size:1020Kb

Brachiopod Paleoecology, Paleobiogeography, And AN ABSTRACT OF THE THESIS OF William Frederick Koch IIfor the degree of Doctor of Philosophy in Geology presented on December 8, 1978 Title: BRACHIOPOD PALEOECOLOGY, PALEOBIOGEOGRAPHY, AND BIOSTRATIGRAPHY IN THE UPPER MIDDLE DEVONIAN OF EASTERN NORTH AMERICA: AN ECOFACIES MODEL FOR THE APPALACHIAN, MICHIGAN, AND ILLINOIS BASINS Abstract approved; Signature redacted for privacy. A. J, Boucot Articulate brachiopod communities sensitive to environmental factors, especially depth and distance from shore, are described from the upper Middle Devonian (upper Eifelian and Givetian; Cazenovia, Tioughnioga, and Taghanic stages of eastern North America) of eastern North America. The Subrensselandia, Cupularos- trum, Mediospirifer, Tropidoleptus, Devonochonetes, Mucrospirifer, Atrypid-Strophodontid, Ambocoeliid, Pacificocoelia, Truncalosia, and Camarotoechia Communities are described from the Hamilton Group of the Appalachian and Illinois Basins. The Cupularostrum, Rhipido thyris, Orthospirifer, Tropidoleptus, Mucrospirifer, Elytha, Spinatrypa, Hypothyridina-Ambocoeliid, Rhys s ochonetes, and Leio- rhynchus Communities are described from the Tully Formation of the Appalachian Basin. The Subrensselaxdia, Stringocephalus, Rhipidothyris, Cupularostrum, Atrypid- Gypidulinid, Devonochonetes, Cyrtina-Athyris, Camarotoechia, and Longispina Communities are described from the sub-Taghanic Traverse Group of the Michigan Basin. The Rens selandia, Chonetid, Pentamerella- Orthospirifer- Cranaena, Spiriferid-Atrypid, Mucrospirifer, Emanuella, and Leiorhynchus Communities are described from the Cedar Valley Formation and correlative strata exclusive of the Appalachian Basin. The Subrens s elandia, Tropidoleptus, Mucrospirifer- Pholidostrophia, Atrypid- Gypidulinid, Chonetid- Leptaena, Br evi s pirife r, Emanu ella, and Warrenella Communities are described from the Dundee and Rogers City Formations and correlative strata exclusive of the Appalachian Basin. The evolution of these brachiopod communities is traced from the Emsian through the early Famennian by assigning related commu- nities to Community Groups. The temporal changes in the Community Groups are discussed in terms of the constituent genera and communi- ties,Communities not assigned to Community Groups are also con- sidered. The Leptaena- Schizophori.a As semblage Zone is defined to include strata correlative with the Union Springs and Cherry Valley Formations of New York. The Fjmbrispirifer-PentagoniaAsemblage Zone is defined to include strata correlative with the Centerfield Mem- ber of New York. The Rhyssochonetes-Hypothyridina Assemblage Zone is defined to include strata which correlate with the Tully Forma- tion of New York.These assemblage zones are the basis for detailed correlation of the upper Middle Devonian strata of eastern North America. The late Middle Devonian fauna of eastern North America represents a mixture of older Eastern Americas Realm and Old World Realm faunas; many older Eastern Americas Realm stocks died out during the earlier Eifelian.Other Old World Realm genera migrated into the Eastern Americas Realm during transgressions associated with the Leptaena- Schizophoria and Rhy s sochonetes - Hypothyridina Assemblage Zones; these genera distinguish these zones from older and younger rocks. The Eastern Americas Realm of the late Middle Devonian is divisible into two subprovinces. The Appohimchi Subprovince occu- pies the Appalachian and Illinois Basins and the clastic shelf to the east of the Appalachian Basin.The Michigan Basin-Hudson Bay Low- land Subprovince occupies a broad carbonate platform extending from Michigan west to Iowa and north to Hudson Bay.Provinciality between these subprovinces rose from the base of the Cazenovia to a peak at the time of the deposition of the Skaneateles Formation, fell during the Fimbrispirifer-Pentagonia As semblage Zone, rose during the upper Tioughnioga, and declined sharply during the Taghanic. The Fimbrispirifer-Pentagonia Assemblage Zone is associated with a transgression and change in current patterns which allowed Appohimchi genera to migrate onto the Michigan carbonate platform. Profiles of depositional topography are constructed for several intervals of late Middle Devonian time.Shelf (undathem), slope (clinothem), and basinal (1 ondathem) deposits are distinguished on these profiles.Chains of communities occur along these profiles. Benthic Assemblages 1 and 2 are on the shelf,Benthic Assemblage 3 ranges from shelf through slope,Benthic Assemblage 4 from slope to basin, and Benthic Assemblage 5 is basinal.Migrations of community chains and shelf margins correspond to transgressionsand regres sions.Biostratigraphic and lithostratigraphic data allow tracing of seven transgressive-regressive events overmuch of eastern North America; these cycles can be used to refine correlationsbased on other stratigraphic techniques. Brachiopod Paleoecology, Paleobiogeography, and Biostratigraphy in the upper Middle Devonian of Eastern North America: An Ecofacies Model for the Appalachian, Michigan, and Illinois Basins by William Frederick Koch II A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Doctor of Philosophy Completed December 8, 1978 Commencement June 1979 ACKNOWLEDGEMENTS I wish to greatly thank Arthur J. Boucot for his support and assistance in all, aspects of this study.I thank J. Granville Johnson for many discussions of the ideas presented in this study.To Keith F. Oles, Andrew G. Carey, Jr., and Henry A. Froelich go thanks for critically reviewing this manuscript and for helpful com ments on my work. Especially great thanks go to G. Arthur Cooper for his assis tance during the summers I spent examining collections at the United States National Museum. Discussions with Dr. Cooper were of the highest value in understanding the stratigraphy and paleontology of the upper Middle Devonian rocks of eastern North America. Also I thank Frederick J. Collier for his assistance at the United States National Museum and William A. Oliver for the helpful discussions of Devonian paleobiogeography. Thanks are also due to Lawrence V. Rickard for discussions of the Middle Devonian stratigraphy of New York and to John Innes for discussions of Pennsylvania stratigraphy.I thank A. W. Norris for the permission to examine collections from the James Bay region at the Institute of Petroleum and Sedimentary Geology in Calgary. Great thanks go to John M. Dennison for discussions of this study and for information on the Middle Devonian stratigraphy of Maryland, Virginia, and West Virginia.I thank Michael R. House for examining ammonites which I collected. Thanks are due to Donald G. Mikulic for showing me the out- crops of the Milwaukee and Lake Church Formations in Wisconsin. Special thanks go to Jed Day for assisting me in the field during the summer of 1977.Similarly, I thank Thomas L. DeKeyser for many hours of stimulating discussions on all aspects of paleontology and sedimentary geology; especially for his help in the development of many ideas on ecofacies modeling.I also thank Thomas J. De Vries for his assistance, particularly in the paleobiogeographic modeling. This study was partially financed by a Grant-In-Aid of Research from Sigma Xi, the Scientific Research Society of North America. Support also was provided through a graduate scholarship from the Standard Oil Company of California, for which I was nominated bythe Graduate Committee of the Oregon State University Geology Depart- ment. TABLE OF CONTENTS INTRODUCTION 1 Limits of Study 2 Previous Studies 4 METHODS OF STUDY 12 BRACHIOPOD COMMUNITY PALEOECOLOGY 15 Brachiopod Communities of the Hamilton Group in the Appalachian and Illinois Basins 19 Brachiopod Communities of the Tully Limestone and Correlative Strata in the Appalachian Basin 34 Brachiopod Communities of the Sub- Taghanic Traverse Group of the Michigan. Basin 42 Brachiopod Communities of the Cedar Valley Limestone and Correlative Strata Outside of the Appalachian Basin 52 Brachiopod Communities of the Dundee and Rogers City Limestones and Correlative Strata Outside of the Appalachian Basin (Leptaena-Schizophoria Assemblage Zone) 58 COMMUNITY EVOLUTION 66 Rensselandiid Community Group 66 Orthospirifer Community Group 67 Devonochonete s Community Group 74 Elytha Community Group 77 Atrypid- Gypidulinid Community Group 81 Ambocoelild Community Group 82 Evolutionary Relationships of Unassigned Communities 83 BIOSTRATIGRAPHY 89 Leptaena-Schizophoria Assemblage Zone 90 Fimbrispirifer-Pentagonia As semblage Z ohe 94 Rhyssochonetes-Hypothyriina Assemblage Zone 96 PALEOBIOGEOGRAPHY 99 Mixture of Eastern Americas Realm and Old World Realm Faunas in the Upper Middle Devonian of Eastern North America 101 Migrations of Old World Brachiopods intothe Eastern Americas Realm During the Late Middle Devonian 102 Provinciality Within the Eastern AmericasRealm 104 Transition Zone Between the Appohimchi andMichigan Basin-Hudson Bay Lowland Subprovinces 117 Boundary Between the Appohimchi Subprovinceand the Michigan Basin-Hudson Bay Lowland Subprovince 118 Boundary Between the Eastern AmericasRealm and the Old World Realm During the Late MiddleDevonian 125 AN ECOFACIES MODEL 130 Fossils and Rocks: A Shelf to Basin Profile 130 Regional Correlation through Local Changesof Sea Level 147 Summary The Late Middle Devonian of Eastern North America 157 REFERENCES CITED 170 Appendix1Locations of Collections 182 Hamilton Group Atrypid Str ophodontid Community 183 Mucrospirifer Community 196 Ambocoeliid
Recommended publications
  • Comments on the Paper by A. May “Micheliniidae and Cleistoporidae (Anthozoa, Tabulata) from the Devonian of Spain”
    Comments on the paper by A. May Micheliniidae and Cleistoporidae (Anthozoa, Tabulata) from the Devonian of Spain YVES PLUSQUELLEC & ESPERANZA FERNÁNDEZ-MARTÍNEZ PLUSQUELLEC,Y.&FERNÁNDEZ-MARTÍNEZ E. 2007. Com- lity for this species is known in Celtiberia, where the speci- ments on the paper by A. May “Micheliniidae and Cleistoporidae mens are preserved in calcite: North of Nogueras, Maripo- (Anthozoa, Tabulata) from the Devonian of Spain”. Bulletin of sas Formation, d4aβ, Lower Emsian. Geosciences 82(1), 85–89 (3 figures). Czech Geological Survey, Prague. ISSN 1214-1119. Manuscript received January 22, 2007; issued March 30, 2007. • DOI 10.3140/bull.geosci.2007.01.85 Pleurodictyum elisabetae May, 2006 Yves Plusquellec, Université de Bretagne Occidentale, UMR 6538 “Domaines océaniques”, Laboratoire de Paléontologie, The identification of Pleurodictyum-like corals is very UFR Sciences & Techniques, 6 av. Le Gorgeu – CS 93837, problematic when the aboral side is unknown. In this case F-29238 Brest cedex 3, France; [email protected] • the specimens could belong to Pleurodictyum Goldfuss, Esperanza Fernández-Martínez, Área de Paleontología, Facul- 1829, Procteria Davis, 1887, Procterodictyum Plusquel- tad de Ciencias Biológicas y Ambientales, Campus de Vegazana lec, 1993 or Amazonodictyum nom. nud. (Plusquellec s/n, Universidad de León, 24071 León, Spain; e.fernandez@uni- 2006, unpublished thesis; type species Pleurodictyum leon.es amazonicum Katzer, 1903). Nevertheless, a more precise identification is possible in a few cases. We have examined the two specimens (stock num- In our opinion the conclusions presented in the paper by bers 13D and 14D, Museo Geominero) figured by May Andreas May in Bulletin of Geosciences 81(3), 163–172 (fig.
    [Show full text]
  • Wisconsin Geological and Natural History Survey 3817 Mineral Point Road Madison, Wisconsin 53705-5100 TEL 608/263.7389 FAX 608/262.8086
    Wisconsin Geological and Natural History Survey 3817 Mineral Point Road Madison, Wisconsin 53705-5100 TEL 608/263.7389 FAX 608/262.8086 www.uwex.edu/wgnhs/ James M. Robertson, Director and State Geologist The Waukesha Fault and Its Relationship to the Michigan Basin: A Literature Compilation Suzanne M. Braschayko 2005 Open-File Report 2005-05 60 p. This report represents work performed by the Wisconsin Geological and Natural History Survey or colleagues and is released to the open files in the interest of making the information readily available. This report has not been edited or reviewed for conformity with Wisconsin Geological and Natural History Survey standards and nomenclature. Introduction......................................................................................................................... 1 Regional Setting.................................................................................................................. 1 Southeast Wisconsin ........................................................................................................... 1 Stratigraphy......................................................................................................................... 1 Precambrian .................................................................................................................... 2 Cambrian......................................................................................................................... 2 Ordovician......................................................................................................................
    [Show full text]
  • Catskill Trails, 9Th Edition, 2010
    Harriman-Bear Mountain Trails, 13th Edition, 2010 New York-New Jersey Trail Conference Index Feature Map (119BM = Bear Mtn Inset) 1777 E Trail 119, 119BM 1777 W Trail 119, 119BM 1779 Trail 119, 119BM Abrams Road 119 ADK Camp Nawakwa 118 Agony Grind 119 Almost Perpendicular 118 American Canoe Association Camp 118 Anchor Monument 119 Anthony Wayne Recreation Area 119 Anthony Wayne Trail 119 Anthonys Nose 119 Appalachian Trail 119, 119BM Arden 119 Arden Brook 119 Arden House 119 Arden Road 119 Arden Valley Road 119 Arden-Surebridge Trail 118, 119 Augusta Mine 118 Baileytown Cemetery 119 Baileytown Road 119 Baker Camp 118 Bald Mountain 118, 119 Bald Rocks Shelter 118, 119 Barnes Lake 119 Barnes Mine 118 Bear Mountain 119, 119BM Bear Mountain Administration Building 119BM Bear Mountain Bridge 119, 119BM Bear Mountain Bridge Road 119 Bear Mountain Dock 119BM Bear Mountain Historical Museum 119BM Bear Mountain Inn 119BM Bear Mountain Merry-Go-Round 119BM Bear Mountain Picnic Area 119BM Bear Mountain Skating Rink 119BM Bear Mountain State Park 119, 119BM Bear Mountain Swimming Pool 119BM Bear Mountain Trailside Museums and Zoo 119BM Beaver Pond Brook 118 Beaver Pond Campground 118, 119 p1 Beech Trail 118, 119 Beech Trail Cemetery 118, 119 Beechy Bottom Road 119 Bensons Point 119 Big Bog Mountain 119 Big Hill 118 Big Hill Shelter 118 Black Ash Mine 118 Black Ash Mountain 118 Black Ash Swamp 118 Black Mountain 119 Black Rock 118, 119 Black Rock Mountain 118, 119 Blauvelt Mountain 118 Blendale Lake 119 Blue Disc Trail 118 Blythea Lake 119 Bockberg
    [Show full text]
  • Cambrian Ordovician
    Open File Report LXXVI the shale is also variously colored. Glauconite is generally abundant in the formation. The Eau Claire A Summary of the Stratigraphy of the increases in thickness southward in the Southern Peninsula of Michigan where it becomes much more Southern Peninsula of Michigan * dolomitic. by: The Dresbach sandstone is a fine to medium grained E. J. Baltrusaites, C. K. Clark, G. V. Cohee, R. P. Grant sandstone with well rounded and angular quartz grains. W. A. Kelly, K. K. Landes, G. D. Lindberg and R. B. Thin beds of argillaceous dolomite may occur locally in Newcombe of the Michigan Geological Society * the sandstone. It is about 100 feet thick in the Southern Peninsula of Michigan but is absent in Northern Indiana. The Franconia sandstone is a fine to medium grained Cambrian glauconitic and dolomitic sandstone. It is from 10 to 20 Cambrian rocks in the Southern Peninsula of Michigan feet thick where present in the Southern Peninsula. consist of sandstone, dolomite, and some shale. These * See last page rocks, Lake Superior sandstone, which are of Upper Cambrian age overlie pre-Cambrian rocks and are The Trempealeau is predominantly a buff to light brown divided into the Jacobsville sandstone overlain by the dolomite with a minor amount of sandy, glauconitic Munising. The Munising sandstone at the north is dolomite and dolomitic shale in the basal part. Zones of divided southward into the following formations in sandy dolomite are in the Trempealeau in addition to the ascending order: Mount Simon, Eau Claire, Dresbach basal part. A small amount of chert may be found in and Franconia sandstones overlain by the Trampealeau various places in the formation.
    [Show full text]
  • University of Michigan University Library
    CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN VOL. XI NO.6, pp. 101-157 (12 pk., 1 map) MARCH25, 1953 TRILOBITES OF THE DEVONIAN TRAVERSE GROUP OF MICHIGAN BY ERWIN C. STUMM UNIVERSITY OF MICHIGAN PRESS ANN ARBOR CONTMBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN MUSEUM OF PALEONTOLOGY Director: LEWIS B. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based chiefly upon the collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and also to individuals upon request. Correspondence should be directed to the University of Michigan Press. A list of the separate papers in Volumes II-IX will be sent upon request. VOL. I. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian, by C. L. Fenton and M. A. Fenton. Pages xi+260. Cloth. $2.75. VOL. 11. Fourteen papers. Pages ix+240. Cloth. $3.00. Parts sold separately in paper covers. VOL. 111. Thirteen papers. Pages viii+275. Cloth. $3.50. Parts sold separately in paper covers. VOL. IV. Eighteen papers. Pages viiif295. Cloth. $3.50. Parts sold separately in paper covers, VOL. V. Twelve papers. Pages viii+318. Cloth. $3.50. Parts sold separately in paper covers. VOL. VI. Ten papers. Pages vii+336. Paper covers. $3.00. Parts sold separately. VOLS. VII-IX. Ten numbers each, sold separately. (Continued on inside back cover) VOL.
    [Show full text]
  • Message from the New Chairman
    Subcommission on Devonian Stratigraphy Newsletter No. 21 April, 2005 MESSAGE FROM THE NEW CHAIRMAN Dear SDS Members: This new Newsletter gives me the pleasant opportunity to thank you for your confidence which should allow me to lead our Devonian Subcommission successfully through the next four years until the next International Geological Congress in Norway. Ahmed El Hassani, as Vice-Chairman, and John Marshall, as our new Secretary, will assist and help me. As it has been our habit in the past, our outgoing chairman, Pierre Bultynck, has continued his duties until the end of the calendar year, and in the name of all the Subcommission, I like to express our warmest thanks to him for all his efforts, his enthusi- asm for our tasks, his patience with the often too slow progress of research, and for the humorous, well organized and skil- ful handling of our affairs, including our annual meetings. At the same time I like to thank all our outgoing Titular Members for their partly long-time service and I express my hope that they will continue their SDS work with the same interest and energy as Corresponding Members. The new ICS rules require a rather constant change of voting members and the change from TM to CM status should not necessarily be taken as an excuse to adopt the lifestyle of a “Devonian pensioner”. I see no reason why constantly active SDS members shouldn´t become TM again, at a later stage. On the other side, the rather strong exchange of voting members should bring in some fresh ideas and some shift towards modern stratigraphical tech- niques.
    [Show full text]
  • Sequence of Post-Moult Exoskeleton Hardening Preserved in a Trilobite Mass Moult Assemblage from the Lower Ordovician Fezouata Konservat-Lagerstätte, Morocco
    Editors' choice Sequence of post-moult exoskeleton hardening preserved in a trilobite mass moult assemblage from the Lower Ordovician Fezouata Konservat-Lagerstätte, Morocco HARRIET B. DRAGE, THIJS R.A. VANDENBROUCKE, PETER VAN ROY, and ALLISON C. DALEY Drage, H.B., Vandenbroucke, T.R.A., Van Roy, P., and Daley, A.C. 2019. Sequence of post-moult exoskeleton hardening preserved in a trilobite mass moult assemblage from the Lower Ordovician Fezouata Konservat-Lagerstätte, Morocco. Acta Palaeontologica Polonica 64 (2): 261–273. Euarthropods have a tough exoskeleton that provides crucial protection from predation and parasitism. However, this is restrictive to growth and must be periodically moulted. The moulting sequence is well-known from extant arthropods, consisting of: (i) the long inter-moult stage, in which no changes occur to the hardened exoskeleton; (ii) the pre-moult stage where the old exoskeleton is detached and the new one secreted; (iii) exuviation, when the old exoskeleton is moulted; and (iv) the post-moult stage during which the new exoskeleton starts as soft, thin, and partially compressed and gradually hardens to the robust exoskeleton of the inter-moult stage. Trilobite fossils typically consist of inter-moult carcasses or moulted exuviae, but specimens preserving the post-moult stage are rare. Here we describe nine specimens assigned to Symphysurus ebbestadi representing the first group of contemporaneous fossils collected that preserve all key stages of the moulting process in one taxon, including the post-moult stage. They were collected from a single lens in the Tremadocian part of the Fezouata Shale Formation, Morocco. Based on cephalic displacement and comparison to other trilobite moults, one specimen appears to represent a moulted exoskeleton.
    [Show full text]
  • Ground-Water Conditions in the Milwaukee-Waukesha Area, Wisconsin
    Ground-Water Conditions in the Milwaukee-Waukesha Area, Wisconsin GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1229 Ground-Water Conditions in the Milwaukee -Waukesha Area, Wisconsin By F. C. FOLEY, W. C. WALTON, and W. J. DRESCHER GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1229 A progress report, with emphasis on the artesian sandstone aquifer. Prepared in cooperation with the University of Wisconsin. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director f For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. - Price 70 cents CONTENTS Page Abstract.............................................................................................................................. 1 Introduction........................................................................................................................ 3 Purpose and scope of report.................................................................................... 4 Acknowledgments...................................................................................................... 5 Description of the area............................................................................................ 6 Previous reports........................................................................................................ 6 Well-numbering system.............................................................................................. 7 Stratigraphy.......................................................................................................................
    [Show full text]
  • Stratigraphic Succession in Lower Peninsula of Michigan
    STRATIGRAPHIC DOMINANT LITHOLOGY ERA PERIOD EPOCHNORTHSTAGES AMERICANBasin Margin Basin Center MEMBER FORMATIONGROUP SUCCESSION IN LOWER Quaternary Pleistocene Glacial Drift PENINSULA Cenozoic Pleistocene OF MICHIGAN Mesozoic Jurassic ?Kimmeridgian? Ionia Sandstone Late Michigan Dept. of Environmental Quality Conemaugh Grand River Formation Geological Survey Division Late Harold Fitch, State Geologist Pennsylvanian and Saginaw Formation ?Pottsville? Michigan Basin Geological Society Early GEOL IN OG S IC A A B L N Parma Sandstone S A O G C I I H E C T I Y Bayport Limestone M Meramecian Grand Rapids Group 1936 Late Michigan Formation Stratigraphic Nomenclature Project Committee: Mississippian Dr. Paul A. Catacosinos, Co-chairman Mark S. Wollensak, Co-chairman Osagian Marshall Sandstone Principal Authors: Dr. Paul A. Catacosinos Early Kinderhookian Coldwater Shale Dr. William Harrison III Robert Reynolds Sunbury Shale Dr. Dave B.Westjohn Mark S. Wollensak Berea Sandstone Chautauquan Bedford Shale 2000 Late Antrim Shale Senecan Traverse Formation Traverse Limestone Traverse Group Erian Devonian Bell Shale Dundee Limestone Middle Lucas Formation Detroit River Group Amherstburg Form. Ulsterian Sylvania Sandstone Bois Blanc Formation Garden Island Formation Early Bass Islands Dolomite Sand Salina G Unit Paleozoic Glacial Clay or Silt Late Cayugan Salina F Unit Till/Gravel Salina E Unit Salina D Unit Limestone Salina C Shale Salina Group Salina B Unit Sandy Limestone Salina A-2 Carbonate Silurian Salina A-2 Evaporite Shaley Limestone Ruff Formation
    [Show full text]
  • Columnals (PDF)
    2248 22482 2 4 V. INDEX OF COLUMNALS 8 Remarks: In this section the stratigraphic range given under the genus is the compiled range of all named species based solely on columnals assigned to the genus. It should be noted that this range may and often differs considerably from the range given under the same genus in Section I, because that range is based on species identified on cups or crowns. All other abbreviations and format follow that of Section I. Generic names followed by the type species are based on columnals. Genera, not followed by the type species, are based on cups and crowns as given in Section I. There are a number of unlisted columnal taxa from the literature that are indexed as genera recognized on cups and crowns. Bassler and Moodey (1943) did not index columnal taxa that were not new names or identified genera with the species unnamed. I have included some of the omissions of Bassler and Moodey, but have not made a search of the extensive literature specifically for the omitted citations because of time constraints. Many of these unlisted taxa are illustrated in the early state surveys of the eastern and central United States. Many of the columnal species assigned to genera based on cups or crowns are incorrect assignments. An uncertain, but significant, number of the columnal genera are synonyms of other columnal genera as they are based on different parts of the stem of a single taxon. Also a number of the columnal genera are synonyms of genera based on cups and crowns as they come from more distal parts of the stem not currently known to be associated with the cup or crown.
    [Show full text]
  • Instituto De Geociências Revisão Sistemática E
    UNIVERSIDADE DE SÃO PAULO INSTITUTO DE GEOCIÊNCIAS REVISÃO SISTEMÁTICA E PALEOBIOGEOGRÁFICA DE TRILOBITAS PHACOPIDA (HOMALONOTIDAE E CALMONIIDAE) DO DEVONIANO DAS BACIAS DO PARNAÍBA E AMAZONAS, BRASIL Felipe van Enck Meira Tese apresentada ao Programa de Pós- Graduação em Geoquímica e Geotectônica do Instituto de Geociências da Universidade de São Paulo, como parte dos requisitos para a obtenção do título de doutor. Orientadora: Prof. Dra. Juliana de Moraes Leme TESE DE DOUTORAMENTO Programa de Pós-graduação em Geoquímica e Geotectônica São Paulo 2016 “Kites rise highest against the wind - not with it.” - Winston Churchill Agradecimentos Agradeço a Deus, por sempre iluminar o caminho durante esses anos de altos e baixos do Doutorado. Agradeço a Ele também por enviar dois verdadeiros anjos da guarda à minha vida – minha esposa Angela Faleiros van Enck Meira e meu filho, Thomas Faleiros van Enck Meira. Agradeço a meus pais, José Carlos e Sylvia, e à minha irmã, Patrícia, pelo apoio durante a jornada, ainda que à distância, por vezes. Sou grato aos meus sogros, Jair e Lucia, que sempre foram como verdadeiros pais e conselheiros. À FAPESP (Processo n° 2012/07075-3), pelo suporte financeiro, sem o qual o Doutorado não seria viável. À minha orientadora, Drª. Juliana de Moraes Leme, pela orientação, discussões e esclarecimentos pertinentes ao projeto. Ao Doutorando Fabio Carbonaro e ao Dr. Renato Ghilardi (UNESP-Bauru), pela parceria e por discussões importantes na realização do trabalho. À Drª. Niède Guidon (FUMDHAM), pelo empréstimo de fósseis da região de São João Vermelho (Piauí), estudados aqui. Sou grato às seguintes pessoas, por permitirem meu acesso às instituições para visita de acervos, e por sua disponibilidade, atenção e ajuda durante minha permanência: Bushra Hussaini (AMNH), Flávia Alessandra Figueiredo, Mônica de Medina Coeli, Dr.
    [Show full text]
  • University of Michigan University Library
    CONTRIBUTIONS FROM TEE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN VOL. VIII, No. 8, pp. 205-220 (5 pls.) AUGUST11, 1950 CORALS OF THE DEVONIAN TRAVERSE GROUP OF MICHIGAN. PART 111, ANTHOLITES, PLEURODICTYUM, AND PROCTERIA BY ERWIN C. STUMM UNIVERSITY OF MICHIGAN PRESS ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY UNIVERSITY OF MICHIGAN Director: LEWISB. KELLUM The series of contributions from the Museum of Paleontology is a medium for the publication of papers based entirely or principally upon the collections in the Museum. When the number of wes issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and also to individuals upon request. Correspondence should be directed to the University of Michigan Press. A list of the separate papers in Vol- umes II-VII will be sent upon request. VOL. I. The Stratigraphy and Fauna of the Hackberry Stage of the Upper Devonian, by C. L. Fenton and M. A. Fenton. Pages xi+260. Cloth. $2.75. VOL. 11. Fourteen papers. Pages ixf240. Cloth. $3.00. Parts sold separately in paper covers. VOL. 111. Thirteen papers. Pages viii+275. Cloth. $3.50. Parts sold separately in paper covers. VOL. IV. Eighteen papers. Pages viii+295. Cloth. $3.50. Parts sold separately in paper covers. VOL. V. Twelve papers. Pages viii+-318. Cloth. $3.50. Part. sold separately in paper covers. VOL. VI. Ten papers. Pages viii+336. Paper covers. $3.00. Parts sold separately. VOL. VII. Ten numbers sold separately. (Continued on inside back cover) VOL.
    [Show full text]