New and Less Known Barremian-Albian Ammonites from Colombia
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Cambrian Cephalopods
BULLETIN 40 Cambrian Cephalopods BY ROUSSEAU H. FLOWER 1954 STATE BUREAU OF MINES AND MINERAL RESOURCES NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY CAMPUS STATION SOCORRO, NEW MEXICO NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY E. J. Workman, President STATE BUREAU OF MINES AND MINERAL RESOURCES Eugene Callaghan, Director THE REGENTS MEMBERS Ex OFFICIO The Honorable Edwin L. Mechem ...................... Governor of New Mexico Tom Wiley ......................................... Superintendent of Public Instruction APPOINTED MEMBERS Robert W. Botts ...................................................................... Albuquerque Holm 0. Bursum, Jr. ....................................................................... Socorro Thomas M. Cramer ........................................................................ Carlsbad Frank C. DiLuzio ..................................................................... Los Alamos A. A. Kemnitz ................................................................................... Hobbs Contents Page ABSTRACT ...................................................................................................... 1 FOREWORD ................................................................................................... 2 ACKNOWLEDGMENTS ............................................................................. 3 PREVIOUS REPORTS OF CAMBRIAN CEPHALOPODS ................ 4 ADEQUATELY KNOWN CAMBRIAN CEPHALOPODS, with a revision of the Plectronoceratidae ..........................................................7 -
Stratigraphic Implications of a New Lower Cretaceous Ammonoid Fauna from the Puez Area (Valanginian – Aptian, Dolomites, Southern Alps, Italy)
Geo.Alp, Vol. 3, S. 55–83, 2006 STRATIGRAPHIC IMPLICATIONS OF A NEW LOWER CRETACEOUS AMMONOID FAUNA FROM THE PUEZ AREA (VALANGINIAN – APTIAN, DOLOMITES, SOUTHERN ALPS, ITALY) Alexander Lukeneder1 & Christian Aspmair2 With 6 figures and 8 plates 1 Natural History Museum, Geological-Palaeontological Department, Burgring 7, A-1010 Wien, Austria, e-mail: [email protected] 2 Prissian 102, I – 39010 Tisens (BZ), Italy Abstract Lower Cretaceous ammonoids (n = 424) were collected at the Puez locality in the Dolomites of Southern Tyrol. The cephalopod fauna from the marly limestones to marls here indicates Late Valanginian to Early Aptian age. The deposition of the marly limestones and marls of this interval occurred during depositional- ly unstable conditions. The underlying Biancone Formation (Maiolica Formation) is of Early Valanginian, whereas the lowermost Rosso Ammonitico is of Jurassic to Berriasian age. The ammonoid fauna consists of 27 different genera, each represented by 1-2 species. The assemblage at the Puez section is dominated by the Phylloceratina (30%) and the Ammonitina (34%). Phyllopachyceras (17%) and Phylloceras (13%) (both Phylloceratina) are the most frequent components, followed by Lytoceras (12%) (Lytoceratina), and Barremites (10%) and Melchiorites (8%) (both Ammonitina). The cephalopod fauna is purely of Mediterranean origin. Zusammenfassung Unterkreide Ammonoideen (424 Exemplare) der Puez Lokalität in den Dolomiten Süd-Tirols wurden unter- sucht. Die Fauna der mergeligen Kalke und Mergel von Puez zeigen ein Alter von Ober-Valanginium bis Unter-Aptium an. Die mergeligen Kalke und Mergel dieses Abschnitts lagerten sich unter instabiler Bedingungen ab. Die unterlagernde Biancone Formation (Maiolica Formation) zeigt Unter-Valanginium an, wogegen die tiefste Formation des Rosso Ammonitico auf Ober-Jura bis Berriasium hindeutet. -
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. -
Smithsonian Miscellaneous Collections
SMITHSONIAN MISCELLANEOUS COLLECTIOXS. 227 AEEANGEMENT FAMILIES OF MOLLUSKS. PREPARED FOR THE SMITHSONIAN INSTITUTION BY THEODORE GILL, M. D., Ph.D. WASHINGTON: PUBLISHED BY THE SMITHSONIAN INSTITUTION, FEBRUARY, 1871. ^^1 I ADVERTISEMENT. The following list has been prepared by Dr. Theodore Gill, at the request of the Smithsonian Institution, for the purpose of facilitating the arrangement and classification of the Mollusks and Shells of the National Museum ; and as frequent applica- tions for such a list have been received by the Institution, it has been thought advisable to publish it for more extended use. JOSEPH HENRY, Secretary S. I. Smithsonian Institution, Washington, January, 1871 ACCEPTED FOR PUBLICATION, FEBRUARY 28, 1870. (iii ) CONTENTS. VI PAGE Order 17. Monomyaria . 21 " 18. Rudista , 22 Sub-Branch Molluscoidea . 23 Class Tunicata , 23 Order 19. Saccobranchia . 23 " 20. Dactjlobranchia , 24 " 21. Taeniobranchia , 24 " 22. Larvalia , 24 Class Braehiopoda . 25 Order 23. Arthropomata , 25 " . 24. Lyopomata , 26 Class Polyzoa .... 27 Order 25. Phylactolsemata . 27 " 26. Gymnolseraata . 27 " 27. Rhabdopleurse 30 III. List op Authors referred to 31 IV. Index 45 OTRODUCTIO^. OBJECTS. The want of a complete and consistent list of the principal subdivisions of the mollusks having been experienced for some time, and such a list being at length imperatively needed for the arrangement of the collections of the Smithsonian Institution, the present arrangement has been compiled for that purpose. It must be considered simply as a provisional list, embracing the results of the most recent and approved researches into the systematic relations and anatomy of those animals, but from which innova- tions and peculiar views, affecting materially the classification, have been excluded. -
Geological Survey of Austria ©Geol
©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt, 120 Berichte der Geologischen Bundesanstalt, Benjamin Sames (Ed.) th 10 International Symposium on the Cretaceous: ABSTRACTS Berichte der Geologischen Bundesanstalt, 120 www.geologie.ac.at Geological Survey of Austria ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt (ISSN 1017-8880) Band 120 10th International Symposium on the Cretaceous Vienna, August 21–26, 2017 — ABSTRACTS BENJAMIN SAMES (Ed.) ©Geol. Bundesanstalt, Wien; download unter www.geologie.ac.at und www.zobodat.at Berichte der Geologischen Bundesanstalt, 120 ISSN 1017-8880 Wien, im Juli 2017 10th International Symposium on the Cretaceous Vienna, August 21–26, 2017 – ABSTRACTS Benjamin Sames, Editor Dr. Benjamin Sames, Universität Wien, Department for Geodynamics and Sedimentology, Center for Earth Sciences, Althanstraße 14, 1090 Vienna, Austria. Recommended citation / Zitiervorschlag Volume / Gesamtwerk Sames, B. (Ed.) (2017): 10th International Symposium on the Cretaceous – Abstracts, 21–26 August 2017, Vienna. – Berichte der Geologischen Bundesanstalt, 120, 351 pp., Vienna. Abstract (example / Beispiel) Granier, B., Gèze, R., Azar, D. & Maksoud, S. (2017): Regional stages: What is the use of them – A case study in Lebanon. – In: Sames, B. (Ed.): 10th International Symposium on the Cretaceous – Abstracts, 21–26 August 2017, Vienna. – Berichte der Geologischen Bundesanstalt, 120, 102, Vienna. Cover design: Monika Brüggemann-Ledolter (Geologische Bundesanstalt). Cover picture: Postalm section, upper Campanian red pelagic limestone-marl cycles (CORBs) of the Nierental Formation, Gosau Group, Northern Calcareous Alps (Photograph: M. Wagreich). 10th ISC Logo: Benjamin Sames The 10th ISC Logo is composed of selected elements of the Viennese skyline with, from left to right, the Stephansdom (St. -
Stable Carbon-Isotope Chemostratigraphy Versus Ammonite Biostratigraphy: Data from Around the Barremian/Aptian Boundary (Lower Cretaceous)
STRATA, 2020, série 2e, vol. 56: 1-31 Stable carbon-isotope chemostratigraphy versus ammonite biostratigraphy: data from around the Barremian/Aptian boundary (Lower Cretaceous) Camille Frau1 Abstract. The complex and ornate carbon-isotope excursion of the lower Aptian Oceanic Anoxic Event (OAE) 1a is used as a potent means of worldwide marine correlations that has the potential to provide an independent control based on controversial ammonite dating. Re-examination of the best-documented expanded sections of the Tethyan, Boreal, and Pacific realms highlight the inconsistent positioning of ammonite key markers – mainly Deshayesitidae and Douvilleiceratidae – relative to the OAE 1a carbon- isotope excursion. This is not only due to taxonomic issues and substantial provincialism but also the weaknesses in the stratigraphic record caused by the sedimentary context of that oceanic anoxic event. Much detailed study and refinement of existing data are needed to reduce volatility in ammonite zonal boundaries from around the Barremian/Aptian boundary. Keywords. Ammonite, Carbon isotope; Chemostratigraphy, Aptian, Cretaceous, Oceanic Anoxic Event. Article history: manuscript receveid Novembre 23, 2020; accepted in revised form Decembre 16, 2020; available on line Decembre 30, 2020. Chimiostratigraphie de l’isotope du carbone versus biostratigraphie des ammonites : données autour de la limite Barrémien/Aptien (Crétacé Inférieur). Résumé. Les motifs caractéristiques de l’excursion du carbone associée à l’Évènement Anoxique Océanique (OAE) 1a de l’Aptien inférieur sont utilisés comme un outil puissant pour corréler mondialement les séries marines, et ont le potentiel pour fournir un contrôle indépendant des datations controversées basées sur les ammonites. Le réexamen des coupes les mieux documentées des domaines Téthysien, Boréal, et Pacifique montre la position irrégulière des marqueurs clefs ammonitiques – surtout ceux des Deshayesitidae et des Douvilleiceratidae – par rapport à l’excursion de l’OAE 1a. -
Xh Ieuican%Mllisdllm 1Soxftates PUBLISHED by the AMERICAN MUSEUM of NATURAL HISTORY CENTRAL PARK WEST at 79TH STREET, NEW YORK 24, N.Y
Xh ieuican%Mllisdllm 1Soxftates PUBLISHED BY THE AMERICAN MUSEUM OF NATURAL HISTORY CENTRAL PARK WEST AT 79TH STREET, NEW YORK 24, N.Y. NUMBER 2005 JUNE 15, 1960 Lower Cretaceous Ammonites from Colombia, South America BY OTTO HAAS INTRODUCTION The present paper attempts to summarize the paleontological re- sults of an investigation carried out early in 1956, under the sponsor- ship of International Petroleum (Colombia), Ltd., in the Cordillera Oriental of Colombia for the purpose of clarifying and refining the lower Cretaceous stratigraphy of that region. I am indebted to the company for permission to publish this paper and to utilize photo- graphs made at the company's expense, and to Prof. Gerardo Botero Arango of the Facultad Nacional de Minas of Medellin, Colombia, for permission to describe specimens collected on a field trip of that institution and now deposited in its collections. For the repositories of illustrated specimens, reference is made to the legends of the figures accompanying the present report; there "I.P." indicates the collec- tions of International Petroleum (Colombia), Ltd., in Bogota and "F.N.M." those of the Facultad Nacional de Minas in Medellin. In addition to most of the forms recognized among the abundant ammonites collected in the course of the above investigation, some interesting specimens that had been in the company's collections earlier are also included in the present report. Unfortunately most of the ammonites here described, especially those preserved in shales, are crushed and flattened or otherwise dis- torted; venters can be examined only exceptionally and even more rarely can suture lines be observed. -
Origin of the Tethyan Hemihoplitidae Tested with Cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an Immigration Event? Didier Bert, Stéphane Bersac
Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an immigration event? Didier Bert, Stéphane Bersac To cite this version: Didier Bert, Stéphane Bersac. Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancylo- ceratina, Ammonoidea, Early Cretaceous): an immigration event?. Carnets de Geologie, Carnets de Geologie, 2014, 14 (13), pp.255-272. insu-01071656 HAL Id: insu-01071656 https://hal-insu.archives-ouvertes.fr/insu-01071656 Submitted on 17 Oct 2014 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Carnets de Géologie [Notebooks on Geology] - vol. 14, n° 13 Origin of the Tethyan Hemihoplitidae tested with cladistics (Ancyloceratina, Ammonoidea, Early Cretaceous): an immigration event? Didier BERT 1, 2 Stéphane BERSAC 2 Abstract: The Late Barremian Hemihoplitidae (Ancyloceratina, Ammonoidea) are widely known in the northern Tethyan Margin and the Essaouira-Agadir Basin (Morocco). Their rapid evolution and diversifi- cation make them one of the key groups for that period, but their origin remains poorly known and several competing hypotheses have been published. These hypotheses are tested here with cladistic analysis in order to reject those receiving the least support and discuss those well supported. -
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. -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
The Douvilleiceratidae (Ammonoidea) of the Lower Aptian Historical Stratotype Area at Cassis-La Bédoule (SE France)
Carnets de Géologie / Notebooks on Geology - Memoir 2008/03 (CG2008_M03) The Douvilleiceratidae (Ammonoidea) of the Lower Aptian historical stratotype area at Cassis-La Bédoule (SE France). 1 Pierre ROPOLO 2 Gabriel CONTE 3 Michel MOULLADE 4 Guy TRONCHETTI 5 Roland GONNET Abstract: Recent biostratigraphic research in the marly limestones of the Cassis-La Bédoule area (SE France) provided a rich macrofauna of Douvilleiceratidae PARONA & BONARELLI, 1897. From the uppermost Barremian (Pseudocrioceras waagenoides Subzone) to the middle Aptian (Parahoplites melchioris Zone), specimens of Procheloniceras, Cheloniceras, Roloboceras, Megatyloceras and Epicheloniceras were collected in succession. In this paper we describe the various genera and species from this material and delimit precisely their stratigraphic positions. Our study shows that each genus or subgenus characterizes a discrete stratigraphic interval. In addition, the Cheloniceras meyendorffi (upper Bedoulian), Epicheloniceras debile, Epicheloniceras gracile, and Epicheloniceras buxtorfi (Gargasian = middle Aptian) subzones, originally defined in England by CASEY (1961a), are identified for the first time in the Lower Aptian stratotypic area of Cassis-La Bédoule. Key Words: Cretaceous; Aptian; ammonites; Douvilleiceratidae; taxonomy; biostratigraphy. Citation: ROPOLO P., CONTE G., MOULLADE M., TRONCHETTI G. & GONNET R. (2008).- The Douvilleiceratidae (Ammonoidea) of the Lower Aptian historical stratotype area at Cassis-La Bédoule (SE France).- Carnets de Géologie / Notebooks on Geology, Brest, Memoir 2008/03 (CG2008_M03) Résumé : Les Douvilleiceratidae (Ammonoidea) de la région du stratotype historique de l'Aptien inférieur à Cassis-La Bédoule (SE de la France).- Des recherches biostratigraphiques récentes dans les sédiments barrémo-aptiens du secteur de Cassis-La Bédoule (SE de la France) ont révélé une riche macrofaune de Douvilleiceratidae PARONA & BONARELLI, 1897. -
Abbreviation Kiel S. 2005, New and Little Known Gastropods from the Albian of the Mahajanga Basin, Northwestern Madagaskar
1 Reference (Explanations see mollusca-database.eu) Abbreviation Kiel S. 2005, New and little known gastropods from the Albian of the Mahajanga Basin, Northwestern Madagaskar. AF01 http://www.geowiss.uni-hamburg.de/i-geolo/Palaeontologie/ForschungImadagaskar.htm (11.03.2007, abstract) Bandel K. 2003, Cretaceous volutid Neogastropoda from the Western Desert of Egypt and their place within the noegastropoda AF02 (Mollusca). Mitt. Geol.-Paläont. Inst. Univ. Hamburg, Heft 87, p 73-98, 49 figs., Hamburg (abstract). www.geowiss.uni-hamburg.de/i-geolo/Palaeontologie/Forschung/publications.htm (29.10.2007) Kiel S. & Bandel K. 2003, New taxonomic data for the gastropod fauna of the Uzamba Formation (Santonian-Campanian, South AF03 Africa) based on newly collected material. Cretaceous research 24, p. 449-475, 10 figs., Elsevier (abstract). www.geowiss.uni-hamburg.de/i-geolo/Palaeontologie/Forschung/publications.htm (29.10.2007) Emberton K.C. 2002, Owengriffithsius , a new genus of cyclophorid land snails endemic to northern Madagascar. The Veliger 45 (3) : AF04 203-217. http://www.theveliger.org/index.html Emberton K.C. 2002, Ankoravaratra , a new genus of landsnails endemic to northern Madagascar (Cyclophoroidea: Maizaniidae?). AF05 The Veliger 45 (4) : 278-289. http://www.theveliger.org/volume45(4).html Blaison & Bourquin 1966, Révision des "Collotia sensu lato": un nouveau sous-genre "Tintanticeras". Ann. sci. univ. Besancon, 3ème AF06 série, geologie. fasc.2 :69-77 (Abstract). www.fossile.org/pages-web/bibliographie_consacree_au_ammon.htp (20.7.2005) Bensalah M., Adaci M., Mahboubi M. & Kazi-Tani O., 2005, Les sediments continentaux d'age tertiaire dans les Hautes Plaines AF07 Oranaises et le Tell Tlemcenien (Algerie occidentale).