Map and Table Describing Fossil Collections and Related Samples in the Ketchikan and Prince Rupert Quadrangles, Southeastern Alaska
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Catalog of Type Specimens of Invertebrate Fossils: Cono- Donta
% {I V 0> % rF h y Catalog of Type Specimens Compiled Frederick J. Collier of Invertebrate Fossils: Conodonta SMITHSONIAN CONTRIBUTIONS TO PALEOBIOLOGY NUMBER 9 SERIAL PUBLICATIONS OF THE SMITHSONIAN INSTITUTION The emphasis upon publications as a means of diffusing knowledge was expressed by the first Secretary of the Smithsonian Institution. In his formal plan for the Insti tution, Joseph Henry articulated a program that included the following statement: "It is proposed to publish a series of reports, giving an account of the new discoveries in science, and of the changes made from year to year in all branches of knowledge." This keynote of basic research has been adhered to over the years in the issuance of thousands of titles in serial publications under the Smithsonian imprint, com mencing with Smithsonian Contributions to Knowledge in 1848 and continuing with the following active series: Smithsonian Annals of Flight Smithsonian Contributions to Anthropology Smithsonian Contributions to Astrophysics Smithsonian Contributions to Botany Smithsonian Contributions to the Earth Sciences Smithsonian Contributions to Paleobiology Smithsonian Contributions to Zoology Smithsonian Studies in History and Technology In these series, the Institution publishes original articles and monographs dealing with the research and collections of its several museums and offices and of profes sional colleagues at other institutions of learning. These papers report newly acquired facts, synoptic interpretations of data, or original theory in specialized fields. These publications are distributed by mailing lists to libraries, laboratories, and other in terested institutions and specialists throughout the world. Individual copies may be obtained from the Smithsonian Institution Press as long as stocks are available. -
Proceedings of the Indiana Academy of Science 83
Proceedings of the Indiana Academy of Science 83 (1993) Volume 102 p. 83-91 CONODONTS FROM COAL BALLS IN THE SPRINGFIELD COAL MEMBER OF THE PETERSBURG FORMATION (DESMOINESIAN, PENNSYLVANIAN) IN SOUTHERN INDIANA Carl B. Rexroad Indiana Geological Survey 611 North Walnut Grove Bloomington, Indiana 47405 ABSTRACT: A well-preserved and moderately diverse conodont faunule was recovered from five coal balls in the Springfield Coal Member of the Petersburg Formation from Peabody Coal Com- pany's Eby Pit, Lynnville Mine, in Warrick County, Indiana. The presence of Neognathodus roundyi and the other species recorded in this study is compatible with the middle Desmoinesian age of the Springfield. Idioprioniodus conjunctus is the most ecologically diagnostic of the conodonts and suggests organic-rich, quiet water with a low pH, which in turn suggests that the conodonts lived in a salt-water marsh bordered on one side by coal swamps and on another by near-normal marine waters. Apparently coal balls had multiple origins, and the origin of the conodont-bearing ones is uncertain. INTRODUCTION Because marine fossils are commonly associated with plant fossils in some coal balls, it is not surprising that conodonts have been reported from them. A half-dozen well-pre- served conodonts from Pennsylvanian coal balls from three different States were figured by Mamay and Yochelson (1962), but no other conodonts were figured; therefore, the overall conodont content in coal balls is unknown. To better understand the distribution of conodonts and their paleoecologic impor- tance in coal balls, samples were processed from coal balls of the middle Desmoinesian Springfield Coal Member of the Petersburg Formation from the Eby Pit of Peabody Coal Company's Lynnville Mine (SW'/4 , SWA, NE'A, Sec. -
On Some Occurrences of Diplognathodus in Carboniferous Strata of Western Europe and North Africa
v.d. Boogaard, Diplognathodus from W. Europe & N. Africa, Scripta Geol., 69 (1983) On some occurrences of Diplognathodus in Carboniferous strata of Western Europe and North Africa M. van den Boogaard Boogaard, M. van den. On some occurrences of Diplognathodus in Carboniferous strata of Western Europe and North Africa. - Scripta Geol., 69: 19-29, 1 fig., 1 pl., October 1983. The occurrence is reported of Diplognathodus coloradoensis, D. orphanus and D. ellesmerensis in some localities in Western Europe and one locality in North Afri- ca. M. van den Boogaard, Rijksmuseum van Geologie en Mineralogie, Hooglandse Kerkgracht 17, 2312 HS Leiden, The Netherlands. Introduction 19 Localities 20 Palaeontology 23 Concluding remarks 25 References 27 Introduction Species of the genus Diplognathodus may be useful for stratigraphie correlation of Carboniferous strata because some of them are probably stratigraphically short-ranging (e.g. D. coloradoensis according to Landing & Wardlaw, 1981, pp. 1255-1256). Because still little is known about the distribution of représentants of the genus outside North America I thought it useful to relate the few occur• rences of D. coloradoensis, D. orphanus and D. ellesmerensis I encountered during my investigation of Carboniferous limestones from Western Europe and North Africa. 20 v.d. Boogaard, Diplognathodus from W. Europe & N. Africa, Scripta Geol., 69 (1983) Acknowledgements Thanks for placing the samples at my disposal are due to Drs C.F. Winkler Prins, H.A. van Adrichem Boogaert, M.J.M. Bless, and A.C. van Ginkel. The informa• tion concerning the Cinderhill sample given by Dr W.H.C. Ramsbottom is much appreciated. Thanks also go to Mr J.G.M. -
Ian, and the Early Upper Devonian Some Icriodus Species Such As
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ian, and the early Upper Devonian some Icriodus species such as /. fusiformis, I. culicellus, I. rectiro- stratus, I. retrodepressus, I. regularicrescens, I. obliquimarginatus and /. subterminus have a wide or so metimes nearly cosmopolite dispersion in different magnafacies areas (type Ardenno-Rhenish and Her- cynian-Bohemian) and there is no marked difference in the earliest occurrence of each species. This means that the geographical dispersion of at least some Icriodus species was due primarily to good com munication seaways which could be modified in the course of time and not to very specialised local fa des factors. Having in mind the SEDDON and SWEET model for conodonts, the dominance of Icrio dus in shallow water shelf environment implies no restriction in geographical dispersion. Particularly in this environment, anomalies in the vertical distribution ofPolygnathus taxa, e. g.,-P. serotinus, P. lingui- formis div. subspecies, P. cooperi cooperi can be noticed. Reexamination of Late Pennsylvanian and Early Permian Conodont Apparatuses Using Clustering Techniques. By T. R. CARR Department of Geology and Geophysics, University of Wisconsin, Madison, Wisconsin 53706, USA. Conodont faunas containing easily identified Pa elements assignable to the genera Diplognathodus and Hindeodus have been reported from Upper Pennsylvanian and Lower Permian strata of North Ame rica. If the seximembrate model for the apparatus of each genus is correct, the remaining elements should also be present. However, previous investigators have normally considered ramiform elements which might be assignable to the two genera as attributable to species of either the Idiognathodus— Streptognathodus plexus or Adetognathus. -
Upper Triassic Corals and Carbonate Reef Facies from the Martin Bridge and Hurwal Formations, Wallowa Terrane (Oregon)
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 2010 UPPER TRIASSIC CORALS AND CARBONATE REEF FACIES FROM THE MARTIN BRIDGE AND HURWAL FORMATIONS, WALLOWA TERRANE (OREGON) Megan Ruth Rosenblatt The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Rosenblatt, Megan Ruth, "UPPER TRIASSIC CORALS AND CARBONATE REEF FACIES FROM THE MARTIN BRIDGE AND HURWAL FORMATIONS, WALLOWA TERRANE (OREGON)" (2010). Graduate Student Theses, Dissertations, & Professional Papers. 1354. https://scholarworks.umt.edu/etd/1354 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. UPPER TRIASSIC CORALS AND CARBONATE REEF FACIES FROM THE MARTIN BRIDGE AND HURWAL FORMATIONS, WALLOWA TERRANE (OREGON) By MEGAN RUTH ROSENBLATT Bachelor of Science, College of Charleston, Charleston SC, 2006 Thesis Presented in partial fulfillment of the requirements for the degree of Master of Science in Geosciences The University of Montana Missoula, MT December 2010 Approved by: Perry Brown, Associate Provost for Graduate Education Graduate School George Stanley, Ph.D., Chair Geosciences Marc Hendrix, Ph.D. Geosciences Jon Graham, Ph.D. Mathematical Sciences i ACKNOWLEDGEMENTS I would like to thank the National Science Foundation for field and laboratory funding from a grant awarded to George Stanley. For tuition and salary as a Research Assistant I would like to thank the Innovative Technology Experiences for Students and Teachers (ITEST) section of the National Science Foundation; a grant awarded to Heather Almquist and George Stanley. -
Scleractinia from the Upper Portlandian of Tisbury, Wiltshire, England
ACT A PAL A EON T 0 LOG ICA POLONICA Vol. XV 1970 No.4 EWA RONIEWICZ SCLERACTINIA FROM THE UPPER PORTLANDIAN OF TISBURY, WILTSHIRE, ENGLAND Abstract. - Four species of Scleractinia: Pseudodiplocoenia oblonga (Fleming), Ellipsasteria gracilis n. gen., n. sp., Edwardsastraea tisburiensis n. gen., n. sp. and Ebrayia dightonthomasi n. sp., from the uppermost Portlandian of Tisbury, west of Salisbury, Wiltshire, England, are here described. The histological structure of the skeleton of Pseudodiplocoenia oblonga, preserved in silicified colonies is presented. INTRODUCTION A little known coral fauna occurs in the uppermost beds of the Upper Portlandian near Tisbury (West of Salisbury, Wiltshire, England). The preservation of colonies in a completely silicified. state is a peculiarity of this fauna which, containing representatives of the Recent families, Helia straeidae and Faviidae, deviates in character from typical Jurassic faunas. Only one of the species which occur at this locality has so far been described by H. Milne-Edwards &J. Haime (1851) in Part II of "A Mono graph of the British Fossil Corals" as Isastraea oblonga (Fleming). This name was subsequently used to designate all corals from Tisbury in the collections of the British Museum and the Geological Survey Museum, including the representatives of the three new species described here. A fairly considerable specific differentiation of the collection under study, which is an accidental collection, suggests that the fauna of corals from Tisbury might be much richer. As a result of a complete silification of the colonies, macroscopic cha racters of the skeleton are clearly visible. In addition, the histological structure of the skeleton is preserved in specimens of P. -
Columactinastraea Anthonii Sp. Nov. (Scleractinia, Astrocoeniina), a New Coral Species from the Maastrichtian (Upper Cretaceous) of the Netherlands
SG126 185-202 leloux 16-01-2007 09:07 Pagina 185 Columactinastraea anthonii sp. nov. (Scleractinia, Astrocoeniina), a new coral species from the Maastrichtian (Upper Cretaceous) of The Netherlands J. Leloux Leloux, J. Columactinastraea anthonii sp. nov. (Scleractinia, Astrocoeniina), a new coral species from the Maastrichtian (Upper Cretaceous) of The Netherlands. Scripta Geologica, 126: 185-201, 4 figs., 1 pl., Lei- den, November 2003. Jacob Leloux, Gortestraat 82, 2311 NM Leiden, The Netherland ([email protected]). Key words — taxonomy, cerioid growth forms, Plesiosiderastraea, St. Pietersberg, Meerssen Member. Only four cerioid species of scleractinian corals have been described from the Maastrichtian in its type area; the montlivaltiid Isastrea angulosa (Goldfuss, 1826), and the astrocoeniids Actinastrea goldfussi d’Orbigny, 1849, A. faujasi (Quenstedt, 1881) and Columastrea fallax Umbgrove, 1925. A lectotype is selected for the latter species. A new cerioid species, Columactinastraea anthonii sp. nov., is recorded from the middle part of the Meerssen Member (Maastricht Formation) at the ENCI Quarry, Zuid Lim- burg, The Netherlands. It is well-preserved and differs from other Columactinastraea species mainly by the relatively large diameter of its lumen. Contents Introduction .................................................................................................................................................. 185 Preservation and association ............................................................................................................... -
Papers in Press
Papers in Press “Papers in Press” includes peer-reviewed, accepted manuscripts of research articles, reviews, and short notes to be published in Paleontological Research. They have not yet been copy edited and/or formatted in the publication style of Paleontological Research. As soon as they are printed, they will be removed from this website. Please note they can be cited using the year of online publication and the DOI, as follows: Humblet, M. and Iryu, Y. 2014: Pleistocene coral assemblages on Irabu-jima, South Ryukyu Islands, Japan. Paleontological Research, doi: 10.2517/2014PR020. doi:10.2517/2017PR023 Missourian (Kasimovian, Late Pennsylvanian) conodonts from limestone boulders, Mizuboradani Valley, Gifu Prefecture, central Japan AcceptedTAKUMI MAEKAWA1, TOSHIFUMI KOMATSU2, GENGO TANAKA3, MARK WILLIAMS4, CHRISTOPHER P. STOCKER4, MASATOSHI OKURA5 and AKIHIRO UMAYAHARA6 1Center for Water Cycle, Marine Environment, and Disaster Management, Marine Science Laboratory, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 850-8555, Japan (e-mail: [email protected]) 2Faculty of Advanced Science and Technology, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 860-8555, Japan ([email protected]) 3Institute of Liberal Arts and Science, Kanazawamanuscript University, Kakuma, Kanazawa, Ishikawa 920-1192, Japan (e-mail: [email protected]) 4School of Geography, Geology and Environment, University of Leicester, University Road, Leicester, LEI 7RH, UK ([email protected]) 5Naka 86, Minamiyama-cho, Konan, Aichi 483-8155, Japan 6Graduate School of Science and Technology, Kumamoto University, 2-39-1 Kurokami, Chuo-ku, Kumamoto 860-8555, Japan Abstract. Two Late Pennsylvanian conodont species, Gondolella sublanceolata Gunnell and Idiognathodus sulciferus Gunnell, were extracted from limestone boulders in the Mizuboradani Valley, Fukuji district, central Japan. -
First Occurrence of Ellisonia, Gondolella and Ubinates (Conodonts) in Itaituba Formation, Pennsylvanian of Amazonas Basin, Brazil
6(2):56-62, jul/dez 2010 © Copyright 2010 by Unisinos - doi: 10.4013/gaea.2010.62.01 First occurrence of Ellisonia, Gondolella and Ubinates (Conodonts) in Itaituba Formation, Pennsylvanian of Amazonas Basin, Brazil Sara Nascimento, Valesca Brasil Lemos Universidade Federal do Rio Grande do Sul. Av. Bento Gonçalves, 9500, Prédio 43.127, sala 211, 91501-470, Porto Alegre, RS, Brasil. [email protected], [email protected] Ana Karina Scomazzon Universidade Federal de Pelotas. Rua Domingos Rodrigues, 2, 96010-440, Pelotas, RS, Brasil. [email protected] Nilo Siguehiko Matsuda PETROBRAS/E&P-EXP/GEO/ES. Av. Chile, 330, Edifício Ventura, 13º andar, 20031-170, Rio de Janeiro, RJ, Brasil. [email protected] Cristiane Pakulski da Silva Universidade Federal do Rio Grande do Sul. Av. Bento Gonçalves, 9500. Prédio 43.127, sala 211, 91501-470, Porto Alegre, RS, Brasil. [email protected] ABSTRACT This paper analyzes and describes a fi rst occurrence of the conodonts Ellisonia, Gondolella and Ubinates in Amazonas Basin, North of Brazil. The recovered material comes from two outcrops along the Tapajos River and from a limestone quarry of Itaituba Formation, whose levels are in- cluded in the Itaituba Formation, with a Pennsylvanian age. Those conodonts are relevant paleoecological indicators of water depth, salinity and environmental energy and have implications in the Late Carboniferous to Triassic biostratigraphy. The fossil remains represent M and S conodont elements, associated to Pa elements of the Idiognathodus, Idiognathoides, Neognathodus, Adetognathus, Hindeodus and Diplognathodus genus. Key words: conodonts, Amazonas Basin, Itaituba Formation, Pennsylvanian. RESUMO PRIMEIRA OCORRÊNCIA DOS GÊNEROS ELLISONIA, GONDOLELLA E UBINATES (CONODONTS) PARA A FORMAÇÃO ITAITUBA, PENSILVANIANO DA BACIA DO AMAZONAS, BRASIL. -
USGS Open-File Report 2006–1068
Condont and Radiolarian Data from the De Long Mountains Quadrangle and Adjacent Areas, Northern Alaska By Julie A. Dumoulin,1 Anita G. Harris,2 Charles D. Blome,3 and Lorne E. Young4 Open-File Report 2006–1068 2006 Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY 1 U.S. Geological Survey, 4200 University Drive, Anchorage, AK 99508. 2 U.S. Geological Survey (retired), 1523 E. Hillsboro Blvd., Apt. 1031, Deerfield Beach, FL 33441. 3 U.S. Geological Survey, Box 25046, MS 973, Denver, CO 80225. 4 12015 North Fairwood Drive, Spokane, WA 99218. CONTENTS INTRODUCTION 1 DATA SOURCES 2 STRATIGRAPHIC AND STRUCTURAL SETTING 4 KUNA FORMATION AND RELATED ROCKS 6 IKALUKROK UNIT 7 Lithofacies 7 Fossil Data 8 KIVALINA UNIT 10 Lithofacies 10 Fossil Data 11 KUNA FORMATION (KEY CREEK PLATE) 12 Lithofacies 13 Fossil Data 14 DEEP-WATER FACIES OF THE LISBURNE GROUP IN THE PICNIC CREEK ALLOCHTON 14 Lithofacies 15 Fossil Data 16 OTHER DEEP-WATER STRATA OF THE LISBURNE GROUP 17 Lithofacies 17 Fossil Data 18 KOGRUK AND UTUKOK FORMATIONS AND RELATED ROCKS 18 KOGRUK FORMATION 20 Lithofacies 21 Wolverine Creek plate, EMA 21 Key Creek plate, EMA 21 KRA 22 Fossil Data 23 Wolverine Creek plate, EMA 24 Key Creek plate, EMA 25 KRA 25 UTUKOK FORMATION AND RELATED ROCKS 27 Lithofacies 27 Wolverine Creek plate, EMA 27 Key Creek plate, EMA 27 KRA 28 Fossil Data 29 Wolverine Creek plate, EMA 29 Key Creek plate, EMA 30 KRA 30 ETIVLUK GROUP AND OKPIKRUAK FORMATION 31 ETIVLUK GROUP 31 Siksikpuk Formation 31 Otuk Formation 33 OKPIKRUAK FORMATION 36 NUKA FORMATION AND RELATED ROCKS 37 ENDICOTT GROUP 38 DEVONIAN CARBONATE ROCKS 39 THERMAL DATA 42 ACKNOWLEDGMENTS 44 REFERENCES 44 FIGURES Figure 1. -
Distribution of Coral-Microbialite Reefs Along the French Jura Platform During the Bimammatum Zone (Oxfordian, Late Jurassic)
Distribution of coral-microbialite reefs along the French Jura platform during the Bimammatum Zone (Oxfordian, Late Jurassic) Nicolas olivier During the Late Jurassic, the Jura platform was the site of major carbonate production involving various reef building components, particularly corals and microbialites. The existence of a detailed stratigraphic framework for the French Jura sedimentary succession during the Late Oxfordian–Early Kimmeridgian interval makes it possible to analyse the nature and distribution of these reefs within a high-resolution time frame, the Bimammatum Zone. Even though these reefs developed in a wide range of settings, their development was never optimal, indicating the presence of limiting factors. When the supply of terrigenous material was lower, the inner platform was characterized by strong carbonate production, with the development of a large ooidal shoal complex including ten-meter scale coral-microbialite patch reefs. The large size and high-density skeletal structure of some colonies indicates a favourable environment for coral and reef development (shallow, agitated, well-oxygenated waters with high light levels), despite the coral assemblage being poorly diversified and characterized by a mixed photo-heterotrophic association. The autocyclic character of the sedimentary system (i.e. major migrations of the ooidal dunes after big storm events) recurrently interrupted reef development. When the French Jura platform was subject to significant terrigenous input, the coral assemblages became well-diversified and characterized by mixed or heterotrophic-dominated associations. In the shallow and proximal areas of the inner ramp, limited available space imposed strong constraints on the reef growth, which only developed biostromal morphologies. Along the mid ramp, the reefs were composed firstly of plurimetric bioherms, then metric patches and finally coral meadows, highlighting the inversely proportional relationship of reef size to water depth. -
Choice of Conodont Idiognathodus Simulator (Sensu Stricto) As The
319 by Philip H. Heckel1, Aleksandr S. Alekseev2, James E. Barrick3, Darwin R. Boardman4, Natalya V. Goreva5, Tatiana N. Isakova6, Tamara I. Nemyrovska7, Katsumi Ueno8, Elisa Villa9 and David M. Work10 Choice of conodont Idiognathodus simulator (sensu stricto) as the event marker for the base of the global Gzhelian Stage (Upper Pennsylvanian Series, Carboniferous System) 1 Department of Geoscience, University of Iowa, Iowa City, Iowa 52242, USA. Email: [email protected] 2 Department of Paleontology, Geology Faculty, Moscow State University, 119992 Moscow, Russia. Email: [email protected] 3 Department of Geosciences, Texas Tech University, Lubbock, Texas 79409, USA. Email: [email protected] 4 School of Geology, Oklahoma State University, Stillwater, Oklahoma 74078, USA. Email: [email protected] 5 Geological Institute, Russian Academy of Sciences, Pyzhevsky per. 7, 110017 Moscow, Russia. Email: [email protected] 6 Geological Institute, Russian Academy of Sciences, Pyzhevsky per. 7, 110017 Moscow, Russia. Email: [email protected] 7 Institute of Geological Sciences, National Academy of Sciences of Ukraine, O. Gonchar Str. 55b, 01054 Kiev, Ukraine. Email: [email protected] 8 Department of Earth System Science, Faculty of Science, Fukuoka University, Fukuoka 814-0180, Japan. Email: [email protected] 9 Department of Geology, University of Oviedo, Arias de Velasco s/n, 33005 Oviedo, Spain. Email: [email protected] 10 Maine State Museum, 83 State House Station, Augusta, Maine 04333, USA. Email: [email protected] We propose that the level at which the conodont species provinciality of the fusulinid faunas, conodonts are being utilized to Idiognathodus simulator (Ellison 1941) (sensu stricto) mark the events that will be used to define the global stages within the Pennsylvanian, because some of their species are more wide- first appears be selected to mark the base of the Gzhe- spread globally than those of the fusulinids.