Ammonite Diversity on the Jurassic
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
2015 Annual Spring Meeting Macey Center New Mexico Tech Socorro, NM
New Mexico Geological Society Proceedings Volume 2015 Annual Spring Meeting Macey Center New Mexico Tech Socorro, NM NEW MEXICO GEOLOGICAL SOCIETY 2015 SPRING MEETING Friday, April 24, 2015 Macey Center NM Tech Campus Socorro, New Mexico 87801 NMGS EXECUTIVE COMMITTEE President: Mary Dowse Vice President: David Ennis Treasurer: Matthew Heizler Secretary: Susan Lucas Kamat Past President: Virginia McLemore 2015 SPRING MEETING COMMITTEE General Chair: Matthew Heizler Technical Program Chair: Peter Fawcett Registration Chair: Connie Apache ON-SITE REGISTRATION Connie Apache WEB SUPPORT Adam Read ORAL SESSION CHAIRS Peter Fawcett, Matt Zimmerer, Lewis Land, Spencer Lucas, Matt Heizler Session 1: Theme Session - Session 2: Volcanology and Paleoclimate: Is the Past the Key to Proterozoic Tectonics: the Future? Auditorium: 8:45 AM - 10:45 AM Galena Room: 8:45 AM - 10:45 AM Chair: Peter Fawcett Chair: Matthew Zimmerer GLOBAL ICE AGES, REGIONAL TECTONISM U-PB GEOCHRONOLOGY OF ASH FALL TUFFS AND LATE PALEOZOIC SEDIMENTATION IN IN THE MCRAE FORMATION (UPPER NEW MEXICO CRETACEOUS), SOUTH-CENTRAL NEW MEXICO — Spencer G. Lucas and Karl Krainer — Greg Mack, Jeffrey M. Amato, and Garland 8:45 AM - 9:00 AM R. Upchurch 8:45 AM - 9:00 AM URANIUM ISOTOPE EVIDENCE FOR PERVASIVE TIMING, GEOCHEMISTRY, AND DISTRIBUTION MARINE ANOXIA DURING THE LATE OF MAGMATISM IN THE RIO GRANDE RIFT ORDOVICIAN MASS EXTINCTION. — Rediet Abera, Brad Sion, Jolante van Wijk, — Rickey W Bartlett, Maya Elrick, Yemane Gary Axen, Dan Koning, Richard Chamberlin, Asmerom, Viorel Atudorei, and Victor Polyak Evan Gragg, Kyle Murray, and Jeff Dobbins 9:00 AM - 9:15 AM 9:00 AM - 9:15 AM FAUNAL AND FLORAL DYNAMICS DURING THE N-S EXTENSION AND BIMODAL MAGMATISM EARLY PALEOCENE: THE RECORD FROM THE DURING EARLY RIO GRANDE RIFTING: SAN JUAN BASIN, NEW MEXICO INSIGHTS FROM E-W STRIKING DIKES AT — Thomas E. -
Waterloo Bay, Larne, Northern Ireland
Michael J. Simms Andrew J. Jeram, Waterloo Bay, Larne, Northern Ireland: Department of Geology, Mullaghdubh House, Ulster Museum, 27 Gobbins Path, Botanic Gardens, Islandmagee, The ammonites of the earliest Jurassic Belfast BT9 5AB, Co. Antrim BT40 3SP, Northern Ireland. Northern Ireland. [email protected] [email protected] Ammonites are a conspicuous element of the earliest 24 34 Jurassic macrofauna at this site. Most taxa are represented by at least some 3-dimensional material, preserved either in pyrite or early diagenetic carbonate 33g concretions. 23 33f Caloceras sp. Selected specimens are illustrated here at actual size, unless indicated otherwise. 33e top Bed 27 22 The strata in the picture to the left encompass the top of Psiloceras cf. plicatulum Caloceras johnstoni top Bed 26 the ‘Pre-planorbis Beds’, the erugatum Horizon (Bed 24) and the stratigraphic range of Neophyllites (beds 25 33d to 27). 21 top Bed 25 The site has significant potential for designation as a Bed 24 nodules Global Stratotype Section and Point for the base of the 33c Jurassic System. In addition, this part of the foreshore 20 top Bed 23 would make an ideal stratotype location for the erugatum, imitans and antecedens biohorizons, for which surface stratotypes have yet to be designated. Psiloceras plicatulum 19 33b Psiloceras plicatulum A diverse macro- and microfauna Specimen from lower 33a part of Bed 25 (ammonites, bivalves, gastropods, 18 Psiloceras cf. sampsoni (enlarged x3) This highly evolute example is the echinoids, crinoids, trace-fossils and 32 stratigraphically highest example of occasional vertebrates) is present in the sampsoni recovered from the site. -
GSSP) for the Base of the Cenomanian Stage, Mont Risou, Hautes-Alpes, France
21 by W.J. Kennedy1, A.S. Gale2, J.A. Lees3, and M. Caron4 The Global Boundary Stratotype Section and Point (GSSP) for the base of the Cenomanian Stage, Mont Risou, Hautes-Alpes, France 1 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW, U.K. 2 Department of Palaeontology, The Natural History Museum, Cromwell Road, London SW7 5BP, U.K. and School of Earth and Environ- mental Sciences, University of Greenwich, Chatham Maritime Campus, Chatham, Kent ME4 4AW, U.K. 3 Research School of Geological and Geophysical Sciences, Birkbeck College and University College London, Gower Street, London WC1E 6BT, U.K. 4 Institut de Géologie, Université de Fribourg, CH-1700 Fribourg, Switzerland. Following the unanimous recommendation of the Inter- Grès Vert Supérieur etc., and taking the name from Touraine national Commission on Stratigraphy, the Global (Roman Turonia). Five years later, he realized that two distinct ammonite and rudist faunas were present, and he restricted the term boundary Stratotype Section and Point (GSSP) for the Turonian to beds corresponding to his third zone of rudists, yielding base of the Cenomanian Stage is defined at a level 36 “Ammonites lewesiensis, peramplus, Vielbancii, Woolgari, Fleuri- metres below the top of the Marnes Bleues Formation, a ausianus, Deverianus etc.”, “le plus beau type côtier étant très prononcé dans toute la Touraine, et nous donnerons à la partie level that corresponds to the the first appearance of the inférieure le nom d’étage Cénomanien, le Mans (Cenomanum), en planktonic foraminiferan Rotalipora globotruncanoides montrant à la fois le type sous-marin” (d'Orbigny, 1848–1851, p. -
Jurassic Coast Fossil Acquisition Strategy Consultation Report
Jurassic Coast World Heritage Site Fossil acquisition strategy for the Jurassic Coast- Consultation Document A study to identify ways to safeguard important scientific fossils from the Dorset and East Devon Coast World Heritage Site – prepared by Weightman Associates and Hidden Horizons on behalf of the Jurassic Coast Team, Dorset County Council p Jurassic Coast World Heritage Site Fossil acquisition strategy for the Jurassic Coast CONTENTS 1. INTRODUCTION…………………………………………………………………………………2 2. BACKGROUND…………………………………………………………………………………..2 3. SPECIFIC ISSUES………………………………………..……………………………………….5 4. CONSULTATION WITH STAKEHOLDERS………………………………………………5 5. DISCUSSION……………………………………………………………………………………..11 6. CONCLUSIONS…………………………..……………………………………………………..14 7. ACKNOWLEDGEMENTS…………………………………………………………………....14 8. APPENDIX..……………………………………………………………………………………...14 1 JURASSIC COAST FOSSIL ACQUISITION STRATEGY 1. Introduction The aim of this project is to identify ways to safeguard important scientific fossils from the Dorset and East Devon Coast World Heritage Site. The identification of placements in accredited museums would enable intellectual access for scientific study and education. Two consulting companies Weightman Associates and Hidden Horizons have been commissioned to undertake this Project. Weightman Associates is a partnership of Gill Weightman and Alan Weightman; they have been in partnership for twenty years working on museum and geology projects. Hidden Horizons Ltd is a museum and heritage consultancy formed in 2013 by Will Watts. When UNESCO granted World Heritage status to the Dorset and East Devon Coast in 2001 it recognised the importance of the Site’s geology and geomorphology. The Jurassic Coast Management Plan 2014-2019 has as one of its aims to “To Conserve and enhance the Site and its setting for science, education and public enjoyment” and the Plan states that a critical success factor is “An increase in the number of scientifically important fossils found along the site that are acquired by or loaned back to local accredited museums”. -
Gallois, R. W. 2005. Proceedings of the Geologists' Association, Vol
CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive Gallois, R. W. 2005. Proceedings of the Geologists’ Association, Vol. 116, 33-43. ON THE KIMMERIDGIAN SUCCESSIONS OF THE NORMANDY COAST , NORTHERN FRANCE . R. W. Gallois Gallois, R. W. 2005. On the Kimmeridgian successions of the Normandy coast, northern France. Proceedings of the Geologists’ Association , Vol. 116, 33-43. ABSTRACT Kimmeridgian rocks crop out on the Normandy coast north and south of the Seine Estuary at Le Havre in a series of small foreshore and cliff exposures separated by beach deposits and landslips. A total thickness of about 45m of richly fossiliferous strata is exposed, ranging from the base of the Baylei Zone to the middle part of the Eudoxus Zone. The sections are mostly unprotected by sea-defence works and are subject to rapid marine erosion and renewal. Taken together, the Normandy exposures currently provide a more complete section through the low and middle parts of the Kimmeridgian Stage than any natural English section, including those of the Dorset type area. Descriptions and a stratigraphical interpretation of the Normandy sections are presented that enable the faunal collections to be placed in their regional chronostratigraphical context. The Kimmeridgian succession at outcrop on the Normandy coast contains numerous sedimentary breaks marked by erosion, hardground and omission surfaces. Some of these are disconformities that give rise to rapid lateral variations in the succession: biostratigraphical studies need therefore to be carried out with particular care. 1. INTRODUCTION The Kimmeridgian rocks of the Dorset type area and the Normandy coast are richly fossiliferous marine mudstones and limestones. -
Phylogeny, Diversity, and Ecology of the Ammonoid Superfamily Acanthoceratoidea Through the Cenomanian and Turonian
PHYLOGENY, DIVERSITY, AND ECOLOGY OF THE AMMONOID SUPERFAMILY ACANTHOCERATOIDEA THROUGH THE CENOMANIAN AND TURONIAN DAVID A.A. MERTZ A Thesis Submitted to the Graduate College of Bowling Green State University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE August 2017 Committee: Margaret Yacobucci, Advisor Andrew Gregory Keith Mann © 2017 David Mertz All Rights Reserved iii ABSTRACT Margaret Yacobucci Both increased extinction and decreased origination, caused by rising oceanic anoxia and decreased provincialism, respectively, have been proposed as the cause of the Cenomanian Turonian (C/T) extinction event for ammonoids. Conflicting evidence exists for whether diversity actually dropped across the C/T. This study used the ammonoid superfamily Acanthoceratoidea as a proxy for ammonoids as a whole, particularly focusing on genera found in the Western Interior Seaway (WIS) of North America, including Texas. Ultimately, this study set out to determine 1) whether standing diversity decreased across the C/T boundary in the WIS, 2) whether decreased speciation or increased extinction in ammonoids led to a drop in diversity in the C/T extinction event, 3) how ecology of acanthoceratoid genera changed in relation to the C/T extinction event, and 4) whether these ecological changes indicate rising anoxia as the cause of the extinction. In answering these questions, three phylogenetic analyses were run that recovered the families Acanthoceratidae, Collignoniceratidae, and Vascoceratidae. Pseudotissotiidae was not recovered at all, while Coilopoceratidae was recovered but reclassified as a subfamily of Vascoceratidae. Seven genera were reclassified into new families and one genus into a new subfamily. After calibrating the trees with stratigraphy, I was able to determine that standing diversity dropped modestly across the C/T boundary and the Early/Middle Turonian boundary. -
Palaeoecology and Palaeoenvironments of the Middle Jurassic to Lowermost Cretaceous Agardhfjellet Formation (Bathonian–Ryazanian), Spitsbergen, Svalbard
NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 1 https://dx.doi.org/10.17850/njg99-1-02 Palaeoecology and palaeoenvironments of the Middle Jurassic to lowermost Cretaceous Agardhfjellet Formation (Bathonian–Ryazanian), Spitsbergen, Svalbard Maayke J. Koevoets1, Øyvind Hammer1 & Crispin T.S. Little2 1Natural History Museum, University of Oslo, P.O. Box 1172 Blindern, 0318 Oslo, Norway. 2School of Earth and Environment, University of Leeds, Leeds LS2 9JT, United Kingdom. E-mail corresponding author (Maayke J. Koevoets): [email protected] We describe the invertebrate assemblages in the Middle Jurassic to lowermost Cretaceous of the Agardhfjellet Formation present in the DH2 rock-core material of Central Spitsbergen (Svalbard). Previous studies of the Agardhfjellet Formation do not accurately reflect the distribution of invertebrates throughout the unit as they were limited to sampling discontinuous intervals at outcrop. The rock-core material shows the benthic bivalve fauna to reflect dysoxic, but not anoxic environments for the Oxfordian–Lower Kimmeridgian interval with sporadic monospecific assemblages of epifaunal bivalves, and more favourable conditions in the Volgian, with major increases in abundance and diversity of Hartwellia sp. assemblages. Overall, the new information from cores shows that abundance, diversity and stratigraphic continuity of the fossil record in the Upper Jurassic of Spitsbergen are considerably higher than indicated in outcrop studies. The inferred life positions and feeding habits of the benthic fauna refine our understanding of the depositional environments of the Agardhfjellet Formation. The pattern of occurrence of the bivalve genera is correlated with published studies of Arctic localities in East Greenland and northern Siberia and shows similarities in palaeoecology with the former but not the latter. -
' Or ''Long'' Rhaetian? Astronomical Calibration of Austrian Key Sections
”Short” or ”long” Rhaetian ? Astronomical calibration of Austrian key sections Bruno Galbrun, Slah Boulila, Leopold Krystyn, Sylvain Richoz, Silvia Gardin, Annachiara Bartolini, Martin Maslo To cite this version: Bruno Galbrun, Slah Boulila, Leopold Krystyn, Sylvain Richoz, Silvia Gardin, et al.. ”Short” or ”long” Rhaetian ? Astronomical calibration of Austrian key sections. Global and Planetary Change, Elsevier, 2020, 192, pp.103253. 10.1016/j.gloplacha.2020.103253. hal-02884087 HAL Id: hal-02884087 https://hal.archives-ouvertes.fr/hal-02884087 Submitted on 29 Jun 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Galbrun B., Boulila S., Krystyn L., Richoz S., Gardin S., Bartolini A., Maslo M. (2020). « Short » or « long » Rhaetian ? Astronomical calibration of Austrian key sections. Global Planetary Change. Vol. 192C. https://doi.org/10.1016/j.gloplacha.2020.103253 « Short » or « long » Rhaetian ? Astronomical calibration of Austrian key sections Bruno Galbruna,*, Slah Boulilaa, Leopold Krystynb, Sylvain Richozc,d, Silvia Gardine, Annachiara -
Cenomanian Invertebrate Assemblage from the Dakota Sandstone Near Ghost Ranch, Rio Arriba County, New Mexico Spencer G
Cenomanian invertebrate assemblage from the Dakota Sandstone near Ghost Ranch, Rio Arriba County, New Mexico Spencer G. Lucas and Larry F. Rinehart, New Mexico Museum of Natural History and Science, 1801 Mountain Road NW, Albuquerque, New Mexico 87104, [email protected]; Shari Kelley, New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, New Mexico 87801 Abstract A small assemblage of invertebrate fossils from the Cretaceous Dakota Sandstone at Arroyo del Yeso near Ghost Ranch, Rio Arriba County, New Mexico, is the first age-diagnostic fossil assemblage documented from the inter- tongued Dakota–Mancos succession in the Chama Basin. The fossils are assigned to the bivalves Legumen sp., Exogyra sp., Inoceramus arvanus Stephenson, and I. prefragilis Stephen- son and the ammonite cf. Acanthoceras amphi- bolum Morrow. They indicate the Acanthoceras amphibolum Zone of middle Cenomanian age and support lithostratigraphic identification of the fossil-bearing strata as the Paguate Sandstone Tongue of the Dakota Sandstone. Introduction Newberry (1876) first identified Cretaceous strata in the Chama Basin of northern New Mexico, and many subsequent workers in the Chama Basin (e.g., Dane 1960; McPeek 1965; Landis and Dane 1967; Landis et al. 1973; Grant and Owen 1974; Saucier 1974) have recognized the Dakota Sandstone as an approximately 30–60-m-thick sandstone- dominated interval at or near the base of the Cretaceous section. The most recent synthe- sis of Dakota Sandstone stratigraphy in the Chama Basin (Owen et al. 2005) identified formal units of the intertongued Dakota– Mancos succession that were first identified to the south, in west-central New Mexico. -
75 the Upper Triassic Events Recorded in Platform and Basin of the Austrian Alps. the Triassic/Jurassic GSSP and Norian/Rhaetian
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt (ISSN 1017-8880), Band 111, Wien 2015 STRATI 2015 The Upper Triassic events recorded in platform and basin of the Austrian Alps. The Triassic/Jurassic GSSP and Norian/Rhaetian GSSP candidate Sylvain Richoz & Leopold Krystyn 47 figures Sylvain Richoz - Institute of Earth Sciences, Graz University, Heinrichstraße 26, 8010 Graz, Austria, [email protected] Leopold Krystyn - Department for Palaeontology, Vienna University, Geozentrum, Althansstr. 9, A-1090 Vienna, Austria; [email protected] Contents Abstract 1. Topics and area of the Field Trip 2. Introduction 2.1. The Northern Calcareous Alps 2.2. Principles of the structural evolution 2.3. Triassic depositional realms 2.3.1. General features 2.3.2. The Dachstein Mountains 2.3.3. The Zlambach facies – the deep shelf environment 2.3.4. The Hallstatt facies – the condensed deep shelf environment 2.3.5. The Eiberg Basin 3. The Field Trip 3.1. Shelf margin (Day 1) 3.1.1. Route 3.1.2. Locality 1 – Pötschenhöhe Quarry 3.1.3. Locality 2 – Großer Zlambach 3.1.4. Locality 3 – Steinbergkogel: Proposed Norian/Rhaetian GSSP section 3.1.5. Locality 4 – Gosausee: The Dachstein margin at Gosaukamm 3.2 Lagoon, fringing reef and Eiberg Basin (Day 2) 3.2.1. Route 3.2.2. Locality 5 – Pass Lueg: The classical Lofer cycle 3.2.3. Locality 6 – Adnet 3.2.4. Locality 7 – Steinplatte 3.2.5. Locality 8 – Eiberg 3.3. The Triassic/Jurassic GSSP (Day 3) 3.3.1. -
Late Jurassic Ammonites from Alaska
Late Jurassic Ammonites From Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 1190 Late Jurassic Ammonites From Alaska By RALPH W. IMLAY GEOLOGICAL SURVEY PROFESSIONAL PAPER 1190 Studies of the Late jurassic ammonites of Alaska enables fairly close age determinations and correlations to be made with Upper Jurassic ammonite and stratigraphic sequences elsewhere in the world UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress catalog-card No. 81-600164 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Page Abstract ----------------------------------------- 1 Ages and correlations ----------------------------- 19 19 Introduction -------------------------------------- 2 Early to early middle Oxfordian -------------- Biologic analysis _________________________________ _ 14 Late middle Oxfordian to early late Kimmeridgian 20 Latest Kimmeridgian and early Tithonian _____ _ 21 Biostratigraphic summary ------------------------- 14 Late Tithonian ______________________________ _ 21 ~ortheastern Alaska ------------------------- 14 Ammonite faunal setting -------------------------- 22 Wrangell Mountains -------------------------- 15 Geographic distribution ---------------------------- 23 Talkeetna Mountains ------------------------- 17 Systematic descriptions ___________________________ _ 28 Tuxedni Bay-Iniskin Bay area ----------------- 17 References -
Curator 10-9 Contents.Qxd
THE GEOLOGICAL CURATOR VOLUME 10, NO. 9 CONTENTS EDITORIAL by Matthew Parkes ............................................................................................................................ 516 PLANT OR ANIMAL, TERRESTRIAL OR MARINE? THOUGHTS ON SPECIMEN CURATION IN UNIVERSITY PALAEONTOLOGICAL TEACHING COLLECTIONS BASED ON AN EXAMPLE FROM OHIO, USA by James R. Thomka ............................................................................................................................ 517 DOMESTIC SCIENCE:THE RECOVERY OF AN ICHTHYOSAUR SKULL Volume 10 Number 9 by Heather Middleton ................................................................................................................ 523 ALEXANDER MURRAY COCKBURN, CURATOR OF THE MUSEUM OF GEOLOGY AT EDINBURGH UNIVERSITY by Peder Aspen ........................................................................................................................... 531 PRESENTATION OF THE A.G. BRIGHTON MEDAL TO GRAHAM WORTON .............................. 535 GEOLOGICAL CURATORS’ GROUP : 43rd ANNUAL GENERAL MEETING .................................. 539 BOOK REVIEWS ............................................................................................................................................. 545 GEOLOGICAL CURATORS’ GROUP - October 2018 GEOLOGICAL CURATORS’ GROUP Registered Charity No. 296050 The Group is affiliated to the Geological Society of London. It was founded in 1974 to improve the status of geology in museums and similar institutions, and to improve