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Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas
Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas GEOLOGICAL SURVEY PROFESSIONAL PAPER 1253 Stratigraphy and Paleontology of Mid-Cretaceous Rocks in Minnesota and Contiguous Areas By WILLIAM A. COBBAN and E. A. MEREWETHER Molluscan Fossil Record from the Northeastern Part of the Upper Cretaceous Seaway, Western Interior By WILLIAM A. COBBAN Lower Upper Cretaceous Strata in Minnesota and Adjacent Areas-Time-Stratigraphic Correlations. and Structural Attitudes By E. A. M EREWETHER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1 2 53 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Cobban, William Aubrey, 1916 Stratigraphy and paleontology of mid-Cretaceous rocks in Minnesota and contiguous areas. (Geological Survey Professional Paper 1253) Bibliography: 52 p. Supt. of Docs. no.: I 19.16 A. Molluscan fossil record from the northeastern part of the Upper Cretaceous seaway, Western Interior by William A. Cobban. B. Lower Upper Cretaceous strata in Minnesota and adjacent areas-time-stratigraphic correlations and structural attitudes by E. A. Merewether. I. Mollusks, Fossil-Middle West. 2. Geology, Stratigraphic-Cretaceous. 3. Geology-Middle West. 4. Paleontology-Cretaceous. 5. Paleontology-Middle West. I. Merewether, E. A. (Edward Allen), 1930. II. Title. III. Series. QE687.C6 551.7'7'09776 81--607803 AACR2 For sale by the Distribution Branch, U.S. -
Post-Carboniferous Stratigraphy, Northeastern Alaska by R
Post-Carboniferous Stratigraphy, Northeastern Alaska By R. L. DETTERMAN, H. N. REISER, W. P. BROSGE,and]. T. DUTRO,JR. GEOLOGICAL SURVEY PROFESSIONAL PAPER 886 Sedirnentary rocks of Permian to Quaternary age are named, described, and correlated with standard stratigraphic sequences UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Detterman, Robert L. Post-Carboniferous stratigraphy, northeastern Alaska. (Geological Survey Professional Paper 886) Bibliography: p. 45-46. Supt. of Docs. No.: I 19.16:886 1. Geology-Alaska. I. Detterman, Robert L. II. Series: United States. Geological Survey. Professional Paper 886. QE84.N74P67 551.7'6'09798 74-28084 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02687-2 CONTENTS Page Page Abstract __ _ _ _ _ __ __ _ _ _ _ _ _ _ _ _ _ _ _ __ __ _ _ _ _ _ _ __ __ _ _ __ __ __ _ _ _ _ __ 1 Stratigraphy__:_Continued Introduction __________ ----------____ ----------------____ __ 1 Kingak Shale ---------------------------------------- 18 Purpose and scope ----------------------~------------- 1 Ignek Formation (abandoned) -------------------------- 20 Geographic setting ------------------------------------ 1 Okpikruak Formation (geographically restricted) ________ 21 Previous work and acknowledgments ------------------ 1 Kongakut Formation ---------------------------------- -
Marine Bivalve Molluscs
Marine Bivalve Molluscs Marine Bivalve Molluscs Second Edition Elizabeth Gosling This edition first published 2015 © 2015 by John Wiley & Sons, Ltd First edition published 2003 © Fishing News Books, a division of Blackwell Publishing Registered Office John Wiley & Sons, Ltd, The Atrium, Southern Gate, Chichester, West Sussex, PO19 8SQ, UK Editorial Offices 9600 Garsington Road, Oxford, OX4 2DQ, UK The Atrium, Southern Gate, Chichester, West Sussex, PO19 8SQ, UK 111 River Street, Hoboken, NJ 07030‐5774, USA For details of our global editorial offices, for customer services and for information about how to apply for permission to reuse the copyright material in this book please see our website at www.wiley.com/wiley‐blackwell. The right of the author to be identified as the author of this work has been asserted in accordance with the UK Copyright, Designs and Patents Act 1988. All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, except as permitted by the UK Copyright, Designs and Patents Act 1988, without the prior permission of the publisher. Designations used by companies to distinguish their products are often claimed as trademarks. All brand names and product names used in this book are trade names, service marks, trademarks or registered trademarks of their respective owners. The publisher is not associated with any product or vendor mentioned in this book. Limit of Liability/Disclaimer of Warranty: While the publisher and author(s) have used their best efforts in preparing this book, they make no representations or warranties with respect to the accuracy or completeness of the contents of this book and specifically disclaim any implied warranties of merchantability or fitness for a particular purpose. -
Ctenoides Ales) Lindsey F
© 2017. Published by The Company of Biologists Ltd | Biology Open (2017) 6, 648-653 doi:10.1242/bio.024570 RESEARCH ARTICLE Do you see what I see? Optical morphology and visual capability of ‘disco’ clams (Ctenoides ales) Lindsey F. Dougherty1,2,3,*, Richard R. Dubielzig4, Charles S. Schobert4, Leandro B. Teixeira4 and Jingchun Li2,3 ABSTRACT considering the evolution of vision, simple light-sensitive cells can The ‘disco’ clam Ctenoides ales (Finlay, 1927) is a marine bivalve that evolve to a complex camera-type eye in a mere few hundred has a unique, vivid flashing display that is a result of light scattering by thousand years (Nilsson and Pelger, 1994), which may explain the silica nanospheres and rapid mantle movement. The eyes of C. ales extreme diversity of vision throughout the animal kingdom. were examined to determine their visual capabilities and whether the Mollusks (bivalves, gastropods, cephalopods, chitons, etc.) have clams can see the flashing of conspecifics. Similar to the congener the most diverse eye morphologies of any phylum (Serb and C. scaber, C. ales exhibits an off-response (shadow reflex) and an on- Eernisse, 2008). Several eye types have evolved within Mollusca: response (light reflex). In field observations, a shadow caused a pit eyes can differentiate between light and shade but do not form significant increase in flash rate from a mean of 3.9 Hz to 4.7 Hz images, and exist in some bivalves and gastropods; pinhole eyes, (P=0.0016). In laboratory trials, a looming stimulus, which increased which provide the directionality of light but poor image quality, light intensity, caused a significant increase in flash rate from a exist in the nautilus and the giant clam; compound eyes, which have median of 1.8 Hz to 2.2 Hz (P=0.0001). -
The Recent Molluscan Marine Fauna of the Islas Galápagos
THE FESTIVUS ISSN 0738-9388 A publication of the San Diego Shell Club Volume XXIX December 4, 1997 Supplement The Recent Molluscan Marine Fauna of the Islas Galapagos Kirstie L. Kaiser Vol. XXIX: Supplement THE FESTIVUS Page i THE RECENT MOLLUSCAN MARINE FAUNA OF THE ISLAS GALApAGOS KIRSTIE L. KAISER Museum Associate, Los Angeles County Museum of Natural History, Los Angeles, California 90007, USA 4 December 1997 SiL jo Cover: Adapted from a painting by John Chancellor - H.M.S. Beagle in the Galapagos. “This reproduction is gifi from a Fine Art Limited Edition published by Alexander Gallery Publications Limited, Bristol, England.” Anon, QU Lf a - ‘S” / ^ ^ 1 Vol. XXIX Supplement THE FESTIVUS Page iii TABLE OF CONTENTS INTRODUCTION 1 MATERIALS AND METHODS 1 DISCUSSION 2 RESULTS 2 Table 1: Deep-Water Species 3 Table 2: Additions to the verified species list of Finet (1994b) 4 Table 3: Species listed as endemic by Finet (1994b) which are no longer restricted to the Galapagos .... 6 Table 4: Summary of annotated checklist of Galapagan mollusks 6 ACKNOWLEDGMENTS 6 LITERATURE CITED 7 APPENDIX 1: ANNOTATED CHECKLIST OF GALAPAGAN MOLLUSKS 17 APPENDIX 2: REJECTED SPECIES 47 INDEX TO TAXA 57 Vol. XXIX: Supplement THE FESTIVUS Page 1 THE RECENT MOLLUSCAN MARINE EAUNA OE THE ISLAS GALAPAGOS KIRSTIE L. KAISER' Museum Associate, Los Angeles County Museum of Natural History, Los Angeles, California 90007, USA Introduction marine mollusks (Appendix 2). The first list includes The marine mollusks of the Galapagos are of additional earlier citations, recent reported citings, interest to those who study eastern Pacific mollusks, taxonomic changes and confirmations of 31 species particularly because the Archipelago is far enough from previously listed as doubtful. -
Organic Carbon Isotope Chemostratigraphy of Late Jurassic Early Cretaceous Arctic Canada
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Geography, Earth and Environmental Sciences Finding the VOICE: organic carbon isotope chemostratigraphy of Late Jurassic Early Cretaceous Arctic Canada Galloway, JM http://hdl.handle.net/10026.1/15324 10.1017/s0016756819001316 Geological Magazine Cambridge University Press (CUP) All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. Proof Delivery Form Geological Magazine Date of delivery: Journal and vol/article ref: geo 1900131 Number of pages (not including this page): 15 This proof is sent to you on behalf of Cambridge University Press. Please check the proofs carefully. Make any corrections necessary on a hardcopy and answer queries on each page of the proofs Please return the marked proof within 2 days of receipt to: [email protected] Authors are strongly advised to read these proofs thoroughly because any errors missed may appear in the final published paper. This will be your ONLY chance to correct your proof. Once published, either online or in print, no further changes can be made. To avoid delay from overseas, please send the proof by airmail or courier. If you have no corrections to make, please email [email protected] to save having to return your paper proof. If corrections are light, you can also send them by email, quoting both page and line number. -
Palaeontological Spitsbergen Studies
POLISH ACADEMY OF SCIENCES INSTITU'TE OF PALEOBIOLOGY PALAEONTOLOGIA POLONICA - NO. 43, 1982 PALAEONTOLOGICAL I SPITSBERGEN STUDIES - Part I (PALEONTOLOGICZNE BL4DANIA SPITSBERGENU - CzeSC I) GERTRUDA BIERNAT- and WANDA SZYMA~~SKA DAWNICTWO NAUKOWE KRZYSZTOF BIRKENMAJER, HALINA PUGACZEWSKA and ANDRZEJ WIERZBOWSKI THE JANUSFJELLET FORMATION (JURASSIC-LOWER CRETACEOUS) AT MYKLEGARDFJELLET, EAST SPITSBERGEN BIRKENMAJER,K; PU~ACZEWSKA,H. and WIERZBOWSKI,A.,: The Janusfjellet Formation (Jurassic-Lower Creiaceous) at Myklegardfjellet, east Spitsbergen. Palaeont. Polonica, 43,107- 140. Fossiliferous marine strata of the Janusfjellet Formation (Jurassic-Lower Cretaceous) are describ- ed from Myklegardfjellet, Agardhbukta area, east Spitsbergen. The invertebrate fauna collected by the first author from these beds in 1977 has been determined by the second author (serpulids, bivalves, belemnites) and by the third author (ammonites). This assemblage allows to distinguish the Upper Callovian, the Kirnrneridgian (Lower and Upper) and the Lower Volgian stages in the lower part of the Janusfjellet Formation (Agardhfjellet Member). The upper part of the Janusfjellet Formation (Rurikfjellet Member) yielded poorly preserved fossils of little stratigraphic value. Key words: Mesozoic, stratigraphy, ammonites, bivalves, belemnites, serpulids, Spitsbergen. K. Birkenmajer, 1nstY~utNauk Geologicznych, Polska Akademia Nauk, 31-002 Krakow, Senacka 3; H. Pugaczewska, Zaklad Paleobiologii, Polska Akadernia Nauk, 02-089 Warszawa,irwirki i Wigury 93; A. Wierzbowski, -
Phylum MOLLUSCA Chitons, Bivalves, Sea Snails, Sea Slugs, Octopus, Squid, Tusk Shell
Phylum MOLLUSCA Chitons, bivalves, sea snails, sea slugs, octopus, squid, tusk shell Bruce Marshall, Steve O’Shea with additional input for squid from Neil Bagley, Peter McMillan, Reyn Naylor, Darren Stevens, Di Tracey Phylum Aplacophora In New Zealand, these are worm-like molluscs found in sandy mud. There is no shell. The tiny MOLLUSCA solenogasters have bristle-like spicules over Chitons, bivalves, sea snails, sea almost the whole body, a groove on the underside of the body, and no gills. The more worm-like slugs, octopus, squid, tusk shells caudofoveates have a groove and fewer spicules but have gills. There are 10 species, 8 undescribed. The mollusca is the second most speciose animal Bivalvia phylum in the sea after Arthropoda. The phylum Clams, mussels, oysters, scallops, etc. The shell is name is taken from the Latin (molluscus, soft), in two halves (valves) connected by a ligament and referring to the soft bodies of these creatures, but hinge and anterior and posterior adductor muscles. most species have some kind of protective shell Gills are well-developed and there is no radula. and hence are called shellfish. Some, like sea There are 680 species, 231 undescribed. slugs, have no shell at all. Most molluscs also have a strap-like ribbon of minute teeth — the Scaphopoda radula — inside the mouth, but this characteristic Tusk shells. The body and head are reduced but Molluscan feature is lacking in clams (bivalves) and there is a foot that is used for burrowing in soft some deep-sea finned octopuses. A significant part sediments. The shell is open at both ends, with of the body is muscular, like the adductor muscles the narrow tip just above the sediment surface for and foot of clams and scallops, the head-foot of respiration. -
Erminlo Caprotti F) L Avole Propriamente Nei Vasti Ammassi Di
\ \ Erminlo Caprotti MOLLUSCHI DEL TABIANIANO (PLIOCENE INFERIORE) DELLA VAL D'ARDA. LORO CONNESSIONI TEMPORALI E SPAZIALI. Gebun und GÈb, Èir cwias Mc.r. - F'n we.-hselnd W€hén Èin slUhcnd t2ben: So schatf ich .m sausendeù WcE sruhl de. z.n Und{i.ke dér Gonhéir lebendig.s (W. C@thé, Faust, I, Nacht) A) Introduzione B) Composizione della fauna e comparazioni - Le associazioni , dominanti C) Origine e divenire D) Descrizioni paleontologiche E) Nota bibliografica F) l avole A) INTRODUZIONE Questo lavoro studia i molluschi reperiti dall'Autore con sue per- sonali ricerche nel Tabianiano (Pliocene inferiore) della Val d'Arda, in provincia di Piacenza. La ricerca e la raccolta del materiale è stata ef- fettuata sulla riva destra dell'Arda nei pressi di Lugagnano, e Piir propriamente nei vasti ammassi di argille azzure che si stendono dall'Arda verso il paese di Vernasca (Foglio I.G.M. n. 72 II N.E.). In particolare le due zone di raccolta, oggetto di questo studio, sono topograficamente racchiuse tm quota 208 (Case Micelli presso la riva destra dell'Arda) e quota 300 circa. Si tratta di un grande ammasso di argille azzurre, situato ad Est ed a Sud-Est della fornace per late- rizi di Lugagnano. Topograficamente sovrapposte a queste argille si trovano sabbie basali del Pliocene inferiore variate con intercalazioni marmose, sab- bie medie e grossolane, marne grigio chiare, sabbie argillo§e, argille marmoso-sabbiose. Da esse non sono stati prelevati che scarsi fram_ menti di molluschi e pertanto queste non fanno oggetto di questo Iavoro. Queste sabbie sooo stratigraficamente sottoposte alle argille prese qui in esame, mentre dal punto di vista topografico esse si e' stcndono fin quasi al paese di Veanasca. -
Pyramidellidae Turbonilla
Pyramidellidae Subfamily Turbonillinae Genus Turbonilla Species recorded from the SCB By Tony Phillips DCE At the October 2010 SCAMIT meeting it was suggested by Pat LaFollette for us to take high quality, detailed photographs of our Turbonilla, Pyrgiscus and Odostomia species (don’t forget scale bars, locality and depth information!) and share with him and with each other. If it is possible to assign it unequivocally to a described species, he will aid us in giving specimens names…... He also suggested we use Abbott 1974 as a primary resource..... Subgenera of Turbonilla (Oldroyd 1927 & Abbot 1974) • Bartschella Iredale 1917 - valid genus • Chemnitzia d’Orbigny 1840 - Turbonilla • Mormula A. Adams 1863 - valid genus, not in subfamily Turbonillinae • Pyrgiscus Philippi 1841 - valid genus • Pyrgolampros Sacco 1892 - Turbonilla • Strioturbonilla Sacco 1892 – valid genus, not in subfamily Turbonillinae • Turbonilla Risso 1826 – valid genus * WoRMS 2016 for subfamily Turbonillinae Genera listed under subfamily Turbonillinae (according to WoRMS 2016) Asmunda Dall & Bartsch 1904 Kleinella A. Adams 1860 Bacteridella Saurin 1959 Nisipyrgiscus Robba 2013 Bartschella Iredale 1916 Nisiturris Dall & Bartsch 1906 Bouchetmella Penas & Rolan 2016 Puposyrnola Cossmann 1921 Careliopsis Morch 1875 Pyrgiscus Philippi 1841 Colsyrnola Iredale 1929 Pyrgolidium Monterosato 1884 Ebalina Thiele 1929 Pyrgostylus Monterosato 1884 Eulimella Forbes & M’Andrew 1846 Raoulostraca Oliver 1915 Exesilla Laseron 1959 Syrnola A. Adams 1860 Gispyrella Laws 1937 Turbolidium Robba 2013 Hamarilla Eames & Wilkins 1959 Turbonilla Risso 1826 Iphiana Dall & Bartsch 1904 Considering the current state of uncertainty of the suprageneric classification, we have preferred not to add to the confusion, and have kept our work at the specific level. Therefore we shall use only the genus name Turbonilla for all the species included….(Penas & Rolan, 2010) ….as most of the turbonillids, the majority of species cannot yet be defensibly seated in an appropriate genus. -
Occurrence of the Hairy Ark Cockle (Anadara Gubernaculum, Reeve 1844) in Mayangan Coastal Waters, Subang – Province West Java: New Distribution Record of Indonesia
Asian Journal of Conservation Biology, December 2016. Vol. 5 No. 2, pp. 70-74 AJCB: FP0075 ISSN 2278-7666 ©TCRP 2016 Occurrence of the hairy ark cockle (Anadara gubernaculum, Reeve 1844) in Mayangan coastal waters, Subang – Province West Java: new distribution record of Indonesia Dewi Fitriawati1*, Nurlisa Alias Butet2 and Yusli Wardiatno2 1Master Program in Aquatic Resources Management, Graduate School of Bogor Agricultural University, Kampus IPB Dramaga – Bogor 16680, Indonesia 2Department of Aquatic Resources Management, Faculty of Fisheries and Marine Science, Bogor Agricultural University, Kampus IPB Dramaga – Bogor 16680, Indonesia (Accepted November 25, 2016) ABSTRACT Thirty six specimens of the hairy ark cockle (Anadara gubernaculum Reeve, 1844) were collected from Mayangan waters, Subang of Province West Java, during marine biodiversity survey along northern coast of Java Island, Indonesia. Previous records of the cockle showed its occurrence in Cilincing, northern coast of Jakarta, Semarang coastal waters of Province Central Java, and Sidoarjo coastal waters located in northern part of Province East Java. The identification of the species was performed by morphological characters and is supported by molecular analysis. This finding represents a new distribution record of the species in Indonesia. Keywords: Arcidae, bivalves, first record, mollusc, north Java. INTRODUCTION A.gubernaculum from Mayangan waters, Subang – Province West Java, Indonesia. At the same time it is a As an aquatic biodiversity hotspot, Indonesia has rich and diverse marine organisms, one of them is the cock- new distribution record of the species in Indonesian les group of Arcidae. The family Arcidae is a large and waters. diverse family of marine bivalve distributed worldwide in warm seas of tropical areas. -
The Cretaceous System in Central Sierra County, New Mexico
The Cretaceous System in central Sierra County, New Mexico Spencer G. Lucas, New Mexico Museum of Natural History, Albuquerque, NM 87104, [email protected] W. John Nelson, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Karl Krainer, Institute of Geology, Innsbruck University, Innsbruck, A-6020 Austria, [email protected] Scott D. Elrick, Illinois State Geological Survey, Champaign, IL 61820, [email protected] Abstract (part of the Dakota Formation, Campana (Fig. 1). This is the most extensive outcrop Member of the Tres Hermanos Formation, area of Cretaceous rocks in southern New Upper Cretaceous sedimentary rocks are Flying Eagle Canyon Formation, Ash Canyon Mexico, and the exposed Cretaceous sec- Formation, and the entire McRae Group). A exposed in central Sierra County, southern tion is very thick, at about 2.5 km. First comprehensive understanding of the Cretaceous New Mexico, in the Fra Cristobal Mountains, recognized in 1860, these Cretaceous Caballo Mountains and in the topographically strata in Sierra County allows a more detailed inter- pretation of local geologic events in the context strata have been the subject of diverse, but low Cutter sag between the two ranges. The ~2.5 generally restricted, studies for more than km thick Cretaceous section is assigned to the of broad, transgressive-regressive (T-R) cycles of 150 years. (ascending order) Dakota Formation (locally deposition in the Western Interior Seaway, and includes the Oak Canyon [?] and Paguate also in terms of Laramide orogenic