3Rd WORKSHOP on EARLY CRETACEOUS CEPHALOPODS
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Bogdanova & Proz
SI-3-4 (Bogdanova & Proz) 15-01-2007 11:52 Pagina 45 Substantiation of the Barremian/Aptian boundary Tamara N. Bogdanova & Vladimir A. Prozorovsky Bogdanova, T.N. & V.A. Prozorovsky. Substantiation of the Barremian/Aptian boundary. — Scripta Geol., Spec. Issue 3: 45-81, 4 figs., 8 pls, Leiden, December 1999. T.N. Bogdanova, All-Russian Geological Institute (VSEGEI), Sredny pr.,74, St.-Petersburg, 199026, Russia; V.A. Prozorovsky, Department of Historical Geology, St.-Petersburg University, University emb., 7/9, St.-Petersburg, 199034, Russia. Key words: Trans-Caspian area, Barremian, Aptian, ammonite zones, correlation, boundary strato- type. This paper focuses on the Barremian/Aptian boundary in the Trans-Caspian area. Results of a strati- graphical study of the uppermost Barremian and the lower Aptian succession in the Trans-Caspian area are presented. The bed-by-bed description of three sections — Keldzhe, Tekedzhik and Utu- ludzha — is given as well as detailed lithologic columns. Five ammonite zones are known in the stud- ied stratigraphic interval — the Turkmeniceras turkmenicum, Deshayesites tuarkyricus, D. weissi, D. deshayesi, and Dufrenoya furcata zones. These zones are correlated with those of Europe. The Bar- remian/Aptian boundary in the Trans-Caspian area should be drawn at the base of the D. tuarkyricus Zone. It corresponds to the layers with the first occurrences of Deshayesites, Prodeshayesites and Para- deshayesites in Europe. It is proposed here to situate the boundary stratotype in the Utuludzha section, where the beds containing zonal representatives of the T. turkmenicum and D. tuarkyricus Zones are almost adjacent. Contents Introduction ........................................................................................................................... 45 History of the Barremian/Aptian boundary ................................................................... -
12. Lower Cretaceous Ammonites from the South Atlantic Leg 40 (Dsdp), Their Stratigraphic Value and Sedimentologic Properties
12. LOWER CRETACEOUS AMMONITES FROM THE SOUTH ATLANTIC LEG 40 (DSDP), THEIR STRATIGRAPHIC VALUE AND SEDIMENTOLOGIC PROPERTIES Jost Wiedmann and Joachim Neugebauer, Geol.-palaont. Institut der Universitat Tubingen, BRD ABSTRACT Eleven ammonites have been cored during Leg 40. They were found concentrated in the lower parts of the drilled section at Sites 363 (Walvis Ridge) and 364 (Angola Basin), and permit recognition of upper Albian, middle Albian, and upper Aptian. So far, no lower Albian could be recognized. A high ammonite density can be assumed for the South Atlantic Mid-Cretaceous. In contrast to data available so far, the Walvis Ridge associations consisting of phylloceratids and desmoceratids show more open- basin relationships than those of the Angola Basin, which are composed of mortoniceratids, desmoceratids, and heteromorphs. Paleobiogeographically, the South Atlantic fauna can be related to the well-known onshore faunas of Angola, South Africa, and Madagascar as well as to the European Mid-Cretaceous. This means that the opening of the South Atlantic and its connection with the North Atlantic occurred earlier as was generally presumed, i.e., in the middle Albian. Records of lower Aptian ammonite faunas from Gabon and Brazil remain doubtful. High rates of sedimentation prevailed especially in the Aptian and Albian, in connection with the early deepening of the South Atlantic basins. The mode of preservation of the ammonites suggests that they were deposited on the outer shelf or on the upper continental slope and were predominantly buried under sediments of slightly reducing conditions. In spite of a certain variability of the depositional environment, the ammonites show a uniform and particular mode of preservation. -
The Barremian Heteromorph Ammonite Dissimilites from Northern Italy: Taxonomy and Evolutionary Implications
The Barremian heteromorph ammonite Dissimilites from northern Italy: Taxonomy and evolutionary implications ALEXANDER LUKENEDER and SUSANNE LUKENEDER Lukeneder, A. and Lukeneder, S. 2014. The Barremian heteromorph ammonite Dissimilites from northern Italy: Taxon- omy and evolutionary implications. Acta Palaeontologica Polonica 59 (3): 663–680. A new acrioceratid ammonite, Dissimilites intermedius sp. nov., from the Barremian (Lower Cretaceous) of the Puez area (Dolomites, northern Italy) is described. Dissimilites intermedius sp. nov. is an intermediate form between D. dissimilis and D. trinodosum. The new species combines the ribbing style of D. dissimilis (bifurcating with intercalating single ribs) with the tuberculation style of D. trinodosum (trituberculation on entire shell). The shallow-helical spire, entirely comprising single ribs intercalated by trituberculated main ribs, is similar to the one of the assumed ancestor Acrioceras, whereas the increasing curvation of the younger forms resembles similar patterns observed in the descendant Toxoc- eratoides. These characters support the hypothesis of a direct evolutionary lineage from Acrioceras via Dissimilites to Toxoceratoides. D. intermedius sp. nov. ranges from the upper Lower Barremian (Moutoniceras moutonianum Zone) to the lower Upper Barremian (Toxancyloceras vandenheckii Zone). The new species allows to better understand the evolu- tion of the genus Dissimilites. The genus appears within the Nicklesia pulchella Zone represented by D. duboise, which most likely evolved into D. dissimilis. In the Kotetishvilia compressissima Zone, two morphological forms developed: smaller forms very similar to Acrioceras and forms with very long shaft and juvenile spire like in D. intermedius sp. nov. The latter most likely gave rise to D. subalternatus and D. trinodosum in the M. -
GB (1990) 20 (5) Pp. 45-77 (Ivanov and Stoykova).Pdf
GEOLOGICA BALCANICA, 20. 5, Sofia, Oct. 1990, p. 45-71. CTpaTHrpa¢HH anTCKOro H anb6CKoro HpycoB B ueHTpanbHOH '-laCTH MH3HHCKOH nnaT¢opMbi Mapwt Hea/-106, KpucmaAuHa Cmoi1Ko6a reo;IO?II'leCnllii 111/Ctnllmym Eo.uapcKOU aKai)e,\fliU nayn, 1113 Cor/iwt ( Jlpun.•tma On!t ony6nuKorJai/UII 19 U/011.'1 1989 ? ) M. 1l'anov, K. Stoykova - Stratigraphy of Aptian and Albian Stages in the central part of Moesia11 P/utfor111e. Aptian Stage is widespread in the Central North Bulgaria, while the Albian is established only in the northern regions. The Aptian se<.:tions are built up of sediments of the Trambes and Svistov Formations. It has been es tablished that the Triimbes and Svistov Formation join laterally along the line Svi stov-Tatari- Osil m. The concretion phosphorites and sandstones, within the range of Albian, are here separated as Dekov Formations. The lithologic and ammonitic sequences in 9 sections are studied and described. Aptian Stage is represented by the Middlt: (Gargasian) and Upper (Clansayesian) Substages. The following ammonitic zones are separated and characterized: Cheloniceras ( Epicheloniceras) martinioides Zone, C. ( E. ) subnodosocostatum Zone, Acuntho hoplites no/alii Zone, Hypacanthoplites ;acobi Zone. Aptian is covered with a wash-out by Albian. The inter ruption of the sedimentation includes Late Aptian (partially), Early and Middle Albian (partially) Substages. Albian Stage is represented by the Middle (partially) and Upper Albian Substages. The following zones are esta blished and characterized: Hoplites ( Hoplites) dematus Zone, Euhoplites loricatus Zone, Euhoplites /aut us Zone, J'yfortoniceras ( Pervinquieriu) inflatum Zone, Stoliczkaia dispar Zone. In some sections the separation of the first four zones is impossible due to the strong condensation in their basement. -
Albian Ammonites from Northern Pakistan
DE DE GRUYTER Acta Geologica Polonica, Vol. 64 (2014), No. 1, pp. 47–98 OPEN DOI: 10.2478/agp-2014-0003 G Albian ammonites from northern Pakistan WILLIAM JAMES KENNEDY1 AND ALI N. FATMI2 1Oxford University Museum of Natural History, Parks Road, Oxford OX1 3W and Department of Earth Sciences, Parks Road, Oxford OX1 3AN, United Kingdom. E-mail: [email protected] 2Formerly of the Geological Survey of Pakistan, Quetta, Pakistan (Dr Fatmi died on 27 March 2012) ABSTRACT: Kennedy, W.J. and Fatmi, A.N. 2014. Albian ammonites from northern Pakistan. Acta Geologica Polonica, 64 (1), 47–98. Warszawa. The occurrence of rich Albian ammonite faunas in what is now northern Pakistan has been known for more than 80 years, but there has been no comprehensive account of the assemblages present. A total of 36 taxa are described below. The middle part of the Lumshiwal Formation yields Upper Aptian ammonites south of the Samana Range. Elsewhere, it yields Douvilleiceras leightonense Casey, 1962, of the lower Lower Albian Leymeriella reg- ularis Zone and the Sonneratia perinflata and S. kitchini Subzones of the Sonneratia chalensis Zone of the north- west European sequence. The top one to two metres of the Lumshiwal yields an abundant fauna of rolled and phos- phatised ammonites that includes elements from much of the Albian. Of these, Prolyelliceras gevreyi (Jacob, 1907) first appears in the lower Lower Albian Leymeriella tardefurcata Zone. The commonest ammonite is Douville- iceras mammillatum (Schlotheim, 1813) sensu lato, which ranges from the perinflata Subzone of the chalensis Zone to the Otohoplites bulliensis Subzone of the O. -
Ammonite Occurrence in the Barremian-Aptian Boundary Beds in North-Eastern Bulgaria T
Докладм Болгарской академии иаук Comptes rendus de l’Académie bulgare des Sciences Tome 36, № 8, 1983 GÉOLOGIE Stratigraphie AMMONITE OCCURRENCE IN THE BARREMIAN-APTIAN BOUNDARY BEDS IN NORTH-EASTERN BULGARIA T. G. Nikolov, K. H. Stoykova, M. I. Ivanov (Submitted, by Corresponding Member V. Tsankov on April 18, 1983) One of the research projects carried out by the Department of Palaentolo- gy at the Sofia University in recent years has been the detailed study of the biostratigraphy of the Lower Cretaceous in North-Eastern Bulgaria. Part of this project was included in the graduation thesis of K. Stoykova on the Aptian stage in the lower reaches of the Yantra River, and also in the studies into the Lower Cretaseous carried out by T. Nikolov in the natural open layers and in the deep drillings between the Yantra and the Black Sea. Very interesting data were obtained from the investigation of the uninter rupted Barrcmian-Aptian section a[ the Katselovo Village, Rousse District. This section presents a monotonous rhythmic alternation of marls, clay lime stones, and sparse seams of rather pure limestones, developed mainly in the upper part. The section provides a very good opportunity for observing the stratigraphic ammonite occurence in a clay-carbonate medium. Viewed from top to bottom, the section at Katselovo Village, Rousse District, reveals the following sequences: ^ 5 ."Thin-layer beige marls exteremely rich in fossil fauna. Predominant Depth are the species of the genus Deshayesites represented by tens of spec- in imens. The following have been determined : m etres : Deshayesites deshayesi (Leym. MS) d’Orb., Deshayesites forbesi Casey, Deshayesites callidiscus Casey, Deshayesites grandis Spath, Deshayesites saxbyi Casey, Deshayesites involutus Spath, Deshayesites eiiglyphus Casey, Deshayesites tenninalis Bogdanova, Paradeshayesites tenuicostatus (v. -
Belemnite Extinction and the Origin of Modern Cephalopods 35 M.Y. Prior to the Cretaceous−Paleogene Event
Belemnite extinction and the origin of modern cephalopods 35 m.y. prior to the Cretaceous−Paleogene event Yasuhiro Iba1,2*, Jörg Mutterlose1, Kazushige Tanabe3, Shin-ichi Sano4, Akihiro Misaki5, and Kazunobu Terabe6 1Institut für Geologie, Mineralogie und Geophysik, Ruhr-Universität Bochum, 44801, Germany 2Department of Geology and Paleontology, National Museum of Nature and Science, Tokyo 169-0073, Japan 3Department of Earth and Planetary Science, University of Tokyo, Tokyo 113-0033, Japan 4Fukui Prefectural Dinosaur Museum, Fukui 911-8601, Japan 5Kitakyushu Museum of Natural History and Human History, Fukuoka 805-0071, Japan 6Arabian Oil Company, Ltd., Tokyo 140-0002, Japan ABSTRACT determination of the strata studied is based on Belemnites, a very successful group of Mesozoic cephalopods, fl ourished in Cretaceous diagnostic ammonite species. Evaluations of oceans until the Cretaceous−Paleogene event, when they became globally extinct. Following museum collections (Mikasa City Museum, and this event the modern types of cephalopods (squids, cuttlefi sh, octopus) radiated in the Ceno- Kyushu University, Japan; California Academy zoic in all oceans. In the North Pacifi c, however, a turnover from belemnites to the modern of Science, USA) have also been done. Details types of cephalopods about 35 m.y. before the Cretaceous−Paleogene event documents a more of the localities, horizons, and the precise strati- complex evolutionary history of cephalopods than previously thought. Here we show that the graphic ages of Albian belemnites are shown in modern types of cephalopods originated and prospered throughout the Late Cretaceous in Table DR1 in the Data Repository.1 the North Pacifi c. The mid-Cretaceous cephalopod turnover was caused by cooling and the closure of the Bering Strait, which led to a subsequent faunal isolation of this area. -
(Ammonoidea, Gassendiceratinae), and New Ammonite Biohorizon for the Upper Barremian of Southeastern France
Carnets de Géologie / Notebooks on Geology - Article 2009/02 (CG2009_A02) Pseudoshasticrioceras bersaci nov. sp. (Ammonoidea, Gassendiceratinae), and new ammonite biohorizon for the Upper Barremian of southeastern France Didier BERT* 1 Gérard DELANOY 2 Abstract: Research in the Feraudianus Subzone of the Sartousiana Zone of the Barremian stage led to the discovery of a new species of Pseudoshasticrioceras: P. bersaci nov. sp. Its study provides evidence concerning the developments of the latest Gassendiceratinae BERT et alii, 2006, and the relationship between the genus Pseudoshasticrioceras DELANOY, 1998, and Gassendiceras BERT et alii, 2006. In particular, this new species is derived from Pseudoshasticrioceras magnini (DELANOY, 1992) by a minor revision in the processes of ontogenesis (retardation of ornamentation - neoteny). However, the evolution towards Pseudoshasticrioceras autrani DELANOY, 1998, implies a "failure" in this process that may possibly be related to parallel changes in environmental conditions. On the other hand, the very closely defined stratigraphic position of Pseudoshasticrioceras bersaci nov. sp., and its position in the anagenetic lineage of Pseudoshasticrioceras, demonstrates its interest as a biostratigraphic marker: a new Bersaci Biohorizon is proposed; it is located between the Magnini and the Autrani biohorizons. Key Words: Ammonitinae; Pseudoshasticrioceras; Gassendiceratinae; Upper Barremian; Sartousiana Zone; Feraudianus Subzone; biozonation; southeastern France. Citation: BERT D. & DELANOY G. (2009).- -
The Appearance of the Genus Deshayesites (Kazansky, 1914, Ammonoidea) in the Lowermost Aptian (Lower Cretaceous) of La Bedoule (Se France)
Rivista Italians di Paleontologia e Stratigrafia volume 105 numero 2 tavole 1-9 pagine 267-286 Settembre 1999 THE APPEARANCE OF THE GENUS DESHAYESITES (KAZANSKY, 1914, AMMONOIDEA) IN THE LOWERMOST APTIAN (LOWER CRETACEOUS) OF LA BEDOULE (SE FRANCE) FABRIZIO CECCA *, PIERRE ROPOLO** & ROLAND GONNET*** Received March 29, 1999; accepted June 4, 1999 Key-words: Palaeontology, Biostratigraphy, Ammonites, Creta- ceous, Aptian, SE France. Abstract. New palaeontological and biostratigraphical investiga- tions were carried out at La Bedoule (SE France), which is the strato- type-area of the Bedoulian (Lower Aptian). The levels that directly overlie the last Barremian Pseudocrioceras-bearing bed have revealed the occurrence of a fauna characterized by previously undescribed macro- conchs of the genus Deshayesites, that we have included in Deshayesites bedouliensis n. sp. and in D. aff. consobrinus (d'Orbigny). These forms are associated with the species Deshayesites antiquus Bogdanova, D. oglanlensis Bogdanova, D. cf. weissiformis Bogdanova, D. aff. weissifor- mis Bogdanova in Delanoy, D. cf. planicostatus Bogdanova, and D. aff. normani Casey. These ammonites characterize the basal Aptian Des- hayesites tuarkyricus Zone. This Zone was defined in Turkmenistan but its recognition in the Mediterranean Tethys is confirmed by the pre- sent study. Contrary to previous assertions, the genus Prodeshayesites (which pre-dates Deshayesites in northern Germany and southern En- gland), whose FAD was taken to mark the base of the Aptian, is ab- sent at La Bedoule. Prodeshayesites is absent also in Turkmenistan and in all other Mediterranean localities. The FAD of the genus Deshayesi- tes is taken to mark the base of the Aptian in the Mediterranean area. -
Geologica Hungarica Series Palaeontologica Fasciculus 57
FASCICULI INSTITUTI GEOLOGICI HUNGARIAE AD ILLUSTRANDAM NOTIONEM GEOLOGICAM ET PALAEONTOLOGICAM GEOLOGICA HUNGARICA SERIES PALAEONTOLOGICA FASCICULUS 57 Aptian–Campanian ammonites of Hungary Editor: OTTILIA SZIVES Written by OTTILIA SZIVES, LÁSZLÓ CSONTOS, LÁSZLÓ BUJTOR, ISTVÁN FÕZY BUDAPEST, 2007 © Copyright Geological Institute of Hungary (Magyar Állami Földtani Intézet), 2007 All rights reserved! Minden jog fenntartva! Serial editor: LÁSZLÓ KORDOS Reviewer: ATTILA VÖRÖS Technical editor: DEZSŐ SIMONYI OLGA PIROS DTP: OLGA PIROS DEZSŐ SIMONYI Cover design: DEZSŐ SIMONYI Published by the Geological Institute of Hungary — Kiadja a Magyar Állami Földtani Intézet Responsible editor: LÁSZLÓ KORDOS Director This book has been subsidized by The comittee on Publishing Scientific Books and Periodicals of Hungarian Academy of Sciences HU ISSN 0374–1893 ISBN 978-963-671-261-7 Geologica Hungarica series Palaeontologica, Fasciculus 57 3 Contents Preface......................................................................................................................................................................... 7 Acknowledgments ................................................................................................................................................. 7 Introduction (OTTILIA SZIVES)...................................................................................................................................... 9 Source of the material ............................................................................................................................................ -
Early Cretaceous (Albian) Ammonites from the Chitina Valley and Talkeetna Mountains, Alaska
Early Cretaceous (Albian) Ammonites From the Chitina Valley and Talkeetna Mountains, Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 354-D Early Cretaceous (Albian) Ammonites From the Chitina Valley and Talkeetna Mountains, Alaska By RALPH W. IMLAY SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 354-D The Early Cretaceous (Albian) ammonites in southern Alaska have strong affinities with those in California and Oregon but are in part of Boreal and Eurasian origin UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1960 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. - Price SO cents (paper cover) CONTENTS Ammonite faunules and correlations Continued Abstract..________________________________________ 87 Bretrericeras breweri and B. cf. B. hulenense faunule__ 91 Introduction _______________________________________ 87 Frebnhliceros singulare faunule____________________ 92 Biologic analysis____________________________________ 87 Other Albian faunules.__________________________ 93 Stratigraphic summary ______________________________ 88 Comparisons with other faunas_______________________ 93 Talkeetna Mountains ___________________________ 88 Geographic distribution._____________________________ 93 Chitina Valley__________________________________ 88 Summary of results _________________________________ 93 Ammonite faunules and correlations.__________________ -
Aptian (Lower Cretaceous) Biostratigraphy and Cephalopods from North Central Tunisia
Cretaceous Research 30 (2009) 895–910 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Aptian (Lower Cretaceous) biostratigraphy and cephalopods from north central Tunisia Jens Lehmann a,*, Matthias Heldt b, Martina Bachmann b, Mohamed E. Hedi Negra c a Geosciences Collection, Faculty of Geosciences, University of Bremen, Klagenfurter Strasse, 28357 Bremen, Germany b Geochronology working-group, Faculty of Geosciences, University of Bremen, Klagenfurter Strasse, 28357 Bremen, Germany c De´partement de Ge´ologie, Faculte´ des Sciences, Universite´ de Tunis, Campus Universitaire, 2092 Manar II, Tunis, Tunisia article info abstract Article history: Thick Aptian deposits in north central Tunisia comprise hemipelagic lower Aptian, reflecting the sea- Received 3 December 2008 level rise of OAE 1a, and an upper Aptian shallow marine environment characterized by the establish- Accepted in revised form 3 February 2009 ment of a carbonate platform facies. Carbon stable isotope data permit recognition of the OAE 1a event in Available online 12 February 2009 the Djebel Serdj section. Cephalopods are rare throughout these successions, but occurrences are sufficient to date the facies changes and the position of the OAE1a event. Ammonite genera include lower Keywords: Aptian Deshayesites, Dufrenoyia, Pseudohaploceras, Toxoceratoides and ?Ancyloceras; and upper Aptian Biostratigraphy Zuercherella, Riedelites and Parahoplites. Correlation of carbon isotope data with those of other Tethyan Lower Cretaceous Aptian sections is undertaken together with the integration of planktonic foraminiferal data. Ammonites Ó 2009 Elsevier Ltd. All rights reserved. Nautiloids Tunisia 1. Introduction limestone, marlstone or claystone facies (e.g. Bernaus et al., 2003); distal carbonate shelf settings often contain at least poor faunas In the lower Aptian, superplume activity in the Pacific realm (e.g.