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Toarcian, Aalenian and Early Bajocian (Jurassic)

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S T U D I A G E O L O G I C A P O L O N I C A Vol. 123, Kraków 2004, pp. 7–131. Geology of the Pieniny Klippen Belt and the Tatra Mts, Carpathians Edited by K. Birkenmajer Part XVII Ryszard MYCZYÑSKI 1 Toarcian, Aalenian and Early Bajocian (Jurassic) ammonite faunas and biostratigraphy in the Pieniny Klippen Belt and the Tatra Mts, West Carpathians2 (Figs 1–39; Tabs 1–5) Abstract. The ammonite faunas here described were derived from the Toarcian (Lower Jurassic) and Lower Bajocian (Middle Jurassic) strata of the Pieniny Klippen Belt and the Lower Subtatric Succession, Polish Tatra Mts (West Carpathians). The ammonites belong to the families: Phyllo- ceratidae, Lytoceratidae, Hildoceratidae, Graphoceratidae, Hammatoceratidae, Sonniniidae, Otoiti- dae and Stephanoceratidae. The associated bivalve faunule is represented by the families Inocera- midae and ?Posidoniidae. Stratigraphic evaluation of the ammonite assemblages helped to redefine age ranges of some lithostratigraphic units in the Pieniny Klippen Belt and the Lower Subtatric Succession, Tatra Mts. Key words: Pieniny Klippen Belt, Tatra Mts, biostratigraphy, Early-Middle Jurassic, ammonites, bivalves. INTRODUCTION The paper presents systematic description and stratigraphic evaluation of new Toarcian through Early Bajocian ammonite and bivalve faunas from the Pieniny Klippen Belt, Polish part (Figs 1, 2), and the Lower Subtatric Nappe, Polish Tatra Mts (Fig. 8), West Carpathians. The specimens elaborated are housed in the Insti- tute of Geological Sciences, Polish Academy of Sciences, Twarda 51/55, 00-818 Warszawa. 1 Institute of Geological Sciences, Polish Academy of Sciences, ul. Twarda 51/55, 00-818 Warszawa, Poland. E-mail: [email protected] 2 Manuscript accepted for publication July 15, 2004. 8 R. MYCZYÑSKI Collections: Ba – Brzeziny II: site 39 (Podskalnia Shale Mbr), coll. R. Myczyñski Br – Brzeziny I: site 38d (Podskalnia Shale Mbr), coll. R. Myczyñski Brb – Brzeziny I: site 38b (Skalnite Marlstone Mbr), coll. R. Myczyñski Brt – Brzeziny I: site 38b (Skalnite Marlstone Mbr), coll. R. Myczyñski CS – site 8 (Krempachy Marl Fm.), coll. R. Myczyñski Cz – Czorsztyn Castle (Skrzypny Shale Fm; loc.: see Birkenmajer, 1963a), coll. L. Watycha Czor. – site 33 (Krempachy Marl Fm.), coll. R. Myczyñski D – site 21 (Krempachy Marl Fm.), coll. R. Myczyñski FiP – site 36 (So³tysia Marlstone Fm.), coll. R. Myczyñski G, GAc – sites 12, 13 (Podzamcze Limstone Fm.), coll. R. Myczyñski HW – site Czorsztyn Castle (Skrzypny Shale Fm.), coll. H. Wierzbowski K – site 31 (Krempachy Marl Fm.), coll. R. Myczyñski KB – sites 21; 23–26; W of Hedeki Wierch (Krempachy Marl Fm., Skrzypny Shale Fm.), coll. K. Birkenmajer Kob – site 38a (Koby³a Limestone Mbr), coll. R. Myczyñski Kp – sites 14–17 (Skrzypny Shale Fm.), coll. R. Myczyñski KrP – site 30 (Skrzypny Shale Fm.), coll. R. Myczyñski KSB – site 23 (Skrzypny Shale Fm.), coll. R. Myczyñski LW – Czorsztyn Castle (Krempachy Marl Fm.; loc.: see Birkenmajer, 1963a), coll. L. Watycha Mc – sites 2–11 (Homole Gorge area: Krempachy Marl Fm., Skrzypny Shale Fm., Harcygrund Shale Fm., Podzamcze Limestone Fm.), coll. R. Myczyñski N – site 28 (Skrzypny Shale Fm.), coll. R. Myczyñski SB – site 23 (Skrzypny Shale Fm.), coll. R. Myczyñski SKA – site Pieniñski Stream (Pliensbachian limestones; loc.: Horwitz, 1937; Birkenmajer & Myczyñski, 1994), coll. R. Myczyñski WS – site 22 (Podzamcze Limestone Fm. – after K. Birkenmajer, personal information, 2004), coll. R. Myczyñski ZA – site 33 (Krempachy Marl Fm.), coll. R. Myczyñski ZN – site 25 (Skrzypny Shale Fm.), coll. R. Myczyñski. PIENINY KLIPPEN BELT: LITHOSTRATIGRAPHIC UNITS SAMPLED In the Pieniny Klippen Belt of Poland, new ammonite and bivalve faunas have been collected from the Toarcian through Lower Bajocian deposits belonging mainly to the Czorsztyn-, Niedzica- and Czertezik successions, partly also to the Branisko and the Pieniny successions (sensu Birkenmajer, 1977). Their location in the field is shown in Figs 1 and 2. The following lithostratigraphic units were sampled: (1) the Krempachy Marl Formation; (2) the Skrzypny Shale Formation; (3) the Harcygrund Shale Forma- tion; (4) the Podzamcze Limestone Formation (for formal description of these units – see Birkenmajer, 1977). Stratigraphic evaluation of the ammonite and bivalve faunas described in this paper (see below), have allowed to revise stratigraphic boundaries of the above units. Remark: Palaeontological determination and stratigraphic evaluation of an am- monite fauna from the Upper Pliensbachian “spotty limestone” (informal unit) of the Pieniny Succession (see Birkenmajer, 1977), including a revision of that col- AMMONITE FAUNAS AND BIOSTRATIGRAPHY 9 Latvia CRACOW A F O R E D E B a l t i c S e a Lithuania E P N D RS L A R E CARPAT F O ER HIA sia T NS us U L A N lor O P O D ye BORISLAV G e r m a n y B WARSAW B Czech AR CRACOW Ukraine R C PAT Republic A E HI k N AN va blic IN S Slo epu BRATISLAVA Austria R Hungary Italy Romania 0 100 km BUDAPEST D NOWY TARG u n B Dun a 0 5 10 km aje je 33 c 23 c 32 29 -26 35 -30 14 21 CZORSZTYN 22 -17 1a-c ZASKALE SZCZAWNICA NIEDZICA ROGONIK KREMPACHY FALSZTYN CASTLE JAWORKI SOBCZAÑSKI SZAFLARY GORGE Y E 34 N ka L 31 I an O c N pi M e u m O BIA£A j EE Kr ea na tr H WODA u ka I S D a³ 27 ³y Bi P ia B -28 10 4-5 18-20 2-3 9, 11 6-8 - 1 - 2 - 3 - 4 31 - 5 RS - 6 Fig. 1. A. Location of the Pieniny Klippen Belt (in black) within the Carpathians (adapted from Birkenmajer, 1963a, 1977); box – area shown in fig. 1B. B. Faunal site location in the Pieniny Klippe Belt; 1 – Magura Nappe (Palaeogene flysch); 2 – Podhale Palaeogene (Palaeogene flysch); 3 – Pieniny Klippen Belt; 4 – northern and southern tectonic boundaries of the Pieniny Klippen Belt; 5 – faunal sites 1–35 (as described in the text); 6 – Republic of Russia lected and determined by Horwitz (1937), has been published by Birkenmajer and Myczyñski (1994). (1) Krempachy Marl Formation This formal lithostratigraphic unit includes spotty, grey, grey-bluish marls and marly-shaly limestones which occur mainly in the Czorsztyn-, Czertezik-, Nie- dzica- and the Branisko successions (Birkenmajer, 1977, 1979). Previously, this unit was being described under the name of the “Opalinum marls”, mainly from the Czorsztyn Succession (see Birkenmajer, 1958, 1963a, b, 1970a, 1977). In the Czorsztyn Succession (northernmost unit of the Pieniny Klippen Belt ba- sin), the rocks are light-grey, becoming darker-coloured in the more southern ones – the Czertezik – through the Branisko successions. They show numerous traces of bioturbation (e.g., Tyszka, 1991). Crinoid-filament-spiculite miocrofacies pre- dominates in the marly limestones. Based on stratigraphic evaluation of previously published faunas, Birkenmajer (1963a, b, 1977) proposed a Late Pliensbachian (Domerian) through lowest Late 10 R. MYCZYÑSKI y tar S a k d ok Grajc to o Pot are o W k P a rn a Cierchliska z P JAW O R K I C o k a to k o £ê G t k g r o o na i aj P t bi ca 14 u re o z z e k P an R o Ubocz 15 C m i to £a ³k a k o³tys 16 ka w B B I A £ A S ia S rio ia ka³a sa ³a ia S Pi W O D A tok Sztoln W Po 17 W o d ¹ a 1a w ó z 1b H 1c olegow o Sm a Krupianka m a G a r b P k o o n l ia e to p C k ru z k K S a S to k ja k o a P Czerwona k a ³ l a o s Ska³a w k P i a o t ski o ow k oni 8 Konio- K K k 9 a o lakow m wiec t etry sk o P a io 7 S P ka³a n z S k c 4 a ze 6 pan 10 11 18 ówka 19 3 20 G a 5 c 12 ó ka w 2 ws k ³o a aw ³a Polana P ka rœ S Cy la 13 Kiczery Durbaszka Polana S tach Pod Wysok¹ ur ów 0 1 km S L O V A K R E P U B L I C ka Fig. 2. Faunal sites 1–20 (see the text) in the Pieniny Klippen Belt between Bia³a Woda and Jaworki (base map adapted from Birkenmajer, 1970a, fig. 2) Aalenian age for the Krempachy Marl Formation. The best documented ammonite zones were: the Pleydellia aalensis Subzone (Late Toarcian); the Leioceras opalinum Zone and the Tmetoceras scissum Zone (Early Aalenian). (2) Skrzypny Shale Formation This formal lithostratigraphic unit includes black and dark-grey/bluish shales with spherosiderite (sideroplesite – see Birkenmajer & Narêbski, 1958) concre- tions. The unit occurs in most stratigraphic successions of the Pieniny Klippen Belt basin, from the Czorsztyn Succession in north, through the Pieniny Succession in the south (see Birkenmajer, 1977). Previously, this lithostratigraphic unit was known under the name of the “Murchisonae shales” (see Birkenmajer, 1958, 1963a, b, 1977). Based on stratigraphic evaluation of previously published faunas from the Czorsztyn Succession, a Late Aalenian through Middle Bajocian age was accepted (Birkenmajer, 1963a, b, 1977). The best documented ammonite zones were: the AMMONITE FAUNAS AND BIOSTRATIGRAPHY 11 Ludwigia murchisonae and the Graphoceras concavum zones (Late Aalenian); and the Sonninia sowerbyi and the Otoites sauzei zones (lower and middle zones of Middle Bajocian – see Birkenmajer, 1963a, b, 1977). (3) Harcygrund Shale Formation This formal lithostratigraphic unit occurs mainly in the basinal Branisko and Pi- eniny successions, moreover in the basinal Magura Succession (Grajcarek Unit) of the Pieniny Klippen Belt (Birkenmajer, 1977).
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  • Front Matter (PDF)

    Front Matter (PDF)

    THE QUARTERLY JOURNAL OF THE GEOLOGICAL SOCIETY OF LONDON Quod si cui mortalium cordi et cur~e sit, non tantum inventis h~erere atque iis uti, sed ad ulteriora penetrare ; atque non disputando adversarium, sed opere naturam vincere ; denique non belle et probabiliter opinari, sed certo et ostensive scire; tales, tanquam veri scientiarum filii, nobis (si videbitur) se adjungant ; ut omissis natur~e atriis, qu~e infiniti contriverunt, aditus aliquando ad interiora patefiat.--Novum Organum, Prefatio. VOLUME XCV FOR I939 LONDON : LONGMANS, GREEN & CO. LTD. PARIS : CHARLES KLINCKSIECK~ I I RUE DE LILLE. SOLD ALSO AT THE APARTMENTS OF THE SOCIETY~ BURLINGTON HOUSE~ W.I, I94O GEOLOGICAL SOCIETY OF LONDON LIST OF THE OFFICERS AND COUNCIL Elected February 17th, 1939 PRESIDENT Prof. Henry Hurd Swinnerton, D.Sc. VIcE-PRESIDENTS Edward Battersby Bailey, M.C.M.A. Prof. Owen Thomas Jones, M.A.D.Se. D.Sc. F.R.S. F.R.S. Prof. William George Fearnsides, M.A. Prof. Cecil Edgar Tilley, Ph.D.B.Se. F.R.S. F.R.S. S ECR~.TARIES Leonard Hawkes, D.Sc. } Prof. William Bernard Robinson King, I O.B.E, M.A. Sc.D. FOREIGN SECRETARY Sir Arthur Smith Woodward, LL.D.F.R.S.F.L.S. TR]iASURHR Frederick Noel Ashcroft, M.A.F.C.S. COUNCIL William Joseelyn Arkell, M.A.D.Sc. Prof. Owen Thomas Jones, M.A.D.Se. D.Phil. F.R.S. Frederick Noel Ashcroft, M.A.F.C.S. Prof. William Bernard Robinson King, Edward Battersby Bailey, M.C.M.A. O.B.E.M.A.
  • Early Bajocian Type Sonniniids and Hammatoceratids SW Germany

    Early Bajocian Type Sonniniids and Hammatoceratids SW Germany

    Boletín del Instituto de Fisiografía y Geología 91, 2021 1 New information on the Early Bajocian types of sonniniids and hammatoceratids (Ammonitina) described by W. Waagen (1867) from Gingen/Fils (SW Germany) Driss Sadki & Volker Dietze Sadki D. & Dietze V., 2021. New information on the Early Bajocian types of sonniniids and hammatoceratids (Ammonitina) described by W. Waagen (1867) from Gingen/Fils (SW Germany). Boletín del Instituto de Fisiografía y Geología 91: 1-16. Rosario, 08/05/2021. ISSN 1666-115X. Abstract. The type specimens of the species of sonniniids and hammatoceratids (Ammonitina) from the Lower Bajocian of Gingen/Fils (SW Germany) described by Waagen in 1867, and deposited in the Bavarian State Collection for Palaeontology and Geology in Munich, are revised. They are referred to the morphogenera Euhoploceras, Shirbuirnia, Papilliceras, Sonninia, Witchellia, and Fissilobiceras: E. adicrum (Waagen, 1867), E. polyacanthum (Waagen, 1867), E. mayeri (Waagen, 1867), S. gingensis (Waagen, 1867), P. mesacanthum (Waagen, 1867), S. patella (Waagen, 1867), W. jugifera (Waagen, 1867), and F. fissilobatum (Waagen, 1867). A lectotype is designated for E. Recibido 17/09/2020 Aceptado 29/10/2020 mayeri (Waagen, 1867). Keywords: Sonniniidae ▪ Hammatoceratidae ▪ Ammonitina ▪ Middle Jurassic ▪ Lower Bajocian ▪ W. Waagen ▪ Disponible vía Internet Southwest Germany. & versión impresa 08/05/2021 Resumen. Nueva información sobre los tipos de sonníniidos y hammatocerátidos (Ammonitina, Cephalopoda) del Editor: H. Parent Bajociano Inferior de Gingen/Fils (SO de Alemania) descriptos por W. Waagen (1867). Los especímenes tipo de sonníniidos y hammatocerátidos (Ammonitina) del Bajociano Inferior de Gingen/Fils (SO de Alemania) descriptos por Waagen en 1867, actualmente depositados en el Bayerischen Staatssammlung für Paläontologie und Geologie in München, son revisados y referidos a los morfogéneros Euhoploceras, Shirbuirnia, Papilliceras, Sonninia, Witchellia, y Fissilobiceras: E.
  • Upper Jurassic Mollusks from Eastern Oregon and Western Idaho

    Upper Jurassic Mollusks from Eastern Oregon and Western Idaho

    Upper Jurassic Mollusks from Eastern Oregon and Western Idaho GEOLOGICAL SURVEY PROFESSIONAL PAPER 483-D Upper Jurassic Mollusks from Eastern Oregon and Western Idaho By RALPH W. IMLAY CONTRIBUTIONS TO PALEONTOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 483-D Faunal evidence for the presence of Upper Jurassic sedimentary rocks in eastern Oregon and westernmost Idaho UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 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, D.C. 20402 CONTENTS Page Abstract.__________________________________________ Dl Ages and correlations Continued Introduction.______________________________________ 1 Trowbridge Formation of Lupher, 1941, in east- Biologic analysis..._________________________________ 2 central Oregon.__________---_-_-__-_-____---_ D9 Stratigraphic summary._____________________________ 2 Lonesome Formation of Lupher, 1941, in east-central Northeastern Oregon and adjoining Idaho. ________ 2 Oregon..________________-_--_____--_--_---__ 9 Mineral area, western Idaho.____________________ 2 Comparisons with other faunas.______________________ 10 East-central Oregon_____________________________ 4 Alaska and western British Columbia-____________ 10 Conditions of deposition.____________________________ 6 Calif ornia. ... _ __-_________--____-___-__---___-_ 10 Ages and correlations______________________________ 6 Unnamed beds in northeastern Oregon and adjoining Western interior of North America._______________ 10 Idaho_______________________________________ Geographic distribution________-_-_____---_---_-.__ 11 Unnamed beds near Mineral, Idaho.______________ Systematic descriptions..._--_--__-__________________ 13 Snowshoe Formation of Lupher, 1941, in east-central Literature cited_____-__-_____---------_-_--_--__-___ 17 Oregon._____________________________________ Index_.______________--____---------_-__---_-_-___ 21 ILLUSTRATIONS [Plates 1-4 follow index] PLATE 1.
  • The Graphoceratid Ammonite Succession in the Aalenian and Lowest Bajocian (Middle Jurassic) at Horn Park, Dorset, UK ROBERT B

    The Graphoceratid Ammonite Succession in the Aalenian and Lowest Bajocian (Middle Jurassic) at Horn Park, Dorset, UK ROBERT B

    The Graphoceratid Ammonite Succession in the Aalenian and lowest Bajocian (Middle Jurassic) at Horn Park, Dorset, UK ROBERT B. CHANDLER Riddlesdown High School, Purley, Surrey, CR8 lEX Summary In 1990 Callomon and Chandler set out a scheme of 16 faunal horizons for the Aalenian-Lower Bajocian of Dorset and Somerset based principally on graphoceratid ammonites. One locality, Horn Park, stands apart in displaying strata from almost all the horizons identified in that work. Yet little material from it has ever been figured. Here a section is given together with exhaustive tables of existing nominal morphospecies collected at each level and with figures that allow the variability of the suc- cessive, probably in most cases, monobiospecific assemblages to be assessed. A revised generic classification of the Graphoceratidae is presented. them precludes almost any satisfactory discussion of phyletic relationships and hence of the overall evolution The highly discontinuous, condensed and rapidly of the group. varying development of the Inferior Oolite in southern England was first perceived by S.S. Buckman (e.g. 1891, The biostratigraphy of the Graphoceratidae has now 1893, 1910) during his attempts to correlate sections by been rather well documented, for example by Rocha et means of ammonites. Leading amongst these in al. (1990), Henriques (1992; et al. 1994) in Portugal; the Aalenian part of the succession are the Linares and Sandoval (1990) in Spain, Sadki (1994) in Graphoceratidae, including such well known genera as Morocco. In Britain, Morton (1990; 1994) and Morton Leioceras, Ludwigia, Brasilia, Graphoceras and and Hudson (1995) have described the succession in Hyperlioceras. Scotland and compared it with Dorset (Morton and Chandler 1994).