DOCSLIB.ORG

(South Sakhalin) Syngenesis

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
(South Sakhalin) Syngenesis bulletin de l'institut royal des sciences naturelles de belgique sciences de la terre. 66: 109-127, 1996 bulletin van het koninklijk belgisch instituut voor natuurwetenschappen, aardwetenschappen. 66: 109-127, 1996 Cretaceous ammonoid succession in the Far East (South Sakhalin) and the basic factors of syngenesis by Yuri D. ZAKHAROV, Alexander V. IGNATYEV, Nataliya G. UKHANEVA & Tamara B. AFANASEVA Abstract Characteristics of the marine Palaeosuccession At the Maastrichtian-Danian boundary in Sakhalin Island radical fau- In the Albian-Danian South Sakhalin mollusk succession nal changes are visible. The repeated influence of three basic factors several can (drop of température, oxygen deficit and enormous eustatic level phases be distinguished, reflecting the diver- fluctuation provoked by thermal perturbation at the core/mantle boun¬ sity in the marine communities at that time. dary and change in rotation regime of the Earth) seems to be the main reason for a great extinction in many groups of marine and terrestrial organisms during the time of the Cretaceous-Tertiary transition. Key-words: K/T boundary - faunal changes - stable isotopes - Sakhalin. Résumé Dans les dépôts de Sakhalin la transition Maastrichtien/ Danien montre un changement radical dans les faunes. Trois facteurs (diminution de la température, un déficit dans la quantité d'oxygène et de fortes fluctua¬ BERING tions eustatiques résultant de la perturbation thermique à la transition SEA noyau-manteau et au changement dans le régime de rotation terrestre) semblent être les causes majeures pour une grande extinction dans de nombreux groupes d'organismes marins et terrestres au moment de la transition Crétacé-Tertiaire. Mots-clefs: Transition K/T - changements fauniques - isotopes stables - Sakhalin. 1000 km Introduction A more than 4000 m thick, well exposed late Early Cretaceous - Late Cretaceous - Early Palaeogene se- quence is present along the Naiba River in Dolinsk ré¬ gion, South Sakhalin (Text-fig. 1). This famous section (Matsumoto, 1938; Vereschagin, 1977; Zakharov et SEA OF al., 1978, 1981. 1984a; Salnikov & Tikhomolov, 1987) OKHOTSK is considered as the basic section for the Upper Creta¬ ceous in the "Far East". This sequence has been sub- divided into four formations : (1) Ai (Albian), (2) Naiba (Albian-Cenomanian), (3) Bykov (Turonian-Santonian), and (4) Krasnoyarka (Campanian-Danian). The present work analyses the Cretaceous palaeosuc¬ 200 km cession of the Far East on the basis of data for the Sakhalin cephalopod fauna and stable isotopes recogni- zed in brachiopod, ammonoid and bivalve shells from South Sakhalin (Naiba, Krasnoyarka and Sary Rivers) Text-fig. 1 — Location of the Naiba River, Sakhalin (1) and and from the Koryak Uplands. Pahacha River, Koryak Uplands (2) sequences. ou o- 0Q m Om 0' o o * BED •• E STAGE MEMBER 0 BB FORMATION LITHOLOGY THICKNESS, • © K» © © fji (A oö O ï i 00 CO Oè Bykov m O h* 4^ -o£o- O oK O Ou! 03 &'iv 3> *>3 •-0 r^'Jt •>3 o ŒD-O O &o O SCF OO iO 0 aO c£ SO- £o O oo-o- £o O o—— -aO a AoavHMVz E2ö <A°^ t^O a Ê Ac. K> ™a O 4- Ut oo vo sanctorum ©O Marshallites-A.s. &o êo- so (A O O ÖÖ O 0W9^ O Oto OO OS OtA O O o<v CENOMANIAN u> Ut •>3 Sp M © «O w w © © hO" K) N> ts> ►O CO- O Naiba uO ipomcum tibilis OO ularis©•- ±.0~ Turjilitescf. ©O— 00 ZeLindites 055costatus Da/nesifis mihoensis damesi ©O CD^- 55O— (AQ- Nipponites Mikasaites ALBIAN jç.tDesmoceras(P.) Gaudrycerasteruiliratum mirt orbh © wO- 3©o o- Cretaceous ammonoid succession in Far East 111 Phase 1 Text-fig. 2 — Lithofacies, distribution and relative abundance of ammonoid taxa for the Upper Ai, Naiba and During phase 1 (Ai and Lower Naiba formations, Albian), Lower Bykov Formations (Albian-Cenoma- most marine nian). Désignation of the beds: T.c. = Turrilites groups in South Sakhalin were poorly di- costatus, Marshallites - A.s. = Marshallites - versified, possibly due to a shallowing marine basin and Acanthoceras sanctorum. Lithology: a - conglo- periodical fresh-water influence during the latest Early merate, b - sandstone, c - sandy siltstone, d - Cretaceous. The main body of the community was for- tuffaceous siltstone, tuffaceous sandstone, tuf- med by foraminifers (about 30 species) (Turenko, 1987), fite, tuffs, e - siltstone, f - mudstone with no¬ radiolarians (about 14 dules; location: g - Naiba River basin, h - species) (Kazintsova, 1987), cri- noids neigbouring territories in South Sakhalin, i - (1 species), echinoids (1 species), bivalves (12 questionably present. Relative abundance of species) (Salnikova, 1987), including some fresh-water ammonoid - very rare, - rare, - species: j k 1 taxa - Anodonta oraria Kalishevich (Zakharov et al., occasional, m - common, n - abundant. 1978, 1981), gastropods (2 species) (Poyarkova, 1987), Species: 1 - Brewericeras ex gr. hulense An¬ and scarce ammonoids dersom 2 - Cleoniceras (Neosaynella?) sp. 3 - ("Phylloceras'' aff. tanit Pervin¬ Puzosia subcorbarica Matsumoto, 4 - Cleoni¬ quière, Anagaudryceras? sp., Parajaubertella cf. kawa¬ ceras? sp., 5 - Desmoceras kossmati Matsumo¬ kitana Matsumoto, Puzosia subcarbarica Matsumoto, to, 6 - Pachydesmoceras cf. denisonianum (Sto- Pachydesmoceras cf. denisonianum (Stoliczka), Brewe¬ liczka), 7 - Parajaubertella kawakitana Matsu¬ riceras ex gr. hulense Anderson, Desmoceras kossmati moto, 8 - "Phylloceras" aff. tanit Pervin- Matsumoto, sp., sp., quière, 9 - Nipponites mirabilis Yabe, 10 - Anahoplitesl Cleoniceras Neogas- Mikasaites orbicularis Matsumoto, 11 - Ana- troplites sp.) (Text-fig. 2) (Zakharov et al., 1978, 1984a; gaudryceras sacya (Forbes), 12 - Marshallites Mirolyubov, 1987). sp., 13 - Epigoniceras sp., 14 - Desmoceras (Pseudouhligella) japonicum Yabe, 15 - Dame- Phase 2 sites damesi (Jimbo) (Pl. 2, Fig. 2-3), 16 - Gaudryceras tenuiliratum Yabe, 17 - Turrilites cf. acutus (Passy), 18-7". cf. costatus (La- Phase 2 (Upper Naiba, Bykov, and Lower Krasnoyarka marck), 19 - Puzosia tenuis Shimizu, 20 - Des¬ Formations, Cenomanian-Campanian) is characterised by moceras aff. inane (Stoliczka), 21 - Puzosia an abundance and high taxonomie diversity of a.o. bival¬ planulata (J. de C. Sowerby), 22 - Marshallites ves (including inoceramids) and ammonoids. This part of cf. olcostephanoides Matsumoto, 23 - "Phyllo¬ the invertebrate succession is ceras" cf. ellipticum Kossmat, 24 - Zelandites represented by foraminifers mihoensis Matsumoto, 25 - Anagaudryceras (about 38 species) (Turenko, 1987), radiolarians (more sp., 26 - Puzosia ex gr. bhima (Stoliczka), 27 than 100 species) (Kazintsova, 1987), crinoids (1 spe¬ - Holcodiscoides popillatus (Stoliczka), 28 - cies), crustaceans (1 species), bivalves (more than 100 Mikasaites matsumotoi Vereschagin, 29 - Acanthoceras hippocastanum (J. de C. Sower¬ species) (Zakharov et ai, 1984a; Salnikova, 1987; by), 30 - A. sussexiense (Mantell), 31 - A. cf. Zonova, 1987), scaphopods (5 species), gastropods (25 rotomagense (Defrance), 32 - Tetragonites ex species) (Poyarkova, 1987), ammonoids (177 species of gr. timotheanus (Pictet), 33 - Eogunnarites uni- Hauericeras, Hypophylloceras, Neophylloceras, Zelandi¬ cus (Yabe), 34 - Eucalycoceras cf. vergonsense tes, Parajaubertella, Anagaudryceras, Gaudryceras, Te¬ Collignon, 35 - Calycoceras asiaticum (Jimbo), tragonites, Saghalinites, Neocrioceras, 36 - Marshallites japonicus Matsumoto, 37 - Turrilites, Anapa- Pachydesmoceras pachydiscoides Matsumoto, chydiscus, Puzosia, Pachydesmoceras, Jimboiceras, 38 - Hypophylloceras seresitense (Pervin- Mesopuzosia, Microdesmoceras, Marshallites, Holcodis¬ quière), 39 - Microdesmoceras applanatum coides, Eogunnarites, Kossmaticeras, Yokoyamaoceras, Grabovskaya, 40 - Jimboiceras planulatiforme Jacobites, Canadoceras, Anapachydiscus, Menuites, Tes- (Jimbo), 41 - Hypophylloceras ononense (Stan- hioites, Urakawites, Mikasaites, Nipponites, Hyphanto- ton), 42 - H. simplificatum Grabovskaya, 43 - Metapuzosia sp., 44 - Anagaudryceras cf. ol¬ ceras, Scalarites, Bostrychoceras, Diplomoceras, Scaphi- costephanoides Matsumoto, 45 - Anagaudryce¬ tes, Ryugasella, Desmoscaphites, Polyptychoceras, Pseu- ras buddha (Forbes), 46 - Puzosia nipponica doxybeloceras, Pseudaspidoceras, Otoscaphites, Peroni- Matsumoto, 47 - Puzosia sp., 48 - Phyllopa- ceras, Calycoceras, Eucalycoceras, Acanthoceras, Fage- chyceras ezoense (Yokoyama), 49 - Hypophyl¬ sia, Submortoniceras, Schlueterella (Text-figs. 3-4) loceras sp., 50 - "Phylloceras" cf. diegoi Boule, Lemoine & Thévenin, 51- Zelandites (Vereschagin, 1977; Zakharov et al., 1984a; Miro- inflatus Matsumoto, 52 - Anagaudryceras uta- yubov, 1987), nautiloids (7 species), and belemnitoids turense Shimizu, 53 - Puzosia cf. furnitana (1 species). Pervinquière, 54 - P. aff. octosulcata Sharpe, Within the ammonoid group, a change of dominance 55 - Desmoceras pseudinane Shimizu, 56 - took Jacobites sp., 57 - Acanthoceras sanctorum place several times: (1) Desmoceras (Pseudouhli¬ Matsumoto & Obata, 58 - Mesopuzosia pacifica gella) japonicum (within the Turrilites costatus beds and Matsumoto, 59 - M. indopacifica (Kossmat), 60 Marshallites - Acanthoceras sanctorum beds, Cenoma- - Tetragonites sp., 61 - Kossmaticeras sp., 62 - nian - bioevent "a") —> Tetragonites epigonus (within Polyptychoceras obstractum (Jimbo), 63 - Neo- the Jimboiceras planulatiforme beds, Turonian - bioevent phylloceras ramosum (Meek), 64 - Epigonice¬ -> ras epigonum (Kossmat), 65 - E. glabrum (Jim¬ "b") (3) Gaudryceras tenuiliratum (within the Jim¬ bo), 66 - Jimboiceras planulatiforme (Jimbo). boiceras mihoense beds, Anapachydiscus naumanni beds TURONIAN CONIACIAN Jimboiceras
Load more

Recommended publications
  • The Upper Cretaceous Dimorphic Pachydiscid Ammonite Menuites in the Western Interior of the United States
    The Upper Cretaceous Dimorphic Pachydiscid Ammonite Menuites in the Western Interior of the United States U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1533 AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications re­ leased prior to the current year are listed in the most recent annual"Price and Availability List" Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may no longer be available. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices listed below. BY MAlL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech­ Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey offices, all of general interest (such as leaflets, pamphlets, booklets), single of which are authorized agents of the Superintendent of Docu­ copies of Earthquakes & Volcanoes, Preliminary Determination of ments. Epicenters, and some miscellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • ANCHORAGE, Alaska-Rm.
    [Show full text]
  • Pdf Ichnospecies Funalichnus Strangulatus (Fritsch 1883), Upper Schlirf, M.; Uchman, A
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Geologica Saxonica - Journal of Central European Geology Jahr/Year: 2016 Band/Volume: 62 Autor(en)/Author(s): Niebuhr Birgit, Wilmsen Markus Artikel/Article: Ichnofossilien 181-238 62: 181 – 238 29 Dec 2016 © Senckenberg Gesellschaft für Naturforschung, 2016. 16. Ichnofossilien 16. Ichnofossils Birgit Niebuhr und Markus Wilmsen Senckenberg Naturhistorische Sammlungen Dresden, Museum für Mineralogie und Geologie, Sektion Paläozoologie, Königsbrücker Land- straße 159, 01109 Dresden, Deutschland; [email protected], [email protected] Revision accepted 18 July 2016. Published online at www.senckenberg.de/geologica-saxonica on 29 December 2016. Kurzfassung Die taxonomische Revision der Spurenfossilien der Elbtal-Gruppe ergab 28 Ichnotaxa, die sich verteilen auf 1. einfache Spuren: Lockeia amygdaloides (Seilacher), Bergaueria klieni (Geinitz), Fluchtspuren; 2. unverzweigte Spuren: Skolithos linearis (Haldeman), Taenidium cameronensis (Brady), Funalichnus strangulatus (Frič), Planolites isp.; 3. verzweigte Spuren: Chondrites targionii (Brongniart), Ophio­ morpha saxonica (Geinitz), O. ramea (Geinitz), Thalassinoides suevicus (Rieth), Keckia annulata Glocker, K. cylindrica von Otto, K. no­ du losa von Otto, Asterosoma? wohlfarthi (von Otto); 4. horizontal-konzentrische Spuren: A. radiciforme von Otto, A. coxii (Lesquereux), Dactyloidites ottoi (Geinitz); 5. dreidimensional-gewundene
    [Show full text]
  • Acta Geologica Polonica, Vol
    Acta Geologica Polonica, Vol. 50 (2000), No. 4, pp. 407-419 On some Late Turonian and Early Coniacian (Upper Cretaceous) heteromorph ammonites from Germany FRANK WIESE Institut für Paläontologie, FU Berlin, Malteserstr. 74-100 D-12249 Berlin. E-mail: [email protected] ABSTRACT: WIESE, F. 2000. On some Late Turonian and Early Coniacian (Upper Cretaceous) heteromorph ammonites from Germany. Acta Geologica Polonica, 50 (4), 407-419. Warszawa. Five heteromorph ammonite taxa belonging to the Nostoceratidae and the Diplomoceratidae are described from the Upper Turonian and Lower Coniacian of northern Germany and Saxony. The investigation serves the presentation of additional material of Hyphantoceras flexuosum, Neocrioceras paderbornense and Scalarites turoniense that are rarely documented in northern Germany and Saxony. Furthermore, one new species, Hyphantoceras ernsti sp. n., is introduced. One taxon is described in open nomenclature as nostoceratid gen. et sp. indet. Key words: Upper Cretaceous, Germany, Turonian, Coniacian, Ammonite Taxonomy, Nostoceratidae, Diplomoceratidae INTRODUCTION northern Germany (WOOD & al. 1984), which attracted the attention of collectors and palaeontologists because The description of the Turonian and Coniacian of its abundant and highly diverse invertebrate fauna ammonite faunas from Germany has a long tradition. (DAHMER & ERNST 1986, KAPLAN 1992, METZDORF The first monographic treatment on Upper Cretaceous 1992, 1993). Above the Hyphantoceras Event, in the ammonites was that of SCHLÜTER (1867) in which he uppermost part of the Lower Limestone Unit and the also described Turonian and Lower Coniacian material. succeeding marl/limestone alternations, the Grau- From Saxony in southeastern Germany, Turonian to Weiße Wechselfolge (WOOD & al. 1984), in the remain- Coniacian ammonites were investigated and figured by, der of the Upper Turonian and Lower Coniacian, amongst others, REUSS (1845), GEINITZ (1843, 1849- ammonites become suddenly and significantly rarer and 1850), PETRASCHECK (1902), WANDERER (1909) and less diverse.
    [Show full text]
  • Scaphitid Ammonite Correlation of the Late Maastrichtian Deposits in Poland and Denmark
    Scaphitid ammonite correlation of the Late Maastrichtian deposits in Poland and Denmark Machalski, M. 1996. Scaphitid ammonite correlation of the Late Maastrichtian deposits in Poland and Denmark. - Acta Palaeontologica Polonica 41,4,369-383. Evolutionary changes in the ribbing density on body chambers in samples of the scaphitid ammonite Hopbscaphites constrictus (J.Sowerby, 1817) are used for time correlation of the Kazimierz Opoka (Late Maastrichtian, Belemnella kazimiro- uiensis Zone, Poland) with the Danish White Chalk succession. It is proposed that the upper part of the Kazimierz Opoka corresponds to the lower part of the B. kazimiroviensis Zone in Denmark while the lower part of the unit probably corresponds to the upper part of the Belemnitellajunior Zone in Denmark. This correlation, if correct, suggests diachronism of the lower boundary of the B. kazimirouiensis Zone. K e y w o r d s : Maastrichtian, Scaphitidae, ammonites, Poland, Denmark, strati- graphy. Marcin Machalski, Instytut Paleobiologii PAN, al. ~wirkii Wigury 93, PL-02-089 Warszawa, Poland Introduction The Kazirnierz Opoka is an informal lithostratigraphical term (Wyrwicka 1980) for the Late Maastrichtian siliceous chalk unit exposed along the Vistula River near Kazimierz Dolny (called also 'Kazimierz' or 'Kazimierz- -on-Vistula'), Central Poland (Fig. 1A-C). This unit yields possibly one of the richest fossil assemblages known from the European Maastrichtian (see Abdel-Gawad 1986 and Radwariski 1996 for comprehensive review). Ammonites from the Kazimierz Opoka were described by Eopuski (1911 ), Poiaryska (1953), and Blaszkiewicz ( 1980). Radwafiski ( 1996) described predation traces on Hoploscaphites constrictus (J. Sowerby, 1817) whereas Marcinowski & Radwanski (1996) commented on two pachydiscids from the top of Kazimierz Opoka [the specimen identified by them as Anapachydiscus cf.
    [Show full text]
  • Cretaceous Ammonites from the Lower Part of the Matanuska Formation Southern Alaska
    Cretaceous Ammonites From the Lower Part of The Matanuska Formation Southern Alaska By DAVID L. JONES With a STRATIGRAPHIC SUMMARY By ARTHUR GRANT2 GEOLOGICAL SURVEY PROFESSIONAL PAPER 547 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. GS 66-286 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) CONTENTS Page Abstract-----------__-------------------------------- 1 Stratigraphic summary of the lower part of the Matanuska Introduction--------------------------------------- 1 Formation-Continued Mid-Cretaceous faunal sequence in southern Alaska- - - - .. 2 Unit B, sandstone of Cenomanian age-- _---------- 3 Unit C, strata of Cenomanian to Santonian(?) age--- Cenomanian - - - - - - _ - - - - - - - - - - - - - - - - - - - - - - - - - - - - 4 Unit Gl, lutite of Cenomanian to Coniacian or Stratigraphic summary of the lower part of the Matanuska Santonian age-____----------------------- Formation, by Arthur Grants -------_______--------- Unit G2, composite sequence of Coniacian and Unit A, strata of Albian age ...................... Santonian(?) age .......................... Limestone Hills area- - ----____-------------- Regional correlation of the lower part of the Matanuska North front of the Chugach Mountains--- - - - - - Forrnation_____---------------------------------- Matanuska Valley---------_-____---------
    [Show full text]
  • Ammonite Faunal Dynamics Across Bio−Events During the Mid− and Late Cretaceous Along the Russian Pacific Coast
    Ammonite faunal dynamics across bio−events during the mid− and Late Cretaceous along the Russian Pacific coast ELENA A. JAGT−YAZYKOVA Jagt−Yazykova, E.A. 2012. Ammonite faunal dynamics across bio−events during the mid− and Late Cretaceous along the Russian Pacific coast. Acta Palaeontologica Polonica 57 (4): 737–748. The present paper focuses on the evolutionary dynamics of ammonites from sections along the Russian Pacific coast dur− ing the mid− and Late Cretaceous. Changes in ammonite diversity (i.e., disappearance [extinction or emigration], appear− ance [origination or immigration], and total number of species present) constitute the basis for the identification of the main bio−events. The regional diversity curve reflects all global mass extinctions, faunal turnovers, and radiations. In the case of the Pacific coastal regions, such bio−events (which are comparatively easily recognised and have been described in detail), rather than first or last appearance datums of index species, should be used for global correlation. This is because of the high degree of endemism and provinciality of Cretaceous macrofaunas from the Pacific region in general and of ammonites in particular. Key words: Ammonoidea, evolution, bio−events, Cretaceous, Far East Russia, Pacific. Elena A. Jagt−Yazykova [[email protected]], Zakład Paleobiologii, Katedra Biosystematyki, Uniwersytet Opolski, ul. Oleska 22, PL−45−052 Opole, Poland. Received 9 July 2011, accepted 6 March 2012, available online 8 March 2012. Copyright © 2012 E.A. Jagt−Yazykova. This is an open−access article distributed under the terms of the Creative Com− mons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
    [Show full text]
  • (Campanian and Maestrichtian) Ammonites from Southern Alaska
    Upper Cretaceous (Campanian and Maestrichtian) Ammonites From Southern Alaska GEOLOGICAL SURVEY PI SSIONAL PAPER 432 Upper Cretaceous (Campanian and Maestrichtian) Ammonites From Southern Alaska By DAVID L. JONES GEOLOGICAL SURVEY PROFESSIONAL PAPER 432 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows: Jones, David Lawrence, 1930- Upper Cretaceous (Campanian and Maestrichtian) am­ monites from southern Alaska. Washington, U.S. Govt. Print. Off., 1963. iv, 53 p. illus., maps, diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 432) Part of illustrative matter folded in pocket. 1. Amnionoidea. 2. Paleontology-Cretaceous. 3. Paleontology- Alaska. I. Title. (Series) Bibliography: p. 47-^9. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract-__________________________ 1 Comparison with other areas Continued Introduction. ______________________ 1 Vancouver Island, British Columbia.. 13 Stratigraphic summary ______________ 2 California. ______________--_____--- 14 Matanuska Valley-Nelchina area. 2 Western interior of North America. __ 14 Chignik Bay area._____._-._____ 6 Gulf coast area___________-_-_--_-- 15 Herendeen Bay area____________ 8 Madagascar. ______________________ 15 Cape Douglas area______________ 9 Antarctica ________________________ 15 Deposition and ecologic conditions___. 11 Geographic distribution ________________ 16 Age and correlation ________________ 12 Systematic descriptions.________________ 22 Comparison with other areas _ _______ 13 Selected references._________--_---__-__ 47 Japan _________________________ 13 Index._____-______-_----_-------_---- 51 ILLUSTRATIONS [Plates 1-5 in pocket; 6-41 follow index] PLATES 1-3.
    [Show full text]
  • Radiolarians, Benthic Foraminifers, Gastropods and Non-Inoceramid Bivalves, Consisting of Mostly Endemic Species and a Few Cosmopolitan Forms
    Campanian integrated biostratigraphy and palaeocommunities of Sakhalin Island (Far East Russia) 2 3 Elena YAl'fKOVA1, Tatjana ZoNoVA , Ludmila KAZINTsovA YAZVKOVA, E., ZoNovA, T. & KA21NrsovA, L., 2002: Campanian integrated biostratigraphy and palaeocom­ munities of Sakhalin Island (Far East Russia). - In: WAGREICH, M. (Ed.): Aspects of Cretaceous Stratigraphy and Palaeobiogeography. - Österr. Akad. Wiss., Schriftenr. Erdwiss. Komm. 15: 269-292, 7 Figs., Wien. Abstract: The lithology and palaeontology of the Campanian succession of Sakhalin Island is described. The Campanian interval of the Cretaceous succession in Sakhalin Island (Far East Russia) presents a rich record of fairly weil preserved ammonites, inoceramids, radiolarians, benthic foraminifers, gastropods and non-inoceramid bivalves, consisting of mostly endemic species and a few cosmopolitan forms. Changes in the faunal biodiversity were investigated within a context of relative sea-level changes and other environmental changes published elsewhere. The maximum diversity of planktic and nektic groups is established at the base of the lower Campanian. The peak of diversity of benthic groups is recorded at the base of the upper Campanian and associated with high diversity of planktonic groups. The end of the Campanian was a time of low diversity of all faunal groups in the Sakhalin palaeobasin. A high-resolution, integrated biostratigraphic zonation based on ammonites, inoceramids and radiolarians is proposed and correlated with adjacent areas. The zonal scheme comprises four ammonite zones, four inoceramid zones and two radiolarian zones. The definition of the Campanian stage and substage boundaries in Sakhalin and some possibilities for global correlation are discussed: the first occurrence of Anapachydiscus (Neopach­ ydiscus) naumanni (YoKOYAMA) and Desmophyllites diphylloides (FoRBEs) are the main index taxa for the base of the Campanian Stage in Sakhalin; the F.O.
    [Show full text]
  • Guidebook to the Geology of Travis County.Pdf (4.815Mb)
    Page | 1 Guidebook to the Geology of Travis County: Preface Geology of the Austin Area, Travis County, Texas Keith Young When Robert T. Hill first came to Austin, Texas, as the first professor of geology, he described Austin and its surrounding area as an ideal site for a school of geology because it offered such varied outcrops representing rocks of many ages and varieties. Although Hill resigned his position about 85 years ago, the opportunities of the local geology have not changed. Hill (Hill, 1889) implies the intent of writing a series of papers to describe the geology of the local area for all who might be interested. The authors of this volume hope that they have fulfilled in large measure Hill's original intent. No product can ever be all things to all users, but we have presented here common geological phenomenon for many, including the description of an ancient volcano, the description of faulting that occurred in the Austin area in the past, a geologic history of the Austin area, a description of the local rocks, including their classification, field trips for interested observers of the geologic scene, collecting localities for the lovers of fossils, and resource places and agencies. We cannot emphasize enough that many unique geological phenomena are on private property. Please do not trespass, obtain permission. And if permission is not granted, observe from a distance. There are sufficient areas of geologic interest in the Austin area to please all without antagonizing landowners and making it even more difficult for the next person. Page | 2 Guidebook to the Geology of Travis County: Author's Note A useful guide to the geology of the Austin area has long been a goal.
    [Show full text]
  • The Largest Menuites Fresvillensis (Seunes, 1890) (Ammonoidea, Pachydiscidae) from the Maastrichtian Quiriquina Formation, Chile
    Boletín del Museo Nacional de Historia Natural, Chile, 62: 41-50 (2013) THE LARGEST MENUITES FRESVILLENSIS (SEUNES, 1890) (AMMONOIDEA, PACHYDISCIDAE) FROM THE MAASTRICHTIAN QUIRIQUINA FORMATION, CHILE Christian Salazara, Wolfgang Stinnesbeckb and David Rubilar-Rogersa a Área Paleontología, Museo Nacional de Historia Natural, Parque Quinta Normal s/n, Casilla 787, Santiago, Chile; [email protected] b Institut für Geowissenschaften, Universität Heidelberg, INF 234, 69120 Heidelberg, Germany. ABSTRACT The pachydiscid ammonite Menuites fresvillensis, which is known from the Abathomphalus mayaroen- sis planktonic foraminifer zone, is considered an index taxon for the lower part of the Upper Maastrich- tian (Upper Cretaceous), with records from Europe, Australia and South America. Two unusually large specimens are described here one of them being the largest individual ever recorded, with a diameter of 425 mm. Previously, the Quiriquina Formation has yielded specimens that reached diameters of 360 mm. Based on the new material and specimens described previously in the literature, it is now possible to reconstruct the later growth stages of M. fresvillensis, in particular for specimens with diameters >117 and up to 425 mm. These data demonstrate that M. fresvillensis maintains its characteristic mor- phology, albeit slight variations, throughout ontogeny, including the largest specimens described here. Key words: Ammonites, Late Cretaceous, size, South America RESUMEN El más grande Menuites fresvillensis (Seunes, 1890) (Ammonoidea, Pachydiscidae) del Maastri- chtiano de la formación Quiriquina. Menuites fresvillensis (Ammonoidea, Pachydiscidae) existe en la zona de foraminíferos planctónicos Abathomphalus mayaroensis y es considerado un taxon índice para la parte baja del Maastrichtiano Superior (Cretácico Superior), con registros en Europa, Australia y Sudamérica.
    [Show full text]
  • Barremian Rhyncholites (Lower Cretaceous Ammonoidea: Calcified Upper Jaws) from the Serre De Bleyton (Département Drôme, SE France)
    ©Naturhistorisches Museum Wien, download unter www.biologiezentrum.at Ann. Naturhist. Mus. Wien, Serie A 112 627-658 Wien, Juni 2010 Barremian rhyncholites (Lower Cretaceous Ammonoidea: calcified upper jaws) from the Serre de Bleyton (Département Drôme, SE France) By Wolfgang RIEGRAF1 & Gero MOOSLEITNER2 (With 2 figures, 2 plates and 1 table) Manuscript submitted on June 10th 2009, the revised manuscript on January 19th 2010 Abstract Seven calcified upper jaw tips of Rhynchoteuthis astieriana D’ORBIGNY and Palaeoteuthis infira (SHIMANSKY) from the Serre de Bleyton section (Dépt. Drôme, SE France) were redeposited from an outer shelf into an upper slope (upper bathyal) environment embedded in a highly fossiliferous Barremian bioclastic limestone. They represent a low diverse and poor preserved small Barremian pelagic rhyncholite fauna, also described from a few Tethyan and Alpine localities between Cuba, the Crimea, and the Caucasus. Rhynchoteuthis and Palaeoteuthis may most probably represent calcified tips of upper jaws of various taxa of Tethyan ammonites, e.g. of the Phylloceratina (Phyl- loceras, Sowerbyceras), Lytoceratina (Tetragonitidae), and/or some Ammonitina (Arnioceras, Eleganticeras, Hildoceras, Aconeceras). But due to their scarcity, poor preservation, and the allochthonous occurrence, the Serre de Bleyton rhynchoteuthids do not contribute further new knowledge to taxonomy, palaeoecology, stratigraphy or basinal history. Kurzfassung Sieben kalkige Oberkieferspitzen – Rhynchoteuthis astieriana D’ORBIGNY und Palaeoteuthis infira (SHIMANSKY) aus einem Profil der Serre de Bleyton (Dépt. Drôme, SE-Frankreich) – gelangten vom Schelf durch Umlagerung in ein oberbathyales Milieu des oberen Kontinentalabhangs, in einen äußerst fossilreichen bioklastischen Kalkstein. Solche geringdiversen und mäßig erhaltenen pe- lagischen Rhyncholithenfaunen des Barremium sind auch von vereinzelten tethyalen und alpinen Fundorten zwischen Kuba, der Krim und dem Kaukasus beschrieben.
    [Show full text]
  • Upper Campanian Ammonites from the Gschliefgraben
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Beiträge zur Paläontologie Jahr/Year: 1984 Band/Volume: 11 Autor(en)/Author(s): Kennedy William James, Summesberger Herbert Artikel/Article: Upper Campanian Ammonites from the Gschliefgraben (Ultrahelvetic, Upper Austria) 149-206 ©Verein zur Förderung der Paläontologie am Institut für Paläontologie, Geozentrum Wien Beitr. Paläont. österr., 11, 149-206, Wien 1984 Upper Campanian Ammonites from the Gschliefgraben (Ultrahelvetic, Upper Austria) Obercampane Ammoniten aus dem Ultrahelvetikum des Gschliefgrabens (Oberösterreich). by William James KENNEDY* and Herbert SUMMESBERGER** KENNEDY, W. J. and SUMMESBERGER, H. 1984: Upper Campanian Ammonites from the Gschliefgraben (Ultrahelvetic, Upper Austria). - Beitr. Paläont. Österr., 11:149-206, Wien. Abstract The Upper Campanian shales and limestones of the Gschliefgraben, Upper Austria, contain a rich and diverse fauna including the following species: Phylloceras (Hypophylloceras) sp., Saghalinites sp. cf. cala. (FORBES, 1846), Tetragonites cf. obscurus (SCHLÜTER, 1872, Gaudrycc- ras jukesii (SHARPE, 1857), Puzosiinae in d et DesmophyHites larteti (SEUNES, 1891), Hauericeras fayoli DE GROSSOUVRE, 1894 , Pachydiscus (Pachydiscus) haldemsis (SCHLÜTER, 1867), Pachy- discus (Pachydiscus) perfidus DE GROSSOUVRE, 1894, Pachy discus (Pachydiscus) cf. subrobustus SEUNES, 1891, Anapachydiscus arrialoorensis (STOLICZKA, 1865), Nostoceras (Nostoceras) sp., Nostoceras
    [Show full text]