Taxa Dedicated to Alberto C. Riccardi
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Abelisaurus Comahuensis 321 Acanthodiscus Sp. 60, 64
Index Page numbers in italic denote figure. Page numbers in bold denote tables. Abelisaurus comahuensis 321 structure 45-50 Acanthodiscus sp. 60, 64 Andean Fold and Thrust Belt 37-53 Acantholissonia gerthi 61 tectonic evolution 50-53 aeolian facies tectonic framework 39 Huitrin Formation 145, 151-152, 157 Andes, Neuqu6n 2, 3, 5, 6 Troncoso Member 163-164, 167, 168 morphostructural units 38 aeolian systems, flooded 168, 169, 170, 172, stratigraphy 40 174-182 tectonic evolution, 15-32, 37-39, 51 Aeolosaurus 318 interaction with Neuqu6n Basin 29-30 Aetostreon 200, 305 Andes, topography 37 Afropollis 76 Andesaurus delgadoi 318, 320 Agrio Fold and Thrust Belt 3, 16, 18, 29, 30 andesite 21, 23, 26, 42, 44 development 41 anoxia see dysoxia-anoxia stratigraphy 39-40, 40, 42 Aphrodina 199 structure 39, 42-44, 47 Aphrodina quintucoensis 302 uplift Late Cretaceous 43-44 Aptea notialis 75 Agrio Formation Araucariacites australis 74, 75, 76 ammonite biostratigraphy 58, 61, 63, 65, 66, Araucarioxylon 95,273-276 67 arc morphostructural units 38 bedding cycles 232, 234-247 Arenicolites 193, 196 calcareous nannofossil biostratigraphy 68, 71, Argentiniceras noduliferum 62 72 biozone 58, 61 highstand systems tract 154 Asteriacites 90, 91,270 lithofacies 295,296, 297, 298-302 Asterosoma 86 92 marine facies 142-143, 144, 153 Auca Mahuida volcano 25, 30 organic facies 251-263 Aucasaurus garridoi 321 palaeoecology 310, 311,312 Auquilco evaporites 42 palaeoenvironment 309- 310, 311, Avil6 Member 141,253, 298 312-313 ammonites 66 palynomorph biostratigraphy 74, -
Contributions in BIOLOGY and GEOLOGY
MILWAUKEE PUBLIC MUSEUM Contributions In BIOLOGY and GEOLOGY Number 51 November 29, 1982 A Compendium of Fossil Marine Families J. John Sepkoski, Jr. MILWAUKEE PUBLIC MUSEUM Contributions in BIOLOGY and GEOLOGY Number 51 November 29, 1982 A COMPENDIUM OF FOSSIL MARINE FAMILIES J. JOHN SEPKOSKI, JR. Department of the Geophysical Sciences University of Chicago REVIEWERS FOR THIS PUBLICATION: Robert Gernant, University of Wisconsin-Milwaukee David M. Raup, Field Museum of Natural History Frederick R. Schram, San Diego Natural History Museum Peter M. Sheehan, Milwaukee Public Museum ISBN 0-893260-081-9 Milwaukee Public Museum Press Published by the Order of the Board of Trustees CONTENTS Abstract ---- ---------- -- - ----------------------- 2 Introduction -- --- -- ------ - - - ------- - ----------- - - - 2 Compendium ----------------------------- -- ------ 6 Protozoa ----- - ------- - - - -- -- - -------- - ------ - 6 Porifera------------- --- ---------------------- 9 Archaeocyatha -- - ------ - ------ - - -- ---------- - - - - 14 Coelenterata -- - -- --- -- - - -- - - - - -- - -- - -- - - -- -- - -- 17 Platyhelminthes - - -- - - - -- - - -- - -- - -- - -- -- --- - - - - - - 24 Rhynchocoela - ---- - - - - ---- --- ---- - - ----------- - 24 Priapulida ------ ---- - - - - -- - - -- - ------ - -- ------ 24 Nematoda - -- - --- --- -- - -- --- - -- --- ---- -- - - -- -- 24 Mollusca ------------- --- --------------- ------ 24 Sipunculida ---------- --- ------------ ---- -- --- - 46 Echiurida ------ - --- - - - - - --- --- - -- --- - -- - - --- -
Abhandlungen Der Geologischen Bundesanstalt in Wien
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Abhandlungen der Geologischen Bundesanstalt in Wien Jahr/Year: 2017 Band/Volume: 71 Autor(en)/Author(s): Summesberger Herbert, Kennedy William James, Skoumal Peter Artikel/Article: Early and middle Santonian Cephalopods from the Gosau Group (Upper Cretaceous, Austria) 1. Nautiloidea and non-heteromorph Ammonoidea 5-99 ABHANDLUNGEN DER GEOLOGISCHEN BUNDESANSTALT Abh. Geol. B.-A. ISSN 0378-0864 ISBN 978-3-85316-093-0 Band 71 S. 5–99 Wien, Oktober 2017 Early and middle Santonian Cephalopods from the Gosau Group (Upper Cretaceous, Austria) 1. Nautiloidea and non-heteromorph Ammonoidea HERBERT SUMMESBERGER1, WILLIAM J. KENNEDY2 & PETER SKOUMAL3 13 Text-Figures, 16 Tables, 23 Plates Österreichische Karte 1:50.000 BMN / UTM 76 Wiener Neustadt / NL 33-03-01 Wiener Neustadt revision 89 Angath / NL 32-03-18 Kundl description 90 Kufstein / NL 33-01-13 Kufstein Cephalopoda 95 Sankt Wolfgang im Salzkammergut / NL 33-01-17 Hallstatt Santonian 96 Bad Ischl / NL 33-01-11 Bad Ischl Gosau Group 98 Liezen / NL 33-02-07 Windischgarsten 99 Rottenmann / NL 33-02-08 Spital am Pyhrn 120 Wörgl Contents Abstract ................................................................................................. 5 Zusammenfassung ......................................................................................... 6 Introduction.............................................................................................. -
Ammonites from Bathonian and Callovian (Middle Jurassic)
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Universität München: Elektronischen Publikationen 253 Zitteliana 89 Ammonites from Bathonian and Callovian (Middle Jurassic) North of Damghan, Paläontologie Bayerische EasternGeoBio- Alborz, North Iran & Geobiologie Staatssammlung Center LMU München LMU München für Paläontologie und Geologie Kazem Seyed-Emami1* & Ahmad Raoufian2 München, 01.07.2017 1School of Mining Engineering, University College of Engineering, University of Tehran, Manuscript received P.O. Box 11365-4563, Tehran, Iran 2 26.09.2016; revision Daneshvar Center, Farhangian University, Neyshapour, Iran accepted 30.10.2016 *Corresponding author; E-mail: [email protected] ISSN 0373-9627 ISBN 978-3-946705-00-0 Zitteliana 89, 253–270. Abstract The following Middle Jurassic ammonite families (subfamilies) are described from the Dalichai Formation north of Damghan (eastern Alborz), some of them for the first time: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Stephanoceratidae (Cadomitinae), Tulitidae and Reineckeiidae. The fauna is typically Northwest-Tethyan and closely related to Central Europe (Subboreal – Submediterra- nean Provinces). Key words: Ammonites, Dalichai Formation, Middle Jurassic, Alborz, Iran Zusammenfassung Aus der Dalichai Formation nördlich von Damghan (Ostalborz) werden einige mitteljurassische Ammoniten, teils zum ersten Mal, beschrieben. Folgende Familien und Unterfamilien sind vertreten: Phylloceratidae, Lytoceratidae, Oppeliidae (Hecticoceratinae), Steph- anoceratidae (Cadomitinae), Tulitidae und Reineckeiidae. Die Fauna ist typisch für die Nordwest-Tethys und zeigt enge Beziehungen zu Zentraleuropa (Subboreale und Submediterrane Faunenprovinz). Schlüsselwörter: Ammoniten, Dalichai Formation, Mittlerer Jura, Alborz, Iran Introduction the frame of a MSc. thesis. For the present study, a new section nearby was chosen and collections The present study is a continuation of a larger re- were made by A. -
New Data on the Stratigraphy of the Lower Cretaceous of the Gerecse Mts
New data on the stratigraphy of the Lower Cretaceous of the Gerecse Mts. (Hungary) and the Lackbach section (Austria) 1 llona Bo0Roc1 , Attila FoGARAs1 2 This paper is dedicated to the memory of C. F. WE101cH (7'" Nov. 1952-10'" Nov. 1992) Bo0Roc1, 1. & foGARASI, A., 2002: New data on the stratigraphy of the Lower Cretaceous of the Gerecse Mts. (Hungary) and the Lackbach section (Austria). - In: WAGREICH, M. (Ed.): Aspects of Cretaceous Stratigraphy and Palaeobiogeography. - Österr. Akad. Wiss„ Schriftenr. Erdwiss. Komm. 15: 295-313, 4 Figs., 3 Pis., Wien. Abstract: Biostratigraphie and lithostratigraphic studies have been made on four boreholes (Ago styan Agt-2, Neszmely N-4, Tatabänya Ta-1472, Ta-1486) in the Gerecse Mts. and the Tatabanya basin in Hungary. The Lower Cretaceous succession of this area comprises the Neszmely Sandstone Formation (NSF, Barremian-Aptian), the Tata Limestone Formation(TLF, Aptian) and the Vertes som16 Formation (VF, Lower and Middle Albian). In its stratotype, borehole N-4, the NSF was subdivided into four integrated ammonite and planktonic foraminifera zones from top to bottom: The Ticinella bejaouensis ivz - Hedbergella gorbachikae ivz (Late Aptian - ?Early Albian), the G/obigerinelloides algerianus trz (early Late Aptian), the Shackoina cabrii trz - Globigerinelloides blowi ivz (Early and Mid Aptian), and the Hedbergella sigali ivz (Barremian). In the lower and middle part of the Sh. cabrii trz - GI. blowi ivz the ammonites Procheloniceras albrechtiaustriae HoH., Pseudosaynella ex gr. matheronites (o'ORBIGNY), and Barremites difficilis (o'ORBIGNY) indicate the Early Aptian Deshayesites weissi ammonite Zone. In the H. sigali ivz Costidiscus redicostatus (o'ORBIGNY) and Spitidiscus vandeckii (o'ORBIGNY) give evidence for a Barremian age. -
Composition and Origin of Jurassic Ammonite Concretions at Gerzen, Germany
JURASSIC AMMONITE CONCRETIONS COMPOSITION AND ORIGIN OF JURASSIC AMMONITE CONCRETIONS AT GERZEN, GERMANY. By MICHAEL DAVID GERAGHTY, B.Sc. A Thesis Submitted to the School of Graduate Studies in Partial Fulfilment of the Requirements for the Degree Master of Science McMaster University (c) Copyright by Michael David Geraghty, April 1990 MASTER OF SCIENCE (1990) McMaster University (Geology) Hamilton, Ontario TITLE: Composition and Origin of Jurassic Ammonite Concretions at Gerzen, Germany. AUTHOR: Michael David Geraghty, B. Sc. (University of Guelph) SUPERVISOR: Professor G.E.G. Westermann NUMBER OF PAGES: xiii, 154, 17 Figs., 10 Pls. ii ACKNOWLEDGEMENTS I would like to express my sincere gratitude to Dr. Gerd Westermann for allowing me the privilege of studying under his supervision on a most interesting research project. His advice, support and patience were greatly appreciated. I deeply indebted to Mr. Klaus Banike of Gottingen, F. R. Germany for opening his home and his collection of concretions to me and also for his help and friendship. To Erhardt Trute and Family of Gerzen, F.R. Germany, I owe many thanks for their warm hospitality and assistance with my field work. Also Dr. Hans Jahnke of Georg-August University, Gottingen deserves thanks for his assistance and guidance. Jack Whorwood's photographic expertise was invaluable and Len Zwicker did an excellent job of preparing my thin sections. Also, Kathie Wright did a great job helping me prepare my figures. Lastly, I would like to thank all those people, they know who they are, from whom I begged and borrowed time, equipment and advice. iii ABSTRACT Study of the ecology of concretion and host sediment fossils from a shell bed in middle Bajocian clays of northwestern Germany indicates a predominantly epifaunal suspension-feeding community living on a firm mud bottom. -
U-Pb Geochronology and Paleogeography of the Valanginian– Hauterivian Neuquén Basin: Implications for Gondwana-Scale
Research Paper GEOSPHERE U-Pb geochronology and paleogeography of the Valanginian– Hauterivian Neuquén Basin: Implications for Gondwana-scale GEOSPHERE, v. 17, no. 1 source areas https://doi.org/10.1130/GES02284.1 E. Schwarz1,*, E.S. Finzel2,*, G.D. Veiga1, C.W. Rapela1, C. Echevarria3,*, and L.A. Spalletti1 1Centro de Investigaciones Geológicas (Universidad Nacional de La Plata–Consejo Nacional de Investigaciones Científicas y Técnicas [CONICET]), Diagonal 113 #256 B1904DPK, La Plata, Argentina 13 figures; 2 tables; 1 set of supplemental files 2Earth and Environmental Science Department, University of Iowa, 115 Trowbridge Hall, Iowa City, Iowa 52242, USA 3Pampa Energía S.A. Gerencia Tight, Dirección de E&P, J.J. Lastra 6000, 8300 Neuquén, Argentina CORRESPONDENCE: [email protected] ABSTRACT starting in the mid-continent region of south- Early Cretaceous was the Neuquén Basin, which CITATION: Schwarz, E., Finzel, E.S., Veiga, G.D., western Gondwana and by effective sorting, was during that time was a backarc basin separated Rapela, C.W., Echevarria, C., and Spalletti, L.A., Sedimentary basins located at the margins bringing fine-grained or finer caliber sand to the from the proto–Pacific Ocean (i.e., to the west) by 2021, U-Pb geochronology and paleogeography of the of continents act as the final base level for con- Neuquén Basin shoreline. This delivery system was a discontinuous volcanic arc (Howell et al., 2005). Valanginian–Hauterivian Neuquén Basin: Implications for Gondwana-scale source areas: Geosphere, v. 17, tinental-scale catchments that are sometimes probably active (though not necessarily continu- This marine basin was bounded by the Sierra no. -
Paleontological Contributions
THE UNIVERSITY OF KANSAS PALEONTOLOGICAL CONTRIBUTIONS May 15, 1970 Paper 47 SIGNIFICANCE OF SUTURES IN PHYLOGENY OF AMMONOIDEA JURGEN KULLMANN AND JOST WIEDMANN Universinit Tubingen, Germany ABSTRACT Because of their complex structure ammonoid sutures offer best possibilities for the recognition of homologies. Sutures comprise a set of individual elements, which may be changed during the course of ontogeny and phylogeny as a result of heterotopy, hetero- morphy, and heterochrony. By means of a morphogenetic symbol terminology, sutural formulas may be established which show the composition of adult sutures as well as their ontogenetic development. WEDEKIND ' S terminology system is preferred because it is the oldest and morphogenetically the most consequent, whereas RUZHENTSEV ' S system seems to be inadequate because of its usage of different symbols for homologous elements. WEDEKIND ' S system includes only five symbols: E (for external lobe), L (for lateral lobe), I (for internal lobe), A (for adventitious lobe), U (for umbilical lobe). Investigations on ontogenetic development show that all taxonomic groups of the entire superorder Ammonoidea can be compared one with another by means of their sutural development, expressed by their sutural formulas. Most of the higher and many of the lower taxa can be solely characterized and arranged in phylogenetic relationship by use of their sutural formulas. INTRODUCTION Today very few ammonoid workers doubt the (e.g., conch shape, sculpture, growth lines) rep- importance of sutures as indication of ammonoid resent less complicated structures; therefore, phylogeny. The considerable advances in our numerous homeomorphs restrict the usefulness of knowledge of ammonoid evolution during recent these features for phylogenetic investigations. -
Upper Cretaceous) of the Anaipadi–Saradamangalam Region of the Cauvery Basin, South-East India
Acta Geologica Polonica, Vol. 68 (2018), No. 4, pp. 663–687 DOI: 10.1515/agp-2018-0036 Inoceramids and associated ammonite faunas from the uppermost Turonian−lower Coniacian (Upper Cretaceous) of the Anaipadi–Saradamangalam region of the Cauvery Basin, south-east India IRENEUSZ WALASZCZYK1, WILLIAM JAMES KENNEDY2 and AMRUTA R. PARANJAPE3 1 Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland. E-mail: [email protected] 2 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW and Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, United Kingdom. 3 Sinhgad College of Science, Ambegaon (Bk.), Pune 411041, India. ABSTRACT: Walaszczyk, I., Kennedy, W.J. and Paranjape, A.R. 2018. Inoceramids and associated ammonite faunas from the uppermost Turonian–lower Coniacian (Upper Cretaceous) of the Anaipadi–Saradamangalam region of the Cauvery Basin, south-east India. Acta Geologica Polonica, 68 (4), 663–687. Warszawa. The lower (but not lowermost) part of the Upper Cretaceous Anaipadi Formation of the Trichinopoly Group in the area between Kulatur, Saradamangalam and Anaipadi, in the south-western part of the Cauvery Basin in south- east India yielded rich inoceramid and ammonite faunas. The ammonites: Mesopuzosia gaudama (Forbes, 1846), Damesites sugata (Forbes, 1846), Onitschoceras sp., Kossmaticeras (Kossmaticeras) theobal dianum (Stoliczka, 1865), Lewesiceras jimboi (Kossmat, 1898), Placenticeras kaffrarium Etheridge, 1904, and Pseudoxybeloceras (Schlueterella) sp., are characteristic of the Kossmaticeras theobaldianum Zone. The absence of Peroniceras (P.) dravidicum (Kossmat, 1895) indicates the presence of only lower part of this zone, referred to the nominative Kossmaticeras theobaldianum Subzone at the localities studied. -
X Congreso Argentino De Paleontología Y Bioestratigrafía VII Congreso Latinoamericano De Paleontología La Plata, Argentina - Septiembre De 2010
X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 Financian Auspician 1 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 2 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 3 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 X Congreso Argentino de Paleontología y Bioestratigrafía y VII Congreso Latinoamericano de Paleontología Resúmenes/coordinado por Sara Ballent ; Analia Artabe ; Franco Tortello. 1a ed. - La Plata: Museo de la Plata; Museo de la Plata, 2010. 238 p. + CD-ROM; 28x20 cm. ISBN 978-987-95849-7-2 1. Paleontología. 2. Bioestratigrafía. I. Ballent, Sara , coord. II. Artabe, Analia, coord. III. Tortello, Franco, coord. CDD 560 Fecha de catalogación: 27/08/2010 4 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología Declarado de Interés Municipal, La Plata (Decreto N° 1158) 5 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 6 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología La Plata, Argentina - Septiembre de 2010 X Congreso Argentino de Paleontología y Bioestratigrafía VII Congreso Latinoamericano de Paleontología Prólogo Una vez más el Congreso Argentino de Paleontología y Bioestratigrafía y el Congreso Latino- americano de Paleontología se realizan de manera conjunta. -
Correlations of Hauterivian and Barremian (Early Cretaceous) Stage Boundaries to Polarity Chrons
EPSL ELSEVIER Earth and Planetary Science Letters 134 (1995) 125-140 Correlations of Hauterivian and Barremian (Early Cretaceous) stage boundaries to polarity chrons J.E.T. Channell a F. Cecca b, E. Erba c a Department of Geology, University of Florida, Gainesville, FL 32611, USA b Servizio Geologico Nazionale, Largo S. Susanna 13, O0187Rome, Italy c Dipartimento di Seienze della Terra, Universith degli Studi di Milano, 20133 Milan, Italy Received 27 March 1995; accepted 5 June 1995 Abstract Recent ammonite finds in Italian Maiolica limestones allow direct correlation of Hauterivian and Barremian ammonite zones (stage boundaries) to polarity chrons. At Laghetto and Alpetto (Lombardy, Italy), Lower Aptian ammonites occur just above polarity zone M0 and below the Selli Level, and Upper Barremian ammonites occur in polarity zone Mln. These correlations are consistent with the Barremian/Aptian boundary being close to older boundary of (polarity chron) CM0. The uppermost Hauterivian ammonite (Faraoni) guide level has been correlated to CM4 at Bosso (Umbria-Marche), confirming the recent correlation of the Hauterivian/Barremian boundary to CM4. At Monte Acuto (Umbria-Marche), ammonites spanning the Valanginian/Hauterivian boundary interval, and the last appearance of the nannofossil T. verenae, occur close to the CMll/CMlln boundary. The Valanginian/Hauterivian boundary has previously been placed between the first appearance of L. bollii and the last appearance of T. verenae, or between CM10 and CMll. The published Polaveno (Lombardy) magnetostratigraphy for the CM3-CMll interval has now been extended to CM16. This 260 m section, recording the CM3-CM16 interval, is the most complete single-section record of Cretaceous M-sequence polarity chrons. -
我mmonoidsinja腿n 一stratigralphic Dlistribution and Bib且iogra]Phy一
Bulletin of the Geological Survey of Japan,vol.51(ll),p. 559-613 2000 , :Notes an且Comments Da流abase of’the Cretaceous 我mmonoidsinJa腿n 一stratigralphic dlistribution and bib且iogra]phy一 Seiichi TosHIMITsul and Hiromichi HIRANo2 Seiichi TosHIMITsu and Hiromichi HIRANo(2000)Database of the Cretaceous ammonoids in Japan -stratigraphic distribution and bibliography一.Bκ1乙 G60乙 Sπ鰍ゆ硯v・1.51(ll),P.559-613,1 fig,19 tables. Abstract:A database with a bibliography on the Japanese Cretaceous ammonoids has been made by the survey of various literature(Tables2-19).This database consists of a list of species,based on higher taxonomy of Wright8砲乙(1996),with their stratigraphic distribution data and a bibliog- raphy on them.As a result,it clarified that790species are detected from the Japanese Cretaceous deposits,and the species-diversity of the Cretaceous ammonoids in Japan changed cyclically, although the diversity of ammonoids in・the Early Cretaceous is much lower than the Late Cretaceous.Diversity changes are controlled by environmental changes,and therefore this database will be useful not only for stratigraphical and biochronological studies but also for paleoenviron- mental study of the Cretaceous Period. genera and65subgenera were recognised in Arke11α α乙(1967),while684genera and l53subgenera were 1. Introduction recognized in Wright6厩孟(1996). Ammonoids are one of the most common fossil On the other hand,Matsumoto (1942e,1943, animals in the Late Paleozoic and Mesozoic Eras.A 1954a)1isted many ammonoid species,obtained from great many species of ammonoids