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Or Early Callovian) Ammonites from Alaska and Montana
Jurassic (Bathonian or Early Callovian) Ammonites From Alaska and Montana By RALPH W. IMLAY SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 374-C Descr$tions and illustrations of ctphalopods of possible late Middle Jurasric (Bathonian) age UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page C- 1 Age of the faunas-Continued C- 1 Callovian versus Bathonian in Greenland- - - - _ - - _ - - C-2 Callovian versus Bathonian in Alaska and Montana- -- - Stratigraphic summary- __ --______ _ - - - -- - ---.- -- -.- - - C-2 Paleogeographic considerations- - -_-- -- ---- ---- Cook Inlet region, Alaska -______--------.-.--..--c-2 Summation of the evidence- - - _._ _ - _ _ - - - - - - - - - - - - Iniskin Peninsula-_-_______----.--------~.--C-2 Comparisons with other faunas---------___----------- Peninsula north of Chinitna Bay----- __._ _ _._ - C-3 \Vestern interior of Canada- - - -- -- -____------- --- Talkeetna Mountains ----___-_ - - -- ---- - - -- - -- C-3 Arctic region-_-_---___-_----------------------- Western Montana- - -----__-----------------.---C-5 other regions--__-__-____----------------------- Rocky Mountain front north of the Sun River- (2-5 Geographic distribution ___-___ --- - ---------- ------ -- - Drummond area--- ---_____ _--- -- -.-- ---- -- - C-10 Summary of results- --_-____-_----_---_-_----------- Age ofthe faunas-----------_----------------------- GI0 Systematic descriptions--_ _ _ - _ - - - - - - - - - - - - - - - - - - - - - - - Evidence from Alaska---____________--------------C-10 Literature cited _-_-_---______----------------------- Evidence from Montana --_-_____ --- - - -- .--- --- - - C-12 Index---__--___-_-_------------------------------- ILLUSTRATIONS [Plates 1-3 follow index] PLATE 1. Holcophylloceras, Oecotraustes (Paroecotraustes) ?, and Arctocephalites (Cranocephalites). 2. -
The Middle Jurassic of Western and Northern Europe: Its Subdivisions, Geochronology and Correlations
The Middle Jurassic of western and northern Europe: its subdivisions, geochronology and correlations John H. Callomon The palaeogeographic settings of Denmark and East Greenland during the Middle Jurassic are outlined. They lay in the widespread epicontinental seas that covered much of Europe in the post-Triassic transgression. It was a period of continuing eustatic sea-level rise, with only distant connections to world oceans: to the Pacific, via the narrow Viking Straits between Greenland and Norway and hence the arctic Boreal Sea to the north; and to the subtropical Tethys, via some 1200 km of shelf-seas to the south. The sedimentary history of the region was strongly influenced by two factors: tectonism and climate. Two modes of tectonic movement governed basinal evolution: crustal extension lead- ing to subsidence through rifting, such as in the Viking and Central Grabens of the North Sea; and subcrustal thermal upwelling, leading to domal uplift and the partition of marine basins through emergent physical barriers, as exemplified by the Central North Sea Dome with its associated volcanics. The climatic gradient across the 30º of temperate latitude spanned by the European seas governed biotic diversity and biogeography, finding expression in rock-forming biogenic carbonates that dominate sediments in the south and give way to largely siliciclastic sediments in the north. Geochronology of unrivalled finesse is provided by standard chronostratigraphy based on the biostratigraphy of ammonites. The Middle Jurassic saw the onset of considerable bioprovincial endemisms in these guide-fossils, making it necessary to construct parallel standard zonations for Boreal, Subboreal or NW European and Submediterranean Provinces, of which the NW European zonation provides the primary international standard. -
New and Poorly Known Perisphinctoidea (Ammonitina) from the Upper Tithonian of Le Chouet (Drôme, SE France)
Volumina Jurassica, 2014, Xii (1): 113–128 New and poorly known Perisphinctoidea (Ammonitina) from the Upper Tithonian of Le Chouet (Drôme, SE France) Luc G. BULOT1, Camille FRAU2, William A.P. WIMBLEDON3 Key words: Ammonoidea, Ataxioceratidae, Himalayitidae, Neocomitidae, Upper Tithonian, Le Chouet, South-East France. Abstract. The aim of this paper is to document the ammonite fauna of the upper part of the Late Tithonian collected at the key section of Le Chouet (Drôme, SE France). Emphasis is laid on new and poorly known Ataxioceratidae, Himalayitidae and Neocomitidae from the upper part of the Tithonian. Among the Ataxioceratidae, a new account on the taxonomy and relationship between Paraulacosphinctes Schindewolf and Moravisphinctes Tavera is presented. Regarding the Himalayitidae, the range and content of Micracanthoceras Spath is discussed and two new genera are introduced: Ardesciella gen. nov., for a group of Mediterranean ammonites that is homoeomorphic with the Andean genus Corongoceras Spath, and Pratumidiscus gen. nov. for a specimen that shows morphological similarities with the Boreal genera Riasanites Spath and Riasanella Mitta. Finally, the occurrence of Neocomitidae in the uppermost Tithonian is documented by the presence of the reputedly Berriasian genera Busnardoiceras Tavera and Pseudargentiniceras Spath. INTRODUCTION known Perisphinctoidea from the Upper Tithonian of this reference section. Additional data on the Himalayitidae in- The unique character of the ammonite fauna of Le Chouet cluding the description and discussion of Boughdiriella (near Les Près, Drôme, France) (Fig. 1) has already been chouetensis gen. nov. sp. nov. are to be published elsewhere outlined by Le Hégarat (1973), but, so far, only a handful of (Frau et al., 2014). -
Suture with Pointed Flank Lobe and ... -.: Palaeontologia Polonica
210 JERZY DZIK Genus Posttornoceras Wedekind, 1910 Type species: Posttornoceras balvei Wedekind, 1910 from the mid Famennian Platyclymenia annulata Zone of the Rhenisch Slate Mountains. Diagnosis. — Suture with pointed flank lobe and angular or pointed dorsolateral lobe. Remarks. — Becker (1993b) proposed Exotornoceras for the most primitive members of the lineage with a relatively shallow dorsolateral lobe. The difference seems too minor and continuity too apparent to make this taxonomical subdivision practical. Becker (2002) suggested that this lineage was rooted in Gundolficeras, which is supported by the data from the Holy Cross Mountains. The suture of Posttornoceras is similar to that of Sporadoceras, but these end−members of unrelated lin− eages differ rather significantly in the geometry of the septum (Becker 1993b; Korn 1999). In Posttornoceras the parts of the whorl in contact with the preceding whorl are much less extensive, the dorsolateral saddle is much shorter and of a somewhat angular appearance. This is obviously a reflection of the difference in the whorl expansion rate between the tornoceratids and cheiloceratids. Posttornoceras superstes (Wedekind, 1908) (Figs 154A and 159) Type horizon and locality: Early Famennian at Nehden−Schurbusch, Rhenish Slate Mountains (Becker 1993b). Diagnosis. — Suture with pointed tip of the flank lobe and roundedly angulate dorsolateral lobe. Remarks.—Gephyroceras niedzwiedzkii of Dybczyński (1913) from Sieklucki’s brickpit was repre− sented by a specimen (probably lost) significantly larger than those described by Becker (1993b). The differ− ence in proportions of suture seem to result from this ontogenetic difference, that is mostly from increase of the whorl compression with growth. Distribution. — Reworked at Sieklucki’s brickpit in Kielce. -
Paleontological Resources at Grand Teton National Park, Northwestern Wyoming Vincent L
University of Wyoming National Park Service Research Center Annual Report Volume 22 22nd Annual Report, 1998 Article 7 1-1-1998 Paleontological Resources at Grand Teton National Park, Northwestern Wyoming Vincent L. Santucci National Park Service William P. Wall Georgia College and State University Follow this and additional works at: http://repository.uwyo.edu/uwnpsrc_reports Recommended Citation Santucci, Vincent L. and Wall, William P. (1998) "Paleontological Resources at Grand Teton National Park, Northwestern Wyoming," University of Wyoming National Park Service Research Center Annual Report: Vol. 22 , Article 7. Available at: http://repository.uwyo.edu/uwnpsrc_reports/vol22/iss1/7 This Grand Teton National Park Report is brought to you for free and open access by Wyoming Scholars Repository. It has been accepted for inclusion in University of Wyoming National Park Service Research Center Annual Report by an authorized editor of Wyoming Scholars Repository. For more information, please contact [email protected]. Santucci and Wall: Paleontological Resources at Grand Teton National Park, Northwest PALEONTOLOGICAL RESOURCES AT GRAND TETON NATIONAL PARK, NORTHWESTERN WYOMING + VINCENT L. SANTUCCI+ NATIONAL PARK SERVICE KEMMERER + WY WILLIAM P. WALL+ DEPARTMENT OF BIOLOGY GEORGIA COLLEGE AND STATE UNIVERSITY MILLEDGEVILLE + GA + ABSTRACT landscape, and though the last great ice masses melted 15 ,000 years ago, some re-established small Paleontological resources occur throughout glaciers still exist. the formations exposed in Grand Teton National Park. A comprehensive paleontological survey has This report provides a preliminary not been attempted previously at Grand Teton assessment of paleontological resources identified at National Park. Preliminary paleontologic resource Grand Teton National Park. data is given in this report in order to establish baseline data. -
Text of Draft
Reconnaissance bedrock geologic map for the northern Alaska Peninsula area, southwest Alaska Including the Dillingham, Iliamna, Lake Clark, Taylor Mountains and the western part of the Kenai and Seldovia 1:250,000-scale quadrangles Compiled by Frederic H. Wilson, Robert B. Blodgett, Charles D. Blomé, Solmaz Mohadjer, Cindi C. Preller, Edward P. Klimasauskas, Bruce M. Gamble, and Warren L. Coonrad DISCLAIMER This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. This World-Wide-Web publication was prepared by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed in this report, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. Although all data and software published on this Web-site have been used by the USGS, no warranty, expressed or implied, is made by the USGS as to the accuracy of the data and related materials and (or) the functioning of the software. The act of distribution shall not constitute any such warranty, and no responsibility is assumed by the USGS in the use of this data, software, or related materials. -
A Review of the Classification of Jurassic Aspidoceratid Ammonites – the Superfamily Aspidoceratoidea
VOLUMINA JURASSICA, 2020, XVIII (1): 47–52 DOI: 10.7306/VJ.18.4 A review of the classification of Jurassic aspidoceratid ammonites – the Superfamily Aspidoceratoidea Horacio PARENT1, Günter SCHWEIGERT2, Armin SCHERZINGER3 Key words: Superfamily Aspidoceratoidea, Aspidoceratidae, Epipeltoceratinae emended, Peltoceratidae, Gregoryceratinae nov. subfam. Abstract. The aspidoceratid ammonites have been traditionally included in the superfamily Perisphinctoidea. However, the basis of this is unclear for they bear unique combinations of characters unknown in typical perisphinctoids: (1) the distinct laevaptychus, (2) stout shells with high growth rate of the whorl section area, (3) prominent ornamentation with tubercles, spines and strong growth lines running in parallel over strong ribs, (4) lack of constrictions, (5) short to very short bodychamber, and (6) sexual dimorphism characterized by minia- turized microconchs and small-sized macroconchs besides the larger ones, including changes of sex during ontogeny in many cases. Considering the uniqueness of these characters we propose herein to raise the family Aspidoceratidae to the rank of a superfamily Aspi- doceratoidea, ranging from the earliest Late Callovian to the Early Berriasian Jacobi Zone. The new superfamily includes two families, Aspidoceratidae (Aspidoceratinae, Euaspidoceratinae, Epipeltoceratinae and Hybonoticeratinae), and Peltoceratidae (Peltoceratinae and Gregoryceratinae nov. subfam.). The highly differentiated features of the aspidoceratoids indicate that their life-histories -
First Record of Non-Mineralized Cephalopod Jaws and Arm Hooks
Klug et al. Swiss J Palaeontol (2020) 139:9 https://doi.org/10.1186/s13358-020-00210-y Swiss Journal of Palaeontology RESEARCH ARTICLE Open Access First record of non-mineralized cephalopod jaws and arm hooks from the latest Cretaceous of Eurytania, Greece Christian Klug1* , Donald Davesne2,3, Dirk Fuchs4 and Thodoris Argyriou5 Abstract Due to the lower fossilization potential of chitin, non-mineralized cephalopod jaws and arm hooks are much more rarely preserved as fossils than the calcitic lower jaws of ammonites or the calcitized jaw apparatuses of nautilids. Here, we report such non-mineralized fossil jaws and arm hooks from pelagic marly limestones of continental Greece. Two of the specimens lie on the same slab and are assigned to the Ammonitina; they represent upper jaws of the aptychus type, which is corroborated by fnds of aptychi. Additionally, one intermediate type and one anaptychus type are documented here. The morphology of all ammonite jaws suggest a desmoceratoid afnity. The other jaws are identifed as coleoid jaws. They share the overall U-shape and proportions of the outer and inner lamellae with Jurassic lower jaws of Trachyteuthis (Teudopseina). We also document the frst belemnoid arm hooks from the Tethyan Maastrichtian. The fossils described here document the presence of a typical Mesozoic cephalopod assemblage until the end of the Cretaceous in the eastern Tethys. Keywords: Cephalopoda, Ammonoidea, Desmoceratoidea, Coleoidea, Maastrichtian, Taphonomy Introduction as jaws, arm hooks, and radulae are occasionally found Fossil cephalopods are mainly known from preserved (Matern 1931; Mapes 1987; Fuchs 2006a; Landman et al. mineralized parts such as aragonitic phragmocones 2010; Kruta et al. -
ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0016–7800 ISBN 3-85316-14-X Band 57 S. 167–180 Wien, Februar 2002 Cephalopods – Present and Past Editors: H. Summesberger, K. Histon & A. Daurer Morphometric Analyses and Taxonomy of Oxyconic Goniatites (Paratornoceratinae n. subfam.) from the Early Famennian of the Tafilalt (Anti-Atlas, Morocco) VOLKER EBBIGHAUSEN, RALPH THOMAS BECKER & JÜRGEN BOCKWINKEL*) 13 Text-Figures and 1 Table A contribution to IGCP 421 Morocco Upper Devonian Ammonoids Morphometry Taxonomy Contents Zusammenfassung ...................................................................................................... 167 Abstract ................................................................................................................. 167 1. Introduction ............................................................................................................. 169 2. Locality and Methods .................................................................................................... 169 3. Morphometric Analyses of Dar Kaoua Paratornoceratinae ................................................................. 170 3.1. Size Distribution .................................................................................................... 170 3.2. Shell Parameters ................................................................................................... 172 4. Systematics ............................................................................................................ -
Revisión De Los Ammonoideos Del Lías Español Depositados En El Museo Geominero (ITGE, Madrid)
Boletín Geológico y Minero. Vol. 107-2 Año 1996 (103-124) El Instituto Tecnológico Geominero de España hace presente que las opiniones y hechos con signados en sus publicaciones son de la exclusi GEOLOGIA va responsabilidad de los autores de los trabajos. Revisión de los Ammonoideos del Lías español depositados en el Museo Geominero (ITGE, Madrid). Por J. BERNAD (*) y G. MARTINEZ. (**) RESUMEN Se revisan desde el punto de vista taxonómico, los fósiles de ammonoideos correspondientes al Lías español que se encuentran depositados en el Museo Geominero. La colección está compuesta por ejemplares procedentes de 67 localida des españolas, pertenecientes a colecciones de diferentes autores. Se identifican los ordenes Phylloceratina, Lytoceratina y Ammonitina, las familias Phylloceratidae, Echioceratidae, eoderoceratidae, Liparoceratidae, Amaltheidae, Dactyliocerati Los derechos de propiedad de los trabajos dae, Hildoceratidae y Hammatoceratidae y las subfamilias Xipheroceratinae, Arieticeratinae, Harpoceratinae, Hildocerati publicados en esta obra fueron cedidos por nae, Grammoceratinae, Phymatoceratinae y Hammatoceratinae correspondientes a los pisos Sinemuriense, Pliensbachien los autores al Instituto Tecnológico Geomi se y Toarciense. nero de España Oueda hecho el depósito que marca la ley. Palabras clave: Ammonoidea, Taxonomía, Lías, España, Museo Geominero. ABSTRACT The Spanish Liassic ammonoidea fossil collections of the Geominero Museum is revised under a taxonomic point of view. The collection includes specimens from 67 Spanish -
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: 2010 Band/Volume: 65 Autor(en)/Author(s): Mandl Gerhard W., Dulai Alfred, Schlögl Jan, Siblik M., Szabo Janos, Szent-Istvanyi Szentistvanyi Gyula, Vörös Attila Artikel/Article: First Results on Stratigraphy and Faunal Content of the Jurassic between Bad Mitterndorf and Toplitzsee (Salzkammergut, Austria) 77-134 ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0378-0864 ISBN 978-3-85316-058-9 Band 65 S. 77–134 Wien, 10. 11. 2010 Fifty Years of Geological Cooperation between Austria, the Czech Republic and the Slovak Republic First Results on Stratigraphy and Faunal Content of the Jurassic between Bad Mitterndorf and Toplitzsee (Salzkammergut, Austria) Gerhard W. Mandl1, alFréd dulai2, jan schlöGl3, MiloŠ siblík4, jános szabó2, istván szente5 & attila vörös2 4 Text-Figures, 17 Plates Österreichische Karte 1:50.000 Northern Calcareous Alps Blatt 97 Bad Mitterndorf Jurassic Olistolith Ammonoidea Brachiopoda Gastropoda Bivalvia Contents Zusammenfassung . 77 Abstract . 78 Introduction . 78 Geological Setting . 78 Stratigraphy . 80 Upper Triassic . 80 Lower Jurassic . 80 Upper Jurassic . 81 Remarks on the Fauna of Olistolith Plk 1 . 84 Ammonoidea (J. Schlögl) . 84 Brachiopoda (A. Dulai) . 85 Gastropoda (J. Szabó) . 85 Bivalvia (I. Szente) . 87 Fossil Sites and Faunal Content . 88 Plates . 98 Conclusions . 132 Acknowledgements . 132 References . 133 Erste Ergebnisse zu Stratigraphie und Faunen-Inhalt der Jura-Gesteine zwischen Bad Mitterndorf und Toplitzsee (Salzkammergut, Österreich) Zusammenfassung Die südwestlichen Ausläufer des Toten Gebirges zeigen eine Schichtfolge aus rhätischem Dachsteinkalk und jurassischen Beckensedimenten, die bis in das Kimmeridgium reichen. -
Significance for International Correlation of the Perapertú Formation in Northern Palencia, Cantabrian Mountains
PERAPERTÚ FM, CANTABRIAN MTS. GONIATITES 127 SIGNIFICANCE FOR INTERNATIONAL CORRELATION OF THE PERAPERTÚ FORMATION IN NORTHERN PALENCIA, CANTABRIAN MOUNTAINS. TECTONIC/STRATIGRAPHIC CONTEXT AND DESCRIPTION OF MISSISSIPPIAN AND UPPER BASHKIRIAN GONIATITES Jürgen KULLMANN1, Robert H. WAGNER2 and Cornelis F. WINKLER PRINS3 1 Institut für Geowissenschaften der Universität Tübingen, Sigwartstraβe 10, D 72076 Tübingen, Germany; e-mail: [email protected] 2 Corresponding author: Centro Paleobotánico, Jardín Botánico de Córdoba, Avda. de Linneo, s/n, E 1�00������������ Córdoba �Spain����������; e-mail: [email protected] 3 Nationaal Natuurhistorisch Museum, Postbus 9517, NL 2300 RA Leiden, The Netherlands; e-mail: [email protected] Kullmann, J., Wagner R. H. & Winkler Prins, C.F. 2007. Significance for international correlation of the Pera- pertú Formation in northern Palencia, Cantabrian Mountains. Tectonic/stratigraphic context and description of Mississippian and Upper Bashkirian goniatites. �������������������������������������������������������������El significado de la Formación Perapertú para la correlación internacional, norte de Palencia, Cordillera Cantábrica. Contexto tectónico/estratigráfico y descripción de go- niatítidos misisípicos y del Bashkiriense Superior.] Revista Española de Paleontología, 22 �2�, 127-1�5. ISSN 0213-6937. ABSTRACT Small ammonoid assemblages are recorded from the Perapertú Formation in northern Palencia. This is a mud- stone unit with local platform limestones characterised by carbonate debris flows